Influence of Soil Moisture on Boundary Layer Cloud Development
Top Cited Papers
Open Access
- 1 February 2004
- journal article
- Published by American Meteorological Society in Journal of Hydrometeorology
- Vol. 5 (1) , 86-99
- https://doi.org/10.1175/1525-7541(2004)005<0086:iosmob>2.0.co;2
Abstract
The daytime interaction of the land surface with the atmospheric boundary layer (ABL) is studied using a coupled one-dimensional (column) land surface–ABL model. This is an extension of earlier work that focused on modeling the ABL for 31 May 1978 at Cabauw, Netherlands; previously, it was found that coupled land–atmosphere tests using a simple land surface scheme did not accurately represent surface fluxes and coupled ABL development. Here, findings from that earlier study on ABL parameterization are utilized, and include a more sophisticated land surface scheme. This land surface scheme allows the land–atmosphere system to respond interactively with the ABL. Results indicate that in coupled land–atmosphere model runs, realistic daytime surface fluxes and atmospheric profiles are produced, even in the presence of ABL clouds (shallow cumulus). Subsequently, the role of soil moisture in the development of ABL clouds is explored in terms of a new relative humidity tendency equation at the ABL top w... Abstract The daytime interaction of the land surface with the atmospheric boundary layer (ABL) is studied using a coupled one-dimensional (column) land surface–ABL model. This is an extension of earlier work that focused on modeling the ABL for 31 May 1978 at Cabauw, Netherlands; previously, it was found that coupled land–atmosphere tests using a simple land surface scheme did not accurately represent surface fluxes and coupled ABL development. Here, findings from that earlier study on ABL parameterization are utilized, and include a more sophisticated land surface scheme. This land surface scheme allows the land–atmosphere system to respond interactively with the ABL. Results indicate that in coupled land–atmosphere model runs, realistic daytime surface fluxes and atmospheric profiles are produced, even in the presence of ABL clouds (shallow cumulus). Subsequently, the role of soil moisture in the development of ABL clouds is explored in terms of a new relative humidity tendency equation at the ABL top w...Keywords
This publication has 45 references indexed in Scilit:
- Idealized Model for Equilibrium Boundary Layer over LandJournal of Hydrometeorology, 2000
- Validation Study of the CAPS Model Land Surface Scheme Using the 1987 Cabauw/PILPS DatasetJournal of Applied Meteorology and Climatology, 1999
- Impact of Atmospheric Surface-layer Parameterizations in the new Land-surface Scheme of the NCEP Mesoscale Eta ModelBoundary-Layer Meteorology, 1997
- Assessment of the Land Surface and Boundary Layer Models in Two Operational Versions of the NCEP Eta Model Using FIFE DataMonthly Weather Review, 1997
- Cabauw Data for the Validation of Land Surface Parameterization SchemesJournal of Climate, 1997
- Cabauw Experimental Results from the Project for Intercomparison of Land-Surface Parameterization SchemesJournal of Climate, 1997
- Note on “Daytime Evolution of Relative Humidity at the Boundary Layer Top”Monthly Weather Review, 1996
- Modeling of land surface evaporation by four schemes and comparison with FIFE observationsJournal of Geophysical Research: Atmospheres, 1996
- The estimation of solar radiation under cloudless skies with atmospheric dustQuarterly Journal of the Royal Meteorological Society, 1974
- Non‐precipitating cumulus convection and its parameterizationQuarterly Journal of the Royal Meteorological Society, 1973