Blinded by Antarctica Reports

Special snow goggles for protection in polar landscapes.

Someone triggered Antarctica for this week’s media alarm blitz.

Antarctic ice loss increases to 200 billion tonnes a year – Climate Action

Antarctica is now melting three times faster than ever before – Euronews

Antarctica is shedding ice at an accelerating rate – Digital Journal

Al Gore Sounds the Alarm on 0.3 inches of Sea Level Rise from Ice Sheets– Daily Caller

Antarctica is losing an insane amount of ice. Nothing about this is good. – Fox News
Looks like it’s time yet again to play Climate Whack-A-Mole.  That means stepping back to get some perspective on the reports and the interpretations applied by those invested in alarmism.

Antarctic Basics

The Antarctic Ice Sheet extends almost 14 million square kilometers (5.4 million square miles), roughly the area of the contiguous United States and Mexico combined. The Antarctic Ice Sheet contains 30 million cubic kilometers (7.2 million cubic miles) of ice. (Source: NSIDC: Quick Facts Ice Sheets)

The Antarctic Ice Sheet covers an area larger than the U.S. and Mexico combined. This photo shows Mt. Erebus rising above the ice-covered continent. Credit: Ted Scambos & Rob Bauer, NSIDC

The study of ice sheet mass balance underwent two major advances, one during the early 1990s, and again early in the 2000s. At the beginning of the 1990s, scientists were unsure of the sign (positive or negative) of the mass balance of Greenland or Antarctica, and knew only that it could not be changing rapidly relative to the size of the ice sheet.

Advances in glacier ice flow mapping using repeat satellite images, and later using interferometric synthetic aperture radar SAR methods, facilitated the mass budget approach, although this still requires an estimate of snow input and a cross-section of the glacier as it flows out from the continent and becomes floating ice. Satellite radar altimetry mapping and change detection, developed in the early to mid-1990s allowed the research community to finally extract reliable quantitative information regarding the overall growth or reduction of the volume of the ice sheets.

By 2002, publications were able to report that both large ice sheets were losing mass (Rignot and Thomas 2002). Then in 2003 the launch of two new satellites, ICESat and GRACE, led to vast improvements in one of the methods for mass balance determination, volume change, and introduced the ability to conduct gravimetric measurements of ice sheet mass over time. The gravimetric method helped to resolve remaining questions about how and where the ice sheets were losing mass. With this third method, and with continued evolution of mass budget and geodetic methods it was shown that the ice sheets were in fact losing mass at an accelerating rate by the end of the 2000s (Veliconga 2009, Rignot et al. 2011b).

Contradictory Findings

NASA Study: Mass Gains of Antarctic Ice Sheet Greater than Losses

A new 2015 NASA study says that an increase in Antarctic snow accumulation that began 10,000 years ago is currently adding enough ice to the continent to outweigh the increased losses from its thinning glaciers.

The research challenges the conclusions of other studies, including the Intergovernmental Panel on Climate Change’s (IPCC) 2013 report, which says that Antarctica is overall losing land ice.

According to the new analysis of satellite data, the Antarctic ice sheet showed a net gain of 112 billion tons of ice a year from 1992 to 2001. That net gain slowed to 82 billion tons of ice per year between 2003 and 2008.

“We’re essentially in agreement with other studies that show an increase in ice discharge in the Antarctic Peninsula and the Thwaites and Pine Island region of West Antarctica,” said Jay Zwally, a glaciologist with NASA Goddard Space Flight Center in Greenbelt, Maryland, and lead author of the study, which was published on Oct. 30 in the Journal of Glaciology. “Our main disagreement is for East Antarctica and the interior of West Antarctica – there, we see an ice gain that exceeds the losses in the other areas.” Zwally added that his team “measured small height changes over large areas, as well as the large changes observed over smaller areas.”

Scientists calculate how much the ice sheet is growing or shrinking from the changes in surface height that are measured by the satellite altimeters. In locations where the amount of new snowfall accumulating on an ice sheet is not equal to the ice flow downward and outward to the ocean, the surface height changes and the ice-sheet mass grows or shrinks.

Snow covering Antarctic peninsula.

Keeping Things in Perspective

Such reports often include scary graphs like this one and the reader is usually provided no frame of reference or context to interpret the image. First, the chart is showing cumulative loss of mass arising from an average rate of 100 Gt lost per year since 2002. Many years had gains, including 2002, and the cumulative loss went below zero only in 2006.  Also, various methods of measuring and analyzing give different results, as indicated by the earlier section.

Most important is understanding the fluxes in proportion to the Antarctic Ice Sheet.  Let’s do the math.  Above it was stated Antarctica contains ~30 million cubic kilometers of ice volume.  One km3 of water is 1 billion cubic meters and weighs 1 billion tonnes, or 1 gigatonne.  So Antarctica has about 30,000,000 gigatonnes of ice.  Since ice is slightly less dense than water, the total should be adjusted by 0.92 for an estimate of 27.6 M Gts of ice comprising the Antarctic Ice Sheet.

So in the recent decade, an average year went from 27,600,100 Gt to 27,600,000, according to one analysis.  Other studies range from losing 200 Gt/yr to gaining 100 Gt/yr.

Even if Antarctica lost 200 Gt/yr. for the next 1000 years, it would only approach 1% of the ice sheet.

If like Al Gore you are concerned about sea level rise, that calculation starts with the ocean area estimated to be 3.618 x 10^8 km2 (361,800,000 km2). To raise that area 1 mm requires 3.618×10^2 km3 or 361.8 km3 water (1 km3 water=1 Gt.) So 200 Gt./yr is about 0.55mm/yr or 6 mm a decade, or 6 cm/century.

By all means let’s pay attention to things changing in our world, but let’s also notice the scale of the reality and not make mountains out of molehills.

Let’s also respect the scientists who study glaciers and their subtle movements over time (“glacial pace”).  Below is an amazing video showing the challenges and the beauty of working on Greenland Glacier.

From Ice Alive: Uncovering the secrets of Earth’s Ice

For more on the Joys of Playing Climate Whack-A-Mole 

Media Raises False Alarms of Ocean Cooling

The RAPID moorings being deployed. Credit: National Oceanography Centre.

The usual suspects, such as BBC, the Guardian, New York Times, Washington Post etc., are reporting that the Atlantic gulf stream is slowing down due to climate change, threatening an ice age.  That’s right, warmists are now claiming fossil fuels do cooling when they are not warming.  As usual the headlines are not supported by the details.

The AMOC is back in the news following a recent Ocean Sciences meeting.  This update adds to the theme Oceans Make Climate. Background links are at the end, including one where chief alarmist M. Mann claims fossil fuel use will stop the ocean conveyor belt and bring a new ice age.  Actual scientists are working away methodically on this part of the climate system, and are more level-headed.  H/T GWPF for noticing the recent article in Science Ocean array alters view of Atlantic ‘conveyor belt’  By Katherine Kornei Feb. 17, 2018 . Excerpts with my bolds.

The powerful currents in the Atlantic, formally known as the Atlantic meridional overturning circulation (AMOC), are a major engine in Earth’s climate. The AMOC’s shallower limbs—which include the Gulf Stream—transport warm water from the tropics northward, warming Western Europe. In the north, the waters cool and sink, forming deeper limbs that transport the cold water back south—and sequester anthropogenic carbon in the process. This overturning is why the AMOC is sometimes called the Atlantic conveyor belt.

Fig. 1. Schematic of the major warm (red to yellow) and cold (blue to purple) water pathways in the NASPG (North Atlantic subpolar gyre ) credit: H. Furey, Woods Hole Oceanographic Institution): Denmark Strait (DS), Faroe Bank Channel (FBC), East and West Greenland Currents (EGC and WGC, respectively), NAC, DSO, and ISO.

In February at the American Geophysical Union’s (AGU’s) Ocean Sciences meeting, scientists presented the first data from an array of instruments moored in the subpolar North Atlantic. The observations reveal unexpected eddies and strong variability in the AMOC currents. They also show that the currents east of Greenland contribute the most to the total AMOC flow. Climate models, on the other hand, have emphasized the currents west of Greenland in the Labrador Sea. “We’re showing the shortcomings of climate models,” says Susan Lozier, a physical oceanographer at Duke University in Durham, North Carolina, who leads the $35-million, seven-nation project known as the Overturning in the Subpolar North Atlantic Program (OSNAP).

Fig. 2. Schematic of the OSNAP array. The vertical black lines denote the OSNAP moorings with the red dots denoting instrumentation at depth. The thin gray lines indicate the glider survey. The red arrows show pathways for the warm and salty waters of subtropical origin; the light blue arrows show the pathways for the fresh and cold surface waters of polar origin; and the dark blue arrows show the pathways at depth for waters that originate in the high-latitude North Atlantic and Arctic.

The research and analysis is presented by Dr. Lozier et al. in this publication Overturning in the Subpolar North Atlantic Program: A New International Ocean Observing System Images above and text excerpted below with my bolds.

