首页> 外文期刊>Geoscience and Remote Sensing, IEEE Transactions on >Validation of Advanced Microwave Scanning Radiometer Soil Moisture Products
【24h】

Validation of Advanced Microwave Scanning Radiometer Soil Moisture Products

机译:先进的微波扫描辐射计土壤水分产品的验证

获取原文
获取原文并翻译 | 示例
           

摘要

Validation is an important and particularly challenging task for remote sensing of soil moisture. A key issue in the validation of soil moisture products is the disparity in spatial scales between satellite and in situ observations. Conventional measurements of soil moisture are made at a point, whereas satellite sensors provide an integrated area/volume value for a much larger spatial extent. In this paper, four soil moisture networks were developed and used as part of the Advanced Microwave Scanning Radiometer–Earth Observing System (AMSR-E) validation program. Each network is located in a different climatic region of the U.S., and provides estimates of the average soil moisture over highly instrumented experimental watersheds and surrounding areas that approximate the size of the AMSR-E footprint. Soil moisture measurements have been made at these validation sites on a continuous basis since 2002, which provided a seven-year period of record for this analysis. The National Aeronautics and Space Administration (NASA) and Japan Aerospace Exploration Agency (JAXA) standard soil moisture products were compared to the network observations, along with two alternative soil moisture products developed using the single-channel algorithm (SCA) and the land parameter retrieval model (LPRM). The metric used for validation is the root-mean-square error (rmse) of the soil moisture estimate as compared to the in situ data. The mission requirement for accuracy defined by the space agencies is 0.06 $hbox{m}^{3}/hbox{m}^{3}$. The statistical results indicate that each algorithm performs differently at each site. Neither the NASA nor the JAXA standard products provide reliable estimates for all the conditions represented by the four watershed sites. The JAXA algorithm performs better than the NASA algorithm under light-vegetation conditions, but the NASA algorithm is more reliable for moderate vegetation. H-n-nowever, both algorithms have a moderate to large bias in all cases. The SCA had the lowest overall rmse with a small bias. The LPRM had a very large overestimation bias and retrieval errors. When site-specific corrections were applied, all algorithms had approximately the same error level and correlation. These results clearly show that there is much room for improvement in the algorithms currently in use by JAXA and NASA. They also illustrate the potential pitfalls in using the products without a careful evaluation.
机译:验证是遥感土壤水分的重要且特别具有挑战性的任务。验证土壤水分产物的关键问题是卫星观测与原位观测之间的空间尺度差异。传统的土壤湿度测量是在一个点上进行的,而卫星传感器在更大的空间范围内提供了一个积分的面积/体积值。在本文中,开发了四个土壤湿度网络,并将其用作高级微波扫描辐射计-地球观测系统(AMSR-E)验证程序的一部分。每个网络都位于美国不同的气候区域,并提供高度仪器化的实验分水岭和周边地区的平均土壤湿度估算值,这些估算值近似于AMSR-E足迹的大小。自2002年以来,在这些验证站点连续进行了土壤湿度测量,为该分析提供了7年的记录。将美国国家航空航天局(NASA)和日本航空航天局(JAXA)的标准土壤水分产品与网络观测结果进行了比较,并使用单通道算法(SCA)和土地参数检索开发了两种替代土壤水分产品模型(LPRM)。用于验证的度量是与原位数据相比的土壤湿度估算的均方根误差(rmse)。空间机构定义的任务精度要求为0.06 $ hbox {m} ^ {3} / hbox {m} ^ {3} $。统计结果表明,每种算法在每个站点上的执行情况都不同。无论是NASA还是JAXA标准产品,都无法对四个分水岭所代表的所有情况提供可靠的估计。在有植被的情况下,JAXA算法的性能优于NASA算法,但对于中等植被,NASA算法更可靠。如今,这两种算法在所有情况下都具有中等到较大的偏差。 SCA的总体均方根值最低,偏差很小。 LPRM具有很大的高估偏差和检索误差。当应用特定于站点的校正时,所有算法都具有大致相同的错误级别和相关性。这些结果清楚地表明,JAXA和NASA当前使用的算法还有很大的改进空间。他们还说明了在未经仔细评估的情况下使用产品的潜在陷阱。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号