Validation of a simple diagnostic relationship for downslope flows

Abstract A simple conceptual view of downslope flows allows a derivation of a diagnostic relationship between the maximum depth of the flow, its speed, the slope angle and the cooling flux. This relationship is obtained considering that the turbulence cooling causing the air to flow downslope is ess...

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Main Authors: Joan Cuxart, Daniel Martínez‐Villagrasa, Ivana Stiperski
Format: Article
Language:English
Published: Wiley 2020-05-01
Series:Atmospheric Science Letters
Subjects:
Online Access:https://doi.org/10.1002/asl.965
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author Joan Cuxart
Daniel Martínez‐Villagrasa
Ivana Stiperski
author_facet Joan Cuxart
Daniel Martínez‐Villagrasa
Ivana Stiperski
author_sort Joan Cuxart
collection DOAJ
description Abstract A simple conceptual view of downslope flows allows a derivation of a diagnostic relationship between the maximum depth of the flow, its speed, the slope angle and the cooling flux. This relationship is obtained considering that the turbulence cooling causing the air to flow downslope is essentially compensated by the warming by compression as the flow reaches higher pressure levels. The obtained relationship is consistent with the bulk heat budget for the along‐slope flows, and its agreement with existing prognostic layer‐averaged models is checked. Finally, the depth of the flow obtained from the diagnostic relationship is compared against the observational estimations of katabatic flows from two experimental campaigns.
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spelling doaj.art-17ee532786b949e6868fde98862e4b3c2022-12-21T23:54:26ZengWileyAtmospheric Science Letters1530-261X2020-05-01215n/an/a10.1002/asl.965Validation of a simple diagnostic relationship for downslope flowsJoan Cuxart0Daniel Martínez‐Villagrasa1Ivana Stiperski2Department of Physics University of the Balearic Islands Palma SpainDepartment of Physics University of the Balearic Islands Palma SpainDepartment of Atmospheric and Cryospheric Sciences University of Innsbruck Innsbruck AustriaAbstract A simple conceptual view of downslope flows allows a derivation of a diagnostic relationship between the maximum depth of the flow, its speed, the slope angle and the cooling flux. This relationship is obtained considering that the turbulence cooling causing the air to flow downslope is essentially compensated by the warming by compression as the flow reaches higher pressure levels. The obtained relationship is consistent with the bulk heat budget for the along‐slope flows, and its agreement with existing prognostic layer‐averaged models is checked. Finally, the depth of the flow obtained from the diagnostic relationship is compared against the observational estimations of katabatic flows from two experimental campaigns.https://doi.org/10.1002/asl.965diagnostic formuladownslope flowkatabatic depthMATERHORN campaignMETCRAX II campaign
spellingShingle Joan Cuxart
Daniel Martínez‐Villagrasa
Ivana Stiperski
Validation of a simple diagnostic relationship for downslope flows
Atmospheric Science Letters
diagnostic formula
downslope flow
katabatic depth
MATERHORN campaign
METCRAX II campaign
title Validation of a simple diagnostic relationship for downslope flows
title_full Validation of a simple diagnostic relationship for downslope flows
title_fullStr Validation of a simple diagnostic relationship for downslope flows
title_full_unstemmed Validation of a simple diagnostic relationship for downslope flows
title_short Validation of a simple diagnostic relationship for downslope flows
title_sort validation of a simple diagnostic relationship for downslope flows
topic diagnostic formula
downslope flow
katabatic depth
MATERHORN campaign
METCRAX II campaign
url https://doi.org/10.1002/asl.965
work_keys_str_mv AT joancuxart validationofasimplediagnosticrelationshipfordownslopeflows
AT danielmartinezvillagrasa validationofasimplediagnosticrelationshipfordownslopeflows
AT ivanastiperski validationofasimplediagnosticrelationshipfordownslopeflows