Showing posts with label global warming. Show all posts
Showing posts with label global warming. Show all posts

Friday, February 23, 2024

Stephen Salter, a giant in combating climate change passes away

   Stephen Salter (2012)
Stephen Hugh Salter, MBE, FRSE, Emeritus Professor of Engineering Design at the University of Edinburgh, was born December 7, 1938, and passed away peacefully on February 23, 2024, at the age of 85.

Stephen Salter was a giant who persisted to dedicate his life to combating climate change, and he did so in many ways until the very end. 

Stephen's work on wave energy led to Salter's Duck (1974), a device able to both generate energy and reduce wave strength. In 1977, Stephen built a multi-directional wave tank at the University of Edinburgh. 

In 2011, Stephen looked at ways to capture methane released in the Arctic, such as by covering lakes and parts of seas by sheets to collect the methane (drawing below).

Empty and filled extruded rubber trough cases with 4 times enlarged views of end and centre

Stephen was perhaps best known for his work on marine cloud brightening, i.e. deploying vessels to spray salt particles into the air in an effort to reduce sea surface temperatures, and thus also reducing sea ice loss and reducing the strength of extreme weather events including storms and hurricanes.

In the video below, Stephen discusses marine cloud brightening in a TEDx talk in 2016. 


Marine cloud brightening | Prof. Stephen Salter | TEDx Talks Published 15 Nov 2016

The image below is from the post Hurricane Moderation at Arctic-news.blogspot.com


In the video below, by theedinburghreporter, Stephen Salter talks about marine cloud brightening.


In the video below, Stephen Salter is interviewed by Nick Breeze (2022). 


Below is a screenshot from the above video by Nick Breeze. 

Stephen Salter discusses sending solar energy back out to space by means of Marine Cloud Brightening.
Screenshot by Sam Carana from video by Nick Breeze.

Stephen Salter (2022): "A jolly small change in reflectivity of the clouds will be sending solar energy back out to space enough to balance what the excess is that's being retained here by greenhouse gases (4:26-4:41). Maybe 10 cubic meters of water a second as sub micron drops sprayed in the right place would offset all the damage we've done since pre-industrial times (5:15-5:24)." 

Our hearts are saddened by this huge loss, and our thoughts are with Stephen's family and his many friends. Stephen's work will not be forgotten.

Added below is a video featuring Stephen Salter, Peter Wadhams, Paul Beckwith, Robert Tulip, Herb Simmens, Alaxandra Price and Win Rampen. 



Links

• Futuristic fleet of 'cloudseeders' - by John Latham (2007)
https://news.bbc.co.uk/2/hi/programmes/6354759.stm

• Sea-going hardware for the cloud albedo method of reversing global warming - by Stephen Salter, Graham Sortino and John Latham (2008)
https://royalsocietypublishing.org/doi/10.1098/rsta.2008.0136

• Can we capture methane from the Arctic seabed? (2011)

• Professor Stephen Salter receives top Academy Award (2012)

• Leading wave energy pioneer Prof Stephen Salter (2012) 
https://www.theengineer.co.uk/content/in-depth/leading-wave-energy-pioneer-prof-stephen-salter

• Coded modulation of computer climate models for the prediction of precipitation and other side-effects of marine cloud brightening (2013)

• Marine cloud brightening | Prof. Stephen Salter | TEDxHeriotWattUniversity |  TEDx talk (2016)
• Hurricane Moderation (2018)
https://arctic-news.blogspot.com/2018/09/hurricane-moderation.html

• Talking to Professor Stephen Salter - TheEdinburghReporter (May 23, 2019)

• Speaking with Professor Stephen Salter - The Edinburgh Report (June 1, 2019)

• Professor Stephen Salter at Holyrood speaking about project to arrest climate change

• John Latham obituary (2021)
https://www.theguardian.com/science/2021/may/30/john-latham-obituay

• Stephen Salter - Whole interview by Nick Breeze ClimateGenn (2022)



Thursday, July 9, 2020

Global warming and ice sheet melting: Portents of a Younger dryas-like stadial event

Global warming and ice sheet melting:
Portents of a Younger dryas-like stadial event
by Andrew Glikson


Linear climate projections by the IPCC are difficult to reconcile with the paleoclimate evidence of stadial cooling events which closely succeeded warming peaks, including the Younger dryas (12.9–11.6 kyr ago), Laurentian melt (~8.3 kyr) and earlier interglacial stadials. Each of these events followed peak interglacial temperatures, leading to extensive melting of the ice sheets and transient stadial cooling events. Current global temperature rises in the range of ~ +1.19 ± 0.13 °C (Northern Hemisphere) and higher in the Arctic are consistent with this pattern, leading to the build-up of ice melt pools south of Greenland and around Antarctica. The growth of these pools is likely to progress toward large-scale to a global stadial, inducing differential warming and cooling effects leading to major weather disruptions and storminess, possibly analogous to the Younger dryas and Laurentian melt events.

Linear temperature rise projections by the IPCC are unlikely in view of (1) amplifying feedbacks of greenhouse gases and global warming on land and ocean, and (2) stadial cooling effects due to the flow of ice melt water from the large ice sheets into the North Atlantic Ocean and the circum-Antarctic ocean (Figure 1). Apart from the absolute GHG level (~500 ppm CO₂-equivalent), the high rise rate of ~2-3 ppm CO₂/year and thereby temperature is driving dangerous weather events. The extreme rise in greenhouse gases in the atmosphere is evident from a comparison with past climate events (Figure 6). Linear temperature projections and thereby environment change are complicated by storminess due to collisions between air masses of contrasted temperatures. As the Arctic jet stream weakens, warm air currents from the south and freezing air masses from the north cross the boundary, a pattern already manifested by Arctic heat waves and fires and by penetration of freezing air masses into mid-latitudes, i.e. the “Beast from the East” snow storms. The increasing extent of cold ice melt pools around Greenland and Antarctica (Figure 1) suggest such a process is already in progress, signifying an onset of an interglacial stadial, as modelled by Hansen et al. 2016 and Bronselaer et al. (2016).

Figure 1 A. The cold ocean region south of Greenland visible on the NASA's 2015 global mean
temperatures (NASA/NOAA; 20 January 2016), the warmest year on record since 1880;
B. Circum-Antarctic summer surface temperatures, showing the large Weddell Sea and other
cold Sub-Antarctic ocean anomalies related to the flow of ice melt water into the ocean, and a seasonal
warming anomaly in the Ross Sea due to upwelling of warm salty water from the circum-Antarctic current.

Stadial events

Late Pleistocene climate cycles were controlled by orbital parameters of the Milankovitch cycles including eccentricity (~100,000 years), obliquity to the ecliptic plane (~41,000 years) and precession/wobble of the Earth’s axis (~19,000 and ~23,000 years). The Younger dryas of 12,900 to 11,600 years ago following the Allerod BÖlling warm peak and marked by cooling of near -20°C in Greenland and (Figure 2A, B), has major implications for climate change projections for the 21-23rd centuries.

