TY - GEN
AU - C. Albergel
AU - W. Dorigo
AU - R. Reichle
AU - Gianpaolo Balsamo
AU - Patricia de Rosnay
AU - J. Munoz-Sabater
AU - L. Isaksen
AU - R. de Jeu
AU - W. Wagner
AB - In situ soil moisture measurements from 2007 to 2010 for 196 stations from five networks across the world (USA, France, Spain, China and Australia) are used to determine the reliability of three soil moisture products: (i) a revised version of the ERA-Interim reanalysis from ECMWF (ERA-Land), (ii) a revised version of the MERRA reanalysis from NASA (MERRA-Land) and (iii) a new, microwave based multi-satellite surface soil moisture dataset (SM-MW). Evaluation of the time series and anomalies from a moving monthly mean shows a good performance of the three products in capturing the annual cycle of surface soil moisture and its short-term variability. On average, correlations (95% confidence interval) are 0.66(±0.038), 0.69(±0.038) and 0.60(±0.061) for ERA-Land, MERRA-Land and SM-MW. The two reanalysis products also capture the root zone soil moisture well; on average correlations are 0.68(±0.035) and 0.73(±0.032) for ERA-Land, MERRA-Land. Global trends analysis for 1988-2010 suggests a decrease of surface soil moisture contents (72% of significant trends are negative, i.e. drying) for ERA-Land and an increase in surface soil moisture (59% of significant trends are positive, i.e. wetting) for MERRA-Land. As the spatial extent and fractions of significant trends in both products differ, the trend reflected in the majority of grid points within different climate classes was investigated and compared to that of SM-MW. The latter is dominated by negative significant trends (73.2%) and is more in line with ERA-Land. For both reanalysis products trends for the upper layer of soil are confirmed in the root zone soil moisture (first meter of soil).
BT - ECMWF Technical Memoranda
DA - 03/2013
DO - 10.21957/4ehqr9d00
LA - eng
M1 - 695
N2 - In situ soil moisture measurements from 2007 to 2010 for 196 stations from five networks across the world (USA, France, Spain, China and Australia) are used to determine the reliability of three soil moisture products: (i) a revised version of the ERA-Interim reanalysis from ECMWF (ERA-Land), (ii) a revised version of the MERRA reanalysis from NASA (MERRA-Land) and (iii) a new, microwave based multi-satellite surface soil moisture dataset (SM-MW). Evaluation of the time series and anomalies from a moving monthly mean shows a good performance of the three products in capturing the annual cycle of surface soil moisture and its short-term variability. On average, correlations (95% confidence interval) are 0.66(±0.038), 0.69(±0.038) and 0.60(±0.061) for ERA-Land, MERRA-Land and SM-MW. The two reanalysis products also capture the root zone soil moisture well; on average correlations are 0.68(±0.035) and 0.73(±0.032) for ERA-Land, MERRA-Land. Global trends analysis for 1988-2010 suggests a decrease of surface soil moisture contents (72% of significant trends are negative, i.e. drying) for ERA-Land and an increase in surface soil moisture (59% of significant trends are positive, i.e. wetting) for MERRA-Land. As the spatial extent and fractions of significant trends in both products differ, the trend reflected in the majority of grid points within different climate classes was investigated and compared to that of SM-MW. The latter is dominated by negative significant trends (73.2%) and is more in line with ERA-Land. For both reanalysis products trends for the upper layer of soil are confirmed in the root zone soil moisture (first meter of soil).
PB - ECMWF
PY - 2013
EP - 29
T2 - ECMWF Technical Memoranda
TI - Skill and global trend analysis of soil moisture from reanalyses and microwave remote sensing
UR - https://www.ecmwf.int/node/7669
ER -