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. Author manuscript; available in PMC: 2018 Apr 9.
Published in final edited form as: J Hydrometeorol. 2016 Mar 15;17(4):1049–1067. doi: 10.1175/JHM-D-15-0196.1

Table 5.

Spatial pattern correlations of subseasonal JJA standard deviations of daily soil moisture between stations and model grid boxes for indicated models.

LSM Local Regional
Noah GLDAS CFSR CFS 20CR GLDAS CFSR CFS 20CR
Surface −0.13 0.06 −0.01 0.06 0.38 0.40 0.30 0.25
Shallow 0.08 0.09 −0.06 0.06 0.39 0.34 0.33 0.30
Deep 0.09 0.00 −0.09 0.00 0.25 0.21 0.22 0.18

Catchment MERRA land MERRA GEOS5 MERRA land MERRA GEOS5
Surface −0.13 −0.11 −0.09 0.08 −0.04 0.21
Shallow 0.07 0.10 0.29 0.21

HTESSEL ERA-In. land ERA Interim IFS ERA-In. land ERA Interim IFS
Surface 0.07 0.03 0.12 0.40 0.50 0.47
Shallow 0.09 0.03 0.34 0.43
Deep −0.02 0.01 0.28 0.32

CLM CLM CCSM CLM CCSM
Surface 0.14 0.07 0.41 0.39
Shallow 0.11 0.05 0.33 0.34
Deep 0.07 −0.03 0.27 0.25

Multi-model Offline Reanal. Free Offline Reanal. Free
Surface −0.01 0.01 0.09 0.31 0.28 0.35
Shallow 0.09 0.06 0.12 0.34 0.36 0.29
Deep 0.03 0.00 0.04 0.27 0.24 0.22

Estimates are grouped by extent of network (local versus regional) and averaged across networks weighted by number of stations used in each network. Surface refers to the top LSM soil level, except CLM where it is the total for the top 3 layers; shallow is the second layer except for CLM where it is layers 4–6; deep is the third layer for Noah and HTESSEL, layers 7–8 for CLM.