The Younger dryas is the longest of three late Pleistocene stadials (Figure 2A) associated with abrupt climatic changes that took place over the last 16,000 years. According to Steffensen et al. 2008 based on deuterium isotopes in ice cores the abrupt onset of the Younger dryas in Greenland occurred over less than 1 year and ended over less than 3 years (Figure 2B), or about 50 years based on stable water isotopes representing the air temperature record. Evidence for the effects of the Younger dryas stadial has also been identified in tropical and subtropical regions (Shakun and Carlson, 2010) (Figure 3). The underlying factors for the Younger dryas and Laurentian (Figure 4) stadial events are the deglaciation of Northernmost America, flow of cold ice melt water into the North Atlantic Ocean and into North American lakes (Lake Agassiz), and the retreat southward of the North Atlantic Thermohaline Current.

Suggestions of a comet impact origin of the Younger dryas are inconsistent with (1) the recurrence of stadial events following peak interglacial temperatures over the last 420,000 years (Figure 5) and (2) the paucity of clear evidence for a large extraterrestrial impact contemporaneous with the Younger dryas, including the little known age of the radar-detected crater below the Hiawatha Glacier In northwest Greenland.

Figure 2A Air temperatures at the Last glacial maximum (20-16 kyr), BÖlling-Allerod warm peak,
Younger dryas (12,900 to 11,600 years ago) and 8.2 kyr Laurentian stadial event. This image
shows temperature changes, determined as proxy temperatures, taken from the central region

of Greenland's ice sheet during the Late Pleistocene and beginning of the Holocene.

Figure 2B. deuterium evidence for onset cooling temperature and terminal
warming of the Younger dryas stadial event (14,740-11,660) (Steffensen et al. 2008).

Figure 3. Magnitude of late Holocene glacial-interglacial temperature changes
in relation to latitude. Black squares are the Northern Hemisphere (NH),
gray circles the Southern Hemisphere (SH) (Shakun and Carlson, 2010).

The youngest recorded stadial, the Laurentian melt, between ~8,500 and ~8.000 years ago (Figure 4), is indicated by distinctive temperature–CO₂ correlation with global CO₂ decline of ≈25 ppm by volume over ≈300 years, consistent with the lowering of North Atlantic sea-surface temperatures and weakening of the AMOC (Atlantic Meridional Ocean Circulation).

Figure 4 A. The ~8.2 kyr Laurentian stadial event in a coupled climate model (Wiersma et al. 2011);
B. Reconstructed CO₂ concentrations for the interval between ~8,700 and ~6,800 BP, based on
CO 2 extracted from air in Antarctic ice of Taylor Dome (Wagner et al. 2002).
The Younger dryas and the Laurentian stadials are not unique, as peak temperatures in every interglacial event over the last 420,000 years were followed by sharp cooling events (Figure 5). Apart from the absolute level of greenhouse gases (GHG) in the atmosphere the high rate at which GHG concentrations are rising, as shown by comparisons with previous extreme warming events (Figure 6), enhances extreme weather events, as well as retards the ability of fauna and flora to adapt to the new conditions.

Figure 5 (a) Evolution of sea surface temperatures in five glacial-interglacial transitions recorded in
ODP 
1089 at the sub-Antarctic Atlantic Ocean (Cortese et al. 2007). Grey lines – δ 18 O measured on
Cibicidoides plankton; Black lines – sea surface temperature. Marine isotope stage numbers are 
indicated on top of diagrams. Note the stadial following interglacial peak temperatures; (b) the last 
glacial maximum and the last glacial termination. Olds- Oldest dryas; Old – Older dryas; Yd – Younger dryas.

Figure 6 (A) Reconstructed atmospheric CO₂ variations during the Late Cretaceous–early Tertiary
derived from the Stomata indices of fossil leaf cuticles calibrated by using inverse regression
and stomatal ratios (Beerling et al. 2002);
(B) Simulated atmospheric CO₂ at and after the Palaeocene-Eocene boundary (after Zeebe et al. (2009).
Compare the CO₂ ppm/year values with the current rise of 2 to 3 ppm/year;
(C) Global CO₂ and temperature during the last glacial termination (After Shakun et al., 2012)
(LGM - Last Glacial Maximum; OD – Older dryas; BA - Bølling–Allerød; YD - Younger dryas);

The average global land and ocean surface temperature for March 2020 was 1.16°C above the 20th century average global level of 12.7°C. Current CO₂ rise and warming rates exceed that of the Last Glacial Termination (LGT) (21–8 kyr) (Figure 6C), the Paleocene-Eocene Thermal Maximum (PETM) (55.9 Ma) (Figure 6B) and the Cretaceous-Tertiary boundary (K-T) (64.98 Ma) impact event (Figure 6A). The relations between warming rates and the migration of climate zones toward the poles (Figure 7), including changes in the atmosphere and ocean current systems, are in the root of the major environmental changes in these zones.
Figure 7. Expansion of the tropical African climate zone (vertical red lines) into subtropical and Mediterranean
climate zones to the north and south (Migration, Environment and Climate Change, International Organization
for Migration, Geneva, Switzerland (Regional Maps on Migration, Environment and Climate Change.

Future Stadial events

IPCC climate change projections for 2100-2300 portray linear to curved temperature progressions (SPM-5). However, amplifying feedbacks and transient cooling events (Stadials) ensuing from the flow of ice melt water into the oceans during peak interglacial warming events, impose abrupt temperature variations (Figure 5). The current flow of ice melt water from Greenland and Antarctica (Figures 8, 9) is leading to regional ocean cooling in the North Atlantic and around Antarctica (Rahmstorf et al, 2015; Hansen et al. (2016); Bronselaer et al. 2018; Purkey et al. 2018; Vernet et al. 2019) (Figures 1, 8). Under high greenhouse gas and temperature rise trajectories (RCP8.5) this implies future stadial events as modelled by Hansen et al. (2016) (Figure 10) and Bronselaer et al. (2018) (Figure 11).

Depending on different greenhouse emission scenarios (IPCC 2019; van Vuren et. al. (2011), including the CO₂ forcing-equivalents of methane (CH4) and nitrous oxide (N2O), the total CO₂–equivalent rise has reached 496 ppm (NOAA, 2019). As the oceans heat contents is rising, upwelling of warm sublayers is melting the leading edges of continental glaciers (Figure 8). This factor and the flow of ice meltwater from leading glacier fronts and grounding lines lead to stratification of the sub-Antarctic ocean and an incipient onset of a southern ocean stadial (Figure 8).

