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A soil moisture and temperature network for SMOS validation in Western Denmark

机译:用于西丹麦的SMOS验证的土壤湿度和温度网络

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The Soil Moisture and Ocean Salinity Mission (SMOS) acquires surface soilmoisture data of global coverage every three days. Product validation for arange of climate and environmental conditions across continents is a crucialstep. For this purpose, a soil moisture and soil temperature sensor networkwas established in the Skjern River Catchment, Denmark. The objectives ofthis article are to describe a method to implement a network suited for SMOSvalidation, and to present sample data collected by the network to verify theapproach. The design phase included (1) selection of a single SMOS pixel(44 × 44 km), which is representative of the land surfaceconditions of the catchment and with minimal impact from open water(2) arrangement of three network clusters along the precipitation gradient,and (3) distribution of the stations according to respective fractions ofclasses representing the prevailing environmental conditions. Overall,measured moisture and temperature patterns could be related to the respectiveland cover and soil conditions. Texture-dependency of the 0–5 cm soilmoisture measurements was demonstrated. Regional differences in 0–5 cm soilmoisture, temperature and precipitation between the north-east and south-westwere found to be small. A first comparison between the 0–5 cm networkaverages and the SMOS soil moisture (level 2) product is in range withworldwide validation results, showing comparable trends for SMOS retrievedsoil moisture (R2 of 0.49) as well as initial soil moisture andtemperature from ECMWF used in the retrieval algorithm (R2 of 0.67 and0.97, respectively). While retrieved/initial SMOS soil moisture indicatesignificant under-/overestimation of the network data (biases of?0.092/0.057 m3 m?3), the initial temperature is in goodagreement (bias of ?0.2 °C). Based on these findings, the networkperforms according to expectations and proves to be well-suited for itspurpose. The discrepancies between network and SMOS soil moisture will besubject of subsequent studies.
机译:土壤水分和海洋盐度任务(SMOS)每三天获取一次全球覆盖的表面土壤水分数据。跨大洲各种气候和环境条件进行产品验证是至关重要的一步。为此,在丹麦的斯凯恩河集水区建立了土壤水分和土壤温度传感器网络。本文的目的是描述一种实现适合SMOS验证的网络的方法,并提出一种由网络收集的样本数据以验证该方法。设计阶段包括(1)选择单个SMOS像素(44×44 km),该像素代表流域的土地表面状况,并且受开放水域的影响最小(2)三个网络簇沿降水梯度的布置, (3)根据代表当时环境条件的类别的各个部分分配站点。总体而言,测得的水分和温度模式可能与各自的土地覆盖和土壤状况有关。证明了0-5 cm土壤湿度测量值的纹理依赖性。东北和西南地区0-5 cm的土壤水分,温度和降水之间的区域差异很小。 0–5 cm网络平均值与SMOS土壤水分(2级)产品之间的首次比较是在全球范围内的验证结果范围内,显示出SMOS再生土壤水分( R 2 0.49)和ECMWF的初始土壤湿度和温度(分别用于 R 2 分别为0.67和0.97)。取回/初始SMOS的土壤湿度表明对网络数据的估计过高/过低(偏向0.092 / 0.057 m 3 m ?3 ),但初始温度是一致的(偏差为±0.2°C)。基于这些发现,该网络可以按照预期执行,并证明非常适合其目的。网络与SMOS土壤水分之间的差异将是后续研究的主题。

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