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Performance of HIRLAM in a semiarid heterogeneous region: evaluation of the land surface and boundary layer description using EFEDA observations
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dc.contributor.authorJochum, Anne M.es_ES
dc.contributor.authorRodríguez Camino, Ernestoes_ES
dc.contributor.authorBruin, Hendrik A. R. dees_ES
dc.contributor.authorHoltslag, Albert A. M.es_ES
dc.date.accessioned2020-04-23T09:17:37Z-
dc.date.available2020-04-23T09:17:37Z-
dc.date.issued2004-
dc.identifier.citationMonthly Weather Review. 2004, 132, p. 2745–2760es_ES
dc.identifier.issn0027-0644-
dc.identifier.issn1520-0493-
dc.identifier.urihttp://hdl.handle.net/20.500.11765/11659-
dc.description.abstractObservations from the European Field Experiment in a Desertification-threatened Area (EFEDA) are used to evaluate the performance of the radiation, land surface, and boundary layer description of the numerical weather prediction (NWP) system High-Resolution Limited Area Model (HIRLAM) in semiarid conditions. Model analysis and 6-h forecast data of the fully coupled three-dimensional model are compared with the comprehensive dataset of a case study representing a sample of 22 days of anticyclonic conditions. Distributed micrometeorological surface stations, radiosondes, flux aircraft, and airborne lidar provide a unique validation dataset of the diurnal cycle of surface and boundary layer processes. The model surface, soil, and boundary layer are found to be too moist and slightly too cold during most of the diurnal cycle. The model radiation and surface energy budgets are biased toward more humid conditions. Model shortcomings are identified essentially in four areas. These are the moisture data assimilation, the land-use and soil classification with its associated physiographic database, the aerosol parameterization in the radiation code, and the boundary layer vertical resolution and entrainment description. Practical steps for immediate improvement of the model performance are proposed. They focus on the use of a land-use and soil classification and physiographic database adapted to Mediterranean landscapes, in combination with the inclusion of aerosol parameters in the radiation scheme, that account for the typically higher aerosol load of arid and semiarid environments.es_ES
dc.description.sponsorshipThe EFEDA 1991 field phase was cofunded by the European Commission under its Environment Program (Grant EV5VCT93- 0271).es_ES
dc.language.isoenges_ES
dc.publisherAmerican Meteorological Societyes_ES
dc.subjectHIRLAMes_ES
dc.subjectBoundary layeres_ES
dc.subjectRadiationes_ES
dc.subjectLand surfacees_ES
dc.titlePerformance of HIRLAM in a semiarid heterogeneous region: evaluation of the land surface and boundary layer description using EFEDA observationses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherversionhttps://doi.org/10.1175/MWR2820.1es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
Colecciones: Artículos científicos 2000-2004


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