Figure 8. The transition from grounded ice sheet to floating ice shelf and icebergs

Figure 9. Greenland and Antarctic ice mass change. GRACE data are extension of Velicogna et al. (2014)
gravity data. MBM (mass budget method) data are from Rignot et al. (2011). Red curves are gravity data
for Greenland and Antarctica only; small Arctic ice caps and ice shelf melt add to freshwater input.
Satellite and mass balance measurements of the large ice sheets indicate their rapid reduction (Figure 9). Variations in ice thickness, ice drainage and ice velocity data in 176 Antarctic basins between 1979 and 2017 indicate a total mass loss rise from 40 ± 9 Gt/year in 1979–1990 to 50 ± 14 Gt/year in 1989–2000, 166 ± 18 Gt/year in 1999–2009, and 252 ± 26 Gt/year in 2009–2017 (Figure 9). This amounts to an increased melting by more than 6-fold in about 40 years, contributing an average sea level rise of 3.6 ± 0.5 mm per decade, with a cumulative 14.0 ± 2.0 mm since 1979 (Rignot et al. 2019). The mass loss concentrated in areas closest to warm, salty, subsurface, circumpolar deep water (CDW), consistent with enhanced polar westerlies pushing CDW toward Antarctica.

The Greenland ice sheet contains approximately 2,900,000 GtI of ice. During the exceptionally warm Arctic summer of 2019, Greenland lost 600 GtI of ice. Under global GHG and temperature rise this rate is likely to be exceeded. The Greenland ice sheet may not last much longer than a Century. The Antarctic ice sheet weighs approximately 26,500 Gigaton. For a loss greater than ~250 GtI/year it could last for 105 years or less. For accelerated ice melt rates under rising GHG concentrations it could last for significantly shorter time, except for possible negative feedbacks associated with stadial cooling?

Hansen et al. (2016) suggest that, depending on ice melt rates of the polar ice sheets, transient cooling events (stadials) can be expected to develop over periods dependent on the rates of ice melt (Fig. 10). Stadial cooling of about -2°C lasting for several decades (Figure 10) may affect temperatures in Europe and North America. The model is consistent with a slowdown of the Atlantic Meridional Ocean Circulation (AMOC) (Weaver et al. 2012) and the exceptional growth of a cold water region southeast of Greenland, (Rahmstorf et al, 2015).
Figure 10. A. Model surface air temperature (◦C) change in 2096;
B. Surface air temperature (◦C) relative to 1880–1920 for several ice melt scenarios.

According to Bronselaer et al. (2018) temporal evolution of the global-mean surface-air temperature (SAT) shows meltwater-induced cooling translates to a reduced rate of global warming (Fig. 11), with a maximum divergence between standard models and models which include the effects of meltwater-induced cooling of 0.38 ± 0.02°C in 2055. As stated by the authors “We demonstrate that the inclusion in the model of ice-sheet meltwater reduces global atmospheric warming, shifts rainfall northwards, and increases sea-ice area”, and “Antarctic meltwater is therefore an important agent of climate change with global impact, and should be taken into account in future climate simulations and climate policy.”
Figure 11. The 2080–2100 meltwater-induced sea-air temperature anomaly relative to the standard
RCP8.5 ensemble. Hatching indicates where the anomalies are not significant at the 95% level.

Conclusions


Based on the paleoclimate record, global warming, penetration of cold and warm air masses across weakened polar boundaries, increased ice melting rates, sea level rise and near-surface cooling of large ocean tracts (Figures 10, 11), collisions between warm and cold air and water masses and thereby storminess are likely to determine the future climate of large parts of Earth. With rising greenhouse gas levels and their amplifying feedbacks from land and oceans these developments are likely to persist in the long term. The continuing migration of climate zones toward the poles is likely to be disrupted by developing stadial effects and differential warming and cooling effects, leading to major weather disruptions and storminess. Continuing release of greenhouse gases and their amplifying feedbacks could lead to tropical Miocene-like conditions about 4 to 5 degrees Celsius warmer than late Holocene climate conditions which allowed agriculture and thereby civilization to emerge.


Andrew Glikson
Dr Andrew Glikson
Earth and Paleo-climate scientist
ANU Climate Science Institute
ANU Planetary Science Institute
Canberra, Australia



Books:
The Asteroid Impact Connection of Planetary Evolution
http://www.springer.com/gp/book/9789400763272
The Archaean: Geological and Geochemical Windows into the Early Earth
http://www.springer.com/gp/book/9783319079073
Climate, Fire and Human Evolution: The Deep Time Dimensions of the Anthropocene
http://www.springer.com/gp/book/9783319225111
The Plutocene: Blueprints for a Post-Anthropocene Greenhouse Earth
http://www.springer.com/gp/book/9783319572369
Evolution of the Atmosphere, Fire and the Anthropocene Climate Event Horizon
http://www.springer.com/gp/book/9789400773318
From Stars to Brains: Milestones in the Planetary Evolution of Life and Intelligence
https://www.springer.com/us/book/9783030106027
Asteroids Impacts, Crustal Evolution and Related Mineral Systems with Special Reference to Australia
http://www.springer.com/us/book/9783319745442



Thursday, August 2, 2018

Global fires, droughts and Orwellian Newspeak while Nero fiddles

By Andrew Glikson

There was a time when the contamination of drinking water constituted a punishable crime. Nowadays those who willfully ignore or promote the destruction of the Earth’s atmosphere and ocean acidification through the rise in emission of carbon gases (2014 ~36.08 billion ton CO₂/year ; 2017 ~36.79 billion ton CO₂/year), hold major sway in the world. Consequently the rise rate of atmospheric CO₂ at 2 ppm/year (from 408.84 ppm in June 2014 to 410.79 ppm in June 2018) is the fastest observed in the geological record since 66 million years ago, when an asteroid hit the Earth, wiping out the dinosaurs. (onlinelibrary.wiley.com/doi/abs/10.1111/gcb.13342). The hapless residents of planet Earth are torn between survival in several parts of the world and sport circuses in other parts, while some of their representatives are playing with chunks of coal in their parliament.

See interactive version of image at:
carbonbrief.org/analysis-global-co2-emissions-set-to-rise-2-percent-in-2017-following-three-year-plateau

The consequences in terms of heat waves, fires, droughts, storms, floods, human lives and devastation of nature are everywhere. From Japan to Sweden, Oman to Texas and California, a global heat wave is setting records, igniting wildfires, and killing hundreds.
nymag.com/daily/intelligencer/2018/07/a-global-heat-wave-has-set-the-arctic-circle-on-fire.html

The south-central region is home to the highest temperatures in the U.S. this week, with nearly 35 million people living under excessive heat warnings issued by the National Weather Service. Temperatures are expected to be in the triple digits across Texas this weekend, marking the most severe heat wave in the state since 2011. The Texas heat has already led to record-breaking days for the Texas power grid twice this week. Things aren’t any better elsewhere in the region, with heat indexes in Oklahoma, Arkansas, and Louisiana reaching up to 110°F.

