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Observations of Moderate to Deep Seasonal Snow in Agricultural Fields with a Radar Scatterometer at Ku- and X-band Frequencies

机译:利用Ku和X波段频率的雷达散射仪观测农业领域中度至深季雪

摘要

The water contained within a snowpack, or the snow water equivalent (SWE), is very important to the hydrological cycle and to populations who depend on it for drinking, agriculture and industry. Measuring SWE over large areas is therefore important, but difficult given the scale of such an endeavor. Radar remote sensing of snow offers the promise of measuring SWE remotely but before we can do so, we must better understand how microwaves and snow interact. This thesis investigates the interaction of Ku- and X-band radar with moderate to deep seasonal snow in agricultural fields over two winters in Ontario. The University of Waterloo Scatterometer (UW-Scat) was used to make measurements of both snow-covered and snow-free fields in Maryhill and Englehart Ontario spanning a range of SWE up to 186 mm. In the 2013-14 season, 4 observations were made in Maryhill. In the 2014-15 season 3 sites were revisited over 6 dates in Maryhill and 3 sites were visited in Englehart. Accompanying the radar observations, in situ observations of snowpack properties including depth, density, stratigraphy, and grain size estimation were made at each site. Sensitivity to SWE was observed at Ku-band but not at X-band. An upper limit of sensitivity was observed around 140 mm after which point, Ku-band backscatter no longer responded to increasing SWE. However an investigation of seasonal depth hoar evolution suggested that the presence of depth hoar layers within the snowpack was the primary influence on backscatter response. Polarimetric data indicated the signal from early season, low-accumulation snowpacks was driven by vegetation where present and this influence decreased with further accumulation of snow.The major contribution of this study is the identification of depth hoar layers as a driver of backscatter response. This outcome points the way to further research on the influence of depth hoar, especially the mechanisms by which it exerts influence on the signal. Another contribution of this study is the identification of early-season influence of agricultural vegetation on backscatter through the use of polarimetric information.
机译:雪袋中包含的水或雪水当量(SWE)对于水文循环以及依赖其进行饮用,农业和工业生产的人们来说非常重要。因此,在大面积上测量SWE很重要,但是鉴于这种努力的规模,这很困难。雷达对雪的遥感提供了远程测量SWE的希望,但是在我们这样做之前,我们必须更好地了解微波和雪如何相互作用。本文研究了安大略省两个冬季农田中Ku波段和X波段雷达与中度至深层季节性降雪的相互作用。滑铁卢大学散射仪(UW-Scat)用于测量Maryhill和安大略省Englehart的积雪场和无雪场,其最大SWE范围为186 mm。在2013-14年度,在Maryhill进行了4次观测。在2014-15赛季,在马里希尔(Maryhill)的6个日期中重新访问了3个站点,并在恩格尔哈特(Englehart)访问了3个站点。伴随雷达观测,在每个站点进行了雪堆特性的原位观测,包括深度,密度,地层学和粒度估计。在Ku波段观察到对SWE的敏感性,而在X波段则没有。在140 mm左右观察到灵敏度上限,此后,Ku波段反向散射不再响应SWE的增加。但是,对季节性深度灰浆演变的研究表明,积雪内部存在深度灰层是对反向散射响应的主要影响。极化数据表明来自早期季节的信号是低积雪积雪是由存在的植被驱动的,随着积雪的进一步积聚,这种影响减小。这项研究的主要贡献是确定了深层灰白层作为反向散射响应的驱动力。这一结果为进一步研究深度灰浆的影响指明了道路,特别是它对信号产生影响的机制。这项研究的另一项贡献是通过使用极化信息确定了农业植被对反向散射的早期季节影响。

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    Thompson Aaron;

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  • 年度 2015
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  • 正文语种 en
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