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南海北部初级生产力遥感反演及其环境调控机制

郝锵 宁修仁 刘诚刚 蔡昱明 乐凤凤

郝锵, 宁修仁, 刘诚刚, 蔡昱明, 乐凤凤. 南海北部初级生产力遥感反演及其环境调控机制[J]. 海洋学报, 2007, 29(3): 58-68.
引用本文: 郝锵, 宁修仁, 刘诚刚, 蔡昱明, 乐凤凤. 南海北部初级生产力遥感反演及其环境调控机制[J]. 海洋学报, 2007, 29(3): 58-68.
HAO Qiang, NING Xiu-ren, LIU Cheng-gang, CAI Yu-ming, LE Feng-feng. Satellite and in situ observations of primary production in the northern South China Sea[J]. Haiyang Xuebao, 2007, 29(3): 58-68.
Citation: HAO Qiang, NING Xiu-ren, LIU Cheng-gang, CAI Yu-ming, LE Feng-feng. Satellite and in situ observations of primary production in the northern South China Sea[J]. Haiyang Xuebao, 2007, 29(3): 58-68.

南海北部初级生产力遥感反演及其环境调控机制

基金项目: 基金国家自然科学基金重大研究计划之重点项目“全球变化及区域响应”(90211021)

Satellite and in situ observations of primary production in the northern South China Sea

  • 摘要: 选取VGPM模式对南海北部海域初级生产力进行反演,通过SeaWiFS和AVHRR提供的Chl a,K490,PAR和SST等遥感数据产品计算得到了模式所需的各项参数,结合现场实测数据对模式进行了修订和误差分析.在此基础上通过反演计算获得了南海北部海域7 a平均(1998~2004年)初级生产力逐月分布图像.研究结果表明,研究海域初级生产力(C)分布趋势为由沿岸带向陆架以及外海逐渐降低,其中沿岸带区高于400 mg/(m2·d),外海区大致在100~300 mg/(m2·d);初级生产力水平冬季最高[平均为608 mg/(m2·d)]、夏季最低[平均为292 mg/(m2·d)],春、秋季基本持平.控制初级生产力时空分布的因子主要有营养盐、温度、光照,其中又以季风和环流驱动下的营养盐变化对初级生产力的调控最为显著.
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出版历程
  • 收稿日期:  2005-07-18
  • 修回日期:  2006-06-28

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