Interactions between dry-air entrainment, surface evaporation and convective boundary-layer development

The influence of dry-air entrainment on surface heat fluxes and the convective boundary-layer (CBL) properties is studied for vegetated land surfaces, using a mixed-layer CBL model coupled to the Penman¿Monteith equation under a wide range of conditions. In order to address the complex behaviour of the system, the feedback mechanisms involved were put into a mathematical framework. Simple expressions for the evaporative fraction and the Priestley¿Taylor parameter were derived, based on the concept of equilibrium evaporation. Dry-air entrainment enhances the surface evaporation under all conditions, but the sensitivity of the evaporation rate to the moisture content of the free troposphere falls as temperature rises. Due to the evaporation enhancement, shallower CBLs develop beneath dry atmospheres. In all cases, dry-air entrainment reduces the relative humidity at the land surface and at the top of the CBL. However, because of dry-air entrainment-induced land¿atmosphere feedback mechanisms, relative humidity at the top of the CBL responds nonlinearly to temperature rise; it decreases as temperature rises beneath a moist free troposphere, whereas it increases beneath a dry free troposphere. Finally, it was found that in certain conditions the evolution of the surface fluxes, relative humidity and CBL height can be as sensitive to the free tropospheric moisture conditions as to the land-surface properties. Therefore, studies of the land surface and of convective clouds have to take into account the influence of dry-air entrainment through land¿atmosphere feedback mechanisms

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Main Authors: van Heerwaarden, C.C., Vilà-Guerau de Arellano, J., Moene, A.F., Holtslag, A.A.M.
Format: Article/Letter to editor biblioteca
Language:English
Subjects:dynamics, equilibrium evaporation, feedbacks, heat, land-surface, models, parameterization, sensitivity, simulations, soil-moisture,
Online Access:https://research.wur.nl/en/publications/interactions-between-dry-air-entrainment-surface-evaporation-and-
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spelling dig-wur-nl-wurpubs-3811582025-01-22 van Heerwaarden, C.C. Vilà-Guerau de Arellano, J. Moene, A.F. Holtslag, A.A.M. Article/Letter to editor Quarterly Journal of the Royal Meteorological Society 135 (2009) 642 ISSN: 0035-9009 Interactions between dry-air entrainment, surface evaporation and convective boundary-layer development 2009 The influence of dry-air entrainment on surface heat fluxes and the convective boundary-layer (CBL) properties is studied for vegetated land surfaces, using a mixed-layer CBL model coupled to the Penman¿Monteith equation under a wide range of conditions. In order to address the complex behaviour of the system, the feedback mechanisms involved were put into a mathematical framework. Simple expressions for the evaporative fraction and the Priestley¿Taylor parameter were derived, based on the concept of equilibrium evaporation. Dry-air entrainment enhances the surface evaporation under all conditions, but the sensitivity of the evaporation rate to the moisture content of the free troposphere falls as temperature rises. Due to the evaporation enhancement, shallower CBLs develop beneath dry atmospheres. In all cases, dry-air entrainment reduces the relative humidity at the land surface and at the top of the CBL. However, because of dry-air entrainment-induced land¿atmosphere feedback mechanisms, relative humidity at the top of the CBL responds nonlinearly to temperature rise; it decreases as temperature rises beneath a moist free troposphere, whereas it increases beneath a dry free troposphere. Finally, it was found that in certain conditions the evolution of the surface fluxes, relative humidity and CBL height can be as sensitive to the free tropospheric moisture conditions as to the land-surface properties. Therefore, studies of the land surface and of convective clouds have to take into account the influence of dry-air entrainment through land¿atmosphere feedback mechanisms en application/pdf https://research.wur.nl/en/publications/interactions-between-dry-air-entrainment-surface-evaporation-and- 10.1002/qj.431 https://edepot.wur.nl/10186 dynamics equilibrium evaporation feedbacks heat land-surface models parameterization sensitivity simulations soil-moisture Wageningen University & Research
institution WUR NL
collection DSpace
country Países bajos
countrycode NL
component Bibliográfico
access En linea
databasecode dig-wur-nl
tag biblioteca
region Europa del Oeste
libraryname WUR Library Netherlands
language English
topic dynamics
equilibrium evaporation
feedbacks
heat
land-surface
models
parameterization
sensitivity
simulations
soil-moisture
dynamics
equilibrium evaporation
feedbacks
heat
land-surface
models
parameterization
sensitivity
simulations
soil-moisture
spellingShingle dynamics
equilibrium evaporation
feedbacks
heat
land-surface
models
parameterization
sensitivity
simulations
soil-moisture
dynamics
equilibrium evaporation
feedbacks
heat
land-surface
models
parameterization
sensitivity
simulations
soil-moisture
van Heerwaarden, C.C.
