The reinvigoration of the Southern Ocean carbon sink

被引：356

作者：

Landschutzer, Peter ^{[1
]}

Gruber, Nicolas ^{[1
,2
]}

Haumann, Alexander ^{[1
,2
]}

Rodenbeck, Christian ^{[3
]}

Bakker, Dorothee C. E. ^{[4
]}

van Heuven, Steven ^{[5
]}

Hoppema, Mario ^{[5
]}

Metzl, Nicolas ^{[6
]}

Sweeney, Colm ^{[7
,8
]}

Takahashi, Taro ^{[9
]}

Tilbrook, Bronte ^{[10
,11
]}

Wanninkhof, Rik ^{[12
]}

机构：

[1] ETH, Inst Biogeochem & Pollutant Dynam, Environm Phys, Zurich, Switzerland

[2] ETH, C2SM, Zurich, Switzerland

[3] Max Planck Inst Biogeochem, D-07745 Jena, Germany

[4] Univ E Anglia, Sch Environm Sci, Ctr Ocean & Atmospher Sci, Norwich NR4 7TJ, Norfolk, England

[5] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bremerhaven, Germany

[6] Univ Paris 06, Sorbonne Univ, CNRS, IRD,MNHN,LOCEAN,IPSL Lab, F-75005 Paris, France

[7] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA

[8] NOAA, Earth Syst Res Lab, Boulder, CO USA

[9] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY USA

[10] CSIRO, Hobart, Tas, Australia

[11] Antarctic Climate & Ecosyst Cooperat Res Ctr, Hobart, Tas, Australia

[12] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA

来源：

SCIENCE | 2015年 / 349卷 / 6253期

基金：

美国国家科学基金会;

关键词：

CO2 FLUX VARIABILITY; ATLANTIC-OCEAN; INVERSION; PCO(2); TRENDS;

D O I：

10.1126/science.aab2620

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

Several studies have suggested that the carbon sink in the Southern Ocean-the ocean's strongest region for the uptake of anthropogenic CO2-has weakened in recent decades. We demonstrated, on the basis of multidecadal analyses of surface ocean CO2 observations, that this weakening trend stopped around 2002, and by 2012 the Southern Ocean had regained its expected strength based on the growth of atmospheric CO2. All three Southern Ocean sectors have contributed to this reinvigoration of the carbon sink, yet differences in the processes between sectors exist, related to a tendency toward a zonally more asymmetric atmospheric circulation. The large decadal variations in the Southern Ocean carbon sink suggest a rather dynamic ocean carbon cycle that varies more in time than previously recognized.

引用

页码：1221 / 1224

页数：4

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