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Evaluation of soil moisture derived from passive microwave remote sensing over agricultural sites in Canada using ground-based soil moisture monitoring networks

机译:利用基于地面的土壤水分监测网络评估加拿大农业现场被动微波遥感获得的土壤水分

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摘要

Passive microwave soil moisture datasets can be used as an input to provide an integrated assessment of climate variability as it relates to agricultural production. The objective of this research was to examine three passive microwave derived soil moisture datasets over multiple growing seasons in contrasting Canadian agricultural environments. Absolute and relative soil moisture was evaluated from two globally available datasets from the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) sensor using different retrieval algorithms, as well as relative soil wetness at a weekly scale from the Special Sensor Microwave/Imager (SSM/I) sensor. At a daily scale, the Land Parameter Retrieval Model (LPRM) provides a better estimate of surface soil moisture conditions than the National Snow and Ice Data Center (NSIDC) dataset, with root mean squared errors ranging from 5 to 10% for LPRM and 12 to 18% for NSIDC soil moisture when a temporal smoothing is applied to the dataset. Both datasets provided better estimates of soil moisture over the temperate site near Elora, Ontario than the prairie site near Davidson, Saskatchewan. The LPRM dataset tends to overestimate soil moisture conditions at both sites, where the NSIDC dataset tends to underestimate absolute soil moisture. These differences in retrieval methods were independent of radiometric frequency used. At weekly scales, the LPRM dataset provides a better relative estimate of wetness conditions when compared to the NSIDC and the Basist Wetness Index (BWI) from SSM/I data, but the SSM/I dataset did provide a reasonably good relative indicator of moisture conditions. The high variability in accuracy of soil moisture estimation related to retrieval algorithms indicates that consistency is needed in these datasets if they are to be integrated in long term studies for yield estimation or data assimilation.
机译:被动微波土壤水分数据集可以用作输入,以提供与农业生产有关的气候变异性的综合评估。这项研究的目的是在与加拿大农业环境形成对比的情况下,研究多个生长季节中三个被动微波衍生的土壤水分数据集。使用不同的检索算法,从EOS先进微波扫描辐射仪(AMSR-E)传感器的两个全球可用数据集中,评估土壤绝对和相对湿度,并通过特殊传感器微波/成像仪(SSM)每周评估相对土壤湿度。 / I)传感器。与美国国家冰雪数据中心(NSIDC)数据集相比,土地参数检索模型(LPRM)每天提供的表层土壤水分状况更好的估计值,LPRM和12的均方根误差范围从5%到10%当对数据集应用时间平滑时,NSIDC土壤湿度可达到18%。与萨斯喀彻温省戴维森附近的大草原地区相比,这两个数据集都提供了对安大略省埃洛拉附近的温带地区土壤湿度的更好估计。 LPRM数据集倾向于高估两个站点的土壤水分状况,而NSIDC数据集倾向于低估绝对土壤水分。检索方法的这些差异与所使用的辐射频率无关。与SSM / I数据中的NSIDC和基础湿度指数(BWI)相比,在每周尺度上,LPRM数据集可提供更好的相对湿度条件估计值,但SSM / I数据集确实提供了相对较好的湿度条件相对指标。与检索算法相关的土壤水分估算准确性的高差异性表明,如果要将这些数据集整合到长期研究中以进行产量估算或数据同化,则需要在这些数据集中保持一致性。

著录项

  • 来源
    《International journal of remote sensing》 |2010年第14期|P.3669-3690|共22页
  • 作者单位

    Department of Geography, University of Guelph, 50 Stone Road East, Guelph, ON, N1G 2W1 Canada Research Branch, Agriculture and Agri-Food Canada, Research Branch, 960 Carling Avenue, Ottawa, ON, K1A-0C6, Canada;

    rnDepartment of Geography, University of Guelph, 50 Stone Road East, Guelph, ON, N1G 2W1 Canada;

    rnDepartment of Geography, University of Guelph, 50 Stone Road East, Guelph, ON, N1G 2W1 Canada;

    Research Branch, Agriculture and Agri-Food Canada, Research Branch, 960 Carling Avenue, Ottawa, ON, K1A-0C6, Canada;

    rnDepartment of Hydrology and GeoEnvironmental Sciences, Vrije Universiteit Amsterdam, De Boelelaan 1085-1081 HV Amsterdam, the Netherlands;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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