For decades oceanographers have assumed the AMOC to be highly susceptible to changes in the production of deep waters at high latitudes in the North Atlantic. A new ocean observing system is now in place that will test that assumption. Early results from the OSNAP observational program reveal the complexity of the velocity field across the section and the dramatic increase in convective activity during the 2014/15 winter. Early results from the gliders that survey the eastern portion of the OSNAP line have illustrated the importance of these measurements for estimating meridional heat fluxes and for studying the evolution of Subpolar Mode Waters. Finally, numerical modeling data have been used to demonstrate the efficacy of a proxy AMOC measure based on a broader set of observational data, and an adjoint modeling approach has shown that measurements in the OSNAP region will aid our mechanistic understanding of the low-frequency variability of the AMOC in the subtropical North Atlantic.

Fig. 7. (a) Winter [Dec–Mar (DJFM)] mean NAO index. Time series of temperature from the (b) K1 and (c) K9 moorings.

Finally, we note that while a primary motivation for studying AMOC variability comes from its potential impact on the climate system, as mentioned above, additional motivation for the measure of the heat, mass, and freshwater fluxes in the subpolar North Atlantic arises from their potential impact on marine biogeochemistry and the cryosphere. Thus, we hope that this observing system can serve the interests of the broader climate community.

Fig. 10. Linear sensitivity of the AMOC at (d),(e) 25°N and (b),(c) 50°N in Jan to surface heat flux anomalies per unit area. Positive sensitivity indicates that ocean cooling leads to an increased AMOC—e.g., in the upper panels, a unit increase in heat flux out of the ocean at a given location will change the AMOC at (d) 25°N or (e) 50°N 3 yr later by the amount shown in the color bar. The contour intervals are logarithmic. (a) The time series show linear sensitivity of the AMOC at 25°N (blue) and 50°N (green) to heat fluxes integrated over the subpolar gyre (black box with surface area of ∼6.7 × 10 m2) as a function of forcing lead time. The reader is referred to Pillar et al. (2016) for model details and to Heimbach et al. (2011) and Pillar et al. (2016) for a full description of the methodology and discussion relating to the dynamical interpretation of the sensitivity distributions.

In summary, while modeling studies have suggested a linkage between deep-water mass formation and AMOC variability, observations to date have been spatially or temporally compromised and therefore insufficient either to support or to rule out this connection.

Current observational efforts to assess AMOC variability in the North Atlantic.

The U.K.–U.S. Rapid Climate Change–Meridional Overturning Circulation and Heatflux Array (RAPID–MOCHA) program at 26°N successfully measures the AMOC in the subtropical North Atlantic via a transbasin observing system (Cunningham et al. 2007; Kanzow et al. 2007; McCarthy et al. 2015). While this array has fundamentally altered the community’s view of the AMOC, modeling studies over the past few years have suggested that AMOC fluctuations on interannual time scales are coherent only over limited meridional distances. In particular, a break point in coherence may occur at the subpolar–subtropical gyre boundary in the North Atlantic (Bingham et al. 2007; Baehr et al. 2009). Furthermore, a recent modeling study has suggested that the low-frequency variability of the RAPID–MOCHA appears to be an integrated response to buoyancy forcing over the subpolar gyre (Pillar et al. 2016). Thus, a measure of the overturning in the subpolar basin contemporaneous with a measure of the buoyancy forcing in that basin likely offers the best possibility of understanding the mechanisms that underpin AMOC variability. Finally, though it might be expected that the plethora of measurements from the North Atlantic would be sufficient to constrain a measure of the AMOC within the context of an ocean general circulation model, recent studies (Cunningham and Marsh 2010; Karspeck et al. 2015) reveal that there is currently no consensus on the strength or variability of the AMOC in assimilation/reanalysis products.

Atlantic Meridional Overturning Circulation (AMOC). Red colours indicate warm, shallow currents and blue colours indicate cold, deep return flows. Modified from Church, 2007, A change in circulation? Science, 317(5840), 908–909. doi:10.1126/science.1147796

In addition we have a recent report from the United Kingdom Marine Climate Change Impacts Partnership (MCCIP) lead author G.D. McCarthy Atlantic Meridional Overturning Circulation (AMOC) 2017.

Figure 1: Ten-day (colours) and three month (black) low-pass filtered timeseries of Florida Straits transport (blue), Ekman transport (green), upper mid-ocean transport (magenta), and overturning transport (red) for the period 2nd April 2004 to end- February 2017. Florida Straits transport is based on electromagnetic cable measurements; Ekman transport is based on ERA winds. The upper mid-ocean transport, based on the RAPID mooring data, is the vertical integral of the transport per unit depth down to the deepest northward velocity (~1100 m) on each day. Overturning transport is then the sum of the Florida Straits, Ekman, and upper mid-ocean transports and represents the maximum northward transport of upper-layer waters on each day. Positive transports correspond to northward flow.

The RAPID/MOCHA/WBTS array (hereinafter referred to as the RAPID array) has revolutionized basin scale oceanography by supplying continuous estimates of the meridional overturning transport (McCarthy et al., 2015), and the associated basin-wide transports of heat (Johns et al., 2011) and freshwater (McDonagh et al., 2015) at 10-day temporal resolution. These estimates have been used in a wide variety of studies characterizing temporal variability of the North Atlantic Ocean, for instance establishing a decline in the AMOC between 2004 and 2013.

Summary from RAPID data analysis

MCCIP reported in 2006 that:

  • a 30% decline in the AMOC has been observed since the early 1990s based on a limited number of observations. There is a lack of certainty and consensus concerning the trend;
  • most climate models anticipate some reduction in strength of the AMOC over the 21st century due to increased freshwater influence in high latitudes. The IPCC project a slowdown in the overturning circulation rather than a dramatic collapse.And in 2017 that:
  • a substantial increase in the observations available to estimate the strength of the AMOC indicate, with greater certainty, a decline since the mid 2000s;
  • the AMOC is still expected to decline throughout the 21st century in response to a changing climate. If and when a collapse in the AMOC is possible is still open to debate, but it is not thought likely to happen this century.

And also that:

  • a high level of variability in the AMOC strength has been observed, and short term fluctuations have had unexpected impacts, including severe winters and abrupt sea-level rise;
  • recent changes in the AMOC may be driving the cooling of Atlantic ocean surface waters which could lead to drier summers in the UK.

Conclusions

  • The AMOC is key to maintaining the mild climate of the UK and Europe.
  • The AMOC is predicted to decline in the 21st century in response to a changing climate.
  • Past abrupt changes in the AMOC have had dramatic climate consequences.
  • There is growing evidence that the AMOC has been declining for at least a decade, pushing the Atlantic Multidecadal Variability into a cool phase.
  • Short term fluctuations in the AMOC have proved to have unexpected impacts, including being linked
    with severe winters and abrupt sea-level rise.

Background:

Oceans Make Climate: SST, SSS and Precipitation Linked

Climate Pacemaker: The AMOC

Evidence is Mounting: Oceans Make Climate

Mann-made Global Cooling

 

 

2018 Hurricane Prediction – Strongest Cycle in 70 Years

Monday, Sept. 18, 2017, GOES East satellite image provided by NASA shows the eye of Hurricane Maria as it nears Dominica and before it struck Puerto Rico. NASA /AP

This prediction comes from Global Weather Oscillations, the only hurricane forecaster to predict the 2017 season accurately.  The story is from 721News 2018 Hurricane Prediction – Strongest Cycle in 70 Years

Links at the end provide more explanation of GWO’s unique model based upon ocean water pulses linked to solar/lunar activities, nothing to do with CO2.  Text below from 712News with my bolds.

Global Weather Oscillations (GWO) was cited by news media as the only major hurricane prediction organization that correctly predicted the hyperactive 2017 Atlantic hurricane season from beginning to end, and the destructive United States hurricane landfalls.

The media also noted that when the hurricane season began last year, “nearly every major weather agency predicted a normal 2017 hurricane season – but only Global Weather Oscillations Inc. (GWO) had an accurate forecast” – with a prediction for a destructive hurricane season with 16 named storms, eight hurricanes, four major hurricanes – and 2 major impact hurricanes for the United States.

GWO also predicted the United States would have 6 named storms and 3 hurricanes making landfall in 2017 – and where they would occur. Just as predicted, the U.S. ended up with six named storms and 3 hurricanes. GWO predicted that the Florida Peninsula would break out of their 12-year hurricane drought with a major category 3-4 hurricane making landfall on the south tip of Florida. GWO also predicted that Texas could break out of their 8-year hurricane drought with a landfalling hurricane just above Corpus Christi – and a Category 1 hurricane striking the upper Gulf Coast. The 2017 landfalling hurricanes ended up being – Harvey, Irma and Nate.

Professor David Dilley – senior research and prediction scientist for Global Weather Oscillations – prepares hurricane and tropical storm predictions for 11 zones stretching from New England to Texas. By using Climate Pulse Technology developed by Mr. Dilley, GWO can issue accurate zone predictions for release in January – well before the beginning of the hurricane season.

