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Empirical parametrization of Envisat freeboard retrieval of Arctic and Antarctic sea ice based on CryoSat-2: progress in the ESA Climate Change Initiative

机译:基于CryoSat-2的北极和南极海冰Envisat干舷检索的经验参数化:ESA气候变化倡议的进展

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In order to derive long-term changes in sea-ice volume, a multi-decadal sea-ice thickness record is required. CryoSat-2 has showcased the potential of radar altimetry for sea-ice mass-balance estimation over the recent years. However, precursor altimetry missions such as Environmental Satellite (Envisat) have not been exploited to the same extent so far. Combining both missions to acquire a decadal sea-ice volume data set requires a method to overcome the discrepancies due to different footprint sizes from either pulse-limited or beam-sharpened radar echoes. In this study, we implemented an inter-mission-consistent surface-type classification scheme for both hemispheres, based on the waveform pulse peakiness, leading-edge width, and surface backscatter. In order to achieve a consistent retracking procedure, we adapted the threshold first-maximum retracker algorithm, previously used only for CryoSat-2, to develop an adaptive retracker threshold that depends on waveform characteristics. With our method, we produce a global and consistent freeboard data set for CryoSat-2 and Envisat. This novel data set features a maximum monthly difference in the mission-overlap period of 2.2 cm (2.7 cm ) for the Arctic (Antarctic) based on all gridded values with spatial resolution of 25?km?×?25?km and 50?km?×?50?km for the Arctic and Antarctic, respectively.
机译:为了得出海冰量的长期变化,需要多年代的海冰厚度记录。近年来,CryoSat-2展示了雷达测高技术在海冰质量平衡估计中的潜力。但是,迄今为止,尚未充分利用诸如环境卫星(Envisat)之类的前身高空飞行任务。结合两个任务以获取十年海冰体积数据集,需要一种方法来克服由于脉冲受限或波束锐化的雷达回波而导致的足迹尺寸不同而导致的差异。在这项研究中,我们基于波形脉冲峰值,前沿宽度和表面反向散射,对两个半球实施了一种任务间一致的表面类型分类方案。为了实现一致的重新跟踪过程,我们对以前仅用于CryoSat-2的阈值第一最大重新跟踪器算法进行了改进,以开发取决于波形特征的自适应重新跟踪器阈值。使用我们的方法,我们为CryoSat-2和Envisat生成了一个全球一致的干舷数据集。这个新颖的数据集基于所有栅格化值(北极分辨率为25?km?×?25?km和50?km)的北极(南极),在任务重叠期间每月最大差异为2.2 cm(2.7 cm)。北极和南极分别为?×?50?km。

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