Title: Cyclonic and anticyclonic motion in the upper ocean
Authors: Annalisa Griffa: Instituto de Scienze Marine, Consiglio Nazional delle Ricerche, Pozzuolo di Lerici, Italy; also at Division of Meteorology and Physical Oceanography, Rosentiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, U.S.A.;
Rick Lumpkin: Physical Oceanography Division, Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration, Miami, Florida, U.S.A.;
Milena Veneziani: Ocean Science Department, University of California, Santa Cruz, California, U.S.A.
Source: Geophysical Research Letters (GRL) paper 10.1029/2007GL032100, 2007; http://dx.doi.org/10.1029/2007GL032100
5. Sea surface stratification caused by global warming is creating shifts in phytoplankton habitat
Many models predict that the rate of ocean overturning will slow as a response to global warming. Recent observations support this, with some showing that oceanic biogeochemical conditions are also changing on decadal scales. To better understand what causes such changes, Watanabe et al. study four 50-year time series of biogeochemical properties from across the northern Pacific Ocean. They find that due to surface stratification caused by
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