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Read Full Article (file size: 319414 bytes) Cited by
GEOPHYSICAL RESEARCH LETTERS,
VOL. 32,
L03606,
doi:10.1029/2004GL021808,
2005
Recent trends in global ocean chlorophyll
Watson W. Gregg
Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
Nancy W. Casey
Science Systems and Applications, Inc., Lanham, Maryland, USA
Charles R. McClain
Laboratory for Hydrospheric Processes, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
Abstract
A 6-year time series of remotely-sensed global ocean chlorophyll was evaluated using linear regression analysis to assess
recent trends. Global ocean chlorophyll has increased 4.1% (P < 0.05). Most of the increase has occurred in coastal regions,
defined as bottom depth < 200 m, where an increase of 10.4% was observed. The main contributors to the increase were the Patagonian
Shelf, Bering Sea, and the eastern Pacific, southwest African, and Somalian coasts. Although the global open ocean exhibited
no significant change, 4 of the 5 mid-ocean gyres (Atlantic and Pacific) showed declines in chlorophyll over the 6 years.
In all but the North Atlantic gyre, these were associated with significant increases in sea surface temperature in at least
one season. These results suggest that changes are occurring in the biology of the global oceans.
Received 21
October
2004;
accepted 12
January
2005;
published 8
February
2005.
Index Terms: 4215 Oceanography: General: Climate and interannual variability (1616, 1635, 3305, 3309, 4513); 0480 Biogeosciences: Remote sensing; 1635 Global Change: Oceans (1616, 3305, 4215, 4513); 1616 Global Change: Climate variability (1635, 3305, 3309, 4215, 4513); 4855 Oceanography: Biological and Chemical: Phytoplankton.
Read Full Article (file size: 319414 bytes) Cited by
Citation: Gregg, W. W., N. W. Casey, and C. R. McClain
(2005),
Recent trends in global ocean chlorophyll,
Geophys. Res. Lett.,
32,
L03606,
doi:10.1029/2004GL021808.
Copyright 2005 by the American Geophysical Union.
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