Can Nature Adapt To Climate Change In Time?
    By News Staff | December 24th 2009 12:00 AM | 4 comments | Print | E-mail | Track Comments
    The climate is changing and the natural world has to adapt to it. But how much time do the multitudes of species and their habitats have before it's too late? A team of environmental researchers has set out to answer that very question, and they say that as the world warms through the 21st century, ecosystems will need to shift about 0.42 kilometers per year (about a quarter mile per year) to keep pace with changing temperatures across the globe.

    In the December 24 issue of Nature, the researchers explain that mountainous habitats will be able to move more slowly, since a modest move up or down slope can result in a large change in temperature. However, flatter ecosystems, such as flooded grasslands, mangroves, and deserts, will need to move much more rapidly to stay in their comfort zone—sometimes more than a kilometer per year.

    The team calculated the velocity of global climate change by combining data on current climate and temperature regimes worldwide with a large suite of climate model projections for the next century. Their calculations are based on an "intermediate" level of projected greenhouse gas emissions over the next century (the A1B emissions scenario from The Intergovernmental Panel on Climate Change). 

    Under these emissions levels, the velocity of climate change is projected to be the slowest in tropical and subtropical coniferous forests (0.08 kilometers per year), temperate coniferous forests (0.11 kilometers per year), and montane grasslands and shrublands (0.11 kilometers per year). The velocity of climate change is expected to be the fastest in flatter areas, including deserts and xeric shrublands (0.71 kilometers per year), mangroves (0.95 kilometers per year), and flooded grasslands and savannas (1.26 kilometers per year).

    The vulnerability of these respective biomes depends not only on the average velocity of climate change they will experience, but also on the sizes of the protected areas in which they are found.  For instance, while the velocity of climate change is expected to be high in deserts, this threat is mediated by the fact that protected areas for deserts tend to be larger. On the other hand, the small size and fragmented nature of most protected areas in Mediterranean temperate broadleaf and boreal forest biomes makes these habitats particularly vulnerable.

    What does this mean for beetles, barnacles, and other groups of species? The researchers note that their index estimates the velocities and residence times of climates, not species. Individual species that have a wide tolerance for a range of temperatures may be able to adapt in place as the climate around them shifts. However, for species that can only tolerate a narrow band of temperatures, the velocity estimates in the study are a close approximation for the migration speeds needed to potentially avoid extinction.

    Nearly a third of the habitats in the study have velocities higher than even the most optimistic plant migration estimates, suggesting that plants in many areas will not be able to keep up with the shifting climate. Even more problematic is the fact that natural habitats have been extensively fragmented by human development, which will leave many species with "nowhere to go," regardless of their migration rates.

    "One of the most powerful aspects of this data is that it allows us to evaluate how our current protected area network will perform as we attempt to conserve biodiversity in the face of global climate change," says Healy Hamilton, Director of the Center for Applied Biodiversity Informatics at the California Academy of Sciences. "When we look at residence times for protected areas, which we define as the amount of time it will take current climate conditions to move across and out of a given protected area, only 8% of our current protected areas have residence times of more than 100 years."

    Citation: Scott R. Loarie, Philip B. Duffy, Healy Hamilton, Gregory P. Asner, Christopher B. Field, David D. Ackerl, 'The velocity of climate change', Nature Dec. 24, 2009, 462, 1052-1055; doi: 10.1038/nature08649


    Will anything at all be able to adapt
    To what's in the offing climate-wise?
    Quien sabe...But on the question at issue:
    If we knew what that will be, we'd be in a better position to advise.

    It stopped warming several years ago.

    All average global temperatures since 1895 are predicted by a simple model. There was no need to consider change to the level of CO2 or any other greenhouse gas.

    The model, with an eye-opening graph, is presented in the October 16 pdf at

    Well, that's awfully funny, Dan considering that both the National Oceanic and Atmospheric Administration (NOAA) and the USGS seem to think otherwise....
    It will be even funnier to see how these change as the atmospheric CO2 continues to increase and the average global temperature doesn't.

    Since 2000 the atmospheric carbon dioxide level has increased by an amount equal to 20% of the increase from 1800 to 2000. According to the average of the five reporting agencies (four since Climategate), the average global temperature has not changed much for several years and during the seven years from 2002 through 2008 the trend shows a DECREASE of 1.8°C/century. This measured SEPARATION between the increasing carbon dioxide level and not-increasing average global temperature is outside of the 'limits' of all of the predictions of the IPCC and 'consensus' of Climate Scientists. The separation has been increasing at an average rate of about 2% per year since 2000. It corroborates that, at the present CO2 level, atmospheric carbon dioxide increase has no significant influence on average global temperature. If you would like to check the data, a list and the links are given at the July 30, 6:52 PM post at

    The sunspot count went back to zero today.