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A Comparison of SNOTEL and AMSR-E Snow Water Equivalent Datasets in Western U.S. Watersheds

机译:美国西部流域SNOTEL和AMSR-E雪水当量数据集的比较

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It is a consensus among earth scientists that climate change will result in an increased frequency of extreme events (e.g., precipitation, snow). Streamflow forecasts and flood/drought analyses, given this high variability in the climatic driver (snowpack), are vital in the western United States. However, the ability to produce accurate forecasts and analyses is dependent upon the quality (accuracy) of these predictors (snowpack). Current snowpack datasets are based upon in-situ telemetry. Recent satellite deployments offer an alternative remote sensing data source of snowpack. The proposed research will investigate (compare) remote sensing datasets in western U.S. watersheds in which snowpack is the primary driver of streamflow. A comparison is made between snow water equivalent (SWE) data from in-situ snowpack telemetry (SNOTEL) sites and the advanced microwave scanning radiometer - earth observing system (AMSR-E) aboard NASA's Aqua satellite. Principal component techniques and Singular Value Decomposition are applied to determine similarities and differences between the datasets and investigate regional snowpack behaviors. Given the challenges (including costs, operation and maintenance) of deploying SNOTEL stations, the objective of the research is to determine if satellite based remote sensed SWE data provide a comparable option to in-situ datasets. Watersheds investigated include the North Platte River, the Upper Green River, and the Upper Colorado River. The time period analyzed is 2003-2008, due to the recent deployment of the NASA Aqua satellite. Two distinct snow regions were found to behave similarly between both datasets using principal component analysis. Singular Value Decomposition linked both data products with streamflow in the region and found similar behaviors among datasets. However, only 11 of the 84 SNOTEL sites investigated correlated at a significance of 90% or greater with its corresponding AMSR-E cell. Also, when comparing SNOTEL data with the corresponding satellite cell, there was a consistent difference in the magnitude (Snow Water Equivalent) of the datasets. Finally, both datasets were utilized and compared in a statistically based streamflowrnforecast of several gages.
机译:地球科学家一致认为,气候变化将导致极端事件(例如降雨,降雪)的发生频率增加。鉴于气候驱动因素(雪堆)的高度变化性,流量预报和洪水/干旱分析在美国西部至关重要。但是,产生准确的预测和分析的能力取决于这些预测器(snowpack)的质量(准确性)。当前的积雪数据集是基于原位遥测的。最近的卫星部署提供了积雪的替代遥感数据源。拟议的研究将调查(比较)美国西部流域的遥感数据集,其中积雪是水流的主要驱动力。将原位积雪遥测(SNOTEL)站点的雪水当量(SWE)数据与NASA Aqua卫星上先进的微波扫描辐射计-地球观测系统(AMSR-E)进行了比较。应用主成分技术和奇异值分解来确定数据集之间的异同,并研究区域积雪的行为。考虑到部署SNOTEL站所面临的挑战(包括成本,运营和维护),该研究的目的是确定基于卫星的遥感SWE数据是否可提供与现场数据集相当的选择。调查的流域包括北普拉特河,绿河上游和科罗拉多河上游。由于最近部署了NASA Aqua卫星,因此分析的时间段是2003年至2008年。使用主成分分析发现两个数据集之间两个不同的降雪区域表现相似。奇异值分解将两个数据产品与区域中的流量关联起来,并在数据集中发现了类似的行为。但是,在所调查的84个SNOTEL位点中,只有11个与其相应的AMSR-E细胞的关联度达到90%或更高。另外,将SNOTEL数据与相应的卫星小区进行比较时,数据集的大小(雪水当量)存在一致的差异。最后,利用了这两个数据集并在基于统计的几个量表的预测流量中进行了比较。

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