Professor David Dilley, states that the “Climate Pulse Technology Model” is based on natural rhythm cycles that control hurricane landfall cycles and the position of the Bermuda High Pressure Center. By utilizing this technology, GWO has issued the most accurate predictions by any organization during the past 10 years. The preseason zone predictions are so accurate – updates to the forecasts are not required during the hurricane season. Although GWO does offer special weekly hurricane outlook webinars and tracking webinars when a storm may threaten the United States. GWO is a working partner with the International Hurricane Protection Association – INHPA.

Prediction: 2018 Atlantic Basin Hurricane Season — (includes the Caribbean Sea and Gulf of Mexico)

As predicted by Mr. Dilley and GWO – last year (2017) was the costliest year on record for the United States, and one of the most destructive. Mr. Dilley says that “some United States zones are currently in their strongest hurricane landfall cycle in 40 to 70-years.” This is a Natural Climate Pulse Cycle that produced extremely active and dangerous hurricane conditions in some zones back in the 1930s and 1940s – and is now repeating.

Mr. Dilley predicts that 2018 will be somewhat of a repeat of 2017 – and possibly another record breaker. Although it will be strikingly similar to last year- some hurricane landfalls will occur in different locations this year. You can expect 16 named storms, 8 hurricanes, 4 major hurricanes, potential for 4 United States hurricane landfalls – 2 of which will likely be major impact storms. There is the potential for 6 named storms making United States landfalls. On the average, the entire Atlantic Basin has 12 named storms, 6 hurricanes and 2.7 major hurricanes.

The reason for another destructive hurricane season is 3-fold. The ocean water temperatures continue to run warmer than normal across most of the Atlantic Basin (red and orange in the graphic), and especially in the Caribbean region and the Atlantic near the United States. This is very similar to the ocean temperatures of last year, and this will again be conducive for tropical storms and/or hurricanes forming and/or strengthening close to the United States. Mr. Dilley also expects the Bermuda-Azores High Pressure Center will again be in a favorable location – thus allowing more named storms to maintain strength – or strengthen as they move from east to west across the Atlantic toward the United States.

Source: Global Weather Oscillations

Then we come to the last item – El Niño. GWO’s Climate Pulse Technology model indicates that the Tropical South Pacific Ocean temperatures where El Niño events typically form – will warm significantly during late winter and approach weak El Niño conditions during the spring- much like the El Niño scare of last year. However, all years are not the same – therefore it could mature enough to form a very weak El Niño, but not strong enough to dampen the hurricane season. Historical records indicate that moderate to strong El Nino events dampen hurricane activity – whereas years with very weak El Niño conditions can be associated with active hurricane seasons if a Climate Pulse Hurricane Enhancement Cycle is in place – and it is.

Background

Global Weather Oscillations

AMO: Atlantic Climate Pulse

Hurricane Science, not Fiction

CO2 Rise ≠ Sea Level Rise

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This recent paper is very topical, since several US coastal states are suing oil companies for damages expected from rising sea levels. Some Alaskan teenagers are making similar claims in a separate lawsuit against the US federal government. The study is Why would sea-level rise for global warming and polar ice-melt? By Aftab Alam Khan published in Geoscience Frontiers. Excerpts below with my bolds. H/T to NoTricksZone

IPCC Alarms over Sea Level Rise

Sea Level Change in the Fifth Assessment Report includes detailed explanation of the changes in the global mean sea level, regional sea level, sea level extremes, and waves (Church et al., 2013). Anthropogenic greenhouse gas emissions are causing sea-level rise (SLR) (Church and White, 2006; Jevrejeva et al., 2009). It is also claimed that ocean thermal expansion and glacier melting have been the dominant contributors to 20th century global mean sea level rise. It is further opined that global warming is the main contributor to the rise in global sea level since the Industrial Revolution (Church and White, 2006). According to Cazenave and Llovel (2010) rising of air temperature can warm and expand ocean waters wherein thermal expansion was the main driver of global sea level rise for 75 to 100 years after the start of the Industrial Revolution.

However, the share of thermal expansion in global sea level rise has declined in recent decades as the shrinking of land ice has accelerated (Lombard et al 2005). Lombard et al. (2006) opined that recent investigations based on new ocean temperature data sets indicate that thermal expansion only explains part (about 0.4 mm/yr) of the 1.8 mm/yr observed sea level rise of the past few decades. However, observation claim of 1.8 mm/yr sea level rise is also limited in scope and accuracy.

Fundamentals of Sea Level Variability

Mean Sea Level (MSL) is defined as the zero elevation for a local area. The zero surface referenced by elevation is called a vertical datum. Since sea surface conforms to the earth’s gravitational field, MSL has also slight hills and valleys that are similar to the land surface but much smoother. The MSL surface is in a state of gravitational equilibrium. It can be regarded as extending under the continents and is a close approximation of geoid. By definition geoid describes the irregular shape of the earth and is the true zero surface for measuring elevations. Because geoid surface cannot directly be observed, heights above or below the geoid surface can’t be directly measured and are inferred by making gravity measurements and modeling the surface mathematically.

Previously, there was no way to accurately measure geoid so it was roughly approximated by MSL. Although for practical purposes geoid and MSL surfaces are assumed to be essentially the same, but in reality geoid differs from MSL by several meters. Geoid moves above MSL where mass is excess and moves below MSL where mass is deficient. Distribution of mass in the crust in terms of ‘excess’ and ‘deficient’ can cause volume expansion and contraction for relative sea-level change. Height of the ocean surface at any given location, or sea level, is measured either with respect to the surface of the solid Earth i.e., relative sea level (RSL) or a eustatic sea level (ESL) (Fig. 1A).

Relative sea level (RSL) change can differ significantly from global mean sea level (GMSL) because of spatial variability in changes of the sea surface and ocean floor height. RSL change over the ocean surface area gives the change in ocean water volume, which is directly related to the sea level change. Sea level changes can be driven either by variations in the masses or volume of the oceans, or by changes of the land with respect to the sea surface. In the first case, a sea level change is defined ‘eustatic’; otherwise, it is defined ‘relative’ (Rovere et al., 2016). According to Kemp et al. (2015) land uplift or subsidence can result in, respectively, a fall or rise in sea level that cannot be considered eustatic as the volume or mass of water does not change. Any sea level change that is observed with respect to a land-based reference frame is defined a relative sea level (RSL) change. Eustatic Sea Level (ESL) changes also occur when the volume of the ocean basins changes due to tectonic seafloor spreading or sedimentation.

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Figure 1. (A) Definition of sea level i.e., eustatic sea level and relative sea level (B) Different types of sea level observation techniques: satellite altimetry (based on NASA educational material), tide gauge and paleo sea level indicators (see text for details). Modern tide gauges are associated with a GPS station that records land movements.

Sea Level Observations

Changes in sea level can be observed at very different time scales and with different techniques (Fig. 1B). Regardless of the technique used, no observation allows to record purely eustatic sea level changes. At multi-decadal time scales, sea level reconstructions are based on satellite altimetry/gravimetry and landbased tide gauges (Cabanes et al., 2001). At longer time scales (few hundreds, thousands to millions of years), the measurement of sea level changes relies on a wide range of sea level indicators (Shennan and Horton, 2002; Vacchi et al., 2016; Rovere et al., 2016a). One of the most common methods to observe sea level changes at multi-decadal time scales is tide gauges.

Modern tide gauges are associated with a GPS station that records land movements (Fig. 1B). However, tide gauges have three main disadvantages: (i) they are unevenly distributed around the world (Julia Pfeffer and Allemand, 2015); (ii) the sea level signal they record is often characterized by missing data (Hay et al., 2015); and (iii) accounting for ocean dynamic changes and land movements might prove difficult in the absence of independent datasets (Rovere et al., 2016). Since 1992, tide gauge data are complemented by satellite altimetry datasets (Cazenave et al., 2002).

The altitude of the satellite is established with respect to an ellipsoid, which is an arbitrary and fixed surface that approximates the shape of the Earth. The difference between the altitude of the satellite and the range is defined as the sea surface height (SSH) (Fig. 1B). Subtracting from the measured SSH a reference mean sea surface (e.g. the geoid), one can obtain a ‘SSH anomaly’. The global average of all SSH anomalies can be plotted over time to define the global mean sea level change, which can be considered as the eustatic, globally averaged sea level change.

The shape of the geoid is crucial for deriving accurate measurements of seasonal sea level variations (Chambers, 2006). According to Rovere et al. (2016) measurements of paleo eustatic sea level (ESL) changes bear considerable uncertainty. Further, sea level changes on Earth cannot be treated as a rigid container although eustasy is defined in view of Earth as a rigid container. In reality, internal and external processes of the earth such as tectonics, dynamic topography, sediment compaction and melting ice all trigger variations of the container and these ultimately affect any sea level observation.

