基于遥感技术的三次“中国”巡航南大洋海气碳通量年变化

Suqing Xu, Tingting Liu, Liqi Chen
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引用次数: 0

摘要

根据中国南极考察队(CHINARE)在南大西洋和南印度洋进行的三次巡航所获得的海面二氧化碳分压、叶绿素-a和海面温度的测量数据,得出了经验关系。利用叶绿素-a和海表温度的遥感数据,采用外推法计算了海水中的pCO2。计算了海气CO2通量的月时空分布。结果表明,总体上1月份的碳吸收强于12月份,2月份碳吸收有所下降。1999年12月和2004年12月的碳吸收量基本持平,2007年12月的碳吸收量比1999年12月下降了9%。2005年1月的碳吸收量比2000年下降了8.4%。而在2008年2月,由于海冰的重整和叶绿素的减少,碳吸收减少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Annually variation of air-sea carbon flux in the southern ocean from three CHINARE cruises by means of remote sensing technology
Empirical relationships were derived from the underway measurements of sea surface pCO2, chlorophyll-a and sea surface temperature obtained from three Chinese Antarctica Research Expedition (CHINARE) cruises conducted in south Atlantic Ocean and south Indian Ocean. pCO2 in sea water was computed from remote sensing chlorophyll-a and SST by extrapolation method. Monthly spatiotemporal distribution of air-sea CO2 flux was calculated. Results showed that in general the carbon absorption was stronger in January than in December, and declined in February. The carbon absorption in Dec 1999 and 2004 was approximately equal, while in Dec 2007 it declined by 9% compared to Dec 1999. For January, the carbon absorption in 2005 declined by 8.4% compared to 2000. While for February 2008, due to the reforming of sea ice and decrease of chlorophyll, the carbon absorption decreased.
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