Analysis of 24 years of mesopause region OH rotational temperature observations at Davis, Antarctica – Part 1: long-term trends

The long-term trend, solar cycle response, and residual variability in 24 years of hydroxyl nightglow rotational temperatures above Davis research station, Antarctica (68◦ S, 78◦ E) are reported. Hydroxyl rotational temperatures are a layer-weighted proxy for kinetic temperatures near 87 km altitude...

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Main Authors: French, W. John R., Mulligan, Frank J., Klekociuk, Andrew R.
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://mural.maynoothuniversity.ie/15935/
https://mural.maynoothuniversity.ie/15935/1/FrankMulligan2022Part1.pdf
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spelling ftunivmaynooth:oai:mural.maynoothuniversity.ie:15935 2023-05-15T13:51:44+02:00 Analysis of 24 years of mesopause region OH rotational temperature observations at Davis, Antarctica – Part 1: long-term trends French, W. John R. Mulligan, Frank J. Klekociuk, Andrew R. 2020 text https://mural.maynoothuniversity.ie/15935/ https://mural.maynoothuniversity.ie/15935/1/FrankMulligan2022Part1.pdf en eng https://mural.maynoothuniversity.ie/15935/1/FrankMulligan2022Part1.pdf French, W. John R. and Mulligan, Frank J. and Klekociuk, Andrew R. (2020) Analysis of 24 years of mesopause region OH rotational temperature observations at Davis, Antarctica – Part 1: long-term trends. Atmospheric Chemistry and Physics, 20 (11). pp. 6379-6394. ISSN 1680-7324 Article PeerReviewed 2020 ftunivmaynooth 2022-06-13T18:49:20Z The long-term trend, solar cycle response, and residual variability in 24 years of hydroxyl nightglow rotational temperatures above Davis research station, Antarctica (68◦ S, 78◦ E) are reported. Hydroxyl rotational temperatures are a layer-weighted proxy for kinetic temperatures near 87 km altitude and have been used for many decades to monitor trends in the mesopause region in response to increasing greenhouse gas emissions. Routine observations of the OH(6-2) band P-branch emission lines using a scanning spectrometer at Davis station have been made continuously over each winter season since 1995. Significant outcomes of this most recent analysis update are the following: (a) a record-low winter-average temperature of 198.3 K is obtained for 2018 (1.7 K below previous low in 2009); (b) a long-term cooling trend of −1.2 ± 0.51 K per decade persists, coupled with a solar cycle response of 4.3±1.02 K per 100 solar flux units; and (c) we find evidence in the residual winter mean temperatures of an oscillation on a quasi quadrennial (QQO) timescale which is investigated in detail in Part 2 of this work. Our observations and trend analyses are compared with satellite measurements from Aura/MLS version v4.2 level-2 data over the last 14 years, and we find close agreement (a best fit to temperature anomalies) with the 0.00464 hPa pressure level values. The solar cycle response (3.4 ± 2.3 K per 100 sfu), long-term trend (−1.3±1.2 K per decade), and underlying QQO residuals in Aura/MLS are consistent with the Davis observations. Consequently, we extend the Aura/MLS trend analysis to provide a global view of solar response and long-term trend for Southern and Northern Hemisphere winter seasons at the 0.00464 hPa pressure level to compare with other observers and models. Article in Journal/Newspaper Antarc* Antarctica Maynooth University ePrints and eTheses Archive (National University of Ireland) Davis Station ENVELOPE(77.968,77.968,-68.576,-68.576) Davis-Station ENVELOPE(77.968,77.968,-68.576,-68.576)
institution Open Polar
collection Maynooth University ePrints and eTheses Archive (National University of Ireland)
op_collection_id ftunivmaynooth
language English
description The long-term trend, solar cycle response, and residual variability in 24 years of hydroxyl nightglow rotational temperatures above Davis research station, Antarctica (68◦ S, 78◦ E) are reported. Hydroxyl rotational temperatures are a layer-weighted proxy for kinetic temperatures near 87 km altitude and have been used for many decades to monitor trends in the mesopause region in response to increasing greenhouse gas emissions. Routine observations of the OH(6-2) band P-branch emission lines using a scanning spectrometer at Davis station have been made continuously over each winter season since 1995. Significant outcomes of this most recent analysis update are the following: (a) a record-low winter-average temperature of 198.3 K is obtained for 2018 (1.7 K below previous low in 2009); (b) a long-term cooling trend of −1.2 ± 0.51 K per decade persists, coupled with a solar cycle response of 4.3±1.02 K per 100 solar flux units; and (c) we find evidence in the residual winter mean temperatures of an oscillation on a quasi quadrennial (QQO) timescale which is investigated in detail in Part 2 of this work. Our observations and trend analyses are compared with satellite measurements from Aura/MLS version v4.2 level-2 data over the last 14 years, and we find close agreement (a best fit to temperature anomalies) with the 0.00464 hPa pressure level values. The solar cycle response (3.4 ± 2.3 K per 100 sfu), long-term trend (−1.3±1.2 K per decade), and underlying QQO residuals in Aura/MLS are consistent with the Davis observations. Consequently, we extend the Aura/MLS trend analysis to provide a global view of solar response and long-term trend for Southern and Northern Hemisphere winter seasons at the 0.00464 hPa pressure level to compare with other observers and models.
format Article in Journal/Newspaper
author French, W. John R.
Mulligan, Frank J.
Klekociuk, Andrew R.
spellingShingle French, W. John R.
Mulligan, Frank J.
Klekociuk, Andrew R.
Analysis of 24 years of mesopause region OH rotational temperature observations at Davis, Antarctica – Part 1: long-term trends
author_facet French, W. John R.
Mulligan, Frank J.
Klekociuk, Andrew R.
author_sort French, W. John R.
title Analysis of 24 years of mesopause region OH rotational temperature observations at Davis, Antarctica – Part 1: long-term trends
title_short Analysis of 24 years of mesopause region OH rotational temperature observations at Davis, Antarctica – Part 1: long-term trends
title_full Analysis of 24 years of mesopause region OH rotational temperature observations at Davis, Antarctica – Part 1: long-term trends
title_fullStr Analysis of 24 years of mesopause region OH rotational temperature observations at Davis, Antarctica – Part 1: long-term trends
title_full_unstemmed Analysis of 24 years of mesopause region OH rotational temperature observations at Davis, Antarctica – Part 1: long-term trends
title_sort analysis of 24 years of mesopause region oh rotational temperature observations at davis, antarctica – part 1: long-term trends
publishDate 2020
url https://mural.maynoothuniversity.ie/15935/
https://mural.maynoothuniversity.ie/15935/1/FrankMulligan2022Part1.pdf
long_lat ENVELOPE(77.968,77.968,-68.576,-68.576)
ENVELOPE(77.968,77.968,-68.576,-68.576)
geographic Davis Station
Davis-Station
geographic_facet Davis Station
Davis-Station
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation https://mural.maynoothuniversity.ie/15935/1/FrankMulligan2022Part1.pdf
French, W. John R. and Mulligan, Frank J. and Klekociuk, Andrew R. (2020) Analysis of 24 years of mesopause region OH rotational temperature observations at Davis, Antarctica – Part 1: long-term trends. Atmospheric Chemistry and Physics, 20 (11). pp. 6379-6394. ISSN 1680-7324
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