Dozens are dead in Japan from record-setting, long duration extreme heat event.
climatesignals.org/headlines/dozens-dead-japan-record-setting-long-duration-extreme-heat-event
theweek.in/news/world/2018/07/23/japanese-heat-wave-pushes-temperature-to-record.html
Across the globe in Kyoto, Japan, Thursday marked the seventh straight day of temperatures that exceeded 100 degrees, breaking all known records for the ancient capital city. At least 30 people have died in Japan during the heat wave, which has complicated rescue efforts following floods and landslides that killed more than 200 in western Japan earlier this month. On Thursday alone ten people died and 2,605 people were sent to hospitals in Tokyo due to heat, the Japan Times reports. The day before, Tokyo rescue workers set a record by responding to more than 3,000 emergency calls.

In Sweden, the Arctic Circle is on fire. High temperatures and a prolonged drought have caused 49 fires to ignite across Sweden, with temperatures reaching 90 degrees as far north as the Arctic Circle this week. According to the Washington Post, temperatures in Scandinavia typically settle in the 60s and 70s this time of year, meaning the current heat wave is making things around 20 degrees hotter than normal. In Quebec, more than 90 people were killed by extreme heat in early July. An Algerian city earlier this month broke the record for the highest temperature ever in Africa when it hit 124.3°F.
nymag.com/daily/intelligencer/2018/07/a-global-heat-wave-has-set-the-arctic-circle-on-fire.html

The current heatwave has been caused by an extraordinary stalling of the jet stream wind, which usually funnels cool Atlantic weather over the continent. This has left hot, dry air in place for two months – far longer than usual. The stalling of the northern hemisphere jet stream is being increasingly firmly linked to global warming, in particular to the rapid heating of the Arctic and resulting loss of sea ice.
theguardian.com/environment/2018/jul/27/heatwave-made-more-than-twice-as-likely-by-climate-change-scientists-find

Prof Michael Mann declares “This is the face of climate change … We literally would not have seen these extremes in the absence of climate change … The impacts of climate change are no longer subtle … We are seeing them play out in real time and what is happening this summer is a perfect example of that … We are seeing our predictions come true …". Mann points out that the link between smoking tobacco and lung cancer is a statistical one, which does not prove every cancer was caused by smoking, but epidemiologists know that smoking greatly increases the risk. “That is enough to say that, for all practical purposes, there is a causal connection between smoking cigarettes and lung cancer and it is the same with climate change.”
theguardian.com/environment/2018/jul/27/extreme-global-weather-climate-change-michael-mann

Australia, emitting 138 million tons of CO₂e in 2017 and in 2017 exporting 200 million tonnes thermal coal and 172 million tons metallurgical coal, is currently suffering major consequences in terms of drought in New South Wales, north-west Victoria and eastern South Australia.

The factors, as explained by Blair Trewin of the Bureau of Meteorology, include: “a stronger than usual sub-tropical ridge over southern Australia. That means that frontal systems that would normally start affecting southern Australia more generally during the winter are instead mostly passing south of the continent, really only affecting Tasmania and perhaps southern Victoria."

Although the polar-ward migration of climate zones pushed southward by the tropical Hadley Cell constitutes an integral feature of global climate change, rarely does the term “climate change” appear in relevant government and farmers’ statements. Orwellian Newspeak has won the day once again, where talk about the “National energy guarantee” appears to divert attention from the global climate crisis to power prices, in a country where the sky is the limit for alternative clean energy—solar, wind and tide.

The cover-up by the compliant mainstream media, radio and TV of the climate change origin of the heat waves and of fires in the northern hemisphere, and of the drought in the southern hemisphere, is now almost complete. In true Orwellian newspeak terms the words “climate change” have now been replaced with “energy security”..

Andrew Glikson
Dr Andrew Glikson
Earth and Paleo-climate science
ANU Climate Change Institute
ANU Planetary Science Institute
Books:
http://www.springer.com/gp/book/9783319079073
http://www.springer.com/gp/book/9789400763272
http://www.springer.com/us/book/9783319745442
http://www.springer.com/gp/book/9783319225111
http://www.springer.com/gp/book/9783319572369
http://www.springer.com/gp/book/9789400773318


Sunday, February 8, 2015

Two degrees of warming closer than you may think

by David Spratt

It has taken a hundred years of human-caused greenhouse emissions to push the global temperature up almost one degree Celsius (1C°), so another degree is still some time away. Right? And there seems to have been a "pause" in warming over the last two decades, so getting to 2C° is going to take a good while, and we may have more time that we thought. Yes?

Wrong on both counts.

The world could be 2C° warmer in as little as two decades, according to the leading US climate scientist and "hockey stick" author, Dr Michael E. Mann. Writing in Scientific American in March 2014 (with the maths explained here), Mann says that new calculations "indicate that if the world continues to burn fossil fuels at the current rate, global warming will rise to 2C° by 2036" and to avoid that threshold "nations will have to keep carbon dioxide levels below 405 parts per million", a level we have just about reached already. Mann says the notion of a warming "pause" is false.

Global temperature over the last 1000 years: the "hockey stick"

Here's why 2C° could be just 20 years away.

Record heat

2014 was the hottest year in the instrumental record. The US government agencies NASA and NOAA announced the 2014 record on 16 January, noting that "the 10 warmest years in the instrumental record, with the exception of 1998, have now occurred since 2000".



NASA's Goddard Institute for Space Studies (GISS) says that since 1880, "Earth’s average surface temperature has warmed by about 1.4 degrees Fahrenheit (0.8C°), a trend that is largely driven by the increase in carbon dioxide (CO2) and other human emissions into the planet’s atmosphere. The majority of that warming has occurred in the past three decades."

GISS Director Gavin Schmidt says that this is “the latest in a series of warm years, in a series of warm decades. While the ranking of individual years can be affected by chaotic weather patterns, the long-term trends are attributable to drivers of climate change that right now are dominated by human emissions of greenhouse gases".

2014 was also Australia’s third-hottest year on record, according to the Bureau of Meteorology: "Overall, 2014 was Australia's third-warmest year on record: the annual national mean temperature was +0.91 °C above average… All States, except the Northern Territory, ranked in the four warmest years on record."

The 2014 record was achieved in neutral ENSO conditions

Fluctuations in the ENSO cycle affect global temperature, with El Niño conditions (a mobile blister of Pacific Ocean heat that affects wind patterns and currents and reduces rainfall in eastern Australia) correlating with warmer global temperatures. Former NASA climate science chief Dr James Hansen and colleagues note that the record global temperature in 2014 "was achieved with little assistance from the tropical ENSO cycle, confirms continuing global warming... and with the help of even a mild El Niño 2015 may be significantly warmer than 2014."

And El Niño conditions are likely to became more frequent with more warming. Last year, Wenju Cai, a climate researcher for Australia’s Commonwealth Scientific and Industrial Research Organisation (CSIRO), warned that the frequency of extreme El Niño events could double with climate change, in a paper that presented "evidence for a doubling in the occurrences in the future in response to greenhouse warming".

There is no "pause" in warming

In releasing the data on 2014's record warmth, NASA charted warming since 1970 and demonstrated that there has been no "pause" or slowing in warming, contrary to the million-times-repeated claims of the climate warming denial industry.

