地中海小山区盆地的雪覆盖动力学:以托尔梅斯河为例(杜埃罗盆地,西班牙)

Antonio Ceballos-Barbancho, José Manuel Llorente-Pinto, Esteban Alonso-González, J. I. López-Moreno
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引用次数: 2

摘要

近年来,利用遥感(AVHRR-NOAA和MODIS)和能量平衡模式(WRF-FSM)建立了西班牙半岛积雪时空动态的同构数据库。这些在区域尺度上使用的数据序列显示了它们在小水源上应用的不确定性,以便更好地了解同一水源的水文气候学。假设应用技术的差异,以及表示估算值的变量(积雪、雪日数、雪深和雪水当量)的多样性,所得结果可以描述研究流域积雪的季节行为及其显著的年际变化。结果表明,与模型序列(WRF-FSM)相比,积雪数据在水文分析中的作用较小,后者报告了雪水当量的厚度和数量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dinámica del manto de nieve en una pequeña cuenca de montaña mediterránea: el caso del río Tormes (Cuenca del Duero, España)
Recently, a homogeneous database has been generated to study the spatial-temporal dynamics of the snow cover in the Spanish peninsular territory, from remote sensing (AVHRR-NOAA and MODIS) and energy balance models (WRF-FSM). These data series used at regional scale show the uncertainty of their application in small headwaters to better understand the hydro-climatology of the same. Assuming the disparity of applied techniques, and the diversity of variables in which the estimates are expressed (snow cover, snow days, snow depth and snow water equivalent), the results obtained allow to describe the seasonal behavior of the snow cover in the study catchment, as well as its marked interannual variability. The results show that snow cover data are less useful for hydrological analysis than modeled series (WRF-FSM), which report the thickness and amount of snow water equivalent.
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