Skeptical Science New Research for Week #9, 2020
Posted on 4 March 2020 by Doug Bostrom
60 Articles
Physical science of global warming & effects
Observations & observational methods of global warming & effects
Detailed quantification of glacier elevation and mass changes in South Georgia (open access)
Poleward shift of the major ocean gyres detected in a warming climate
Flash droughts present a new challenge for subseasonal-to-seasonal prediction
Marine Heatwaves in China's marginal seas and adjacent offshore waters: Past, Present, and Future
Modeling, simulation & analysis of global warming & global warming effects
Terrestrial Evaporation and Moisture Drainage in a Warmer Climate
Sandy coastlines under threat of erosion
Can we extrapolate climate in an inner basin? The case of the Red Sea
Future soil loss in highland Ethiopia under changing climate and land use
Shifting velocity of temperature extremes under climate change (open access)
Climate model advancement
Biology & global warming
Light availability modulates the effects of warming in a marine N2 fixer (open access)
Pathway dependence of ecosystem responses in China to 1.5 °C global warming (open access)
Woody plant encroachment intensifies under climate change across tundra and savanna biomes
GHG sources & sinks, flux
The role of northern peatlands in the global carbon cycle for the 21st century
Climate change communications & cognition
Reporting on Climate Change by Broadcast Meteorologists: A National Assessment (open access)
Public views of Scotland's path to decarbonization: Evidence from citizens' juries and focus groups
Humans dealing with our global warming
Socio-technical energy scenarios: state-of-the-art and CIB-based approaches (open access)
Influence of climate change impacts and mitigation costs on inequality between countries
Understanding interdependent climate change risks using a serious game (open access)
Influence of climate change impacts and mitigation costs on inequality between countries
Climate change impacts on viticulture in Croatia; viticultural zoning and future potential
Global warming to increase violent crime in the United States (open access)
Defining and classifying personal and household climate change adaptation behaviors
Climate adaptation pathways for agriculture: Insights from a participatory process
Inclusive and adaptive business models for climate-smart value creation
Other
Global Wetting by Seasonal Surface Water Over the Last Decades (open access)
AWARE: The Atmospheric Radiation Measurement (ARM) West Antarctic Radiation Experiment (open access)
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Can anyone refer me to the source of the idea that it takes thousands of years for the planet to reach equilibrium from the relatively modest rising "rate" of greenhouse gas levels and that the planet is still warming from the effects of 260ppm about 1,500 years ago? (not in just a few decades). I have been told that a study by Goreau in 1990 and another by Rohling in 2009 addresses this "stretched" delayed effect?
swampfoxh @1,
Your question doesn't 'ring any bells' with me and the authors you mention don't seem to lead anywhere that I can see.
The 1,500 year timescale is occasionally mentioned as the time it takes the ocean waters to re-appear at the surface and so reach CO2-quilibrium with the atmosphere. That is part of what Goreau (1990) 'Balancing Atmospheric Carbon Dioxide' addresses but it is not the same as timescales for temperature equilibrium under otherwise-fixed CO2 levels.
Rohling is the lead author of Rohling et al (2009) 'Antarctic temperature and global sea level closelycoupled over the past five glacial cycles' and this does consider multi-millennial equilibrium timescales but this concerns sea level. There is a connection in that the melt-out of, say, Greenland would both impact sea level and temperature as the albedo change constitutes a slow climate feedback (see this SkS post). But over such multi-millennial timescales with Milankovitch cycles in operation, it would require more than "modest" climate forcings to be significant.
More directly addressing your question, the ice cores do show a small increase in CO2 levels over the last 8,000 years. This would provide roughly a 0.3Wm^-2 climate forcing which (slow and fast feedbacks so perhaps a sensitivity of 6ºC) could have given a total temperature rise of +0.5ºC. Yet spread over eight milennia, any residual effect today would be now miniscule.
MAR, "More directly addressing your question, the ice cores do show a small increase in CO2 levels over the last 8,000 years..."
The Marcott study here shows global temperatures falling over about the last 3500 years until about 1900. So perhaps the milankovitch cycle cancelled out the slow low level rise of CO2 concentrations over the same period?
This graphic shows both global temperatures and CO2 levels over the past 10,000 years:
IIRC, Ruddiman's hypothesis helps account for some of that discrepancy that you note.