HR: 14:25h
AN: H53H-04    [Abstracts]
TI: Pathways of soil moisture controls on boundary layer dynamics
AU: * Siqueira, M
EM: mbs4@duke.edu
AF: Nicholas School of the Environment and Earth Sciences - Duke University, LSRC, Duke University, Durham, NC 27708, United States
AU: * Siqueira, M
EM: mbs4@duke.edu
AF: Dept of Mechanical Engineering - UnB, Faculdade de Tecnologia, Universidade de Brasila, Brasilia, DF 70000, Brazil
AU: Katul, G
EM: gaby@duke.edu
AF: Nicholas School of the Environment and Earth Sciences - Duke University, LSRC, Duke University, Durham, NC 27708, United States
AU: Porporato, A
EM: amilcare@duke.edu
AF: Pratt School of Engineering - Duke University, Hudson Hall, Duke University, Durham, NC 27708, United States
AB: Soil moisture controls on precipitation are now receiving significant attention in climate systems because the memory of their variability is much slower than the memory of the fast atmospheric processes. We propose a new model that integrates soil water dynamics, plant hydraulics and stomatal responses to water availability to estimate root water uptake and available energy partitioning, as well as feedbacks to boundary layer dynamics (in terms of water vapor and heat input to the atmospheric system). Using a simplified homogenization technique, the model solves the intrinsically 3-D soil water movement equations by two 1-D coupled Richards' equations. The first resolves the radial water flow from bulk soil to soil-root interface to estimate root uptake (assuming the vertical gradients in moisture persist during the rapid lateral flow), and then it solves vertical water movement through the soil following the radial moisture adjustments. The coupling between these two equations is obtained by area averaging the soil moisture in the radial domain (i.e. homogenization) to calculate the vertical fluxes. For each vertical layer, the domain is discretized in axi-symmetrical grid with constant soil properties. This is deemed to be appropriate given the fact that the root uptake occurs on much shorter time scales closely following diurnal cycles, while the vertical water movement is more relevant to the inter-storm time scale. We show that this approach was able to explicitly simulate known features of root uptake such as diurnal hysteresis of canopy conductance, water redistribution by roots (hydraulic lift) and downward shift of root uptake during drying cycles. The model is then coupled with an atmospheric boundary layer (ABL) growth model thereby permitting us to explore low-dimensional elements of the interaction between soil moisture and ABL states commensurate with the lifting condensation level.
DE: 1813 Eco-hydrology
DE: 1843 Land/atmosphere interactions (1218, 1631, 3322)
DE: 1847 Modeling
DE: 1875 Vadose zone
DE: 1878 Water/energy interactions (0495)
SC: Hydrology [H]
MN: 2007 Fall Meeting