Importance of water mass formation regions for the air-sea CO2flux estimate in the Southern Ocean

Author:

Barbero Leticia1,Boutin Jacqueline1,Merlivat Liliane1,Martin Nicolas1,Takahashi Taro2,Sutherland Stewart C.2,Wanninkhof Rik3

Affiliation:

1. Laboratoire d'Océanographie et du Climat: Expérimentations et approches numériques; IPSL, CNRS, IRD, UPMC; Paris; France

2. Lamont-Doherty Earth Observatory; Columbia University; Palisades; New York; USA

3. Atlantic Oceanographic and Meteorological Laboratory; NOAA; Miami; Florida; USA

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science,General Environmental Science,Environmental Chemistry,Global and Planetary Change

Reference47 articles.

1. Antonov , J. I. R. A. Locarnini T. P. Boyer A. V. Mishonov H. E. Garcia 2006 World Ocean Atlas 2005, vol. 2, Salinity NOAA Atlas NESDIS 62 S Levitus U.S. Govt. Print. Off. Washington, D. C.

2. Intercomparison of shipboard and moored CARIOCA buoy seawater fCO(2) measurements in the Sargasso Sea;Bates;Mar. Chem.,2000

3. New in situ estimates of carbon biological production rates in the Southern Ocean from CARIOCA drifter measurements;Boutin;Geophys. Res. Lett.,2009

4. Air-sea CO2 flux variability in frontal regions of the Southern Ocean from Carbon Interface Ocean Atmosphere drifters;Boutin;Limnol. Oceanogr.,2008

5. Global average of air-sea CO2 transfer velocity from QuikSCAT scatterometer wind speeds;Boutin;J. Geophys. Res.,2009

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