An estimated, observed, and possible future amounts of global sea level rise from 1800 to 2100, relative to the year 2000 has been proposed by Melillo et al. (2014) based on the works of Church and White (2011), Kemp et al. (2011) and Parris et al. (2012) (Fig. 2). The main concern of the predicted future global sea level rise shown in Melillo et al. (2014) is the forecast beyond 2012 up to 2100. Although sea level rise is shown by 0.89 ft in 209 years (between 1800 and 2009) at the rate of 0.0043 ft/yr, the prediction of 4–6 ft at the rate of 0.044 ft/yr and 0.066 ft/yr respectively in 91 years between 2009 and 2100) is highly questionable. An abrupt jump in the sea level rise after 2009 is definitely a conjecture.

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Figure 2. Estimated, observed, and predicted global sea level rise from 1800 to 2100. Estimates from proxy data are shown in red between 1800 and 1890, pink band shows uncertainty. Tide gauge data is shown in blue for 1880–2009. Satellite observations are shown in green from 1993 to 2012. The future scenarios range from 0.66 ft to 6.6 ft in 2100 (Redrawn from Melillo et al., 2014).

Sea Level Distribution is Determined by the Earth Surface

This study is based on the geophysical aspects of the earth wherein shape of the earth is the fundamental component of global sea level distribution. The physical surface of the earth adjusted to the mathematical surface of the earth is spheroidal. This spheroidal surface always coincides with the global mean sea level (Fig. 3). Having relationship between the shape of the earth and the global sea level, gravitational attraction of the earth plays a dominant role against sea level rise. Gravity is a force that causes earth to form the shape of a sphere by pulling the mass of the earth close to the center of gravity i.e., each mass-particle is attracted perpendicular towards the center of gravity of the earth (Fig. 4A).

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Figure 3. Physical surface (light green undulating line) of the earth adjusted to spheroidal surface (yellow broken line) by removing mass from continent above mean sea level and filling same mass in ocean below mean sea level. Geoid surface (light blue solid line), on the other hand, depends on the internal mass distribution i.e., geoid moves below spheroid where mass is deficient and it moves above spheroid where mass is excess. Where geoid surface and spheroidal surface coincides is accounted for mass balanced. By definition geoid describes the irregular shape of the earth and is the true zero surface for measuring elevations. Because geoid surface cannot be directly observed, heights above or below the geoid surface can’t be directly measured and are inferred by making gravity measurements and modeling the surface mathematically. MSL surfaces are assumed to be essentially the same, at some spots the geoid can actually differ from MSL by several meters.

The sphere-like shape of the earth is distorted by (i) greater gravity attraction of the polar region causing polar flattening and lesser gravity attraction of the equatorial region causing equatorial bulging, and (ii) the centrifugal force of its rotation. This force causes the mass of the earth to move away from the center of gravity, which is located at the equator. Ocean-fluid surface takes a outward normal vector due to centrifugal force which is maximum at the equator and zero at the poles (Fig. 4B). Mathematical surface, an imaginary surface coinciding with the mean sea level of the Earth is a spheroidal surface due to its spin, and it is the centrifugal force due to the Earth’s spin caused polar flattening and equatorial bulge. The polar flattening ratio (eccentricity) of 1/298 implied that sea level at the equator is about 21 km further from the center of the Earth than it is at the poles. Water would find its hydrostatic level which is curvilinear, and this level is influenced by the gravity as well as centrifugal force. Centrifugal force acts as much on the oceans as it does on the solid Earth, which is maximum at the equator and minimum at the pole (Fig. 4B). Any addition of water to the oceans is supposed to flow uphill towards equator from the poles causing sea level rise everywhere, but it does not. Hence, although ocean water at the equator makes a level difference of 21 km higher than at the poles, it is the centrifugal force maximum at the equator and zero at the poles would prevent ocean water-column from moving down-hill toward poles effectively restricting sea level rise at the higher latitudes. On the other hand high gravity attraction and zero centrifugal force at the poles and low gravity attraction and maximum centrifugal force at the equator effectively balance sea-level and restrict sea-level rise. While, equatorial ocean-fluid surface always attains relatively higher altitude than that of polar ocean-fluid surface, ocean water column from polar region would not move towards equatorial region.

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Figure 4. The shape of a sphere by pulling the mass of the earth close to the center of gravity. Blue arrows point from Earth’s surface toward its center. Their lengths represent local gravitational field strength. Gravity is strongest at the poles because they are closest to the center of mass. This difference is enhanced by the increasing density toward the center. Red arrows show the direction and magnitude of the centrifugal effect. On the equator, it is large and straight up. Near the poles, it is small and nearly horizontal. Vector addition of the blue and red arrows gives the net result of gravity plus centrifugal effect. This is shown by the green arrows. Rotation of the earth produces more centrifugal force at the equator, less as latitude increases, and zero at pole.

A mass of fluid under the rotation assumes a form such that its external form is an equipotential of its own attraction and the potential of the centripetal acceleration. Above analogy reveals that even if entire polar-ice melts due to the global warming, the melt-water will not flow towards equatorial region where surface has an upward gradient and gravity attraction is also significantly low in comparison to the polar region. However, conditions at both the poles are different. Arctic Ocean in the north is surrounded by the land mass thus can restrict the movement of the floating ice, while, Antarctic in the south is surrounded by open ocean thus floating ice can freely move to the north. But this movement is likely to be limited maximum up to 60°S latitude where spheroidal surface has the maximum curvature (Fig. 6B). As usual, water can not flow from higher gravity attraction to lower gravity attraction rather it is other way around wherein higher gravity attraction of the poles would attract water from moving towards equatorial region and water column would be static at every ‘gz’ direction. Further, greater horizontal gravity gradient toward poles would also help melt-water to remain attracted toward polar region.

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Figure 6. (A) Surface of the earth is defined in terms of gravity values at all surface points known as the reference spheroid. It is related to the mean sea-level (MSL) surface with excess land masses removed and ocean deeps filled. Thus it is an equipotential surface, that is, the force of gravity (gz) (red arrows) is everywhere normal to this surface, or the plumb line is vertical at all points directed to the center of the earth having maximum at the poles and minimum at the equator. Two components work against sea level rise i.e., greater gravity attraction of the polar region and the equatorial bulge (B) Maximum curvature of the spheroidal surface of the Earth coincides with 60oN latitude. Floating ice from Antarctica surrounded by open ocean can freely move to the north likely to be limited maximum upto 60oS latitude where spheroidal surface has the maximum curvature.

A geoid surface thus prepared exhibits bulges and hollows of the order of hundreds of kilometers in diameter and up to hundred meter in elevation occurring in the zone mostly between 60°N and 60°S latitudes. Marked changes in the contour pattern of the geoid height in the zone between 60°N and 60°S suggests maximum curvature along 60°N and 60°S. Hence any change of the global sea level due to the predicted ice melt would not extend beyond 60°N and 60°S. However the reality is that no sea-level rise actually would occur due to ice melt as a result of same volumetric replacement between melt-water and floating ice.

Lindsay and Schweiger (2015) provide a longer-term view of ice thickness, compiling a variety of subsurface, aircraft, and satellite observations. They found that ice thickness over the central Arctic Ocean has declined from an average of 3.59 m (11.78 ft) to only 1.25 m (4.10 ft), a reduction of 65% over the period 1975 to 2012. Map shows sea ice thickness in meters in the Arctic Ocean from March 29, 2015 to April 25, 2015 (Fig. 9B). Total volume of ice-melt water of more than 2,500,000 km3 has been added to ocean water over an area more than 14,500,000 km2 of the central Arctic Ocean (Fig. 9B blue shaded area). By now this additional water should have caused sea level rise more than 178 mm which is much greater than what has been projected and predicted. However there is no record of such sea level rise.

Arctic sea-ice has already reduced its volume due to melting from 33,000 km3 in 1979 to 16,000 km3 in 2016 without showing any sea level rise. Although Arctic sea-ice has reduced its volume, Antarctic has gained (Zhang and Rothrock, 2003) (http://psc.apl.uw.edu). In contrast to the melting of the Arctic sea-ice, sea-ice around Antarctica was expanding as of 2013 (Bintanja et al., 2013). NASA study shows an increase in Antarctic snow accumulation that began 10,000 years ago is currently adding enough ice to the continent to outweigh the increased losses from its thinning glaciers.

From the above statement it is clearly understood that about 23,000 km3 sea-ice of Antarctica can freely float northward into the warmer water where it eventually melts every year without showing any sea level rise in the lower latitudes. Further, melting of such a huge volume of floating sea-ice of Antarctica not only can reoccupy volume of the displaced water but also can cool ocean-water in the lower latitudes of the southern oceans thus can prevent sea level rise due to thermal expansion of the ocean water. According to Zhang (2007) thermal expansion in the lower latitude is unlikely because of the reduced salt rejection and upper-ocean density and the enhanced thermohaline stratification tend to suppress convective overturning, leading to a decrease in the upward ocean heat transport and the ocean heat flux available to melt sea ice. The ice melting from ocean heat flux decreases faster than the ice growth does in the weakly stratified Southern Ocean, leading to an increase in the net ice production and hence an increase in ice mass.