Joe Romm of Climate Progress says this chart (below) shows that: "The human-caused rise in surface air temperatures never paused, never even slowed significantly. And that means we are likely headed toward a period of rapid surface temperature warming. "




A year ago, Prof Matthew England of University of NSW suggested that temperatures were likely to rise quickly:
Scientists have long suspected that extra ocean heat uptake has slowed the rise of global average temperatures, but the mechanism behind the hiatus remained unclear…. But the heat uptake is by no means permanent: when the trade wind strength returns to normal –- as it inevitably will –- our research suggests heat will quickly accumulate in the atmosphere. So global [surface] temperatures look set to rise rapidly….
The oceans are warming very rapidly

Of all the additional heat trapped by higher levels of greenhouse gases, more than 90 per cent goes to warming the oceans, and thus ocean heat content (OHC) is by far the most significant and reliable indicator of global warming. By contrast only two per cent goes to warming the atmosphere, so small heat exchanges between oceans and the atmosphere (caused by changing sea surface, ocean circulation and wind conditions) can have a significant impact on atmospheric temperature, but not on ocean temperature.

The NOAA's State of the Climate for 2014 reports:
During 2014, the globally-averaged sea surface temperature was 1.03°F (0.57°C) above the 20th century average. This was the highest among all years in the 1880-2014 record, surpassing the previous records of 1998 and 2003 by 0.09°F (0.05°C).


The rate of OHC incease appears to be accelerating, with Romm noting that:
... ocean warming has sped up, and sea level rise has accelerated more than we thought, and Arctic sea ice has melted much faster than the models expected, as have the great ice sheets in Greenland and Antarctica.
And as Matthew England has told us, when the trade wind strength returns to normal, some ocean heat will quickly accumulate in the atmosphere.

You can check all the NOAA ocean heat content charts here.

Human greenhouse gas emissions are not slowing

Data from the Global Carbon Project shows annual carbon dioxide emissions are continuing to increase, and that the rate of increase since 2000 is at least double that of the 1990-99 decade. Emissions are projected to continue on the current growth path till 2020.


Fossil fuel emissions 1990-2014 and projected to 2019

To summarise the story so far: 2014 was a record hot year (without El Nino conditions); there has been no pause in warming; ocean heat content is rising at an increasing rate; global annual carbon dioxide emissions are continuing to grow; and more frequent El Nino conditions and a return to more normal trade wind strength will release some ocean heat to the atmosphere; so we are likely headed for a period of rapid surface temperature warming.

But there is more to the story.

A reservoir of heat already in the system

Increased levels of atmospheric greenhouse gases create an energy imbalance between incoming and outgoing radiation, which is resolved by elements of the earth system (land and oceans) absorbing the additional heat until the system reaches a new balance (equilibrium) at a higher temperature. But that process takes time, due to thermal inertia (as with an electric oven: once energy is applied, it takes time for all the structure to heat up and is not instantaneous). As a rule of thumb, about one-third of the heating potential of an increase in atmospheric carbon dioxide will be felt straight away, another third take around 30 years, and the last third is not fully realised for a century.

Thus there is more warming to come for the carbon dioxide already emitted, amounting to about another 0.6°C of warming. And because the rate of emissions is increasing, that figure is also increasing.

From this we can conclude that around 1.5°C of warming is locked into the system for current CO2 levels, though very large-scale carbon drawdown could reduce levels slowly over decadal time frames.

As well as long-lived CO2, there are other greenhouse gases with shorter lifetimes, particularly methane (lifetime approx. 10 years) and nitrous oxide (lifetime approx. 100 years). Because emissions of these gases are also continuing unabated, they also contribute to warming temperatures on decadal time frames.

In fact, the current level of greenhouse gases if maintained is already more than enough to produce 2°C of warming over time: in 2008 two scientists, Ramanathan and Feng, in On avoiding dangerous anthropogenic interference with the climate system: Formidable challenges ahead found that if greenhouse gases were maintained at their 2005 levels, the inferred warming is 2.4˚C (range 1.4˚C to 4.3˚C).

The current level of greenhouse gases is around 400 parts per million (ppm) CO2, and 470 ppm CO2 equivalent (CO2e) when other greenhouse gases are included. The last time CO2 levels were as high as they are today, humans didn't exist, and over the last 20 million years such levels are associated with major climate transitions. Tripati, Roberts et al. found that, big changes in significant climate system elements such as ice sheets, sea levels and carbon stores are likely to occur for the current level of CO2:
During mid-Miocene climatic optimum [16-14 million years ago] CO2 levels were similar to today, but temperatures were ~3–6°C warmer and sea levels 25 to 40 metres higher than at present… When CO2 levels were last similar to modern values (greater than 350 ppmv to 400 pmv), there was little glacial ice on land, or sea ice in the Arctic, and a marine-based ice mass on Antarctica was not viable…
But the question remains as to how quickly this warming will occur, and for that we need to look at two further factors: climate sensitivity and the role of aerosols.

Climate sensitivity

The measure of how much warming occurs for an increase in greenhouse gases is known as climate sensitivity, and is expressed as the temperature rise resulting from a doubling of greenhouse gas levels.

As Michael E. Mann explains:
Although the earth has experienced exceptional warming over the past century, to estimate how much more will occur we need to know how temperature will respond to the ongoing human-caused rise in atmospheric greenhouse gases, primarily carbon dioxide. Scientists call this responsiveness “equilibrium climate sensitivity” (ECS). ECS is a common measure of the heating effect of greenhouse gases. It represents the warming at the earth's surface that is expected after the concentration of CO2 in the atmosphere doubles and the climate subsequently stabilizes (reaches equilibrium)… The more sensitive the atmosphere is to a rise in CO2, the higher the ECS, and the faster the temperature will rise. ECS is shorthand for the amount of warming expected, given a particular fossil-fuel emissions scenario.
As discussed previously here, some elements of the climate system respond quickly to temperature change, including the amount of water vapour in the air and hence level of cloud cover, sea-level changes due to ocean temperature change, and the extent of sea-ice that floats on the ocean in the polar regions. These changes amplify (increase) the temperature change and are known as short-term or “fast” feedbacks, and it is on this basis that (short-term) ECS is well established as being around 3°C for a doubling of greenhouse gas levels (see, for example, Climate sensitivity, sea level, and atmospheric carbon dioxide).

But there are also longer-term or “slow” feedbacks, which generally take much longer (centuries to thousands of years) to occur. These include changes in large, polar, land-based ice sheets, changes in the carbon cycle (changed efficiency of carbon sinks such as permafrost and methane clathrate stores, as well as biosphere stores such as peat lands and forests), and changes in vegetation coverage and reflectivity (albedo). When these are taken into account, the sensitivity is significantly higher at 4.5°C or more, dependent on the state of the poles and carbon stores. Importantly, the rate of change at present is so fast that some of these long-term feedbacks are being triggered now on short-term timeframes (see Carbon budgets, climate sensitivity and the myth of "burnable carbon").

