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Monitoring Snow Using Geostationary Satellite Retrievals During the SAAWSO Project

机译:在SAAWSO项目期间使用对地静止卫星取回监测雪

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The SAAWSO (Satellite Applications for Arctic Weather and SAR (Search And Rescue) Operations) field programs were conducted by Environment Canada near St. Johns, NL and Goose Bay, NL in the winters of 2012-13 and 2013-14, respectively. The goals of these programs were to validate satellite-based nowcasting products, including snow amount, wind intensity, and cloud physical parameters (e.g., cloud cover), over northern latitudes with potential applications to Search And Rescue (SAR) operations. Ground-based in situ sensors and remote sensing platforms were used to measure microphysical properties of precipitation, clouds and fog, radiation, temperature, moisture and wind profiles. Multi-spectral infrared observations obtained from Geostationary Operational Environmental Satellite (GOES)-13 provided estimates of cloud top temperature and height, phase (water, ice), hydrometer size, extinction, optical depth, and horizontal wind patterns at 15 min intervals. In this work, a technique developed for identifying clouds capable of producing high snowfall rates and incorporating wind information from the satellite observations is described. The cloud top physical properties retrieved from operational satellite observations are validated using measurements obtained from the ground-based in situ and remote sensing platforms collected during two precipitation events: a blizzard heavy snow storm case and a moderate snow event. The retrieved snow precipitation rates are found to be comparable to those of ground-based platform measurements in the heavy snow event.
机译:SAAWSO(用于北极天气和SAR(搜索和救援)操作的卫星应用)实地计划是由加拿大环境部在NL-13圣约翰斯和NL Goose Bay附近分别于2012-13和2013-14冬季进行的。这些计划的目标是验证北部纬度上基于卫星的临近预报产品,包括积雪量,风强度和云物理参数(例如,云量),并有可能应用于搜索救援(SAR)作业。基于地面的原位传感器和遥感平台用于测量降水,云雾,辐射,温度,湿度和风廓线的微物理特性。从地球静止运行环境卫星(GOES)-13获得的多光谱红外观测值提供了每15分钟间隔一次的云顶温度和高度,相(水,冰),比重计大小,消光,光学深度和水平风向的估计值。在这项工作中,描述了一种技术,该技术用于识别能够产生高降雪率的云并结合来自卫星观测的风信息。使用在两次降水事件(暴风雪和大雪事件)中收集的地面实地和遥感平台获得的测量结果,可以验证从运行卫星观测中获得的云顶物理特性。发现在大雪事件中,所获得的积雪降水率与地面平台测量的积雪率相当。

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