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My oh Miocene!

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Guest commentary by Sarah Feakins

Our recent study in Nature Geoscience reconstructed conditions at the Antarctic coast during a warm period of Earth’s history. Today the Ross Sea has an ice shelf and the continent is ice covered; but we found the Antarctic coast was covered with tundra vegetation for some periods between 20 million and 15.5 million years ago. These findings are based on the isotopic composition of plant leaf waxes in marine sediments.

That temperatures were warm at that time was not a huge surprise; surprising, was how much warmer things were – up to 11ºC (20ºF) warmer at the Antarctic coast! We expected to see polar amplification, i.e. greater changes towards the poles as the planet warms. This study found those coastal temperatures to be as warm as 7ºC or 45ºF during the summer months. This is a surprise because conventional wisdom has tended to think of Antarctica being getting progressively colder since ice sheets first appeared on Antarctica 34 million years ago (but see Ruddiman (2010) for a good discussion of some of the puzzles).
[Read more…] about My oh Miocene!

References

  1. S.J. Feakins, S. Warny, and J. Lee, "Hydrologic cycling over Antarctica during the middle Miocene warming", Nature Geoscience, vol. 5, pp. 557-560, 2012. http://dx.doi.org/10.1038/NGEO1498
  2. W.F. Ruddiman, "A Paleoclimatic Enigma?", Science, vol. 328, pp. 838-839, 2010. http://dx.doi.org/10.1126/science.1188292

Tree Rings and Climate: Some Recent Developments

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by Michael E. Mann, Gavin Schmidt, and Eric Steig

Update 7/12/12: Media Matters comments on the latest misrepresentations of the Esper et al study discussed in our article: ‘Surprise: Fox News Fails Paleoclimatology’
Update 7/13/12: Further comment from Bob Ward of the Grantham Institute in Huffington Post UK “The World’s Most Visited Newspaper Website Continues to Regurgitate Nonsense from Climate Change ‘Sceptics'”
Update 7/14/12: Some additional context provided by this LiveScience article

It’s been a tough few months for tree-rings, perhaps unfairly. Back in April, we commented on a study [that one of us (Mike) was involved in] that focused on the possibility that there is a threshold on the cooling recorded by tree-ring composites that could limit their ability to capture the short-term cooling signal associated with larger volcanic eruptions. Mostly lost in the discussion, however, was the fact–emphasized in the paper—that the trees appeared to be doing a remarkably good job in capturing the long-term temperature signal—the aspect of greatest relevance in discussions of climate change.

This week there have been two additional studies published raising questions about the interpretation of tree-ring based climate reconstructions.
[Read more…] about Tree Rings and Climate: Some Recent Developments

Far out in North Carolina

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The extensive salt marshes on the Outer Banks of Carolina offer ideal conditions for unravelling the mysteries of sea level change during past centuries. Here is a short report from our field work there – plus some comments on strange North Carolina politics as well as two related new papers published today in Nature Climate Change.


The Outer Banks of Carolina are particularly vulnerable to coastal erosion and sea-level rise, partly because the land is subsiding and the banks are naturally moving landward. On the ocean front, land is continually being lost.
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What makes sea-level rise?

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Last week the science community was shocked by the claim that 42% of the sea-level rise of the past decades is due to groundwater pumping for irrigation purposes. What could this mean for the future – and is it true?

The causes of global sea level rise can be roughly split into three categories: (1) thermal expansion of sea water as it warms up, (2) melting of land ice and (3) changes in the amount of water stored on land. There are independent estimates for these contributions, and obviously an important question is whether their sum is consistent with the total sea level rise actually observed.


foto (c) Stefan Rahmstorf 2012
 [Read more…] about What makes sea-level rise?

Real Video

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Guest post by Kelly Levin, WRI; Paul Higgins, AMS; Brian Helmuth, University of South Carolina; and Andy Dessler, Texas A&M

Scientists have made massive progress in understanding the climate system and how human activities are altering it. Despite that progress, decision makers continue to struggle with climate change risk management.

RealClimate and other initiatives have shown that new media can be effective in enhancing communication of climate science. The speed by which new information can be transmitted has increased significantly, and new media has provided new learning opportunities, including discussion, debate, and links to further information.

This month, WRI, supported by google.org, launched a pilot project to further build the capacity of the scientific community to more effectively relay their recent scientific findings. The project stemmed from the Google Science Communication Fellow program, which aims to foster more accessible, open, and transparent scientific dialogue.

The project assesses whether video can be a compelling way for a scientist to describe his/her discoveries and, if so, which type of video works best. Imagine video being embedded one day into journal websites and Google scholar, not only offering the option of downloading a recent publication but also a video associated with the publication. Imagine videos sitting alongside newspaper and magazine articles, where you can hear about findings directly from the scientist in his or her own words. Like RealClimate, the project aims to connect viewers to the scientists themselves.

This project has the potential to improve scientific communication and enhance the public understanding of science. Ultimately, if done right scientific communication can help shape the public debate and lead to more informed decisions. That’s critical because societal decisions have the greatest chance to benefit the public when they are grounded in the best available knowledge and understanding. We need RealClimate’s reader’s help.