Mann says uncertainty about ECS can arise from questions of the role of clouds and water vapour, with the most recent IPCC report simply giving a range of 1.5–4.5°C but no "best-fit" figure. Factors such as changing rates of heat flux between oceans and atmosphere (including the El Nino/La Nina cycle), and volcanic eruptions, can cloud the short-term picture, as has the focus on the non-existent "pause".

What would happen if ECS is a bit lower that the "best-fit" value of 3°C of warming for doubling of greenhouse gas levels? Mann explains:
I recently calculated hypothetical future temperatures by plugging different ECS values into a so-called energy balance model, which scientists use to investigate possible climate scenarios. The computer model determines how the average surface temperature responds to changing natural factors, such as volcanoes and the sun, and human factors—greenhouse gases, aerosol pollutants, and so on. (Although climate models have critics, they reflect our best ability to describe how the climate system works, based on physics, chemistry and biology. And they have a proved track record: for example, the actual warming in recent years was accurately predicted by the models decades ago.)

I then instructed the model to project forward under the assumption of business-as-usual greenhouse gas emissions. I ran the model again and again, for ECS values ranging from the IPCC's lower bound (1.5°C) to its upper bound (4.5°C). The curves for an ECS of 2.5 degrees and 3°C fit the instrument readings most closely. The curves for a substantially lower ECS did not fit the recent instrumental record at all, reinforcing the notion that they are not realistic.

To my wonder, I found that for an ECS of 3°C, our planet would cross the dangerous warming threshold of 2°C in 2036, only 22 years from now. When I considered the lower ECS value of 2.5°C, the world would cross the threshold in 2046, just 10 years later.
This is charted as:

Michael E. Mann's graph of future temperature for different climate sensitivities. Click to enlarge.
Mann concludes that "even if we accept a lower ECS value, it hardly signals the end of global warming or even a pause. Instead it simply buys us a little bit of time—potentially valuable time—to prevent our planet from crossing the threshold."

As I have explained repeatedly, including in Dangerous climate warming: Myth and reality, 2°C is far from a safe level of warming. In fact, a strong case is made that climate change is already dangerous at less than 1°C of warming and, in James Hansen's analysis, “goals of limiting human made warming to 2°C and CO2 to 450 ppm are prescriptions for disaster” because significant tipping points – where significant elements of the climate system move from one discrete state to another – will be crossed.

Aerosol's Faustian bargain

Mann also indicated what level of CO2 would be consistent with 2°C of warming:
These findings have implications for what we all must do to prevent disaster. An ECS of 3°C means that if we are to limit global warming to below 2°C forever, we need to keep CO2 concentrations far below twice pre-industrial levels, closer to 450 ppm. Ironically, if the world burns significantly less coal, that would lessen CO2 emissions but also reduce aerosols in the atmosphere that block the sun (such as sulfate particulates), so we would have to limit CO2 to below roughly 405 ppm.
The aerosol question is central but often not well understood. Human activities also influence the greenhouse effect by releasing non-gaseous substances such as aerosols (small particles) into the atmosphere. Aerosols include black-carbon soot, organic carbon, sulphates, nitrates, as well as dust from smoke, manufacturing, windstorms, and other sources.

Aerosols have a net cooling effect because they reduce the amount of sunlight that reaches the ground, and they increase cloud cover. This effect is popularly referred to as ‘global dimming’, because the overall aerosol impact is to reduce, or dim, the sun’s radiation, thus masking some of the effect of the increased greenhouse gas levels. This is of little comfort, however, because aerosols last only about ten days before being washed out of the atmosphere by rain; so we have to keep putting more and more into the air to maintain the temporary cooling effect.

Unfortunately, the principal source of aerosols is the burning of fossil fuels, which causes a rise in CO2 levels and global warming that lasts for many centuries. The dilemma is that if you cut the aerosols, the globe will experience a pulse of warming as their dimming effect is lost; but if you keep pouring aerosols together with CO2 into the air, you cook the planet even more in the long run. A Faustian bargain.

There has been an effort to reduce emissions from some aerosols because they cause acid rain and other forms of pollution. However, in the short term, this is warming the air as well as making it cleaner. As Mann notes above, likely reductions in coal burning in coming decades will reduce aerosol levels and boost warming

Some recent research suggest aerosol cooling is in the range of 0.5–1.2°C over the long run:
  • Leon Rotstayn in The Conversation explains that "results from CSIRO climate modelling suggest that the extra warming effect from a decline in aerosols could be about 1°C by the end of the century". 
  • Present-day aerosol cooling effect will be strongly reduced by 2030 as more stringent air pollution controls are implemented in Europe and worldwide, and as advanced environmental technologies come on stream. These actions are projected to increase the global temperature by 1°C and temperatures over Europe by up to 2–4°C, depending on the severity of the action. This is one of the main research outcomes of the European Integrated project on Aerosol Cloud Climate and Air Quality Interaction project. 
  • In 2011, NASA climate science chief James Hansen and co-authors warned that the cooling impact of aerosols appears to have been underestimated in many climate models and inferred that: "Aerosol climate forcing today is inferred to be −1.6±0.3Wm−2," which is equivalent to a cooling of about 1.2°C. In that case, they wrote, "humanity has made itself a Faustian bargain more dangerous than commonly supposed". 
Conclusion

Michael E. Mann's analysis is sobering, especially when aerosols are accounted for.

The world is already hitting 400 ppm CO2 (the daily average at the measuring station at Mauna Loa first exceeded 400 ppm on 10 May 2013 and currently rising at a rate of approximately 2 ppm/year and accelerating), so the message is very clear that today we have circumstances that can drive us to 2°C of warming, and that emissions from now on are adding to warming above 2°C and towards 3°C or more. This reinforces my conclusion last year that there is no carbon budget left for 2°C of warming, and claims to the contrary are a dangerous illusion.

Mann concludes in not dis-similar terms:
The conclusion that limiting CO2 below 450 ppm will prevent warming beyond 2°C is based on a conservative definition of climate sensitivity that considers only the so-called fast feedbacks in the climate system, such as changes in clouds, water vapor and melting sea ice. Some climate scientists, including James E. Hansen… say we must also consider slower feedbacks such as changes in the continental ice sheets. When these are taken into account, Hansen and others maintain, we need to get back down to the lower level of CO2 that existed during the mid-20th century — about 350 ppm. That would require widespread deployment of expensive “air capture” technology that actively removes CO2 from the atmosphere.

Furthermore, the notion that 2°C of warming is a “safe” limit is subjective. It is based on when most of the globe will be exposed to potentially irreversible climate changes. Yet destructive change has already arrived in some regions. In the Arctic, loss of sea ice and thawing permafrost are wreaking havoc on indigenous peoples and ecosystems. In low-lying island nations, land and freshwater are disappearing because of rising sea levels and erosion. For these regions, current warming, and the further warming (at least 0.5°C) guaranteed by CO2 already emitted, constitutes damaging climate change today.

