Characteristics of the Atmospheric Boundary Layer at Different Scales
The behaviour of the atmospheric boundary layer at different scales is described with an emphasis on the largest contributions to the total turbulence kinetic energy. First, large sudden wind-direction shifts and submesoscale motions under very stable atmospheric conditions over land are examined. S...
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Monash University
2019
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ftdatacite:10.26180/5b9f109845b99 2023-05-15T18:25:08+02:00 Characteristics of the Atmospheric Boundary Layer at Different Scales FRANCISCO ANDRES LANG TASSO 2019 https://dx.doi.org/10.26180/5b9f109845b99 https://bridges.monash.edu/articles/Characteristics_of_the_Atmospheric_Boundary_Layer_at_Different_Scales/7093271 unknown Monash University In Copyright http://rightsstatements.org/vocab/InC/1.0/ Atmospheric Sciences FOS Earth and related environmental sciences 40107 Meteorology Text Thesis article-journal ScholarlyArticle 2019 ftdatacite https://doi.org/10.26180/5b9f109845b99 2021-11-05T12:55:41Z The behaviour of the atmospheric boundary layer at different scales is described with an emphasis on the largest contributions to the total turbulence kinetic energy. First, large sudden wind-direction shifts and submesoscale motions under very stable atmospheric conditions over land are examined. Second, we explore changes in the thermodynamic structure of the Marine Atmospheric Boundary Layer (MABL) over the Southern Ocean (SO) in relation to the synoptic meteorology. In the last part of this research, shipborne observations have been used to evaluate the WRF model, in simulating the MABL under cold front passages over the SO. Thesis Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Southern Ocean |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
language |
unknown |
topic |
Atmospheric Sciences FOS Earth and related environmental sciences 40107 Meteorology |
spellingShingle |
Atmospheric Sciences FOS Earth and related environmental sciences 40107 Meteorology FRANCISCO ANDRES LANG TASSO Characteristics of the Atmospheric Boundary Layer at Different Scales |
topic_facet |
Atmospheric Sciences FOS Earth and related environmental sciences 40107 Meteorology |
description |
The behaviour of the atmospheric boundary layer at different scales is described with an emphasis on the largest contributions to the total turbulence kinetic energy. First, large sudden wind-direction shifts and submesoscale motions under very stable atmospheric conditions over land are examined. Second, we explore changes in the thermodynamic structure of the Marine Atmospheric Boundary Layer (MABL) over the Southern Ocean (SO) in relation to the synoptic meteorology. In the last part of this research, shipborne observations have been used to evaluate the WRF model, in simulating the MABL under cold front passages over the SO. |
format |
Thesis |
author |
FRANCISCO ANDRES LANG TASSO |
author_facet |
FRANCISCO ANDRES LANG TASSO |
author_sort |
FRANCISCO ANDRES LANG TASSO |
title |
Characteristics of the Atmospheric Boundary Layer at Different Scales |
title_short |
Characteristics of the Atmospheric Boundary Layer at Different Scales |
title_full |
Characteristics of the Atmospheric Boundary Layer at Different Scales |
title_fullStr |
Characteristics of the Atmospheric Boundary Layer at Different Scales |
title_full_unstemmed |
Characteristics of the Atmospheric Boundary Layer at Different Scales |
title_sort |
characteristics of the atmospheric boundary layer at different scales |
publisher |
Monash University |
publishDate |
2019 |
url |
https://dx.doi.org/10.26180/5b9f109845b99 https://bridges.monash.edu/articles/Characteristics_of_the_Atmospheric_Boundary_Layer_at_Different_Scales/7093271 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_rights |
In Copyright http://rightsstatements.org/vocab/InC/1.0/ |
op_doi |
https://doi.org/10.26180/5b9f109845b99 |
_version_ |
1766206360198840320 |