Both the polar regions exhibit reduction in ice-load in the crust due to melting and removal of ice-cover from the continental blocks every year. Reduction of such weight in the continent thus can cause isostasy to come into play and land start to uplift due to elastic rebound to maintain its isostatic equilibrium which is load-dependent and would prevent sea level rise.

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Figure 13. (A) Layered beach at Bathurst Inlet, Nunavut signifying post-glacial isostatic rebound (B) Some of the most dramatic uplift is found in Iceland. Evidence of isostatic rebound (C) Massive coral (Pavona clavus) exposed in 1954 by tectonic uplift in the Galapagos Islands, Ecuador (D) Beach ridges on the coast of Novaya Zemlya in arctic Russia, an example of Holocene glacio-isostatic rebound (E) A beach in Juneau, Alaska where sea level is not rising, but dropping due to glacial isostatic adjustment (F) Boat-houses in Scandinavia now considerably farther away from the water’s edge where they were built demonstrates land uplift (G) An 8000-year old-well off the coast of Israel now submerged, which is a land mark of crustal subsidence (H) The “City beneath the Sea”; Port Alexandria on the Nile delta and the drowned well off the coast of Israe (panel (G), both subsided due to subduction-pull of the downgoing African crustal slab as it enters trench.

Postglacial rebound continues today albeit very slowly wherein the land beneath the former ice sheets around Hudson Bay and central Scandinavia, is still rising by over a centimetre a year, while those regions which had bulged upwards around the ice sheet are subsiding such as the Baltic states and much of the eastern seaboard of North America. Snay et al. (2016) have found large residual vertical velocities, some with values exceeding 30 mm/yr, in southeastern Alaska. The uplift occurring here is due to present-day melting of glaciers and ice fields formed during the Little Ice Age glacial advance that occurred between 1550 A.D. and 1850 A.D.

When the land area shrinks globally, this corresponds to a global rise in sea level. From the curve it is certain that sea level has changed in geologic time scale due to geologic events. Hence, polar ice-melting would not contribute to sea-level rise rather sea-level would drop around the Arctic region as long as isostatic rebound will continue. Claim and prediction of 3 mm/yr rise of sea-level due to global warming and polar ice-melt is definitely a conjecture. Prediction of 4–6.6 ft sea level rise in the next 91 years between 2009 and 2100 is highly erroneous.

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Figure 12. Vail and Hallam curves of global paleo sea level fluctuations from the last 542 million years (Copied and redrawn from https://en.wikipedia.org/wiki/Sea-level_curve).

A negative sea level trend implied that Alaska is being uplifted continuously and corresponding sea level is dropping. However, permanent uplift and corresponding sea level drop of Alaska will occur through ultimate fault rupture between land and sea. Until that time it will continue to show the pattern of sea level as of Fig. 14A.

Conclusion
Geophysical shape of the earth is the fundamental component of the global sea level distribution. Global warming and ice-melt, although a reality, would not contribute to sea-level rise. Gravitational attraction of the earth plays a dominant role against sea level rise. As a result of low gravity attraction in the region of equatorial bulge and high gravity attraction in the region of polar flattening, melt-water would not move from polar region to equatorial region. Further, melt-water of the floating ice-sheets will reoccupy same volume of the displaced water by floating ice-sheets causing no sea-level rise. Arctic Ocean in the north is surrounded by the land mass thus can restrict the movement of the floating ice, while, Antarctic in the south is surrounded by open ocean thus floating ice can freely move to the north. Melting of huge volume of floating sea-ice around Antarctica not only can reoccupy volume of the displaced water but also can cool ocean-water in the region of equatorial bulge thus can prevent thermal expansion of the ocean water. Melting of land ice in both the polar region can substantially reduce load on the crust allowing crust to rebound elastically for isostatic balancing through uplift causing sea level to drop relatively. Palaeo-sea level rise and fall in macro-scale are related to marine transgression and regression in addition to other geologic events like converging and diverging plate tectonics, orogenic uplift of the collision margin, basin subsidence of the extensional crust, volcanic activities in the oceanic region, prograding delta buildup, ocean floor height change and sub-marine mass avalanche.

Summary

This  research paper reads like a tutorial on sea level rise, and explains the geoscience behind fluctuations in observed sea levels over all time scales.  It should be required reading for Judge Alsup, lawyers and litigants in these multiple lawsuits.

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Food, Conflict and Climate

From data versus models department, a recent study contradicts claims linking human conflict to climate change by means of food shortages. From Dartmouth College March 1, 2018 comes Food Abundance and Violent Conflict in Africa.  by Ore Koren.  American Journal of Agricultural Economics, 2018; Synopsis is from Science Daily (here) with my bolds.

Food abundance driving conflict in Africa, not food scarcity

The study refutes the notion that climate change will increase the frequency of civil war in Africa as a result of food scarcity triggered by rising temperatures and drought. Most troops in Africa are unable to sustain themselves due to limited access to logistics and state support, and must live off locally sourced food. The findings reveal that the actors are often drawn to areas with abundant food resources, whereby, they aim to exert control over such resources.

To examine how the availability of food may have affected armed conflict in Africa, the study relies on PRIO-Grid data from over 10,600 grid cells in Africa from 1998 to 2008, new agricultural yields data from EarthStat and Armed Conflict Location and Event Dataset, which documents incidents of political violence, including those with and without casualties. The data was used to estimate how annual local wheat and maize yields (two staple crops) at a local village/town level may have affected the frequency of conflict. To capture only the effects of agricultural productivity on conflict rather than the opposite, the analysis incorporates the role of droughts using the Standardized Precipitation Index, which aggregates monthly precipitation by cell year.

The study identifies four categories in which conflicts may arise over food resources in Africa, which reflect the interests and motivations of the respective group:

  1. State and military forces that do not receive regular support from the state are likely to gravitate towards areas, where food resources are abundant in order to feed themselves.
  2. Rebel groups and non-state actors opposing the government may be drawn to food rich areas, where they can exploit the resources for profit.
  3. Self-defense militias and civil defense forces representing agricultural communities in rural regions, may protect their communities against raiders and expand their control into other areas with arable land and food resources.
  4. Militias representing pastoralists communities live in mainly arid regions and are highly mobile, following their cattle or other livestock, rather than relying on crops. To replenish herds or obtain food crops, they may raid other agriculturalist communities.

These actors may resort to violence to seek access to food, as the communities that they represent may not have enough food resources or the economic means to purchase livestock or drought-resistant seeds. Although droughts can lead to violence, such as in urban areas; this was found not to be the case for rural areas, where the majority of armed conflicts occurred where food crops were abundant.

Food scarcity can actually have a pacifying effect.“Examining food availability and the competition over such resources, especially where food is abundant, is essential to understanding the frequency of civil war in Africa,” says Ore Koren, a U.S. foreign policy and international security fellow at Dartmouth College and Ph.D. candidate in political science at the University of Minnesota. “Understanding how climate change will affect food productivity and access is vital; yet, predictions of how drought may affect conflict may be overstated in Africa and do not get to the root of the problem. Instead, we should focus on reducing inequality and improving local infrastructure, alongside traditional conflict resolution and peace building initiatives,” explains Koren.

Summary:

In Africa, food abundance may be driving violent conflict rather than food scarcity, according to a new study. The study refutes the notion that climate change will increase the frequency of civil war in Africa as a result of food scarcity triggered by rising temperatures and drought.

Reading the study itself shows considerable rigor in sorting out dependent and independent variables.  It is certain that armed conflicts destroy food resources, while it is claimed that food shortages from climate events like drought cause the conflicts in the first place.  From Koren:

Moreover, in addition to illustrating the validity of this mechanism by the process of elimination—that is, by empirically accounting for a variety of alternative mechanisms— figure 2 further highlights the interactions between economic inequality, food resources, and conflict. Here, nonparametric regression plots—which do not enforce a modeling structure on the data and hence provide a more flexible method of visualizing relationships between different factors—show the correlations of local yields and conflict with respect to economic development as approximated using nighttime light levels. As shown, conflict occurs more frequently in cells with more crop productivity, but relatively low levels of economic development, where—based on anecdotal evidence at least—limitations on food access are more likely (Roncoli, Ingram, and Kirshen 2001).

Background Resource

Climates Don’t Start Wars, People Do

Climate Kills Wildflower! (False Alarm)

This is Androsace septentrionalis (Northern rock jasmine). Credit: Anne Marie Panetta

Breathless news out of Colorado Climate warming causes local extinction of Rocky Mountain wildflower species  Excerpts below with my bolds.

New University of Colorado Boulder-led research has established a causal link between climate warming and the localized extinction of a common Rocky Mountain flowering plant, a result that could serve as a herald of future population declines.