[Originally posted at Climate Code Red

Monday, April 7, 2014

Permafrost thawing could accelerate global warming


"If the permafrost melts entirely, there would be 5x the amount of carbon in the atmosphere than there is now" - Jeff Chanton

Jeff Chanton, the John Widmer
Winchester Professor of
Oceanography at Florida State.
A team of researchers lead by Florida State University have found new evidence that permafrost thawing is releasing large quantities of greenhouse gases into the atmosphere via plants, which could accelerate warming trends.

The research is featured in the newest edition of the Proceedings of the National Academy of Sciences.

“We’ve known for a while now that permafrost is thawing,” said Suzanne Hodgkins, the lead author on the paper and a doctoral student in chemical oceanography at Florida State. “But what we’ve found is that the associated changes in plant community composition in the polar regions could lead to way more carbon being released into the atmosphere as methane.”

Permafrost is soil that is frozen year round and is typically located in polar regions. As the world has gotten slightly warmer, that permafrost is thawing and decomposing, which is producing increased amounts of methane.

Relative to carbon dioxide, methane has a disproportionately large global warming potential. Methane is 33 times more effective at warming the Earth on a mass basis and a century time scale relative to carbon dioxide.

Changes in plant community composition in the polar regions could lead to way more carbon being released into the atmosphere as methane

As the plants break down, they are releasing carbon into the atmosphere. And if the permafrost melts entirely, there would be five times the amount of carbon in the atmosphere than there is now, said Jeff Chanton, the John Widmer Winchester Professor of Oceanography at Florida State.

“The world is getting warmer, and the additional release of gas would only add to our problems,” he said.

Chanton and Hodgkins’ work, “Changes in peat chemistry associated with permafrost thaw increase greenhouse gas production,” was funded by a three-year, $400,000 Department of Energy grant. They traveled to Sweden multiple times to collect soil samples for the study.

The research is a multicontinent effort with researchers from North America, Europe and Australia all contributing to the work.

Monday, October 28, 2013

How Do We Act in the Face of Climate Chaos?

Guy McPherson


Guy R. McPherson is Professor Emeritus of Natural Resources
and 
Ecology & Evolutionary Biology at University of Arizona.
Below are some (slighly edited) extracts from a post at Guy
McPherson's website: 
summary and update on climate change.




The Warning

As described by the United Nations Advisory Group on Greenhouse Gases in 1990, temperature rise “beyond 1 degree C may elicit rapid, unpredictable and non-linear responses that could lead to extensive ecosystem damage”.

We’ve clearly triggered the types of positive feedbacks the United Nations warned about in 1990. Yet my colleagues and acquaintances think we can and will work our way out of this horrific mess with permaculture (which is not to denigrate permaculture, the principles of which are implemented at the mud hut). Reforestation doesn’t come close to overcoming combustion of fossil fuels, as pointed out in the 30 May 2013 issue of Nature Climate Change. Furthermore, forested ecosystems do not sequester additional carbon dioxide as it increases in the atmosphere, as disappointingly explained in the 6 August 2013 issue of New Phytologist.

Here’s the bottom line: On a planet 4 C hotter than baseline, all we can prepare for is human extinction (from Oliver Tickell’s 2008 synthesis in the Guardian).

John Davies concludes: “The world is probably at the start of a runaway Greenhouse Event which will end most human life on Earth before 2040.” He considers only atmospheric carbon dioxide concentration, not the many self-reinforcing feedback loops described below. 


Positive feedbacks
Positive feedbacks
Methane hydrates are bubbling out the Arctic Ocean (Science, March 2010). According to NASA’s CARVE project, these plumes were up to 150 kilometers across as of mid-July 2013. Whereas Malcolm Light’s 9 February 2012 forecast of extinction of all life on Earth by the middle of this century appears premature because his conclusion of exponential methane release during summer 2011 was based on data subsequently revised and smoothed by U.S. government agencies, subsequent information — most notably from NASA’s CARVE project — indicates the grave potential for catastrophic release of methane. Catastrophically rapid release of methane in the Arctic is further supported by Nafeez Ahmed’s thorough analysis in the 5 August 2013 issue of the Guardian as well as Natalia Shakhova’s 29 July 2013 interview with Nick Breeze (note the look of abject despair at the eight-minute mark).
Warm Atlantic water is defrosting the Arctic as it shoots through the Fram Strait (Science, January 2011).
Siberian methane vents have increased in size from less than a meter across in the summer of 2010 to about a kilometer across in 2011 (Tellus, February 2011)
Drought in the Amazon triggered the release of more carbon than the United States in 2010 (Science, February 2011). In addition, ongoing deforestation in the region is driving declines in precipitation at a rate much faster than long thought, as reported in the 19 July 2013 issue of Geophysical Research Letters.
Peat in the world’s boreal forests is decomposing at an astonishing rate (Nature Communications, November 2011)
Invasion of tall shrubs warms the soil, hence destabilizes the permafrost (Environmental Research Letters, March 2012)
Methane is being released from the Antarctic, too (Nature, August 2012). According to a paper in the 24 July 2013 issue of Scientific Reports, melt rate in the Antarctic has caught up to the Arctic.
Russian forest and bog fires are growing (NASA, August 2012), a phenomenon consequently apparent throughout the northern hemisphere (Nature Communications, July 2013). The New York Times reports hotter, drier conditions leading to huge fires in western North America as the “new normal” in their 1 July 2013 issue. A paper in the 22 July 2013 issue of the Proceedings of the National Academy of Sciences indicates boreal forests are burning at a rate exceeding that of the last 10,000 years.
Cracking of glaciers accelerates in the presence of increased carbon dioxide(Journal of Physics D: Applied Physics, October 2012)
The microbes have joined the party, too, according to a paper in the 23 February 2013 issue of New Scientist
Summer ice melt in Antarctica is at its highest level in a thousand years: Summer ice in the Antarctic is melting 10 times quicker than it was 600 years ago, with the most rapid melt occurring in the last 50 years (Nature Geoscience, April 2013). Although scientists have long expressed concern about the instability of the West Atlantic Ice Sheet (WAIS), a research paper published in the 28 August 2013 of Nature indicates the East Atlantic Ice Sheet (EAIS) has undergone rapid changes in the past five decades. The latter is the world’s largest ice sheet and was previously thought to be at little risk from climate change. But it has undergone rapid changes in the past five decades, signaling a potential threat to global sea levels. The EAIS holds enough water to raise sea levels more than 50 meters.
Surface meltwater draining through cracks in an ice sheet can warm the sheet from the inside, softening the ice and letting it flow faster, according to a study accepted for publication in the Journal of Geophysical Research: Earth Surface (July 2013). It appears a Heinrich Event has been triggered in Greenland. Consider the description of such an event as provided by Robert Scribbler on 8 August 2013:
In a Heinrich Event, the melt forces eventually reach a tipping point. The warmer water has greatly softened the ice sheet. Floods of water flow out beneath the ice. Ice ponds grow into great lakes that may spill out both over top of the ice and underneath it. Large ice damns (sic) may or may not start to form. All through this time ice motion and melt is accelerating. Finally, a major tipping point is reached and in a single large event or ongoing series of such events, a massive surge of water and ice flush outward as the ice sheet enters an entirely chaotic state. Tsunamis of melt water rush out bearing their vast floatillas (sic) of ice burgs (sic), greatly contributing to sea level rise. And that’s when the weather really starts to get nasty. In the case of Greenland, the firing line for such events is the entire North Atlantic and, ultimately the Northern Hemisphere.
Breakdown of the thermohaline conveyor belt is happening in the Antarctic as well as the Arctic, thus leading to melting of Antarctic permafrost (Scientific Reports, July 2013)
Loss of Arctic sea ice is reducing the temperature gradient between the poles and the equator, thus causing the jet stream to slow and meander. One result is the creation of weather blocks such as the recent very high temperatures in Alaska. As aresultboreal peat dries and catches fire like a coal seam. The resulting soot enters the atmosphere to fall again, coating the ice surface elsewhere, thus reducing albedo and hastening the melting of ice. Each of these individual phenomena has been reported, albeit rarely, but to my knowledge the dots have not been connected beyond this space. The inability or unwillingness of the media to connect two dots is not surprising, and has been routinely reported (recently including here with respect to climate change and wildfires) (July 2013)
Earthquakes trigger methane release, and consequent warming of the planet triggers earthquakes, as reported by Sam Carana at Arctic-news (October 2013)
Arctic drilling was fast-tracked by the Obama administration during the summer of 2012
Supertankers are taking advantage of the slushy Arctic, demonstrating that every catastrophe represents a business opportunity, as pointed out by Professor of journalism Michael I. Niman and picked up by Truthout (ArtVoice, September 2013)
As nearly as I can distinguish, only the latter feedback process is reversible at a temporal scale relevant to our species. Once you pull the tab on the can of beer, there’s no keeping the carbon dioxide from bubbling up and out. These feedbacks are not additive, they are multiplicative. Now that we’ve entered the era of expensive oil, I can’t imagine we’ll voluntarily terminate the process of drilling for oil and gas in the Arctic (or anywhere else). Nor will we willingly forgo a few dollars by failing to take advantage of the long-sought Northwest Passage.

