A study of Indian Ocean Subtropical Mode Water: subduction rate and water characteristics

MA Jie LAN Jian ZHANG Ningning

马杰, 兰健, 张宁宁. 关于印度洋副热带模态水的研究:潜沉率及其水体性质[J]. 海洋学报英文版, 2016, 35(1): 38-45. doi: 10.1007/s13131-016-0794-0
引用本文: 马杰, 兰健, 张宁宁. 关于印度洋副热带模态水的研究:潜沉率及其水体性质[J]. 海洋学报英文版, 2016, 35(1): 38-45. doi: 10.1007/s13131-016-0794-0
MA Jie, LAN Jian, ZHANG Ningning. A study of Indian Ocean Subtropical Mode Water: subduction rate and water characteristics[J]. Acta Oceanologica Sinica, 2016, 35(1): 38-45. doi: 10.1007/s13131-016-0794-0
Citation: MA Jie, LAN Jian, ZHANG Ningning. A study of Indian Ocean Subtropical Mode Water: subduction rate and water characteristics[J]. Acta Oceanologica Sinica, 2016, 35(1): 38-45. doi: 10.1007/s13131-016-0794-0

关于印度洋副热带模态水的研究:潜沉率及其水体性质

doi: 10.1007/s13131-016-0794-0

A study of Indian Ocean Subtropical Mode Water: subduction rate and water characteristics

  • 摘要: 通过分析1950-2008年的SODA资料对印度洋区域的潜沉率进行了计算。在副热带西南印度洋区域,以位势密度为函数的潜沉率峰值对应着印度洋副热带模态水的密度分布区间。在副热带模态水生成区,潜沉率主要是由深的混合层,强大的混合层锋面以及相对快速的流场组合所产生的强的侧向导入项控制的,而垂直抽吸项对潜沉率贡献较小。为了不失一般性,根据对垂向温度梯度极小值所在层的水体性质进行细致分析,我们认为印度洋副热模态水是温度均一的巨大水体,且具有较小的位势涡度(<200 10-12 m-1s-1)以及弱的垂向温度梯度(< 1.5 ℃/100米)。印度洋副热带模态水大致分布在印度洋副热带区域:东经25°-50°,南纬30°-39°。此外,我们计算了最近60年左右印度洋副热带模态水气候态平均性质:温度(16.38 0.29, 盐度(35.46±0.04), 位势密度(26.02±0.04) σθ
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  • 收稿日期:  2014-10-22
  • 修回日期:  2015-03-23

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