Abstract

Abstract. Soil moisture (SM) plays a critical role in the water and energy cycles of the Earth system; consequently, a long-term SM product with high quality is urgently needed. In this study, five SM products, including one microwave remote sensing product – the European Space Agency's Climate Change Initiative (ESA CCI) – and four reanalysis data sets – European Centre for Medium-Range Weather Forecasts (ECMWF) Reanalysis – Interim (ERA-Interim), National Centers for Environmental Prediction (NCEP), the 20th Century Reanalysis Project from National Oceanic and Atmospheric Administration (NOAA), and the ECMWF Reanalysis 5 (ERA5) – are systematically evaluated using in situ measurements during 1981–2013 in four climate regions at different timescales over the Chinese mainland. The results show that ESA CCI is closest to the observations in terms of both the spatial distributions and magnitude of the monthly SM. All reanalysis products tend to overestimate soil moisture in all regions but have higher correlations than the remote sensing product except in Northwest China. The largest inconsistency is found in southern Northeast China region, with an unbiased root mean square error (ubRMSE) value larger than 0.04. However, all products exhibit certain weaknesses in representing the interannual variation in SM. The largest relative bias of 144.4 % is found for the ERA-Interim SM product under extreme and severe wet conditions in northeastern China, and the lowest relative bias is found for the ESA CCI SM product, with the minimum of 0.48 % under extreme and severe wet conditions in northwestern China. Decomposing mean square errors suggests that the bias terms are the dominant contribution for all products, and the correlation term is large for ESA CCI. As a result, the ESA CCI SM product is a good option for long-term hydrometeorological applications on the Chinese mainland. ERA5 is also a promising product, especially in northern and northwestern China in terms of low bias and high correlation coefficient. This long-term intercomparison study provides clues for SM product enhancement and further hydrological applications.

Highlights

  • Soil moisture (SM) is a key state variable in the climate system and controls the exchange of water, energy, and carbon fluxes between land surface and atmosphere

  • The results show that European Space Agency’s Climate Change Initiative (ESA Climate Change Initiative (CCI)) is closest to the observations in terms of both the spatial distributions and magnitude of the monthly SM

  • Most SM products are able to capture the overall spatial distribution of the SM value, the National Oceanic and Atmospheric Administration (NOAA) SM is highly overestimated throughout the region

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Summary

Introduction

Soil moisture (SM) is a key state variable in the climate system and controls the exchange of water, energy, and carbon fluxes between land surface and atmosphere Despite the small total mass of SM compared to other water cycle components, it is essential for numerical weather prediction (An et al, 2016) and has been recognized as an essential climate variable (ECV; GCOS, 2010)

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