Robin Westenra provides an assessment of these positive feedbacks at Seemorerocks on 14 July 2013. It’s worth a look.


Earth-system scientist Clive Hamilton concludes in his April 2013 book Earthmasters that “without [atmospheric sulphates associated with industrial activity] … Earth would be an extra 1.1 C warmer.” In other words, collapse takes us directly to 2 C within a matter of weeks. 

Several other academic scientists have concluded, in the refereed journal literature no less, that the 2 C mark is essentially impossible (for example, see the review paper by Mark New and colleagues published in the 29 November 2010 issue of the Philosophical Transactions of the Royal Society A). 

The German Institute for International and Security Affairs concluded 2 June 2013 that a 2 C rise in global-average temperature is no longer feasible (and Spiegel agrees, finally, in their 7 June 2013 issue), while the ultra-conservative International Energy Agency concludes that, “coal will nearly overtake oil as the dominant energy source by 2017 … without a major shift away from coal, average global temperatures could rise by 6 degrees Celsius by 2050, leading to devastating climate change.” 

Image from: The two epochs of Marcott, by Jos Hagelaars

At the 11:20 mark of this video, climate scientist Paul Beckwith indicates Earth could warm by 6 C within a decade. 

If you think his view is extreme, consider: 
  1. the 5 C rise in global-average temperature 55 million years ago during a span of 13 years (reported in the 1 October 2013 issue of Proceedings of the National Academy of Sciences); and also 
  2. the reconstruction of regional and global temperature for the past 11,300 years published in Science in March 2013. One result is shown in the above figure.

How Do We Act in the Face of Climate Chaos?

Below is a video of a recent presentation by Guy McPherson. 

Presentation by Guy McPherson in Boulder, Colorado on October 16, 2013.

Below are some extracts from the video, again slightly edited.

Malcolm Light in 2012 concluded, based on data from NOAA and NASA, that methane release had gone exponential and was leading to the demise of all life on Earth, not just human extinction, by the middle of the century.

So 3.5 C to 4 C is almost certainly a death sentence for all human beings on the planet, not because it'll be a warmer planet, but because the warming of the planet will remove all habitat for human beings. Ultimately we're human animals like other animals, we need habitat to survive.

Changes we see in three or four decades happen as a result of what we do today. There's a huge lag between our actions today in the consequences down the road in terms of the Earth's planetary systems.

Without plankton in the ocean, there goes roughly half the global food supply. The ability to lose land plants is growing rapidly and there goes the other half for the food supply for human beings. If we have up to 5 C by 2050, that'll certainly do the trick.

Why is this happening? It's civilization that drove us into population overshoot. We cannot go back anymore since 1939, since we invented nuclear armageddon. There's no going back. If we ceased the set of living arrangements at this point, the world's 400 or so nuclear power plants melt down catastrophically and we're all dead in a month. We cannot terminate industrial civilization until we decommission all nuclear power plants. It takes at least 20 years to decommission a nuclear power plant.

The bad news is that means that the world's four hundred or so nuclear power plants meltdown catastrophically in a short period of time. Fukushima represent a major threat to humanity. If they fail in moving the spent fuel rods next month, according to nuclear researcher Christina Consola, if one of those MOX fuel rods is exposed to the air, one of the 1565, it will kill 2.89 billion people on the planet in a matter of weeks, so nuclear catastrophe is right there on the horizon. 

People ask me: Why are you presenting this horrible information?

Action is the antidote to despair even if the action is hopeless. When a medical doctor knows that somebody has cancer, it's malpractice if they don't tell that. So I'm doing that. I think Bill McKibben and James Hansen and a whole bunch of climate scientists are guilty of malpractice. Because they know what I know. Almost every politician in the country knows what I know. All the leaders of the big banks know what I know. And they're lying to us.

I'm just presenting the information from other scientists here. I'm trying to the widest extent possible not to infuse my opinion in the situation. It's John Davies who on September 20, 2013, taking into account only carbon dioxide, says there will be few people left on the planet by 2040. It's Malcolm Light, writing in February 2012, who assesses the methane situation. And so on.

Yes, I agree with them, and that agreement is illustrated by me showing you that information.

I promote resistance against this omnicidal culture, not in the hope that it will save our species, but in the hope that it will save other species. Because as E.O. Wilson, biologist at Harvard, points out, it only takes 10 million years after a great extinction event, before you have a blossoming full rich planet again. That's what we're working toward. We're saving habitat for other species at this point.