东海有机碳存量估算

Estimation of organic carbon stocks in the East China Sea

  • 摘要: 海洋有机碳存量估算对研究碳循环过程和预估气候变化趋势有重要的作用。海洋有机碳存量可以通过遥感反射率、水体光学特性等参数反演得到。根据东海水域的水体特性,对比了多种有机碳反演算法,并结合东海有机碳垂直分布情况,得到一套完整的东海有机碳存量估算模型。利用2010年MODIS提供的遥感反射率数据和Argo提供的温盐数据,对中国东海区域的有机碳储量分季节进行计算分析。结果表明东海全水柱有机碳储量在1.530×1014 g到2.125×1014 g之间,真光层有机碳储量在4.119×1013 g到7.980×1013 g之间。全水柱有机碳储量整体呈现冬季高、春季低的特点,真光层有机碳储量整体呈现夏季高、冬季低的特点。从2006年至2015年,有机碳存量呈波动上升趋势。对东海有机碳存量进行了较为准确的估算,为今后我国海洋碳储量的评估提供了可供参考的思路。

     

    Abstract: The estimation of ocean organic carbon stocks plays an important role in researching on the process of carbon cycle and predicting climate changes. The ocean organic carbon stocks can be estimated using remote sensing reflectance, water optical properties and other parameters. According to the properties of water in the East China Sea, the estimation results of several algorithms of organic carbon were compared in this paper. Combining with the vertical distribution models, a complete estimation model of organic carbon in the East China Sea was obtained. Based on the remote-sensing reflectance, the temperature data and the salinity data of 2010 provided by MODIS and Argo, the organic carbon stocks in the East China Sea were estimated and analyzed according to seasons. The results show that the organic carbon stocks of the all water column in the East China Sea in 2010 are between 1.530×1014 g and 2.125×1014 g, and the organic carbon stocks of the euphotic layer are between 4.119×1013 g and 7.980×1013 g. The organic carbon stocks in the all water columns are high in winter and low in spring, while organic carbon stocks in the euphotic layer are high in summer and low in winter. It shows a fluctuating upward trend from 2006 to 2015. The organic carbon stocks of the East China Sea is estimated. It provides a method for the determination of ocean carbon stocks in China in the future.

     

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