Signatures of gravity wave-induced instabilities in balloon lidar soundings of polar mesospheric clouds
The Balloon Lidar Experiment (BOLIDE), which was part of the Polar Mesospheric Cloud Turbulence (PMC Turbo) Balloon Mission has captured vertical profiles of PMCs during a 6 d flight along the Arctic circle in July 2018. The high-resolution soundings (20 m vertical and 10 s temporal resolution) reve...
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2023
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ftdoajarticles:oai:doaj.org/article:5ce0df2e6d38430a8c41cb5e179a1445 2023-05-15T15:07:04+02:00 Signatures of gravity wave-induced instabilities in balloon lidar soundings of polar mesospheric clouds N. Kaifler B. Kaifler M. Rapp D. C. Fritts 2023-01-01T00:00:00Z https://doi.org/10.5194/acp-23-949-2023 https://doaj.org/article/5ce0df2e6d38430a8c41cb5e179a1445 EN eng Copernicus Publications https://acp.copernicus.org/articles/23/949/2023/acp-23-949-2023.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-23-949-2023 1680-7316 1680-7324 https://doaj.org/article/5ce0df2e6d38430a8c41cb5e179a1445 Atmospheric Chemistry and Physics, Vol 23, Pp 949-961 (2023) Physics QC1-999 Chemistry QD1-999 article 2023 ftdoajarticles https://doi.org/10.5194/acp-23-949-2023 2023-01-22T01:32:04Z The Balloon Lidar Experiment (BOLIDE), which was part of the Polar Mesospheric Cloud Turbulence (PMC Turbo) Balloon Mission has captured vertical profiles of PMCs during a 6 d flight along the Arctic circle in July 2018. The high-resolution soundings (20 m vertical and 10 s temporal resolution) reveal highly structured layers with large gradients in the volume backscatter coefficient. We systematically screen the BOLIDE dataset for small-scale variability by assessing these gradients at high resolution. We find longer tails of the probability density distributions of these gradients compared to a normal distribution, indicating intermittent behaviour. The high occurrence rate of large gradients is assessed in relation to the 15 min averaged layer brightness and the spectral power of short-period (5–62 min) gravity waves based on PMC layer altitude variations. We find that variability on small scales occurs during weak, moderate, and strong gravity wave activity. Layers with below-average brightness are less likely to show small-scale variability in conditions of strong gravity wave activity. We present and discuss the signatures of this small-scale variability, and possibly related dynamical processes, and identify potential cases for future case studies and modelling efforts. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic Atmospheric Chemistry and Physics 23 2 949 961 |
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Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
Physics QC1-999 Chemistry QD1-999 |
spellingShingle |
Physics QC1-999 Chemistry QD1-999 N. Kaifler B. Kaifler M. Rapp D. C. Fritts Signatures of gravity wave-induced instabilities in balloon lidar soundings of polar mesospheric clouds |
topic_facet |
Physics QC1-999 Chemistry QD1-999 |
description |
The Balloon Lidar Experiment (BOLIDE), which was part of the Polar Mesospheric Cloud Turbulence (PMC Turbo) Balloon Mission has captured vertical profiles of PMCs during a 6 d flight along the Arctic circle in July 2018. The high-resolution soundings (20 m vertical and 10 s temporal resolution) reveal highly structured layers with large gradients in the volume backscatter coefficient. We systematically screen the BOLIDE dataset for small-scale variability by assessing these gradients at high resolution. We find longer tails of the probability density distributions of these gradients compared to a normal distribution, indicating intermittent behaviour. The high occurrence rate of large gradients is assessed in relation to the 15 min averaged layer brightness and the spectral power of short-period (5–62 min) gravity waves based on PMC layer altitude variations. We find that variability on small scales occurs during weak, moderate, and strong gravity wave activity. Layers with below-average brightness are less likely to show small-scale variability in conditions of strong gravity wave activity. We present and discuss the signatures of this small-scale variability, and possibly related dynamical processes, and identify potential cases for future case studies and modelling efforts. |
format |
Article in Journal/Newspaper |
author |
N. Kaifler B. Kaifler M. Rapp D. C. Fritts |
author_facet |
N. Kaifler B. Kaifler M. Rapp D. C. Fritts |
author_sort |
N. Kaifler |
title |
Signatures of gravity wave-induced instabilities in balloon lidar soundings of polar mesospheric clouds |
title_short |
Signatures of gravity wave-induced instabilities in balloon lidar soundings of polar mesospheric clouds |
title_full |
Signatures of gravity wave-induced instabilities in balloon lidar soundings of polar mesospheric clouds |
title_fullStr |
Signatures of gravity wave-induced instabilities in balloon lidar soundings of polar mesospheric clouds |
title_full_unstemmed |
Signatures of gravity wave-induced instabilities in balloon lidar soundings of polar mesospheric clouds |
title_sort |
signatures of gravity wave-induced instabilities in balloon lidar soundings of polar mesospheric clouds |
publisher |
Copernicus Publications |
publishDate |
2023 |
url |
https://doi.org/10.5194/acp-23-949-2023 https://doaj.org/article/5ce0df2e6d38430a8c41cb5e179a1445 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
Atmospheric Chemistry and Physics, Vol 23, Pp 949-961 (2023) |
op_relation |
https://acp.copernicus.org/articles/23/949/2023/acp-23-949-2023.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-23-949-2023 1680-7316 1680-7324 https://doaj.org/article/5ce0df2e6d38430a8c41cb5e179a1445 |
op_doi |
https://doi.org/10.5194/acp-23-949-2023 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
23 |
container_issue |
2 |
container_start_page |
949 |
op_container_end_page |
961 |
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1766338635892785152 |