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首页> 外文会议>international symposium on LAPAN-IPE satellite (LISAT) for food security and environmental monitoring >The seasonal variability of sea surface temperature and chlorophyll-a concentration in the south of Makassar Strait
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The seasonal variability of sea surface temperature and chlorophyll-a concentration in the south of Makassar Strait

机译：海面温度和叶绿素 - 麦克塞萨海峡南部浓度的季节变异性

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The sea surface temperature (SST) and chlorophyll-a (Chl-a) variabilities in the south of Makassar Strait were mostly affected by monsoonal wind speed/directions and riverine freshwater inflows. The east-southeast (ESE) wind (May-October) played a major role in an upwelling formation in the region starting in the southern tip of the southern Sulawesi Island. Of the 17 years time period, the variability of the SST values ranged from 25.7°C (August 2004)-30.89°C (March 2007). An upwelling initiation typically occurred in early May when ESE wind speed was at <5 m/s, a fully developed upwelling event usually occurred in June when ESE wind speed reached >5 m/s, whereas the largest upwelling event always occurred in August of each year. Upwelling event generally diminished in September and terminated in October. At the time of the maximum upwelling events (August), the formation of upwelling could be observed up to about 330 km toward the southwest of the southern tip of the Sulawesi island. Interannually, El Nino Southern Oscillation (ENSO) intensified the upwelling event during the east season through an intensification of the ESE wind speed.
机译：海洋表面温度（SST）和氯鱼 - A（CHL-A）毛皮海峡南部的可变性主要受季速风速/方向和河流淡水流入的影响。东南（ESE）风（10月）风（10月）在苏拉威西岛南端开始的地区的升高形成中发挥了重要作用。在17岁的时间段内，SST值的可变性范围从25.7°C（2004年8月）-30.89°C（2007年3月）。当ESE风速为5米/秒时，通常在6月份发生完全发达的升值事件时，通常发生的升值启动，当时风速达到> 5米/秒，而最大的升值事件总是发生在八月每年。 Upwelling活动通常在9月减少并于10月终止。在最大的升值事件（8月）时，可以朝着苏拉威西岛南端的西南部观察到升值的形成。彻夜地，El Nino Southern振荡（ENSO）通过强化ESE风速期间加强了东季期间的升值事件。

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