How accurate is the estimation of anthropogenic carbon in the ocean?: An evaluation of the ΔC* method -: art. no. GB3014

被引:91
作者
Matsumoto, K
Gruber, N
机构
[1] Natl Inst Adv Ind Sci & Technol, Geol Survey Japan, Tsukuba, Ibaraki, Japan
[2] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY USA
[3] Univ Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90095 USA
[4] Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA 90095 USA
关键词
D O I
10.1029/2004GB002397
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Delta C* method of Gruber et al. ( 1996) is widely used to estimate the distribution of anthropogenic carbon in the ocean; however, as yet, no thorough assessment of its accuracy has been made. Here we provide a critical re- assessment of the method and determine its accuracy by applying it to synthetic data from a global ocean biogeochemistry model, for which we know the " true'' anthropogenic CO2 distribution. Our results indicate that the Delta C* method tends to overestimate anthropogenic carbon in relatively young waters but underestimate it in older waters. Main sources of these biases are ( 1) the time evolution of the air- sea CO2 disequilibrium, which is not properly accounted for in the Delta C* method, ( 2) a pCFC ventilation age bias that arises from mixing, and ( 3) errors in identifying the different end- member water types. We largely support the findings of Hall et al. ( 2004), who have also identified the first two bias sources. An extrapolation of the errors that we quantified on a number of representative isopycnals to the global ocean suggests a positive bias of about 7% in the Delta C*- derived global anthropogenic CO2 inventory. The magnitude of this bias is within the previously estimated 20% uncertainty of the method, but regional biases can be larger. Finally, we propose two improvements to the Delta C* method in order to account for the evolution of air-sea CO2 disequilibrium and the ventilation age mixing bias.
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页码:1 / 17
页数:17
相关论文
共 44 条
[1]   REDFIELD RATIOS OF REMINERALIZATION DETERMINED BY NUTRIENT DATA-ANALYSIS [J].
ANDERSON, LA ;
SARMIENTO, JL .
GLOBAL BIOGEOCHEMICAL CYCLES, 1994, 8 (01) :65-80
[2]   Temporal changes in dissolved oxygen of the intermediate water in the subarctic North Pacific - art. no. 1689 [J].
Andreev, A ;
Watanabe, S .
GEOPHYSICAL RESEARCH LETTERS, 2002, 29 (14)
[3]   Temporal evolution of CFC 11 and CFC 12 concentrations in the ocean interior [J].
Beining, P ;
Roether, W .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1996, 101 (C7) :16455-16464
[4]   DIRECT OBSERVATION OF OCEANIC CO2 INCREASE [J].
BREWER, PG .
GEOPHYSICAL RESEARCH LETTERS, 1978, 5 (12) :997-1000
[5]  
Broecker W.S., 1982, Tracers in the Sea
[6]   THE DISTRIBUTION OF BOMB RADIOCARBON IN THE OCEAN [J].
BROECKER, WS ;
PENG, TH ;
OSTLUND, G ;
STUIVER, M .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1985, 90 (NC4) :6953-6970
[7]   GRADUAL INCREASE OF OCEANIC CO2 [J].
CHEN, GT ;
MILLERO, FJ .
NATURE, 1979, 277 (5693) :205-206
[8]   Comparison of two approaches to quantify anthropogenic CO2 in the ocean:: Results from the northern Indian Ocean [J].
Coatanoan, C ;
Goyet, C ;
Gruber, N ;
Sabine, CL ;
Warner, M .
GLOBAL BIOGEOCHEMICAL CYCLES, 2001, 15 (01) :11-25
[9]   Evaluation of ocean model ventilation with CFC-11: comparison of 13 global ocean models [J].
Dutay, J. -C. ;
Bullister, J. L. ;
Doney, S. C. ;
Orr, J. C. ;
Najjar, R. ;
Caldeira, K. ;
Campin, J. -M. ;
Drange, H. ;
Follows, M. ;
Gao, Y. ;
Gruber, N. ;
Hecht, M. W. ;
Ishida, A. ;
Joos, F. ;
Lindsay, K. ;
Madec, G. ;
Maier-Reimer, E. ;
Marshall, J. C. ;
Matear, R. J. ;
Monfray, P. ;
Mouchet, A. ;
Plattner, G. -K. ;
Sarmiento, J. ;
Schlitzer, R. ;
Slater, R. ;
Totterdell, I. J. ;
Weirig, M. -F. ;
Yamanaka, Y. ;
Yool, A. .
OCEAN MODELLING, 2002, 4 (02) :89-120
[10]   The biological pump in the subtropical North Pacific Ocean: Nutrient sources, Redfield ratios, and recent changes [J].
Emerson, S ;
Mecking, S ;
Abell, J .
GLOBAL BIOGEOCHEMICAL CYCLES, 2001, 15 (03) :535-554