A Simplified Land Model (SLM) for use in cloud‐resolving models: Formulation and evaluation. (18th September 2015)

• Record Type: Journal Article
• Authors: Lee, Jungmin M.; Khairoutdinov, Marat
• Is Part Of: Journal of advances in modeling earth systems. Volume 7:Number 3(2015:Sep.)
• Page Start: 1368
• Page End: 1392
• Publication Date: 2015-09-18
• Subjects: Land Surface Models -- shallow cumulus convection -- evolution of planetary boundary layer -- land‐atmosphere interaction -- large eddy simulation -- diurnal cycle; Geological modeling -- Periodicals; Climatology -- Periodicals; Geochemical modeling -- Periodicals; 551.5011
• DOI: 10.1002/2014MS000419
• Languages: English
• ISSNs: 1942-2466

Abstract

Abstract: A Simplified Land Model (SLM) that uses a minimalist set of parameters with a single‐layer vegetation and multilevel soil structure has been developed distinguishing canopy and undercanopy energy budgets. The primary motivation has been to design a land model for use in the System for Atmospheric Modeling (SAM) cloud‐resolving model to study land‐atmosphere interactions with a sufficient level of realism. SLM uses simplified expressions for the transport of heat, moisture, momentum, and radiation in soil‐vegetation system. The SLM performance has been evaluated over several land surface types using summertime tower observations of micrometeorological and biophysical data from three AmeriFlux sites, which include grassland, cropland, and deciduous‐broadleaf forest. In general, the SLM captures the observed diurnal cycle of surface energy budget and soil temperature reasonably well, although reproducing the evolution of soil moisture, especially after rain events, has been challenging. The SLM coupled to SAM has been applied to the case of summertime shallow cumulus convection over land based on the Atmospheric Radiation Measurements (ARM) Southern Great Plain (SGP) observations. The simulated surface latent and sensible heat fluxes as well as the evolution of thermodynamic profiles in convective boundary layer agree well with the estimates based on the observations. Sensitivity of atmospheric boundary layer development to the soil moisture and different land cover types has been also examined. Key Points: Simplified Land Model (SLM) has been developed for cloud‐resolving models SLM has been tested using observations from three sites Development of shallow convection over different land types was simulated