Acceleration of the Arctic Water Cycle: evidence from the Lena River Basin, SIBERIA

Collaborators on this work include Vladimir Alexeev (Univ. Alaska Fairbanks), Beate Liepert (Columbia Univ.), Pavel Groisman (NOAA-NCDC), and Vladimir Romanovsky (Univ. Alaska Fairbanks).

My work on land surface processes and land-atmosphere-ocean interactions has so far focused on the question of how the hydrologic cycle is changing in a changing climate. I utilize measurements of those components of the hydrologic system that I believe are reliable (runoff, snow depth, surface air temperature, ground-based cloud and radiation observations). For Siberia, I have analyzed more than 60 years of these observations for trends and co-variation that indicate physical processes and interactions. In the satellite era, I examine the potential role of decreasing sea ice coverage as a moisture source in the Arctic and Sub-arctic. To look at changes in processes which are difficult to measure, I have run several conceptual experiments with the NSIPP catchment-based land surface model.  My first paper on this topic has been presented at several conferences during 2006 and will be submitted shortly.
This work, as well as the PASR was mentioned in two Nature news articles: “Arctic water flow speeding up” (http://www.nature.com/news/2006/060403/full/060403-9.html) and “Arctic stations need human touch” Nature 441, 133-133 (11 May 2006) News.