Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet
In the southern winter polar stratosphere, the distribution of gravity wave momentum flux in many state-of-the-art climate simulations is inconsistent with long-time satellite and superpressure balloon observations around 60 ∘ S. Recent studies hint that a lateral shift between prominent gravity wav...
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ftcopernicus:oai:publications.copernicus.org:acp93099 2023-05-15T18:02:19+02:00 Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet Strube, Cornelia Preusse, Peter Ern, Manfred Riese, Martin 2021-12-22 application/pdf https://doi.org/10.5194/acp-21-18641-2021 https://acp.copernicus.org/articles/21/18641/2021/ eng eng doi:10.5194/acp-21-18641-2021 https://acp.copernicus.org/articles/21/18641/2021/ eISSN: 1680-7324 Text 2021 ftcopernicus https://doi.org/10.5194/acp-21-18641-2021 2021-12-27T17:22:18Z In the southern winter polar stratosphere, the distribution of gravity wave momentum flux in many state-of-the-art climate simulations is inconsistent with long-time satellite and superpressure balloon observations around 60 ∘ S. Recent studies hint that a lateral shift between prominent gravity wave sources in the tropospheric mid-latitudes and the location where gravity wave activity is present in the stratosphere causes at least part of the discrepancy. This lateral shift cannot be represented by the column-based gravity wave drag parameterisations used in most general circulation models. However, recent high-resolution analysis and re-analysis products of the European Centre for Medium-Range Weather Forecasts Integrated Forecast System (ECMWF-IFS) show good agreement with the observations and allow for a detailed investigation of resolved gravity waves, their sources, and propagation paths. In this paper, we identify resolved gravity waves in the ECMWF-IFS analyses for a case of high gravity wave activity in the lower stratosphere using small-volume sinusoidal fits to characterise these gravity waves. The 3D wave vector together with perturbation amplitudes, wave frequency, and a fully described background atmosphere are then used to initialise the Gravity Wave Regional or Global Ray Tracer (GROGRAT) gravity wave ray tracer and follow the gravity waves backwards from the stratosphere. Finally, we check for the indication of source processes on the path of each ray and, thus, quantitatively attribute gravity waves to sources that are represented within the model. We find that stratospheric gravity waves are indeed subject to far ( >1000 km) lateral displacement from their sources, which already take place at low altitudes ( <20 km). Various source processes can be linked to waves within stratospheric gravity wave (GW) patterns, such as the orography equatorward of 50 ∘ S and non-orographic sources above the Southern Ocean. These findings may explain why superpressure balloons observe enhanced gravity wave momentum fluxes in the lower stratosphere over the Southern Ocean despite an apparent lack of sources at this latitude. Our results also support the need to improve gravity wave parameterisations to account for meridional propagation. Text polar night Southern Ocean Copernicus Publications: E-Journals Southern Ocean Atmospheric Chemistry and Physics 21 24 18641 18668 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
In the southern winter polar stratosphere, the distribution of gravity wave momentum flux in many state-of-the-art climate simulations is inconsistent with long-time satellite and superpressure balloon observations around 60 ∘ S. Recent studies hint that a lateral shift between prominent gravity wave sources in the tropospheric mid-latitudes and the location where gravity wave activity is present in the stratosphere causes at least part of the discrepancy. This lateral shift cannot be represented by the column-based gravity wave drag parameterisations used in most general circulation models. However, recent high-resolution analysis and re-analysis products of the European Centre for Medium-Range Weather Forecasts Integrated Forecast System (ECMWF-IFS) show good agreement with the observations and allow for a detailed investigation of resolved gravity waves, their sources, and propagation paths. In this paper, we identify resolved gravity waves in the ECMWF-IFS analyses for a case of high gravity wave activity in the lower stratosphere using small-volume sinusoidal fits to characterise these gravity waves. The 3D wave vector together with perturbation amplitudes, wave frequency, and a fully described background atmosphere are then used to initialise the Gravity Wave Regional or Global Ray Tracer (GROGRAT) gravity wave ray tracer and follow the gravity waves backwards from the stratosphere. Finally, we check for the indication of source processes on the path of each ray and, thus, quantitatively attribute gravity waves to sources that are represented within the model. We find that stratospheric gravity waves are indeed subject to far ( >1000 km) lateral displacement from their sources, which already take place at low altitudes ( <20 km). Various source processes can be linked to waves within stratospheric gravity wave (GW) patterns, such as the orography equatorward of 50 ∘ S and non-orographic sources above the Southern Ocean. These findings may explain why superpressure balloons observe enhanced gravity wave momentum fluxes in the lower stratosphere over the Southern Ocean despite an apparent lack of sources at this latitude. Our results also support the need to improve gravity wave parameterisations to account for meridional propagation. |
format |
Text |
author |
Strube, Cornelia Preusse, Peter Ern, Manfred Riese, Martin |
spellingShingle |
Strube, Cornelia Preusse, Peter Ern, Manfred Riese, Martin Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet |
author_facet |
Strube, Cornelia Preusse, Peter Ern, Manfred Riese, Martin |
author_sort |
Strube, Cornelia |
title |
Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet |
title_short |
Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet |
title_full |
Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet |
title_fullStr |
Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet |
title_full_unstemmed |
Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet |
title_sort |
propagation paths and source distributions of resolved gravity waves in ecmwf-ifs analysis fields around the southern polar night jet |
publishDate |
2021 |
url |
https://doi.org/10.5194/acp-21-18641-2021 https://acp.copernicus.org/articles/21/18641/2021/ |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
polar night Southern Ocean |
genre_facet |
polar night Southern Ocean |
op_source |
eISSN: 1680-7324 |
op_relation |
doi:10.5194/acp-21-18641-2021 https://acp.copernicus.org/articles/21/18641/2021/ |
op_doi |
https://doi.org/10.5194/acp-21-18641-2021 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
21 |
container_issue |
24 |
container_start_page |
18641 |
op_container_end_page |
18668 |
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1766172124588802048 |