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Robert S. Arthur, Katherine A. Lundquist, Jeffrey D. Mirocha, and Fotini K. Chow

are also initialized following Lundquist et al. (2010) . These include spatially uniform values of soil type (sandy loam), land use (savannah), and vegetation fraction (0.1). The initial soil temperature is equal to the initial surface atmospheric temperature, and the soil moisture is set to 0.0868 m 3 m −3 (a 20% saturation rate for sandy loam). Lateral boundary conditions are periodic for all variables. At the immersed boundary, either Dirichlet or Neumann boundary conditions can be used

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Raquel Lorente-Plazas and Joshua P. Hacker

: The GEOS moisture analysis . Mon. Wea. Rev. , 128 , 3268 – 3282 , doi: 10.1175/1520-0493(2000)128<3268:DAITPO>2.0.CO;2 . 10.1175/1520-0493(2000)128<3268:DAITPO>2.0.CO;2 Dee , D. P. , and S. Uppala , 2009 : Variational bias correction of satellite radiance data in the ERA-Interim reanalysis . Quart. J. Roy. Meteor. Soc. , 135 , 1830 – 1841 , doi: 10.1002/qj.493 . 10.1002/qj.493 Derber , J. C. , and W.-S. Wu , 1998 : The use of TOVS cloud-cleared radiances in the NCEP SSI analysis

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