【摘 要】
：
基于POM( Princeton Ocean model)水动力模型的温盐场输出驱动陆架海碳循环模型中的海-气界面交换环节,模拟东中国陆架海50m以深海区仅在海-气亝换过程下表层DIC,pCO2w 以及
【机 构】
：
TianjingScienceandTechnologyUniversity
【出 处】
：
The First Xiamen Symposium on Marine Environmental Sciences(
论文部分内容阅读
基于POM( Princeton Ocean model)水动力模型的温盐场输出驱动陆架海碳循环模型中的海-气界面交换环节,模拟东中国陆架海50m以深海区仅在海-气亝换过程下表层DIC,pCO2w 以及源汇格局的季节变化.通过与实测站位DH22(28.6°N,122.5°E),DH25(27.7°N,124.0°E)的温度、盐度、DIC 数据对比,认为模拟的温度、盐度、DIC 能够抓住主要的季节变化特征.
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