Simulationof14CinIAP/LASGL30T63OceanModel

被引：3

作者：

李清泉 ^{[1
]}

石广玉 ^{[2
]}

机构：

[1] Laboratory for Climate Studies of China Meteorological Administration, National Climate Center, Beijing

[2] State Key Laboratory of Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of AtmosphericPhysics, Chinese Academy of Sciences, Beijing

来源：

ActaMeteorologicaSinica | 2005年 / 04期

关键词：

ocean circulation model; 14C; carbon cycle; numerical simulation;

D O I：

暂无

中图分类号：

P731.27 [大洋环流];

学科分类号：

0707 ;

摘要：

14C plays an important role in the study of ocean circulation and anthropogenic CO2. Radioactive 14Cis usually used in ocean carbon circulation model to test the physical performance of model. In the presentpaper, a 14C model is established and coupled with the IAP/LASG L30T63 global ocean circulation modelto simulate the distribution of natural 14C in oceans and the penetration and uptake of 14C in oceans afterindustrial revolution and nuclear bomb test. The simulation of natural 14C reveals the basic characteristicsof oceanic ventilation. However, simulation value is "younger" than observation in the Pacific and IndianOceans, and "older" than observation in the Atlantic deep ocean. The simulation of bomb 14C agrees wellwith GEOSECS observation, but the volume inventory and averaged penetration depth of bomb 14C inoceans are smaller than observation. The probable reasons for these discrepancies are analyzed.

引用

页码：436 / 446

页数：11

共 3 条

[1]

Fundamental framework and experiments of the third generation of IAP / LASG world ocean general circulation model[J] . Xiangze Jin,Xuehong Zhang,Tianjun Zhou.Advances in Atmospheric Sciences . 1999 (2)

[2]

Ocean-circulation model of the carbon cycle[J] . R Bacastow,E Maier-Reimer.Climate Dynamics . 1990 (2)

[3]

Transport and storage of CO 2 in the ocean ——an inorganic ocean-circulation carbon cycle model[J] . E. Maier-Reimer,K. Hasselmann.Climate Dynamics . 1987 (2)

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