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MESOSCALE ICE-OCEAN FEATURES IN THE MARGINAL ICE ZONE OFF SYOWA STATION OBSERVED IN NOAA AVHRR IMAGERY

机译:在NOaa aVHRR ImaGERY中观察到的sYOWa站的边缘冰区的中尺度冰海特征

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摘要

Mesoscale ice-ocean features off Syowa Station are examined using NOAA advanced very high resolution radiometer (AVHRR) data during the summers of 1987 and 1988. Visible-band (channel 2) and infrared-band (channel 4) images are used to examine ice and sea surface temperature distributions, respectively. As the melting season progresses, mesoscale ice tongues and eddies are found in the marginal ice zone. The growth of these features is not correlated with the wind field in this area. Comparison between visible and infrared images reveals that the mesoscale ice features are accompanied by corresponding patterns of cold water off the ice edge. Namely, regions of cold water extend off the ice tongues and eddies. This suggests that advection of ice by ocean currents generates the mesoscale features.
机译:在1987年和1988年夏季,使用NOAA先进的超高分辨率辐射计(AVHRR)数据检查了Syowa站附近的中尺度冰洋特征。使用可见带(通道2)和红外带(通道4)图像检查冰和海面温度分布。随着融化季节的进行,在边缘冰区发现了中尺度的冰舌和涡流。这些特征的增长与该地区的风场无关。可见光图像和红外图像之间的比较表明,中尺度的冰特征伴随着冰边缘附近冷水的相应模式。即,冷水区域从冰舌和涡流延伸。这表明洋流对冰的平流产生了中尺度特征。

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