Abstract

The European Space Agency (ESA) Climate Change Initiative (CCI) project combines multi-sensors at different microwave frequencies to derive three harmonized soil moisture products using active, passive and combined approaches. These long-term soil moisture products assist in understanding the global water and carbon cycles. However, extensive validations are a prerequisite before applying the retrieved soil moisture into climatic or hydrological models. To fulfill this objective, we assess the performances of three CCI soil moisture products (active, passive and combined) with respect to in-situ soil moisture networks located in China, Spain and Canada. In order to compensate the scale differences between ground stations and the CCI product’s coarse resolution, we adopted two upscaling approaches of Inverse Distance Weighting (IDW) interpolation and simple Arithmetic Mean (AM). The temporal agreements between the satellite retrieved and ground-measured soil moisture were quantified using the unbiased root mean square error (ubRMSE), RMSE, correlation coefficients (R) and bias. Furthermore, the temporal variability of the CCI soil moisture is interpreted and verified with respect to the Tropical Rainfall Measuring Mission (TRMM) precipitation observations. The results show that the temporal variations of CCI soil moisture agreed with the in-situ ground measurements and the precipitation observations over the China and Spain test sites. In contrast, a significant overestimation was observed over the Canada test sites, which may be due to the strong heterogeneity in soil and vegetation characteristics in accordance with the reported poor performance of soil moisture retrieval there. However, despite a retrieval bias, the relatively temporal variation of the CCI soil moisture also followed the ground measurements. For all the three test sites, the soil moisture retrieved from the combined approach outperformed the active-only and passive-only methods, with ubRMSE of 0.034, 0.050, and 0.050–0.054 m3/m3 over the test sites in China, Spain and Canada, respectively. Thus, the CCI combined soil moisture product is suggested to drive the climatic and hydrological studies.

Highlights

  • IntroductionSoil moisture (SM) is one of the most important land surface parameters, as it has a significant impact on vegetation growth, ecosystems, water cycle, agricultural production and climate change [1]

  • Soil moisture (SM) is one of the most important land surface parameters, as it has a significant impact on vegetation growth, ecosystems, water cycle, agricultural production and climate change [1].monitoring of soil moisture at regional and global scales is essential to deepen our insights into the physical processes of the global water cycle [2], crop growth [3] and drought events [4]

  • The European Space Agency (ESA) Climate Change Initiative (CCI) contributed to long-term soil moisture products which may benefit the study of global climate and hydrology

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Summary

Introduction

Soil moisture (SM) is one of the most important land surface parameters, as it has a significant impact on vegetation growth, ecosystems, water cycle, agricultural production and climate change [1]. Monitoring of soil moisture at regional and global scales is essential to deepen our insights into the physical processes of the global water cycle [2], crop growth [3] and drought events [4]. Sensors 2019, 19, 2718 the hydrological [5] and climate change [6] factors, the long-term soil moisture is necessary, which acts as a key driving parameter for the land surface process models. The remote-sensing techniques provide an efficient tool to estimate soil moisture at varying spatiotemporal scales using the electromagnetic waves. Compared to the visible electromagnetic spectrum, the microwaves at long wavelength are less affected by the atmosphere and clouds, allowing us to penetrate vegetation and operate at all-weather conditions [7]

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