Characteristics of Gravity Waves over an Antarctic Ice Sheet during an Austral Summer

While occurrences of wavelike motion in the stable boundary layer due to the presence of a significant restoring buoyancy force are rarely disputed, their modalities and interaction with turbulence remain a subject of active research. In this work, the characteristics of gravity waves and their impa...

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Published in:Atmosphere
Main Authors: Daniela Cava, Umberto Giostra, Gabriel Katul
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2015
Subjects:
Online Access:https://doi.org/10.3390/atmos6091271
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spelling ftmdpi:oai:mdpi.com:/2073-4433/6/9/1271/ 2023-08-20T04:01:22+02:00 Characteristics of Gravity Waves over an Antarctic Ice Sheet during an Austral Summer Daniela Cava Umberto Giostra Gabriel Katul agris 2015-08-25 application/pdf https://doi.org/10.3390/atmos6091271 EN eng Multidisciplinary Digital Publishing Institute Biosphere/Hydrosphere/Land–Atmosphere Interactions https://dx.doi.org/10.3390/atmos6091271 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 6; Issue 9; Pages: 1271-1289 Antarctica gravity waves multiresolution decomposition stable boundary layer turbulent fluxes Text 2015 ftmdpi https://doi.org/10.3390/atmos6091271 2023-07-31T20:46:01Z While occurrences of wavelike motion in the stable boundary layer due to the presence of a significant restoring buoyancy force are rarely disputed, their modalities and interaction with turbulence remain a subject of active research. In this work, the characteristics of gravity waves and their impact on flow statistics, including turbulent fluxes, are presented using data collected above an Antarctic Ice sheet during an Austral Summer. Antarctica is an ideal location for exploring the characteristics of gravity waves because of persistent conditions of strong atmospheric stability in the lower troposphere. Periods dominated by wavelike motion have been identified by analysing time series measured by fast response instrumentation. The nature and characteristic of the dominant wavy motions are investigated using Fourier cross-spectral indicators. Moreover, a multi-resolution decomposition has been applied to separate gravity waves from turbulent fluctuations in case of a sufficiently defined spectral gap. Statistics computed after removing wavy disturbances highlight the large impact of gravity waves on second order turbulent quantities including turbulent flux calculations. Text Antarc* Antarctic Antarctica Ice Sheet MDPI Open Access Publishing Antarctic Austral Atmosphere 6 9 1271 1289
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Antarctica
gravity waves
multiresolution decomposition
stable boundary layer
turbulent fluxes
spellingShingle Antarctica
gravity waves
multiresolution decomposition
stable boundary layer
turbulent fluxes
Daniela Cava
Umberto Giostra
Gabriel Katul
Characteristics of Gravity Waves over an Antarctic Ice Sheet during an Austral Summer
topic_facet Antarctica
gravity waves
multiresolution decomposition
stable boundary layer
turbulent fluxes
description While occurrences of wavelike motion in the stable boundary layer due to the presence of a significant restoring buoyancy force are rarely disputed, their modalities and interaction with turbulence remain a subject of active research. In this work, the characteristics of gravity waves and their impact on flow statistics, including turbulent fluxes, are presented using data collected above an Antarctic Ice sheet during an Austral Summer. Antarctica is an ideal location for exploring the characteristics of gravity waves because of persistent conditions of strong atmospheric stability in the lower troposphere. Periods dominated by wavelike motion have been identified by analysing time series measured by fast response instrumentation. The nature and characteristic of the dominant wavy motions are investigated using Fourier cross-spectral indicators. Moreover, a multi-resolution decomposition has been applied to separate gravity waves from turbulent fluctuations in case of a sufficiently defined spectral gap. Statistics computed after removing wavy disturbances highlight the large impact of gravity waves on second order turbulent quantities including turbulent flux calculations.
format Text
author Daniela Cava
Umberto Giostra
Gabriel Katul
author_facet Daniela Cava
Umberto Giostra
Gabriel Katul
author_sort Daniela Cava
title Characteristics of Gravity Waves over an Antarctic Ice Sheet during an Austral Summer
title_short Characteristics of Gravity Waves over an Antarctic Ice Sheet during an Austral Summer
title_full Characteristics of Gravity Waves over an Antarctic Ice Sheet during an Austral Summer
title_fullStr Characteristics of Gravity Waves over an Antarctic Ice Sheet during an Austral Summer
title_full_unstemmed Characteristics of Gravity Waves over an Antarctic Ice Sheet during an Austral Summer
title_sort characteristics of gravity waves over an antarctic ice sheet during an austral summer
publisher Multidisciplinary Digital Publishing Institute
publishDate 2015
url https://doi.org/10.3390/atmos6091271
op_coverage agris
geographic Antarctic
Austral
geographic_facet Antarctic
Austral
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
op_source Atmosphere; Volume 6; Issue 9; Pages: 1271-1289
op_relation Biosphere/Hydrosphere/Land–Atmosphere Interactions
https://dx.doi.org/10.3390/atmos6091271
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos6091271
container_title Atmosphere
container_volume 6
container_issue 9
container_start_page 1271
op_container_end_page 1289
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