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Space-derived parameters of coastal upwelling in the SE Baltic Sea

机译:SE波罗的海沿海上升的空间衍生参数

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In this work we present a basic statistics of coastal upwelling parameters inferred from satellite infrared (IR) Terra/Aqua MODIS sea surface temperature (SST) maps acquired over the South-Eastern (SE) Baltic Sea between 2000 and 2013. The maximum observed SST gradients across the front were up to 1.6 °C/km, temperature drop up to 14°C with total upwelling-affected area up to 16000 km2. The observed horizontal scale of the upwelling is about 100–400 km along the coast, and 10–20 km (max 70–80 km) cross-shore. The duration of the upwelling in this part of the sea is from several days up to several weeks. It is also shown that intensive coastal upwelling in the SE Baltic may lead up to the 40-km long intrusion of relatively cold and saline sea water into the Curonian Lagoon forming very pronounced property gradients there and affecting nearly a half of the Lithuanian part of the lagoon.
机译:在这项工作中,我们展示了从2000年至2013年之间的卫星红外线(IR)Terra / Aqua Modis海面温度(SST)地图推断的沿海上升率参数的基本统计数据。最大观察到SST前线的梯度高达1.6°C / km,温度降至14°C,总升高受影响的区域高达16000平方公里。观察到的升值水平规模沿海岸约100-400公里,交叉10-20公里(最多70-80公里)。在这部分海上升值的持续时间从几天到几周。也表明,在SE波罗的海中,密集的沿海升值可能导致40公里的侵入相对寒冷和盐水海水的侵入,进入库尔尼亚泻湖,在那里形成非常明显的财产梯度并影响立陶宛人的几半泻湖。

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