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评估西藏玛曲地区卫星湿度粗尺度验证的时间稳定性。

Assessing temporal stability for coarse scale satellite moisture validation in the Maqu area, Tibet.

机构信息

Department of Water Resources, Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands.

出版信息

Sensors (Basel). 2013 Aug 16;13(8):10725-48. doi: 10.3390/s130810725.

Abstract

This study evaluates if the temporal stability concept is applicable to a time series of satellite soil moisture images so to extend the common procedure of satellite image validation. The area of study is the Maqu area, which is located in the northeastern part of the Tibetan plateau. The network serves validation purposes of coarse scale (25-50 km) satellite soil moisture products and comprises 20 stations with probes installed at depths of 5, 10, 20, 40, 80 cm. The study period is 2009. The temporal stability concept is applied to all five depths of the soil moisture measuring network and to a time series of satellite-based moisture products from the Advance Microwave Scanning Radiometer (AMSR-E). The in-situ network is also assessed by Pearsons's correlation analysis. Assessments by the temporal stability concept proved to be useful and results suggest that probe measurements at 10 cm depth best match to the satellite observations. The Mean Relative Difference plot for satellite pixels shows that a RMSM pixel can be identified but in our case this pixel does not overlay any in-situ station. Also, the RMSM pixel does not overlay any of the Representative Mean Soil Moisture (RMSM) stations of the five probe depths. Pearson's correlation analysis on in-situ measurements suggests that moisture patterns over time are more persistent than over space. Since this study presents first results on the application of the temporal stability concept to a series of satellite images, we recommend further tests to become more conclusive on effectiveness to broaden the procedure of satellite validation.

摘要

本研究评估了时间稳定性概念是否适用于卫星土壤水分图像时间序列,以扩展卫星图像验证的常见程序。研究区域是位于青藏高原东北部的玛曲地区。该网络用于验证粗尺度(25-50 公里)卫星土壤水分产品,由 20 个站点组成,探头安装在 5、10、20、40 和 80 厘米的深度。研究期间为 2009 年。时间稳定性概念应用于土壤水分测量网络的所有五个深度以及来自高级微波扫描辐射计(AMSR-E)的卫星土壤水分时间序列产品。也通过皮尔逊相关分析对现场网络进行了评估。时间稳定性概念的评估被证明是有用的,结果表明,10 厘米深度的探头测量最能与卫星观测结果相匹配。卫星像素的平均相对差异图表明,可以识别 RMSM 像素,但在我们的案例中,该像素不在任何现场站之上。此外,RMSM 像素也不在五个探头深度的代表性平均土壤水分(RMSM)站的任何一个之上。现场测量的皮尔逊相关分析表明,随着时间的推移,湿度模式比空间模式更持久。由于本研究首次提出了将时间稳定性概念应用于一系列卫星图像的结果,因此我们建议进行进一步的测试,以更明确地确定该方法对扩大卫星验证程序的有效性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b72/3812625/13072062e675/sensors-13-10725f1.jpg

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