The new study, which was published today in the journal Science Advances, found that warmer, drier conditions in line with future climate predictions decimated experimental populations of Androsace septentrionalis (Northern rock jasmine), a mountain wildflower found at elevations ranging from around 6,000 feet in Colorado’s foothills to over 14,000 feet at the top of Mt. Elbert.

The findings paint a bleak picture for the persistence of native flowering plants in the face of climate change and could serve as a herald for future species losses in mountain ecosystems over the next century.

Always the curious one, I went looking for context to interpret this report.  Thank goodness for the Internet; it didn’t take long to find information left out of the alarming news release.  From the US Wildflower Database (here) we can see the bigger picture.

Androsace Septentrionalis, Rock Jasmine

Androsace septentrionalis is a small-flowered and rather inconspicuous plant, and is the most common member of this genus in the West, out of six in the US. Plants are very variable in size, reflecting the wide range of habitats and elevations – from near sea level to over 11,000 feet. Stalkless leaves grow at the base, in a flat rosette, and often have a few teeth along the margins, and ciliate hairs. Leaf surfaces may be hairless or sparsely short hairy.

Common names: Rock jasmine, pygmyflower
Family: Primrose (Primulaceae)
Scientific name: Androsace septentrionalis
Main flower color: White
Range: The Rocky Mountain states, westwards to the Great Basin, and small areas of neighboring states
Height: Between 1 and 8 inches
Habitat: Grassland, forest, tundra; generally open areas, from sea level to 11,500 feet
Leaves: Basal, oblanceolate, up to 1.2 inches long and 0.4 inches across; entire or coarsely toothed edges
Season: March to September

Look at the range and habitat and ask yourself if this plant is adaptive, as well as the fact this species is the most common out of six in the genus.

And in Minnesota (here), on the eastern edge of the range, it is rare compared to the Western Rock Jasmine (Androsace occidentalis).

If American lotus (Nelumbo lutea) is noted as Minnesota’s largest native wildflower, Western Rock Jasmine  certainly vies for its smallest. It can have very dense populations but it takes a discerning and determined eye to pick it out of the landscape, and is only of interest to those who celebrate the diversity of nature. It is easily distinguished from its rare cousin, Northern Androsace (Androsace septentrionalis) which is larger in stature and has rather narrower bracts at the base of the flower cluster.

The preferred habitat features sun; dry sandy soil, grassy meadows, open fields, disturbed soil, which along with “rock” in the name suggests that these plants tolerate arid conditions.

Summary

Far from going extinct, these flowers abound and like humans adapt readily to their surroundings. As has been stated previously, when alarmists project large numbers of extinctions due to future climate change, always ask for the names and the dead bodies.  What the headlines claim is refuted by the facts on the ground.

 

Rainfall Climate Paradox

A recent article displays the intersection of fears and facts comprising the climate paradox, in this case the issue of precipitation.  Rainfall’s natural variation hides climate change signal appeared today in phys.org by Kate Prestt, Australian National University.  Excerpts with my bolds.

New research from The Australian National University (ANU) and ARC Centre of Excellence for Climate System Science suggests natural rainfall variation is so great that it could take a human lifetime for significant climate signals to appear in regional or global rainfall measures.

Even exceptional droughts like those over the Murray Darling Basin (2000-2009) and the 2011 to 2017 Californian drought fit within the natural variations in the long-term precipitation records, according to the statistical method used by the researchers.

This has significant implications for policymakers in the water resources, irrigation and agricultural industries.

“Our findings suggest that for most parts of the world, we won’t be able to recognise long term or permanent changes in annual rainfall driven by climate change until they have already occurred and persisted for some time,” said Professor Michael Roderick from the ANU Research School of Earth Sciences.

“This means those who make decisions around the construction of desalination plants or introduce new policies to conserve water resources will effectively be making these decisions blind.

“Conversely, if they wait and don’t act until the precipitation changes are recognised they will be acting too late. It puts policymakers in an invidious position.”

To get their results the researchers first tested the statistical approach on the 244-year-long observational record of precipitation at the Radcliffe Observatory in Oxford, UK. They compared rainfall changes over 30-year-intervals. They found any changes over each interval were indistinguishable from random or natural variation.

They then applied the same process to California, which has a record going back to 1895, and the Murray Darling Basin from 1901-2007. In both cases the long dry periods seem to fit within expected variations.

Finally, they applied the process to reliable global records that extended from 1940-2009. Only 14 per cent of the global landmass showed, with 90 per cent confidence, increases or decreases in precipitation outside natural variation.

Professor Graham Farquhar AO also from the ANU Research School of Biology said natural variation was so large in most regions that even if climate change was affecting rainfall, it was effectively hidden in the noise.

“We know that humans have already had a measurable influence on streamflows and groundwater levels through extraction and making significant changes to the landscape,” Professor Farquhar said.

“But the natural variability of precipitation found in this paper presents policymakers with a large known unknown that has to be factored into their estimates to effectively assess our long-term water resource needs.”  The research has been published in the journal Proceedings of the National Academy of Sciences.

us-wet-dry-co2rev-1

Summary

Much like sea level rise, scientists fearing the worst seek and hope to find a nanosignal inside noisy imprecise measurements of a naturally varying phenomenon.

Sea Level Hype

It seems that alarmists get their exercise mainly by jumping to conclusions. Using datasets as trampolines they make great leaps of faith, oftentimes turning reality upside down in the process.

Update Feb. 17 at bottom

The latest example is the mass media excitement and exaggerations concerning sea level rise. Just consider the listing from Google News Feb. 13:

Miami could be underwater in your kid’s lifetime as sea level rise accelerates
USA Today

Yes, sea level rise really is accelerating
Ars Technica

Study: Sea level rise is accelerating and its rate could double in next century
Chicago Tribune

“It’s a big deal”: Melting ice sheets are accelerating sea level rise
CBS News Feb 13, 201

Satellites: Sea level rise to reach 2 feet by 2100
Minnesota Public Radio News (blog)

Satellite observations show sea levels rising, and climate change is accelerating it
CNN

The sea is coming for us
The Outline

Etc. Etc.Etc.

Although the principle author gave those juicy sound bites so craved by unreflective journalists, still the actual paper is quite restrained in its claims.  After all, they are only looking at 25 years of a very noisy dataset which has a quasi 60-year oscillation.  The paper is:

Climate-change–driven accelerated sea-level rise detected in the altimeter era By R. S. Nerem et al.

Abstract

Using a 25-y time series of precision satellite altimeter data from TOPEX/Poseidon, Jason-1, Jason-2, and Jason-3, we estimate the climate-change–driven acceleration of global mean sea level over the last 25 y to be 0.084 ± 0.025 mm/y2. Coupled with the average climate-change–driven rate of sea level rise over these same 25 y of 2.9 mm/y, simple extrapolation of the quadratic implies global mean sea level could rise 65 ± 12 cm by 2100 compared with 2005, roughly in agreement with the Intergovernmental Panel on Climate Change (IPCC) 5th Assessment Report (AR5) model projections.

Dr. John Ray provides a skeptical commentary, writing from Brisbane, Australia, at his blog (here) with my bolds.

Dedicated Warmist Seth Borenstein sets out a coherent story about warming causing sea-level rise. He regurgitates all the usual Warmist talking points regardless of their truth. He says, for instance, that the Antarctic is melting when it is not.

So we have to go back to the journal article behind Seth’s splurge to see what the scientists are saying.

And what we see there is very different from Seth’s confident pronouncements. We see a very guarded article indeed which rightly lists many of the difficulties in measuring sea level rise. And they can surmount those difficulties only by a welter of estimates and adjustments. Anywhere in that process there could be errors and biases. And as a result, we see that the journal authors describe their findings as only a”preliminary estimate” of sea level rise.

And it gets worse. When we look further into the journal article we see that the sea level rise is measured in terms of only 84 thousandths of one millimeter. So we are in the comedy of the absurd. Such a figure is just a statistical artifact with no observable physical equivalent.

So the sea level rise Seth talks about with great confidence ends up being an unbelievably small quantity measured with great imprecision! Amazing what you find when you look at the numbers, isn’t it?

Many advances in science start with a leap of imagination.  I seem to remember a chemist who woke up one morning with the first correct diagram of benzene.  And a man I admired said before sleeping he brought to mind things that were puzzling him.  Often in the morning he found answers combing out his hair.  Of course any such notions must then be validated through experimentation and measurement to become scientific knowledge.  A leap of faith is another matter altogether.

Sea Level Measurement Contortions

What’s involved in estimating sea level by means of satellites? Albert Parker is a seasoned researcher and explains to us laymen in this interview, followed by links to his recent publications. Senior Researcher Questions Satellite Measurements of Global Sea-Level By Ernest Dempsey with my bolds.

