“…The key areas are (1) improve simulations of the storage and transmission of water in the soil matrix, obtained through (a) implementing the mixed form of Richards' equation [Celia et al, 1990;Maxwell and Miller, 2005] and (b) explicitly representing macropore flow [Beven and Germann, 1982;Weiler, 2005;Nimmo, 2010;Yu et al, 2014]; (2) improve representation of hydraulic gradients throughout the soil-plantatmosphere continuum to improve simulations of root water uptake and evapotranspiration [Baldocchi and Meyers, 1998;Mackay et al, 2003;Bonan et al, 2014]; (3) improve representation of groundwater dynamics across a hierarchy of spatial scales, including improving ''among grid'' and ''within grid'' groundwater representations [Famiglietti and Wood, 1994;Troch et al, 2003;Miguez-Macho et al, 2007]; and (4) improve simulations of streamflow, by explicitly representing stream-aquifer interactions and improving parameterizations of channel/floodplain routing [Qu and Duffy, 2007;Shen and Phanikumar, 2010;MiguezMacho and Fan, 2012a;Pappenberger et al, 2012]. Underpinning all of these areas is the need to improve data sets on geophysical attributes, especially data on bedrock depth and permeability [Tesfa et al, 2009;Fan et al, 2015] and data sets on the physical characteristics of rivers [Getirana et al, 2013;Mersel et al, 2013;Gleason and Smith, 2014].…”