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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Global snow cover estimation with Microwave Brightness Temperature measurements and one-class in situ observations
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Global snow cover estimation with Microwave Brightness Temperature measurements and one-class in situ observations

机译:利用微波亮度温度测量和一类原位观测进行全球积雪估算

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Brightness temperature (BT), which is remotely sensed by the space-borne microwave radiometer, is widely used in snow cover monitoring for its long time series imaging capabilities in all-weather conditions. Traditional linear fitting and stand-alone methods are usually uncertain with respect to the spatial distribution and temporal variation of derived snow cover, as they rarely consider local conditions and scene characteristics but fit the model with static empirical coefficients. In this paper, a novel method utilizing daily ground in situ observations is proposed and evaluated, with the purpose for accurate estimation of long-term daily snow cover. To solve the challenge that ground snow-free records are insufficient, a one-class classifier, namely the Presence and Background Learning (PBL) algorithm, is employed to identify daily global snow cover. Benefiting from daily ground in situ observations on a global scale, the proposed method is temporally and spatially dynamic such that estimation errors are globally independent during the entire study period. The proposed method is applied to the estimation of global daily snow cover from 1987 to 2010; the results are validated by ground in situ observations and compared with available optical-based and microwave-based snow cover products. Promising accuracy and model stability are achieved in daily, monthly and yearly validations as compared against ground observations (global omission error <0.13, overall accuracy >0.82 in China region, and keep stable in monthly and yearly averages). The comparison against the MODIS daily snow cover product (MOD10C1) shows good agreement under cloud-free conditions (Cohen's kappa = 0.715). The comparison against the NOAA daily Interactive Multisensor Snow and Ice Mapping System (IMS) dataset suggests promising agreement in the Northern Hemisphere. Another comparison against the AMSR-E daily SWE dataset (AE_DySno) demonstrates the efficiency of the proposed method regarding to the overestimation problem in thin snow cover region. (C) 2016 Elsevier Inc. All rights reserved.
机译:星载微波辐射计可对亮温度(BT)进行遥感,由于其在全天候条件下的长时间序列成像能力,被广泛用于积雪监测。传统的线性拟合和独立方法对于派生积雪的空间分布和时间变化通常是不确定的,因为它们很少考虑局部条件和场景特征,而是使用静态经验系数来拟合模型。本文提出并评估了一种利用每日地面实地观测的新方法,旨在准确估算长期的每日积雪量。为了解决地面无雪记录不足的挑战,采用一类分类器(即存在和背景学习(PBL)算法)来识别每日的全球积雪。受益于全球范围内每天的地面实地观测,该方法在时间和空间上都是动态的,因此在整个研究期间,估计误差在全球范围内都是独立的。该方法适用于1987年至2010年全球日积雪量的估计。通过地面实地观察验证了结果,并与可用的基于光学和基于微波的积雪产品进行了比较。与地面观测相比,在每日,每月和每年的验证中都实现了有希望的准确性和模型稳定性(全球遗漏误差<0.13,中国地区的整体准确性> 0.82,并且在每月和每年的平均值中保持稳定)。与MODIS日常积雪产品(MOD10C1)的比较显示,在无云条件下(Cohen卡伯值= 0.715),一致性良好。与NOAA每日互动式多传感器冰雪制图系统(IMS)数据集的比较表明,北半球有希望达成协议。与AMSR-E每日SWE数据集(AE_DySno)的另一比较表明,该方法对于薄雪覆盖地区高估问题的有效性。 (C)2016 Elsevier Inc.保留所有权利。

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