Please assist us in identifying the most effective means for communicating the latest findings of climate science via video. Go to http://www.wri.org/communicating-climate-science to watch the three videos.

Three scientists (also Google Fellows) — Andy Dessler from Texas A&M University; Brian Helmuth from University of South Carolina; and Paul Higgins from the American Meteorological Society – participated, and the videos showcase one of their recent studies that is either in production or recently published:

Dessler’s paper (Science, Vol. 330., http://geotest.tamu.edu/userfiles/216/dessler10b.pdf) focused on quantifying the cloud feedback. Using the ENSO to study changing cloud patterns during climatic variability, he found that the feedback is likely positive, consistent with the feedback that climate models yield.

Helmuth’s paper (Ecology Letters, forthcoming) examined the impact of variations in water and aerial temperatures on predator-prey interactions between sea stars and mussels in the intertidal zone. He and his colleagues found that predation rates decreased during non-coincident interactions between the two temperature stressors. Their paper underscores the need for taking into account temporal fluctuations in environmental stress, which can be ignored in experiments and models.

Higgins focuses on his recent research (Journal of Climate, in press) to more fully quantify the potential range in the terrestrial carbon cycle response to climate warming. This research suggests that plants and soils could release large amounts of carbon dioxide as global climate warms. That would push GHG concentrations higher and lead to even more climate warming. This is important because we’ve been counting on plants and soils to soak up and store some of the carbon we’re releasing.

Three videos were produced for each of the abovementioned papers:

  • The first is comprised of a slideshow of relevant images with a voiceover of the scientist discussing his finding.
  • For the second video, Dessler, Helmuth and Higgins filmed their own videos.
  • For the third video, Dessler, Helmuth and Higgins each came into WRI’s offices, and were filmed conducting a white board talk describing their findings.

    • Which video do you think works best? Click here to cast your vote and tell us about why you think it is most effective. Your votes will inform any scaling up of this project in the future.

    Fresh hockey sticks from the Southern Hemisphere

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    In the Northern Hemisphere, the late 20th / early 21st century has been the hottest time period in the last 400 years at very high confidence, and likely in the last 1000 – 2000 years (or more). It has been unclear whether this is also true in the Southern Hemisphere. Three studies out this week shed considerable new light on this question. This post provides just brief summaries; we’ll have more to say about these studies in the coming weeks. [Read more…] about Fresh hockey sticks from the Southern Hemisphere

    OHC Model/Obs Comparison Errata

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    This is just a brief note to point out that a few graphs that I have put together showing Ocean Heat Content changes in recent decades had an incorrect scaling for the GISS model data. My error was in assuming that the model output (which were in units W yr/m2) were scaled for the ocean area only, when in fact they were scaled for the entire global surface area (see fig. 2 in Hansen et al, 2005). Therefore, in converting to units of 1022 Joules for the absolute ocean heat content change, I had used a factor of 1.1 (0.7 x 5.1 x 365 x 3600 x 24 x 10-8), instead of the correct value of 1.61 (5.1 x 365 x 3600 x 24 x 10-8). This problem came to light while we were redoing this analysis for the CMIP5 models and from conversations with dana1981 at skepticalscience.com.

    These graphs appeared in Dec 2009, May 2010, Jan 2011 and Feb 2012. In each case, I have replaced the graph with a corrected version while leaving a link to the incorrect version. Links to the figures will return the corrected image (and this is noted on the image itself). Where possible I used the data that were current at the time of the original post. Fortunately this only affects the figures used in these blog postings and not in any publications. Apologies for any confusion.

    This figure shows the comparison using the most up-to-date observational products (NODC, PMEL):

    The basic picture is unchanged – model simulations were able to capture the historical variance in OHC (as best we know it now – there remains significant structural uncertainty in those estimates). There are clear dips related volcanic eruptions (Agung, El Chichon, Pinatubo), and an sharp increase in the 1990s. Note that in GISS-EH (same AGCM but with a different ocean model) OHC increases at a slightly slower rate than seen with GISS-ER above. Looking at the last decade, it is clear that the observed rate of change of upper ocean heat content is a little slower than previously (and below linear extrapolations of the pre-2003 model output), and it remains unclear to what extent that is related to a reduction in net radiative forcing growth (due to the solar cycle, or perhaps larger than expected aerosol forcing growth), or internal variability, model errors, or data processing – arguments have been made for all four, singly and together.

    Analyses of the CMIP5 models will provide some insight here since the historical simulations have been extended to 2012 (including the last solar minimum), and have updated aerosol emissions. Watch this space.

    References

    1. J. Hansen, L. Nazarenko, R. Ruedy, M. Sato, J. Willis, A. Del Genio, D. Koch, A. Lacis, K. Lo, S. Menon, T. Novakov, J. Perlwitz, G. Russell, G.A. Schmidt, and N. Tausnev, "Earth's Energy Imbalance: Confirmation and Implications", Science, vol. 308, pp. 1431-1435, 2005. http://dx.doi.org/10.1126/science.1110252