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Ho-Chun Huang, Xin-Zhong Liang, Kenneth E. Kunkel, Michael Caughey, and Allen Williams

. Biases generated in the RCM meteorological conditions and emissions ultimately affect the accuracy of AQM simulations. In this study, LBCs constructed from global reanalysis data actually possess substantial uncertainties, especially over the oceans and the Tropics ( Liang et al. 2001 , 2004 ). These uncertainties may limit the ability of RCMs to reproduce observed regional climate variations. Without independent observational data to validate the EM directly, it was beyond the scope of this study

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Jesse O. Bash, Patricia Bresnahan, and David R. Miller

concentration, and H is Henry’s constant for an air–water mercury equilibrium. A sink term representing the up- and downwelling of deep-water areas in modeling domains will be necessary to more realistically portray the oceanic system. b. Atmosphere–soil interface Recent experimental evidence indicates that the transport between the soil particles and the soil water solution is mediated by chemical sorption and desorption processes ( Ravichandran 2004 ; Moreno et al. 2005a ; Johnson et al. 2003

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