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Measurements of microwave emission from new and young saline ice during the 1993 CRREL pond experiment

机译:1993年克雷尔池塘试验期间新生儿盐水冰微波排放的测量

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The goals of this study were to observe multifrequency microwave brightness temperatures and emissivities in new and young saline ice, and to assess the effects of ice growth and structural changes on the microwave signatures. The authors were particularly interested in investigating the later stages of young ice growth for comparison with surface-based field observations of first-year (FY) and multiyear (MY) sea ice. Two particular points of interest were: (i) to compare certain roughened surfaces with an undisturbed surface evolving under the same growth conditions, and (ii) to isolate the changes in physical properties which accompany the transition of the microwave signature from young ice to FY ice. Young ice typically has a high polarization ratio (PRe) of about 0.08 as compared with values near 0.018 for FY and MY ice (Grenfell et al., 1992), where polarization ratio is defined as PR/sub e/(v)=[e(v, V)-e(v,H)]/[e(V, V)+e(v, H)], e is the ice emissivity as defined below, v is the observation frequency, and V and H refer to vertical and horizontal polarization respectively.
机译:本研究的目标是观察新生和青少年盐冰的多频微波亮度温度和发射性,并评估冰增长和结构变化对微波签名的影响。作者特别兴趣调查年轻冰增长的后期阶段,以便与一年(FY)和多年(我的)海冰的基于表面的现场观测相比。两个特定的兴趣点是:(i)将某些粗糙表面与在相同的生长条件下的不受干扰的表面进行比较,并在(ii)下分离物理性质的变化,这些物理性质随着微波签名从年轻冰转变为FY冰。与FY和MY ICE(GRENFELL等人,1992)附近的值相比,杨冰通常具有约0.08的高偏振率(前),而偏振率被定义为PR / SUB E /(V)= [ E(v,v)-e(v,h)] / [e(v,v)+ e(v,h)],e是如下所定义的冰发射率,V是观察频率,v和h分别参见垂直和水平极化。

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