西部和中部赤道太平洋地表水 PCO2 的十年变化
Taro Takahashi1, Stewart C Sutherland, Richard A Feely
1Lamont-Doherty Earth Observatory (LDEO) of Columbia University, Palisades, NY 10964, USA. taka@ldeo.columbia.edu
概括
在赤道太平洋的太平洋.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 生物地质化学生物地质化学
背景情况:
- 赤道太平洋是大气中二氧化碳 (CO2) 的关键,可变的来源.
- 了解该地区的二氧化碳动态对于气候建模至关重要.
研究的目的:
- 研究太平洋十年振荡 (PDO) 阶段转移对赤道太平洋二氧化碳化学的影响.
- 分析PDO转移之前和之后的二氧化碳 (PCO2) 表面水部分压力变化.
主要方法:
- 对1979年至2001年初的地表水PCO2数据的分析.
- 为温度变化和大气二氧化碳吸收进行PCO2数据的校正.
主要成果:
- 在中央和西赤道太平洋的地表水中,PCO2在PDO转变 (1988-1992) 之前减少了大约-20微原子/十年.
- 在PDO转移后,地表水的PCO2增加了大约15微原子/十年.
- 这些变化大大改变了赤道太平洋的二氧化碳汇和源流.
结论:
- 太平洋十年振荡的相位转移对赤道太平洋的二氧化碳化学物质产生了实质性和可测量的影响.
- PCO2趋势的变化表明海洋作为碳汇或碳源的作用发生了重大变化.
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