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- W3141723963 abstract "在从南船座介绍的 situ 观察，与卫星相结合的漂流检索了 SST，雨率被用来通过 2012 年 8 月 29 日从 20 调查上面的海洋回答到台风 Bolaven。在台风 Bolaven 的经过以后，加深混合的层深度(MLD ) ，并且冷却混合的层温度(MLT ) 被观察。在混合的层咸度(MLS ) 的变化显示出因为在混合的层的导致台风的咸度变化被降水，蒸发，狂暴的混合和 thermocline 水的 upwelling 影响，增加并且减少的一个相等的数字。加深 MLD 并且冷却 MLT 显示了重要向右偏爱，而 MLS 被添到台风轨道的左边并且在另外的方面上增加了。铱漂流观察的集中的温度和咸度侧面使在台风的经过以后在上面的海洋看反应过程可能。冷却在近表面并且温暖在表面下被在暴风雨的开发阶段期间定位到气旋的磁道的左边的二铱漂流观察，在远处，最大值的半径相对台风中心弯屈。在混合的层的底和 thermocline 的顶的水咸度增加是那些二漂流观察的最明显的变化。在轨道并且在台风中心附近的右边上当台风被加强时，从海表面的重要冷却到 200 的深度" @default.
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- W3141723963 date "2014-01-01" @default.
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- W3141723963 title "An upper ocean response to Typhoon Bolaven analyzed with Argo profiling floats" @default.
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