With a lot of rhetoric about the claimed sea-level rise and threat of global warming due to carbon emissions from human activities, the actual science of sea-level measurements and scientific inquiry of the verifiable degree of climate change has been lost in the noise. The following correspondence with Albert Parker, PhD, author of the 2014 paper Problems and reliability of the satellite altimeter based Global Mean Sea Level computation casts light on how reliable the various sea-level measurements are and whether the actual, on-ground science verifies the narrative of carbon-based climate change and alarming sea-level rise.

Ernest: Albert, thanks for taking my call for this Q&A. Would you please tell us about your academic and research background briefly?

Albert Parker: I received my MSc and PhD in Engineering many years ago, before the age of the commercial universities. I have been working after the PhD for 30 years in companies and universities. I started to work on climate change as an independent scientist, for my personal understanding, after the leaked Climategate emails in 2009, as I was curious to see what was really going on in the raw data.

Ernest: Can you please tell our readers the various methods scientists have used to measure the mean sea level at any point?

Albert Parker: Relative sea levels have been locally measured by tidal gauges for many years. A tidal gauge signal is characterized by oscillations on many different time scales. The tidal gauge signal is monthly averaged. A linear fitting of the monthly average values collected over a sufficiently long time window returns the trend. As the tide gauge instrument can move up and down, these sea levels are relative to the instrument.

The absolute global sea level is a hypothetical measure of the status of the ocean waters. Somebody has produced global mean sea level reconstructions from tide gauges since the 1700 or the 1800. These reconstructions are not reliable. Before the end of the 1800s, there was for example not a single tide gauge covering all the southern hemisphere. To compute a proper global mean sea level from tide gauges, you should need many gridded tide gauges along the world coastline, and a measure of their absolute vertical motion, both based on a sufficiently long common time window. There is not such a thing yet. As the trends significantly vary from one location to the other, it therefore only makes sense to focus on the average acceleration rather than the global mean sea level trend.

Ernest: In your 2014 paper, you inform that tide gauge measurements of mean sea level show negligibly small annual rise in mean sea level while satellite measurements give us a notably larger rise in sea level globally. Which of these two would you call more reliable and why?

Albert Parker: The only results to consider are local and global average trends and accelerations from tidal gauges of sufficient quality and length. If a global mean sea level from tide gauges can hardly be computed, you may still look at the individual tide gauges of enough length and quality to understand if there is acceleration or not. And so far, there has been very little acceleration in any tide gauge record over the 20th century and what is passed of the 21th century. Therefore, coastal management can be local, with adaptation measures needed where the sea level rises significantly because of extreme subsidence, and not certainly where the sea levels are rising slowly or are falling.

Regarding the satellite global mean sea level, this result is more a computation than a true measurement and it is not reliable. If you try to track by global positioning system (GPS) the position of selected fixed points, such as few GPS domes on land, and you try to compute the GPS time series to derive a GPS velocity, you may then discover that this much simpler computation, also constrained by the geodetic dimensions, still suffers significant uncertainties, because of satellite drift and other technicalities. It is therefore impossible to measure with nanometric precision the instantaneous height of all the water volume to then derive a time rate of change. The only thing that you can get from the satellite altimeter measurements is an almost detrended, noisy signal, as it was clear in the first results of the project. If subjective corrections are then applied to this signal, for any reason you get the satellite altimeter results that is not a measure, it is a computation, that lacking validation has very little value.

Ernest: Tell us about calibration and its role in sea level readings.

Albert Parker: It is not just a problem of calibration. You are trying to measure with a satellite altimeter the instantaneous, absolute, height, with accuracy up to the nanometer, of a continuously oscillating mass of water bounded by an irregular, continuously moving surface. With the much more established and reliable GPS system that serves many more goals than the monitoring of a climate change parameter, it is hard to compute with accuracy better than a couple of millimeters per year the time rate of change of the position of fixed GPS domes. The global mean sea level results of the satellite altimeter are unfortunately never validated computations, not certainly very accurate measurements.

Ernest: The observable change in sea level can be due to increase in amount of water in the oceans or upward tectonic movement of the seafloor, right? Is there any way to tell how much rise resulted from either?

Albert Parker: The situation is little bit more complicated. If you look at the relative sea level trends across the world, they rise and fall because of changing water conditions and land movements. If you are along the Pacific coast of the US for example, in Alaska, the sea levels are generally falling because the land is moving up (uplift). Conversely, if you look at California, the sea levels are rising mostly because the land is moving down (subsidence). Local factors produce significant differences in between the rates of sea level rise (trends).

Changes in tide levels over time evidenced in Fiji.

To get an accurate measure of the sea level rise by thermal expansion and mass addition from tide gauges, this is not easy. What we can see from the individual tide gauges, is that the contribution from mass addition and thermal expansion is about constant since the start of the 20th century. Since the year 1900, the warming of the oceans and the melting of the ices on land has therefore basically provided an almost constant contribution to the rate of rise of sea levels. Same time, the anthropogenic carbon dioxide emission has increased exponentially. This would be enough to conclude that the anthropogenic carbon dioxide emissions have from very little influence to no influence at all on the rate of rise of sea levels.

Ernest: Then there is the question of periodicity. Far as I get it from your paper, it is more scientific or reasonable to look at sea level change over the past least 60 years. Why is that?

Albert Parker: The sea levels are very well known to oscillate with many periodicities up to a quasi-60 years well shown in almost all the world tide gauges. If you study a tide gauge record and you want to compute a trend by linear fitting, you do need data collected over a time window long enough to understand what is a multidecadal natural oscillation and what is a sea level acceleration produced by intensifying mass addition and thermal expansion. It is unfortunately common to find peoples who cherry pick the short-term positive oscillation in selected locations to sell this result as the proof that global warming is real.

Obviously, the cherry pickers do not pick up the cherries in areas of opposite short-term oscillation where same approach could prove there is global cooling equally real. Similarly, they do not consider the fact that in the long-term locations, positive and negative phases of the oscillations have regularly followed each other over the time, and “unprecedented” short term sea level rises have been measured already about 60 years ago.

Ernest: Since you pointed out the shortcomings in sea level measurements by satellite altimetry and GPS, has the environmental science community responded to your work?

Albert Parker: The shortcomings of satellite altimetry to compute sea levels are very well known. The most part of the independent scientists, unfortunately mostly retired, acknowledges that there is something not that straight going on in the satellite altimeter result. Nils-Axel Morner and many others have written wonderful papers questioning the sea level claims. Problem are the dependent scientists, working in a commercial academy, and more than them, the general press and the politicians that have a clear interest to force the peoples to believe that global warming is real and they need more administration and control and more taxes.

Ernest: Speaking of press, we hear a lot in media about new researches finding links between anthropogenic carbon in atmosphere and sea level rise. And some have claimed disastrous consequences of this supposedly impending sea level threat. What’s your response when you read those stories?

Albert Parker: In the recent scientific paper reference [1], that of course will not receive any attention by the alarmists, we discuss how different experimental data sets of tide gauges show relatively small sea level trends, from +0.4 to +2 millimeters per year, and negligibly small sea level accelerations, just a few micrometers per year squared. These results demonstrate that the sea levels have not been driven by the anthropogenic carbon dioxide emission over the last 120 years, and it is very unlikely they will start be driven by magic right now. These trends and accelerations translate in forecasts to the year 2100 of 100-200 mm sea level rise, not certainly the 850 mm by the IPCC, nor the 1,670 or the 3,050 mm of works such as reference [2] or [3].

The figures below are a comparison of sea level measurements vs. sea level computations over the time window 1970 to 2017, and evidence based forecasts to the year 2100 vs. the model predictions. The difference amongst latest models and reality is increasing as opposed to being lessened. It should be the opposite. Many may certainly claim new links between the anthropogenic carbon dioxide in the atmosphere and the sea level rise, with disastrous consequences of this supposedly impending sea level threat. This does not mean they are correct.

Fig. 1 – Comparison of sea level rises predicted by the local panels [2] (BOS-NRC) and [3] (H++), predicted by the IPCC AR5 RCP8.5 (IPCC RCP8.5), and measured by the tide gauges (averages of different data sets, California-8, PSMSL-301, Mitrovica-23, Holgate-9, NOAA-199, US-71). Further details in [1].

From these graphs, we already know that up to 2017 the models have been wrong, and it is increasingly unlikely to expect more rather than less sea level rise by 2100 vs. the already exaggerated IPCC predictions.

Fig. 2 – Comparison of sea level rises by 2100 predicted by the local panels [2] (BOS-NRC) and [3] (H++), predicted by the IPCC AR5 RCP8.5 (IPCC RCP8.5), and inferred from tide gauge measurements of different data sets (California-8, PSMSL-301, Mitrovica-23, Holgate-9, NOAA-199, US-71). Further details in [1].