Vilà-Guerau de Arellano, J.
Moene, A.F.
Holtslag, A.A.M.
Interactions between dry-air entrainment, surface evaporation and convective boundary-layer development
description The influence of dry-air entrainment on surface heat fluxes and the convective boundary-layer (CBL) properties is studied for vegetated land surfaces, using a mixed-layer CBL model coupled to the Penman¿Monteith equation under a wide range of conditions. In order to address the complex behaviour of the system, the feedback mechanisms involved were put into a mathematical framework. Simple expressions for the evaporative fraction and the Priestley¿Taylor parameter were derived, based on the concept of equilibrium evaporation. Dry-air entrainment enhances the surface evaporation under all conditions, but the sensitivity of the evaporation rate to the moisture content of the free troposphere falls as temperature rises. Due to the evaporation enhancement, shallower CBLs develop beneath dry atmospheres. In all cases, dry-air entrainment reduces the relative humidity at the land surface and at the top of the CBL. However, because of dry-air entrainment-induced land¿atmosphere feedback mechanisms, relative humidity at the top of the CBL responds nonlinearly to temperature rise; it decreases as temperature rises beneath a moist free troposphere, whereas it increases beneath a dry free troposphere. Finally, it was found that in certain conditions the evolution of the surface fluxes, relative humidity and CBL height can be as sensitive to the free tropospheric moisture conditions as to the land-surface properties. Therefore, studies of the land surface and of convective clouds have to take into account the influence of dry-air entrainment through land¿atmosphere feedback mechanisms
format Article/Letter to editor
topic_facet dynamics
equilibrium evaporation
feedbacks
heat
land-surface
models
parameterization
sensitivity
simulations
soil-moisture
author van Heerwaarden, C.C.
Vilà-Guerau de Arellano, J.
Moene, A.F.
Holtslag, A.A.M.
author_facet van Heerwaarden, C.C.
Vilà-Guerau de Arellano, J.
Moene, A.F.
Holtslag, A.A.M.
author_sort van Heerwaarden, C.C.
title Interactions between dry-air entrainment, surface evaporation and convective boundary-layer development
title_short Interactions between dry-air entrainment, surface evaporation and convective boundary-layer development
title_full Interactions between dry-air entrainment, surface evaporation and convective boundary-layer development
title_fullStr Interactions between dry-air entrainment, surface evaporation and convective boundary-layer development
title_full_unstemmed Interactions between dry-air entrainment, surface evaporation and convective boundary-layer development
title_sort interactions between dry-air entrainment, surface evaporation and convective boundary-layer development
url https://research.wur.nl/en/publications/interactions-between-dry-air-entrainment-surface-evaporation-and-
work_keys_str_mv AT vanheerwaardencc interactionsbetweendryairentrainmentsurfaceevaporationandconvectiveboundarylayerdevelopment
AT vilagueraudearellanoj interactionsbetweendryairentrainmentsurfaceevaporationandconvectiveboundarylayerdevelopment
AT moeneaf interactionsbetweendryairentrainmentsurfaceevaporationandconvectiveboundarylayerdevelopment
AT holtslagaam interactionsbetweendryairentrainmentsurfaceevaporationandconvectiveboundarylayerdevelopment
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