Evaluation of the Stratospheric Contribution to the Inter‐Annual Variabilities of Tropospheric Methane Growth Rates
Abstract Tropospheric methane (CH4) shows large inter‐annual variability in its growth rates on top of decadal trends, which is usually interpreted as changes in sources or sinks. The contribution of the stratosphere‐troposphere exchange (STE) is often omitted in such analyses. Here, we quantify ann...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2023
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Online Access: | https://doi.org/10.1029/2023GL103350 https://doaj.org/article/9e1a6203d9fa45b4a425897cf1f5931c |
_version_ | 1821774102774415360 |
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author | Peixuan Zhang Yuzhong Zhang Ruosi Liang Wei Chen Xinchun Xie |
author_facet | Peixuan Zhang Yuzhong Zhang Ruosi Liang Wei Chen Xinchun Xie |
author_sort | Peixuan Zhang |
collection | Directory of Open Access Journals: DOAJ Articles |
container_issue | 12 |
container_title | Geophysical Research Letters |
container_volume | 50 |
description | Abstract Tropospheric methane (CH4) shows large inter‐annual variability in its growth rates on top of decadal trends, which is usually interpreted as changes in sources or sinks. The contribution of the stratosphere‐troposphere exchange (STE) is often omitted in such analyses. Here, we quantify annual anomalies of stratosphere‐troposphere CH4 fluxes using varied model‐ or observation‐based methods. Globally, the inter‐annual variability (standard deviation) of this flux during 2000–2020 is 2.0 Tg a−1, producing a variability of ∼0.6 ppb a−1 at the surface, which is only ∼20% of observed surface CH4 growth rate variability. Compared to global averages, high latitudes experience a larger STE‐induced surface variability, which is 80% of the observed surface anomalies in the Antarctic and 44% in the Arctic. Our results suggest that although the STE process is a minor contributor globally, it has a considerable impact over polar regions on the inter‐annual variability of surface CH4 growth rates. |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctic Arctic |
genre_facet | Antarc* Antarctic Arctic |
geographic | Antarctic Arctic The Antarctic |
geographic_facet | Antarctic Arctic The Antarctic |
id | ftdoajarticles:oai:doaj.org/article:9e1a6203d9fa45b4a425897cf1f5931c |
institution | Open Polar |
language | English |
op_collection_id | ftdoajarticles |
op_doi | https://doi.org/10.1029/2023GL103350 |
op_relation | https://doi.org/10.1029/2023GL103350 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL103350 https://doaj.org/article/9e1a6203d9fa45b4a425897cf1f5931c |
op_source | Geophysical Research Letters, Vol 50, Iss 12, Pp n/a-n/a (2023) |
publishDate | 2023 |
publisher | Wiley |
record_format | openpolar |
spelling | ftdoajarticles:oai:doaj.org/article:9e1a6203d9fa45b4a425897cf1f5931c 2025-01-16T19:40:31+00:00 Evaluation of the Stratospheric Contribution to the Inter‐Annual Variabilities of Tropospheric Methane Growth Rates Peixuan Zhang Yuzhong Zhang Ruosi Liang Wei Chen Xinchun Xie 2023-06-01T00:00:00Z https://doi.org/10.1029/2023GL103350 https://doaj.org/article/9e1a6203d9fa45b4a425897cf1f5931c EN eng Wiley https://doi.org/10.1029/2023GL103350 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL103350 https://doaj.org/article/9e1a6203d9fa45b4a425897cf1f5931c Geophysical Research Letters, Vol 50, Iss 12, Pp n/a-n/a (2023) Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL103350 2024-08-05T17:49:23Z Abstract Tropospheric methane (CH4) shows large inter‐annual variability in its growth rates on top of decadal trends, which is usually interpreted as changes in sources or sinks. The contribution of the stratosphere‐troposphere exchange (STE) is often omitted in such analyses. Here, we quantify annual anomalies of stratosphere‐troposphere CH4 fluxes using varied model‐ or observation‐based methods. Globally, the inter‐annual variability (standard deviation) of this flux during 2000–2020 is 2.0 Tg a−1, producing a variability of ∼0.6 ppb a−1 at the surface, which is only ∼20% of observed surface CH4 growth rate variability. Compared to global averages, high latitudes experience a larger STE‐induced surface variability, which is 80% of the observed surface anomalies in the Antarctic and 44% in the Arctic. Our results suggest that although the STE process is a minor contributor globally, it has a considerable impact over polar regions on the inter‐annual variability of surface CH4 growth rates. Article in Journal/Newspaper Antarc* Antarctic Arctic Directory of Open Access Journals: DOAJ Articles Antarctic Arctic The Antarctic Geophysical Research Letters 50 12 |
spellingShingle | Geophysics. Cosmic physics QC801-809 Peixuan Zhang Yuzhong Zhang Ruosi Liang Wei Chen Xinchun Xie Evaluation of the Stratospheric Contribution to the Inter‐Annual Variabilities of Tropospheric Methane Growth Rates |
title | Evaluation of the Stratospheric Contribution to the Inter‐Annual Variabilities of Tropospheric Methane Growth Rates |
title_full | Evaluation of the Stratospheric Contribution to the Inter‐Annual Variabilities of Tropospheric Methane Growth Rates |
title_fullStr | Evaluation of the Stratospheric Contribution to the Inter‐Annual Variabilities of Tropospheric Methane Growth Rates |
title_full_unstemmed | Evaluation of the Stratospheric Contribution to the Inter‐Annual Variabilities of Tropospheric Methane Growth Rates |
title_short | Evaluation of the Stratospheric Contribution to the Inter‐Annual Variabilities of Tropospheric Methane Growth Rates |
title_sort | evaluation of the stratospheric contribution to the inter‐annual variabilities of tropospheric methane growth rates |
topic | Geophysics. Cosmic physics QC801-809 |
topic_facet | Geophysics. Cosmic physics QC801-809 |
url | https://doi.org/10.1029/2023GL103350 https://doaj.org/article/9e1a6203d9fa45b4a425897cf1f5931c |