台湾海峡西部海域溶解氧收支趋势初探

摘要: 本文根据1984年2月—1985年2月在台湾海峡西部海域综合调查的资料,以季节收支法计算台湾海峡西海域溶解氧的海-气交换系数和交换速率,当秋冬季氧的交换系数出现负值、交换速率与现场现象产生矛盾时,本文用各季节自然增氧与耗氧速度的平衡运动趋势予以解释,最后,根据所计算出的氧交换系数估算了台湾海峡西部海域溶解氧的海-气交换通量,得出了氧在本海域从海水向大气的释放量比从大气溶入海水的量大得多的结论.

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