Midday Boundary-Layer Collapse in the Altiplano Desert : The Combined Effect of Advection and Subsidence

Observations in the Altiplano region of the Atacama Desert show that the atmospheric boundary layer (ABL) suddenly collapses at noon. This rapid decrease occurs simultaneously to the entrance of a thermally driven, regional flow that causes a rise in wind speed and a marked temperature decrease. We identify the main drivers that cause the observed ABL collapse by using a land–atmosphere model. The free atmosphere lapse rate and regional forcings, such as advection of mass and cold air as well as subsidence, are first estimated by combining observations from a comprehensive field campaign and a regional model. Then, to disentangle the ABL collapse, we perform a suite of numerical experiments with increasing level of complexity: from only considering local land–atmosphere interactions, to systematically including the regional contributions of mass advection, cold air advection, and subsidence. Our results show that non-local processes related to the arrival of the regional flow are the main factors explaining the boundary-layer collapse. The advection of a shallower boundary layer (≈ - 250 m h- 1 at noon) causes an immediate decrease in the ABL height (h) at midday. This occurs simultaneously with the arrival of a cold air mass, which reaches a strength of ≈ - 4 K h- 1 at 1400 LT. These two external forcings become dominant over entrainment and surface processes that warm the atmosphere and increase h. As a consequence, the ABL growth is capped during the afternoon. Finally, a wind divergence of ≈ 8 × 10 - 5 s- 1 contributes to the collapse by causing subsidence motions over the ABL from 1200 LT onward. Our findings show the relevance of treating large and small-scale processes as a continuum to be able to understand the ABL dynamics.

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Main Authors: Aguirre-Correa, Francisca, de Arellano, Jordi Vilà Guerau, Ronda, Reinder, Lobos-Roco, Felipe, Suárez, Francisco, Hartogensis, Oscar
Format: Article/Letter to editor biblioteca
Language:English
Subjects:Advection, Altiplano, Boundary-layer collapse, CLASS, WRF,
Online Access:https://research.wur.nl/en/publications/midday-boundary-layer-collapse-in-the-altiplano-desert-the-combin
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spelling dig-wur-nl-wurpubs-6152932024-12-04 Aguirre-Correa, Francisca de Arellano, Jordi Vilà Guerau Ronda, Reinder Lobos-Roco, Felipe Suárez, Francisco Hartogensis, Oscar Article/Letter to editor Boundary-Layer Meteorology 187 (2023) 3 ISSN: 0006-8314 Midday Boundary-Layer Collapse in the Altiplano Desert : The Combined Effect of Advection and Subsidence 2023 Observations in the Altiplano region of the Atacama Desert show that the atmospheric boundary layer (ABL) suddenly collapses at noon. This rapid decrease occurs simultaneously to the entrance of a thermally driven, regional flow that causes a rise in wind speed and a marked temperature decrease. We identify the main drivers that cause the observed ABL collapse by using a land–atmosphere model. The free atmosphere lapse rate and regional forcings, such as advection of mass and cold air as well as subsidence, are first estimated by combining observations from a comprehensive field campaign and a regional model. Then, to disentangle the ABL collapse, we perform a suite of numerical experiments with increasing level of complexity: from only considering local land–atmosphere interactions, to systematically including the regional contributions of mass advection, cold air advection, and subsidence. Our results show that non-local processes related to the arrival of the regional flow are the main factors explaining the boundary-layer collapse. The advection of a shallower boundary layer (≈ - 250 m h- 1 at noon) causes an immediate decrease in the ABL height (h) at midday. This occurs simultaneously with the arrival of a cold air mass, which reaches a strength of ≈ - 4 K h- 1 at 1400 LT. These two external forcings become dominant over entrainment and surface processes that warm the atmosphere and increase h. As a consequence, the ABL growth is