[1] Parker, A. & Ollier, C.D., CALIFORNIA SEA LEVEL RISE: EVIDENCE BASED FORECASTS VS. MODEL PREDICTIONS, Ocean and Coastal Management, Ocean & Coastal Management, Available online 19 July 2017, In Press, Corrected Proof. doi: 10.1016/j.ocecoaman.2017.07.008

More Resources:

Sea Level Rise: Just the Facts

Cutting Edge Sea Level Data

Fear Not For Fiji

Footnote:  Climate alarmists may be jumping the shark as well as jumping to conclusions.
“Jumping the shark” is attempting to draw attention to or create publicity for something that is perceived as not warranting the attention, especially something that is believed to be past its peak in quality or relevance. The phrase originated with the TV series “Happy Days” when an episode had Fonzie doing a water ski jump over a shark. The stunt was intended to perk up the ratings, but it marked the show’s low point ahead of its demise.

Update Feb. 17

Prompted by a question from hunter, I found this informative recent letter on this topic(my bolds):

From Reply from Nils-Axel Mörner on the problems of estimating Future Sea Level Changes as asked by Albert Parker in letter of January 2, 2018

There are physical frames to consider. Ice melting requires time and heating, strictly bounded by physical laws. At the largest climatic jump in the last 20,000 years – viz. at the Pleistocene/Holocene boundary about 11,000 years BP – ice melted under extreme temperature forcing; still sea level only rose at a rate of about 10 mm/yr (or just a little more if one would consider more extreme eustatic reconstructions). Today, under interglacial climatic conditions with all the glacial ice caps gone climate forcing can only rise global sea level by a fraction of the 11,000 BP rate, which in comparison with the values of Garner et al. [1] would imply:
well below 0.4 m at 2050 instead of +0.6 m
well below 0.9 m at 2100 instead of +2.6 m
well below 2.9 m at 2300 instead of +17.5 m

Consequently, the values given by Garner et al. [1] violate physical laws and common glaciological knowledge. Therefore, their values must not be set as standard in coastal planning (point 2 above).

The mean sea level rise over the last 125 years is +0.81 ±0.18 mm/yr. At Stockholm in Sweden, the absolute uplift over the last 3000 years is strictly measured at +4.9 mm/yr. The mean tide-gauge change is -3.8 mm/yr, giving a eustatic component of +1.1 mm/yr for the last 150 years. In Amsterdam, the long-term subsidence is known as +0.4 mm/yr. The Amsterdam/Ijmuiden stations record a relative rise of +1.5 mm/yr, which give a eustatic component of +1.1 mm/yr.

Global Loading Adjustment has been widely used in order to estimate global sea level changes. Obviously, the globe must adjust its rate of rotation and geoid relief in close agreement with the glacial eustatic rise in sea level after the last Ice Age. The possible internal glacial loading adjustment is much more complicated, and even questionable, however.

Direct coastal analysis of morphology, stratigraphy, biological criteria, coastal dynamics, etc usually offers the far best means of recording the on-going sea level variations in a correct and meaningful way. It calls for hard work in the field and deep knowledge in a number of subjects. We have, very successfully, applied it in the Maldives, in Bangladesh, in Goa in southern India, and now also in the Fiji Islands. In all these sites, direct coastal analyses indicate full eustatic stability over the last 50-70 years, and long-term variations over the last 500 years that are consistent with “rotational eustasy” or “Global Solar Cycle Oscillations” (GSCO).

 

 

 

 

On Coastal Climate Risk

Matthew Kahn raises the question at his blog Is Oakland “Inconsistent” as it Sues Fossil Fuel Companies While Downplaying Climate Risk in its Municipal Bond Prospectus? Excerpts below with my bolds.

Wall Street Journal: California localities warn of disaster when suing oil companies. So how come they don’t tell investors?

The WSJ has published a fascinating piece that points out an inconsistency in the expressed views of the leaders of Oakland’s city government. This coastal city is suing Exxon and other fossil fuel companies for engaging in business that threatens Oakland’s future (i.e fossil fuel burning causes sea level rise that will impose costs on Oakland). Oakland’s inconsistency occurs in the municipal bond market. Oakland seeks to borrow a large amount of $ by selling bonds. In the bond risk disclosures, climate change is played down. In this setting, Oakland has a strong incentive to state that it is a low risk because low risk borrowers can borrow at a lower interest rate.

The author of the WSJ asks a simple question; which truth does Oakland believe? Is it over-exaggerating the risk it faces to win the Exxon law suit while simultaneously downplaying a possible risk in the municipal bond market? Did Oakland’s officials anticipate that they could engage in such “mixed messaging”?

In truth, Oakland will need to borrow $ to help it engage in capital upgrades to prepare for sea level rise. The market will set the equilibrium interest rate to reflect the risk. If investors know that coastal cities have an incentive to lie and understate the true risk then new risk providers such as the nascent Jupiter project will emerge to provide this information. To put this simply, when you buy a used car — do you just ask the current owner for her assessment of its quality? Don’t be a sucker, do your homework.

The Exxon lawsuit raises major issues. I understand transaction costs but why aren’t the litigants suing gasoline car makers and gasoline car buyers? This lawsuit is an indirect court induced carbon tax. If the litigants succeed, what would be the economic incidence of this tax? Would Exxon’s profit decline? (More on the legal issues below)

A good debater might argue that the municipal bonds are issued for 30 years and over this time horizon, coastal cities do not face a serious challenge and thus the bond default risk is low. But, as you make these arguments think back in time. 1988 was 30 years ago. Technology has made some progress. By the year 2048, I have a feeling that our technological frontier will have leaped forward to help us to adapt to the new normal. The coastal capital stock will be less durable and we will be prepared.

Note: By the term “durable” in the last sentence, Kahn refers to the possibility of structures in vulnerable places being movable in the face of erosion or flooding. He and Devin Bunten discuss how developers are likely to adapt to localized climate risks in their paper Optimal Real Estate Capital Durability and Localized Climate Change Disaster Risk Devin Bunten and Matthew E. Kahn January 2017
(Board of Governors of the Federal Reserve System, University of Southern California and NBER)

Abstract
The durability of the real estate capital stock could hinder climate change adaptation because past construction anchors the population in beautiful and productive but increasingly-risky coastal areas. However, coastal developers anticipate that their assets face increasing risk and this creates an incentive to seek adaptation strategies. This paper models climate change as a joint process of (1) increasingly destructive storms and (2) a risk of sea-level rise that submerges coastal property. We study how forward-looking developers and real estate investors respond to the new risks along a number of dimensions including their choices of location, capital durability, capital mobility (modular real estate), and maintenance of existing properties. The net effect of such investments is a more resilient urban population.

The above referenced WSJ article is paywalled, but this post by CEI gets at the securities fraud issue: SEC Should Investigate California Municipalities for Climate-Related Securities Fraud

It appears a variety of California municipalities have gotten themselves in hot water. To investors of their bonds, they have claimed that they are unable to predict sea level rise or other climate risks. But they recently filed suit against a variety of oil and gas companies claiming the companies are causing the sea level to rise. The municipalities in their lawsuits give very explicit predictions as to how much they think the sea level will rise.

Today CEI asked the Securities and Exchange Commission to investigate these activities as possible securities fraud. Federal law prohibits deceiving investors through untrue material facts or material omissions. The municipalities claim to the court that they are able to predict these sea level changes. If that is true, then they are deceiving investors. The SEC’s mission is to protect investors from such false statements.

A few examples of the conflicting statements:

  • The City of San Francisco to bond investors: “The City is unable to predict whether sea-level rise or other impacts of climate change or flooding from a major storm will occur, when they may occur.” But to the court, the city predicts “0.3 to as much as 0.8 feet of additional sea level rise.”
  • The City of Oakland to bond investors: “The City is unable to predict when seismic events, fires or other natural events, such as sea rise or other impacts of climate change or flooding from a major storm, could occur, when they may occur.” But to the court, the city predicts “66 inches of sea level rise.”
  • The County of San Mateo to bond investors: “County is unable to predict whether sea-level rise or other impacts of climate change or flooding from a major storm will occur, when they may occur.” But to the court, the county states: “The County anticipates and is planning for significant sea level rise.”
  • The County of Santa Cruz to bond investors states that “may be subject to unpredictable climatic conditions, such as flood.” But to the court, the county states that there is a “98% chance that the County experiences a devastating three-foot flood before the year 2050.”

There are two possible reasons why these municipalities have told the courts different statements than investors. First the municipalities may be trying to get more money from bonds then they would be able to get if they were honest about their true beliefs. For instance, the City of Oakland predicts the costs of “between $22 and $38 billion.” Would the city even be solvent trying to pay those costs? No investor would give their money to a city which expects not to be able to pay them back. If the municipalities were forced to explain what they claim are the expected impacts of climate change to their budget, they would no longer be able to raise as much money from bonds.

The second possible reason is that these municipalities are actually lying to the courts instead of investors by fabricating their predictions of sea level rise. Or perhaps they’re misrepresenting things to both investors and the courts.

Regardless, we hope the SEC can get to the bottom of this.

On the legal flaws with these lawsuits by cities: Is Global Warming A Public Nuisance?