首页> 外文会议>2010 IEEE International Geoscience and Remote Sensing Symposium >Quikscat backscatter sensitivity to landscape freeze/thaw state over ALECTRA sites in Alaska from 2000 to 2007: Application to SMAP validation planning
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Quikscat backscatter sensitivity to landscape freeze/thaw state over ALECTRA sites in Alaska from 2000 to 2007: Application to SMAP validation planning

机译:从2000年到2007年,阿拉斯加ALECTRA站点的Quikscat反向散射对景观冻结/融化状态的敏感性:在SMAP验证计划中的应用

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The mapping of freeze/thaw state of the landscape is one of the main objectives of NASA's upcoming SMAP (Soil Moisture Active and Passive) mission. This study applies ALECTRA (Alaska Ecological Transect) biophysical network and QuikSCAT scatterometer data to evaluate some of the validation issues regarding the SMAP freeze/thaw measurements. Although the QuikSCAT data is at Ku-band frequency, rather than the L-band of the SMAP instrument, the data is utilized due to its uniquely high temporal resolution over the ALECTRA sites. The results show that multiple temperature measurements representative of individual landscape (soil, snow cover, vegetation and atmosphere) elements and spatial heterogeneity within the satellite field-of-view are important for understanding the radar backscatter process and aggregate freeze/thaw signal. The backscatter temporal dynamics and relative contribution of these landscape elements to the freeze-thaw signal varies with land cover type, seasonal weather and climate conditions.
机译:冻结/解冻状态的绘图是美国国家航空航天局即将推出的液体液体(土壤水分活跃和被动)任务的主要目标之一。本研究适用于alectra(阿拉斯加生态横断)生物物理网络和Quikscat散射仪数据,以评估关于SmaP冻结/解冻测量的一些验证问题。虽然QuikScat数据处于Ku波段频率,而不是SMAP仪器的L带,但由于其在Alectra位点上的唯一高度的时间分辨率,因此使用数据。结果表明,多个温度测量代表各个景观(土壤,雪覆盖,植被和大气)元件和空间异质性在卫星视野中对理解雷达反向散射过程和聚合冻结/解冻信号很重要。这些横向元素与冻融信号的反向散射时间动态和相对贡献因土地覆盖类型,季节性天气和气候条件而异。

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