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BibEntryCargo > Year: June 2012 & Pages : n/a–n/a or None

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California reanalysis downscaling at 10 km using an ocean-atmosphere coupled regional model system: REGIONAL COUPLED DOWNSCALING (1) · Ecosystem processes at the watershed scale: Hydrologic vegetation gradient as an indicator for lateral hydrologic connectivity of headwater catchments: HYDROLOGIC VEGETATION GRADIENT OF HEADWATER CATCHMENTS (1) · Effects of uncertainties in the geothermal heat flux distribution on the Greenland Ice Sheet: An assessment of existing heat flow models: HEAT FLOW EFFECTS ON GREENLAND ICE SHEET (1) · Evaluation of nonlocal and local planetary boundary layer schemes in the WRF model: EVALUATION OF PBL SCHEMES IN WRF (1) · Handling of Non-Periodic Contra Rotating Open Rotor Data (1) · Local and large-scale atmospheric responses to reduced Arctic sea ice and ocean warming in the WRF model: ATMOSPHERIC RESPONSE TO SEA ICE LOSS (1) · Modeling methane emissions from the Alaskan Yukon River basin, 1986-2005, by coupling a large-scale hydrological model and a process-based methane model: CH 4 EMISSIONS IN THE YUKON RIVER BASIN (1) · Sensitivity Analysis of Pine Island Glacier ice flow using ISSM and DAKOTA: PIG SENSITIVITY ANALYSIS (1) · Since “Groundwater and Surface Water–A Single Resource”: some U.S. Geological Survey advances in modeling groundwater/surface-water interactions (2) · Sub-kilometer dynamical downscaling of near-surface winds in complex terrain using WRF and MM5 mesoscale models: SUB-KILOMETER DYNAMICAL DOWNSCALING (1) · Targeted Lagrangian sampling of submesoscale dispersion at a coastal frontal zone: LIDEX10-REP10 (1) · The Case for Counter-Rotation of Installed Contra-Rotating Open Rotor Propulsion Systems (1) · The effect of wind waves on the development of river mouth bars: EFFECT OF WIND WAVES ON RIVER MOUTH BARS (1) · Using hilltop curvature to derive the spatial distribution of erosion rates: HILLTOP CURVATURE PREDICTS EROSION RATES (1) · WRF simulations of convectively generated gravity waves in opposite QBO phases: WRF SIMULATIONS OF GW (1) · Widespread late Cenozoic increase in erosion rates across the interior of eastern Tibet constrained by detrital low-temperature thermochronometry: EROSION HISTORY OF EASTERN TIBET (1)
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