Ice regimes in the Antarctic and the Arctic using satellite multichannel passive microwave data

J. Comiso
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Abstract

Monthly and weekly brightness temperature data from the various SSMI channels, especially the 85 GHz channel, show the existence of ice covered areas associated with persistent brightness temperatures. The physical characteristics of the ice cover in each of these areas are studied for possible association with different regimes of the sea ice cover. In general, the ice cover can be divided into different ice regimes that are associated with extensive new ice formation, young ice regions, first year ice areas with or without thick snow cover and a few types of multiyear ice areas. Unsupervised identification of the regimes is done with multichannel cluster analysis. The interpretation of the different regimes is based mainly on extensive field measurements, radiative transfer calculations, comparisons with other satellite data, and time series development of the surface ice cover from early fall through winter. The key to proper identification of some of this region is the use of the 85 GHz data, which is the most sensitive to surface effects among the SSM/I channels.<>
利用卫星多通道无源微波数据研究南极和北极的冰况
来自SSMI各通道,特别是85 GHz通道的月和周亮度温度数据表明,存在与持续亮度温度相关的冰覆盖区域。研究了这些地区的冰盖的物理特征,以寻找与不同海冰覆盖状况的可能联系。总的来说,冰盖可分为与广泛的新冰形成有关的不同冰况、年轻冰区、有或没有厚积雪的第一年冰区以及几种类型的多年冰区。用多通道聚类分析来进行无监督识别。对不同情况的解释主要基于广泛的野外测量、辐射传输计算、与其他卫星数据的比较以及从初秋到冬季地表冰盖的时间序列发展。正确识别某些区域的关键是使用85ghz数据,这是SSM/I信道中对表面效应最敏感的。
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