Regression Models for Soil Water Storage Estimation Using the ESA CCI Satellite Soil Moisture Product: A Case Study in Northeast Portugal

被引:6
作者
de Figueiredo, Tomas [1 ]
Royer, Ana Caroline [1 ]
Fonseca, Felicia [1 ]
de Araujo Schutz, Fabiana Costa [2 ]
Hernandez, Zulimar [3 ]
机构
[1] Inst Politecn Braganca, Ctr Invest Montanha CIMO, Campus Santa Apolonia, P-5300253 Braganca, Portugal
[2] Fed Technol Univ Parana, BR-85884000 Medianeira, Brazil
[3] Mt Res Collaborat Lab MORE, P-5300358 Braganca, Portugal
关键词
remote sensing; radar satellite data; active and passive microwave sensors; ESA CCI SM product; soil water balance; soil water storage; regression models; hysteresis; SPATIOTEMPORAL VARIABILITY; HYDROLOGICAL MODELS; CLIMATE-CHANGE; LAND-USE; BUDGET; GRACE; ASSIMILATION; SMOS; ZONE; PRECIPITATION;
D O I
10.3390/w13010037
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The European Space Agency Climate Change Initiative Soil Moisture (ESA CCI SM) product provides soil moisture estimates from radar satellite data with a daily temporal resolution. Despite validation exercises with ground data that have been performed since the product's launch, SM has not yet been consistently related to soil water storage, which is a key step for its application for prediction purposes. This study aimed to analyse the relationship between soil water storage (S), which was obtained from soil water balance computations with ground meteorological data, and soil moisture, which was obtained from radar data, as affected by soil water storage capacity (Smax). As a case study, a 14-year monthly series of soil water storage, produced via soil water balance computations using ground meteorological data from northeast Portugal and Smax from 25 mm to 150 mm, were matched with the corresponding monthly averaged SM product. Linear (I) and logistic (II) regression models relating S with SM were compared. Model performance (r(2) in the 0.8-0.9 range) varied non-monotonically with Smax, with it being the highest at an Smax of 50 mm. The logistic model (II) performed better than the linear model (I) in the lower range of Smax. Improvements in model performance obtained with segregation of the data series in two subsets, representing soil water recharge and depletion phases throughout the year, outlined the hysteresis in the relationship between S and SM.
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页数:26
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