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ReportsRecent Changes in Phytoplankton Communities Associated with Rapid Regional Climate Change Along the Western Antarctic Peninsula
The climate of the western shelf of the Antarctic Peninsula (WAP) is undergoing a transition from a cold-dry polar-type climate to a warm-humid sub-Antarctic–type climate. Using three decades of satellite and field data, we document that ocean biological productivity, inferred from chlorophyll a concentration (Chl a), has significantly changed along the WAP shelf. Summertime surface Chl a (summer integrated Chl a
1 Coastal Ocean Observation Lab, Institute of Marine and Coastal Sciences, School of Environmental and Biological Sciences, Rutgers University, New Brunswick, NJ 08901, USA. 63% of annually integrated Chl a) declined by 12% along the WAP over the past 30 years, with the largest decreases equatorward of 63°S and with substantial increases in Chl a occurring farther south. The latitudinal variation in Chl a trends reflects shifting patterns of ice cover, cloud formation, and windiness affecting water-column mixing. Regional changes in phytoplankton coincide with observed changes in krill (Euphausia superba) and penguin populations.
2 Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. 3 The Ecosystems Center, Marine Biological Laboratory, Woods Hole, MA 02543, USA. 4 Polar Oceans Research Group, Post Office Box 368, Sheridan, MT 59749, USA. 5 Lamont-Doherty Earth Institute, Palisades, NY 10964, USA. 6 Ocean Sciences, University of California, Santa Cruz, CA 95064, USA. *To whom correspondence should be addressed. E-mail: montes{at}marine.rutgers.edu
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Science. ISSN 0036-8075 (print), 1095-9203 (online)