Assessments of anthropogenic CO2 distribution in the tropical Atlantic Ocean

被引:19
|
作者
Touratier, F
Goyet, C
Coatanoan, C
Andrié, C
机构
[1] Univ Perpignan, BDSI, F-66860 Perpignan, France
[2] IFREMER, Ctr Brest, F-29280 Plouzane, France
[3] Univ Paris 06, CNRS, IRD, LODYC, F-75252 Paris, France
关键词
carbon cycle; water mass; Atlantic Ocean; tropical belt;
D O I
10.1016/j.dsr.2005.09.001
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
With a limited number of properties (salinity, temperature, total dissolved inorganic carbon, total alkalinity, and oxygen) from a recent cruise in the tropical Atlantic Ocean, We use the simple and recent approach TrOCA (Tracer combining Oxygen, inorganic Carbon, and total Alkalinity) to estimate the distribution of anthropogenic CO(2) along three latitudinal sections. In order to assess the quality of the anthropogenic CO(2) distribution, results from the method are compared to the CFC-11 measurements. We discuss the large-scale distribution of the main water masses of the tropical Atlantic Ocean in the light of the anthropogenic CO(2) and the CFC-11 distributions. Keeping in mind that the anthropogenic CO(2) emission began similar to 60 years earlier than that of CFC-11, the former provides new insight on the local circulation and efficiency of the tropical waters to store the atmospheric carbon. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2275 / 2284
页数:10
相关论文
共 50 条
  • [21] Distribution of anthropogenic CO2 in the Pacific Ocean -: art. no. 1083
    Sabine, CL
    Feely, RA
    Key, RM
    Bullister, JL
    Millero, FJ
    Lee, K
    Peng, TH
    Tilbrook, B
    Ono, T
    Wong, CS
    GLOBAL BIOGEOCHEMICAL CYCLES, 2002, 16 (04)
  • [22] The impact of the North Atlantic Oscillation on the uptake and accumulation of anthropogenic CO2 by North Atlantic Ocean mode waters
    Levine, Naomi Marcil
    Doney, Scott C.
    Lima, Ivan
    Wanninkhof, Rik
    Bates, Nicholas R.
    Feely, Richard A.
    GLOBAL BIOGEOCHEMICAL CYCLES, 2011, 25
  • [23] Decadal increases of anthropogenic CO2 in the subtropical South Atlantic Ocean along 30°S
    Murata, Akihiko
    Kumamoto, Yuichiro
    Sasaki, Ken'ichi
    Watanabe, Shuichi
    Fukasawa, Masao
    JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2008, 113 (C6)
  • [24] Anthropogenic CO2 and CFCs in the North Atlantic Ocean - A comparison of man-made tracers
    Department of Marine Chemistry, Institute of Marine Research, University of Kiel, Düsternbrooker Weg 20, Kiel
    24105, Germany
    不详
    18119, Germany
    不详
    28334, Germany
    Geophys. Res. Lett., 14 (2065-2068):
  • [25] Anthropogenic CO2 and CFCs in the North Atlantic Ocean -: A comparison of man-made tracers
    Körtzinger, A
    Rhein, M
    Mintrop, L
    GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (14) : 2065 - 2068
  • [26] Significant CO2 fixation by small prymnesiophytes in the subtropical and tropical northeast Atlantic Ocean
    Jardillier, Ludwig
    Zubkov, Mikhail V.
    Pearman, John
    Scanlan, David J.
    ISME JOURNAL, 2010, 4 (09): : 1180 - 1192
  • [27] Contrasting Sea-Air CO2 Exchanges in the Western Tropical Atlantic Ocean
    Monteiro, Thiago
    Batista, Matheus
    Henley, Sian
    Machado, Eunice da Costa
    Araujo, Moacyr
    Kerr, Rodrigo
    GLOBAL BIOGEOCHEMICAL CYCLES, 2022, 36 (08)
  • [28] Significant CO2 fixation by small prymnesiophytes in the subtropical and tropical northeast Atlantic Ocean
    Ludwig Jardillier
    Mikhail V Zubkov
    John Pearman
    David J Scanlan
    The ISME Journal, 2010, 4 : 1180 - 1192
  • [29] A significant CO2 sink in the tropical Atlantic Ocean associated with the Amazon River plume
    Kortzinger, A
    GEOPHYSICAL RESEARCH LETTERS, 2003, 30 (24)
  • [30] The role of ocean transport in the uptake of anthropogenic CO2
    Cao, L.
    Eby, M.
    Ridgwell, A.
    Caldeira, K.
    Archer, D.
    Ishida, A.
    Joos, F.
    Matsumoto, K.
    Mikolajewicz, U.
    Mouchet, A.
    Orr, J. C.
    Plattner, G. -K.
    Schlitzer, R.
    Tokos, K.
    Totterdell, I.
    Tschumi, T.
    Yamanaka, Y.
    Yool, A.
    BIOGEOSCIENCES, 2009, 6 (03) : 375 - 390