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Diagnosing snow accumulation errors in a rain-snow transitional environment with snow board observations

机译:利用积雪板观测诊断雨雪过渡环境中的积雪误差

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摘要

Diagnosing the source of errors in snow models requires intensive observations, a flexible model framework to test competing hypotheses, and a methodology to systematically test the dominant snow processes. We present a novel process-based approach to diagnose model errors through an example that focuses on snow accumulation processes (precipitation partitioning, new snow density, and snow compaction). Twelve years of meteorological and snow board measurements were used to identify the main source of model error on each snow accumulation day. Results show that modeled values of new snow density were outside observational uncertainties in 52% of days available for evaluation, while precipitation partitioning and compaction were in error 45% and 16% of the time, respectively. Precipitation partitioning errors mattered more for total winter accumulation during the anomalously warm winter of 2014-2015, when a higher fraction of precipitation fell within the temperature range where partition methods had the largest error. These results demonstrate how isolating individual model processes can identify the primary source(s) of model error, which helps prioritize future research.
机译:诊断积雪模型中的错误源需要进行深入观察,需要使用灵活的模型框架来测试竞争假设,还需要系统地测试主要降雪过程的方法。我们通过一个着重于积雪过程(降水分配,新积雪密度和积雪压实)的示例,提出了一种基于过程的新颖方法来诊断模型错误。十二年来的气象和积雪板测量被用来确定每个积雪日的模型误差的主要来源。结果表明,新雪密度的模型值在52%的可评估天数中处于观测不确定性之外,而降水分配和压实的误差分别为45%和16%。在2014-2015年异常温暖的冬季,降水分配误差对冬季总蓄积的影响更大,当较高比例的降水落在分配方法误差最大的温度范围内时。这些结果表明,隔离单个模型过程可以如何识别模型错误的主要来源,从而有助于对未来的研究进行优先排序。

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