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Hi all,
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<div class="">I thought it might be strategic to contribute a presentation to this session at AGU (Marcia McNutt is one of the invited speakers, and Lauren Everett the PRB program officer is one of the conveners): </div>
<div class=""><b class="">Responding to Rapid Environmental Change at the Poles</b></div>
<div class="">(it’s a Global Environmental Change session)</div>
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<div class="">So, I put together the following abstract with all of you as co-authors (actually the process is different this year - you submit an abstract as a lead author and THEN if its accepted, you add co-authors ). <i class=""><font color="#e32400" class="">Let
me know if you want to see edits. </font></i>I thought I would put together the broad story on synthesis but look toward the future for differing recovery or change timescales across the system with an eye toward what happens in the coming ‘warming’ decades…
Thanks.</div>
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<div class="">TITLE: The Past as a Window to the Future of Antarctic Ecosystems - What does 20+ Years of Scientific Research in the McMurdo Dry Valleys, Antarctica Tell Us About the Trajectory of Polar Ecosystems?</div>
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<div class="">ABSTRACT: The McMurdo Dry Valleys of Antarctica represent the largest ice-free area of the continent. The landscape is dominated by glaciers, exposed soils, streams, and ice-covered lakes, and hosts an incredible ecosystem that is largely driven
by microbes and some invertebrates. Given the low air temperatures (-18C annual mean), little precipitation (<10 cm water equivalent/yr), and lack of vegetation cover, the Dry Valleys ecosystem is strongly influenced by physical processes. In the past two
decades, summer conditions have been observed to fluctuate significantly. From 1986-2001, the area experienced a cooling trend and the ecosystem responded with decreasing soil invertebrate populations, decreased streamflow, decreased primary productivity in
lakes, and decreased algal biomass in streams. Since 2001, 3 very high glacial melt years have occurred producing record stream flows and extensive wetted soils. During this most recent decade, the levels of closed-basin lakes have risen substantially, with
increasing heat contents, and we have observed increased permafrost degradation along streambanks. Here we assess the ecosystem responses of the cooling 'press' that occurred from 1986-2001 and the more most recent decade that has had several strong pulses
of energy driving the system to develop expectations for the future state and function of this polar desert ecosystem. We propose that the future trajectory of climate and energy input to the region will likely be more inconsistent than the cooling period
was. Hence, the ecosystem will be consistently responding to pulses of change over varying time periods. We also expect that recovery of the ozone layer over Antarctica may play an important role in modifying both regional climate and the Dry Valleys ecosystem.</div>
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<div class="">cheers</div>
<div class="">-Mike</div>
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<div class="">Michael Gooseff, Associate Professor</div>
<div class="">Institute of Arctic and Alpine Research</div>
<div class="">Civil, Architectural, and Environmental Engineering</div>
<div class="">University of Colorado</div>
<div class="">Boulder, CO 80309-0450</div>
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<div class="">email: <a href="mailto:michael.gooseff@colorado.edu" class="">michael.gooseff@colorado.edu</a></div>
<div class="">web: <a href="http://goosefflab.weebly.com/" class="">http://goosefflab.weebly.com</a> </div>
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phone: 303.735.5333</div>
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