Blog Archive

Wednesday, January 1, 2014

2013 in Review: a Productive Year for Skeptical Science

by Dana Nuccitelli, Skeptical Science, December 31, 2013

2013 is coming to a close, and so we take a look back at some of the important climate-related events of our year.

Skeptical Science Makes Significant Scholarly Contributions

The Skeptical Science team published several high-impact papers this year, starting with the Cook et al. (2013) consensus paper, co-authored by nine Skeptical Science volunteers.  The paper showed that there is a 97% consensus in the peer-reviewed climate science literature that humans are causing global warming.  The paper has already been cited in a broad range of scholarly journals and made a big splash in the media, even being the subject of two presidential Tweets.  It was also the 11th-most talked about academic paper in 2013.
Kevin Cowtan and Robert Way later published an important paper showing that much of the slowed global surface warming was an artifact of poor global temperature station coverage, mainly in the Arctic.  The Cowtan and Way (2013) paper has received extensive praise among scientists with relevant expertise due to the quality and importance of the paper.  Most recently, Richard Alley discussed their results in testimony to the Pennsylvania House of Representatives.
Nuccitelli et al. (2013) also debunked a paper by Akasofu that tried to blame global warming on a magical 'natural recovery' from the Little Ice Age.  As Nuccitelli et al. showed, climate changes must be caused by physical mechanisms, and Akasofu's argument lacked any physical basis.
Richardson (2013) demonstrated that the modern increase in atmospheric CO2 is entirely human-caused, debunking a paper by Humlum, Stordahl and Solheim that wrongly claimed otherwise.
John Cook's climate science and denial textbook with G. Thomas Farmer was published in January, and John was also invited to give three talks at the AGU fall meeting to discuss what his research tells us about effective climate communications.

The 'Pause' Myth Debunked Once and for All

Over the past year, the myth of the global warming 'pause' has become a favorite among climate contrarians.  The argument has always been fundamentally flawed, because asThe Escalator shows, it's based entirely on cherry picking short-term noise in the data.
escalator
Moreover, as Cowtan and Way (2013) demonstrated, even the short-term slowing of global surface temperatures was largely an artifact of poor Arctic temperature station coverage.
Additionally, by incorporating data from Nuccitelli et al. (2012), the Skeptical Science heat widget pointed out that during the time since global warming was supposed to have 'paused', the global climate accumulated over 2 billion Hiroshima atomic bomb detonations worth of heat.
Skeptical Science has now thus debunked the 'pause' myth from three different angles.

Important Climate Research in 2013

Several other climate papers this year helped to debunk the 'pause' myth and explain the short-term slowing of global surface warming.  Kosaka and Xie (2013) showed that changes in the Pacific Ocean could account for most of the short-term global surface temperature changes.  Along those lines, Watanabe et al. (2013) showed that ocean heat uptake has become more efficient over the past decade, which is consistent with the observations of Balmaseda et al. (2013), who found an unprecedented transfer of heat to the deep oceans over the past decade, consistent with the modeling in Meehl et al. (2013).
Putting it all together, we have an increasingly clear picture that while the warming of global surface temperatures has slowed over the past decade, it has not slowed as much as previously thought.  The slowed surface warming is due in large part to changes in ocean cycles, particularly in the Pacific Ocean, causing more efficient ocean heat uptake, thus leaving less heat to warm surface temperatures.  External factors, like decreased solar and increased volcanic activity, have also played a role in the slowed surface warming, but internal variability due to ocean cycles appears to be the main culprit.  In any case, as the 2013 IPCC Fifth Assessment Report showed, the observed global surface warming remains within the range of climate model projections.
IPCC AR5 Figure 1.4.  Solid lines and squares represent measured average global surface temperature changes by NASA (blue), NOAA (yellow), and the  UK Hadley Centre (green).  The colored shading shows the projected range of surface warming in the IPCC First Assessment Report (FAR; yellow), Second (SAR; green), Third (TAR; blue), and Fourth (AR4; red). 
IPCC AR5 Figure 1.4. Solid lines and squares represent measured average global surface temperature changes by NASA (blue), NOAA (yellow), and the UK Hadley Centre (green). The colored shading shows the projected range of surface warming in the IPCC First Assessment Report (FAR; yellow), Second (SAR; green), Third (TAR; blue), and Fourth (AR4; red).
Marcott et al. (2013) also showed that the warming we’ve witnessed in the last 100 years is unlike anything that happened in the previous 11,300 years, and that the warming yet to come in a business-as-usual scenario looks downright scary.
Shakun_Marcott_HadCRUT4_A1B 
The temperature reconstruction of Shakun et al. (green, shifted manually by 0.25 degrees), of Marcott et al. (blue), combined with the instrumental period data from HadCRUT4 (red) and the model average of IPCC projections for the A1B scenario up to 2100 (orange). Created by Jos Hagelaars.
A brand new study by Sherwood et al. (2013) tackles the question of how cloud cover will change and interact with global warming as the climate continues to change. The cloud feedback question is one of the largest remaining uncertainties in future climate predictions, so this is an important new paper. Unfortunately it finds that clouds will act to amplify global warming, suggesting that the planet will warm at least 3 °C in response to a doubling of atmospheric carbon dioxide, which also suggests at least 4 °C global surface warming by 2100 if we continue with business as usual policies.

Mixed Bag of Climate Policies

With regards to those policies, 2013 was a bit of a mixed bag.  Australia elected a majority government that has pledged to eliminate its carbon tax.  In Canada, the government has paid service to climate change while muzzling its scientists and doing everything possible to increase its emissions through maximum development of the tar sands.
However, on a local level, British Columbia's revenue-neutral carbon tax remains highly popular and successful, and California implemented a similarly popular carbon cap and trade system in 2013.  And the national news isn't all bad, as the US government has issued draft regulations on greenhouse gas emissions from new power plants, and is working on regulations for existing power plants.  There are also encouraging signs that China is beginning to address its rapid emissions growth.
However, on an international level, 2013 passed with very little progress in terms of establishing a new international climate agreement.  2015 is the target date for new emissions reductions plans.

2013 Summary

Overall 2013 was a productive year in terms of reducing the consensus gap and debunking the 'pause' myth.  Climate policies were a mixed bag, with some steps backwards and some steps forward.  Climate media coverage was likewise a mixed bag, with continued false balance and inaccurate reporting from the politically conservative media, also seeping into the BBCThe New York Times eliminated its environment desk, but The Guardian stepped in to fill the gap with its new Environment Blogs.
2013 was a productive year for Skeptical Science, which also saw the number of followers on its Facebook page grow rapidly and surpass 16,000, and its Twitter page to over 8,500.  A lot of interesting new climate research was published during the year, including a new IPCC synthesis report.  However, progress toward solving the climate problem remained far too slow.  Here's to 2014 being a more productive year for climate solutions.

No comments: