金心,石广玉. 2000. 海洋对人为CO2吸收的三维模式研究[J]. 气象学报, 58(1):40-48, doi:10.11676/qxxb2000.004
海洋对人为CO2吸收的三维模式研究
A SIMULATION OF CO2 UPTAKE IN A THREE DIMEN-SIONAL OCEAN CARBON CYCLE MODEL
投稿时间:1998-11-27  修订日期:1999-05-21
DOI:10.11676/qxxb2000.004
中文关键词:  人为CO2  海洋吸收  三维模式  纬度分布  碳循环
英文关键词:Anthropogenic CO2  Ocean uptake  Three-dimensional model  Ocean carbon cycle model  Regional distributions
基金项目:国家自然科学基金(49794030);国家“九五”重中之重项目“我国短期气候预测系统的研究”(96-908-01-06)
作者单位
金心 中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室(LASG), 北京, 100029 
石广玉 中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室(LASG), 北京, 100029 
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中文摘要:
      文中用包含海洋化学过程和一个简单生物过程的三维碳循环模式模拟了海洋对大气CO2的吸收,并分析了碳吸收的纬度分布。模拟工业革命以来海洋对大气CO2的吸收表明:海洋碳吸收再加上大气CO2的增加只占由化石燃料燃烧、森林砍伐和土地利用的变化而释放到大气中的CO2的2/3。1980~1989年期间海洋年平均吸收2.05GtC。海洋人为CO2的吸收有明显的纬度特征。模式计算的海洋CO2的吸收在总量与纬度分布上与观测结果比较相符。
英文摘要:
      A three-dimensional ocean carbon cycle model, which is a general circulati on model coupled with simple biogeochemical processes, is used to simulate CO2 uptake by the ocean. The OGCM is used a modified version of the Geophysical Fluid Dynamics Laboratory modular ocean model (MOM2). The ocean chemistry and a simple ocean biota model is included. Principal variables are total CO2, alkali nity and phosphate. The vertical profile of POC flux observed by sediment traps is adopted, the rain ratio,a ratio of production rate of calcite against that of POC, and the bio-production efficiency should be 0.06 and 2 per year, separately. The uptake of anthropogenic CO2 by the Ocean is studied. Calculated oceanic uptake of anthropogenic CO2 during the 1980's is 2.05 Pg per year. The regional distributions of global oceanic CO2 are discussed.
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