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Young-Hee Ryu, James A. Smith, Mary Lynn Baeck, Luciana K. Cunha, Elie Bou-Zeid, and Witold Krajewski

samples, for example, 91 days (3 months) in 2013. b. Atmospheric water balance analyses In this section, we examine components of the atmospheric water balance during the IFloodS campaign period and compare the 2013 observations to observations from other years. A particular focus of analyses presented in this section is the diurnal cycle of water cycle components. The area-averaged precipitable water derived from GPS observations ( Fig. 6 ) shows a weak but clear diurnal variation with an amplitude

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Huan Wu, Robert F. Adler, Yudong Tian, Guojun Gu, and George J. Huffman

VIC (for runoff generation) and a DRT-based routing (DRTR) model (for runoff routing). VIC solves for full water and energy balances with good skill for water budget estimation, based on its proven methodology, addressing both rainfall- and snowmelt-dominated runoff generation processes and soil frost dynamics (e.g., Storck et al. 2002 ; Cherkauer and Lettenmaier 1999 ; Christensen et al. 2004 ; Hamlet and Lettenmaier 2007 ; Hamlet et al. 2010 ; Elsner et al. 2010 ; Peters-Lidard et al

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Di Wu, Christa Peters-Lidard, Wei-Kuo Tao, and Walter Petersen

fraction for parameterization of the surface energy balance . Water Resour. Res. , 29 , 3681 – 3690 , doi: 10.1029/93WR01958 . Peters-Lidard, C. D. , and Coauthors , 2007 : High-performance Earth system modeling with NASA/GSFC’s Land Information System. Innovations Syst. Software Eng. , 3 , 157–165 , doi: 10.1007/s11334-007-0028-x . Peters-Lidard, C. D. , and Coauthors , 2015 : Integrated modeling of aerosol, cloud, precipitation and land processes at satellite-resolved scales . Environ

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