capped during the afternoon. Finally, a wind divergence of ≈ 8 × 10 - 5 s- 1 contributes to the collapse by causing subsidence motions over the ABL from 1200 LT onward. Our findings show the relevance of treating large and small-scale processes as a continuum to be able to understand the ABL dynamics. en application/pdf https://research.wur.nl/en/publications/midday-boundary-layer-collapse-in-the-altiplano-desert-the-combin 10.1007/s10546-023-00790-5 https://edepot.wur.nl/631851 Advection Altiplano Boundary-layer collapse CLASS WRF https://creativecommons.org/licenses/by/4.0/ https://creativecommons.org/licenses/by/4.0/ 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 Advection
Altiplano
Boundary-layer collapse
CLASS
WRF
Advection
Altiplano
Boundary-layer collapse
CLASS
WRF
spellingShingle Advection
Altiplano
Boundary-layer collapse
CLASS
WRF
Advection
Altiplano
Boundary-layer collapse
CLASS
WRF
Aguirre-Correa, Francisca
de Arellano, Jordi Vilà Guerau
Ronda, Reinder
Lobos-Roco, Felipe
Suárez, Francisco
Hartogensis, Oscar
Midday Boundary-Layer Collapse in the Altiplano Desert : The Combined Effect of Advection and Subsidence
description Observations in the Altiplano region of the Atacama Desert show that the atmospheric boundary layer (ABL) suddenly collapses at noon. This rapid decrease occurs simultaneously to the entrance of a thermally driven, regional flow that causes a rise in wind speed and a marked temperature decrease. We identify the main drivers that cause the observed ABL collapse by using a land–atmosphere model. The free atmosphere lapse rate and regional forcings, such as advection of mass and cold air as well as subsidence, are first estimated by combining observations from a comprehensive field campaign and a regional model. Then, to disentangle the ABL collapse, we perform a suite of numerical experiments with increasing level of complexity: from only considering local land–atmosphere interactions, to systematically including the regional contributions of mass advection, cold air advection, and subsidence. Our results show that non-local processes related to the arrival of the regional flow are the main factors explaining the boundary-layer collapse. The advection of a shallower boundary layer (≈ - 250 m h- 1 at noon) causes an immediate decrease in the ABL height (h) at midday. This occurs simultaneously with the arrival of a cold air mass, which reaches a strength of ≈ - 4 K h- 1 at 1400 LT. These two external forcings become dominant over entrainment and surface processes that warm the atmosphere and increase h. As a consequence, the ABL growth is capped during the afternoon. Finally, a wind divergence of ≈ 8 × 10 - 5 s- 1 contributes to the collapse by causing subsidence motions over the ABL from 1200 LT onward. Our findings show the relevance of treating large and small-scale processes as a continuum to be able to understand the ABL dynamics.
format Article/Letter to editor
topic_facet Advection
Altiplano
Boundary-layer collapse
CLASS
WRF
author Aguirre-Correa, Francisca
de Arellano, Jordi Vilà Guerau
Ronda, Reinder
Lobos-Roco, Felipe
Suárez, Francisco
Hartogensis, Oscar
author_facet Aguirre-Correa, Francisca
de Arellano, Jordi Vilà Guerau
Ronda, Reinder
Lobos-Roco, Felipe
Suárez, Francisco
Hartogensis, Oscar
author_sort Aguirre-Correa, Francisca
title Midday Boundary-Layer Collapse in the Altiplano Desert : The Combined Effect of Advection and Subsidence
title_short Midday Boundary-Layer Collapse in the Altiplano Desert : The Combined Effect of Advection and Subsidence
title_full Midday Boundary-Layer Collapse in the Altiplano Desert : The Combined Effect of Advection and Subsidence
title_fullStr Midday Boundary-Layer Collapse in the Altiplano Desert : The Combined Effect of Advection and Subsidence
title_full_unstemmed Midday Boundary-Layer Collapse in the Altiplano Desert : The Combined Effect of Advection and Subsidence
title_sort midday boundary-layer collapse in the altiplano desert : the combined effect of advection and subsidence
url https://research.wur.nl/en/publications/midday-boundary-layer-collapse-in-the-altiplano-desert-the-combin
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