Humidity trends imply increased sensitivity to clouds in a warming Arctic

Infrared radiative processes are implicated in Arctic warming and sea-ice decline. The infrared cloud radiative effect (CRE) at the surface is modulated by cloud properties; however, CRE also depends on humidity because clouds emit at wavelengths that are semi-transparent to greenhouse gases, most n...

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Published in:Nature Communications
Main Authors: Cox, Christopher J., Walden, Von P., Rowe, Penny M., Shupe, Matthew D.
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1240604
https://www.osti.gov/biblio/1240604
https://doi.org/10.1038/ncomms10117
id ftosti:oai:osti.gov:1240604
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spelling ftosti:oai:osti.gov:1240604 2023-07-30T04:00:28+02:00 Humidity trends imply increased sensitivity to clouds in a warming Arctic Cox, Christopher J. Walden, Von P. Rowe, Penny M. Shupe, Matthew D. 2023-06-26 application/pdf http://www.osti.gov/servlets/purl/1240604 https://www.osti.gov/biblio/1240604 https://doi.org/10.1038/ncomms10117 unknown http://www.osti.gov/servlets/purl/1240604 https://www.osti.gov/biblio/1240604 https://doi.org/10.1038/ncomms10117 doi:10.1038/ncomms10117 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.1038/ncomms10117 2023-07-11T09:05:10Z Infrared radiative processes are implicated in Arctic warming and sea-ice decline. The infrared cloud radiative effect (CRE) at the surface is modulated by cloud properties; however, CRE also depends on humidity because clouds emit at wavelengths that are semi-transparent to greenhouse gases, most notably water vapour. Here we show how temperature and humidity control CRE through competing influences between the mid- and far-infrared. At constant relative humidity, CRE does not decrease with increasing temperature/absolute humidity as expected, but rather is found to be approximately constant for temperatures characteristic of the Arctic. This stability is disrupted if relative humidity varies. Our findings explain observed seasonal and regional variability in Arctic CRE of order 10Wm 2 . With the physical properties of Arctic clouds held constant, we calculate recent increases in CRE of 1–5Wm 2 in autumn and winter, which are projected to reach 5–15Wm 2 by 2050, implying increased sensitivity of the surface to clouds. Other/Unknown Material Arctic Sea ice SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic Nature Communications 6 1
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Cox, Christopher J.
Walden, Von P.
Rowe, Penny M.
Shupe, Matthew D.
Humidity trends imply increased sensitivity to clouds in a warming Arctic
topic_facet 54 ENVIRONMENTAL SCIENCES
description Infrared radiative processes are implicated in Arctic warming and sea-ice decline. The infrared cloud radiative effect (CRE) at the surface is modulated by cloud properties; however, CRE also depends on humidity because clouds emit at wavelengths that are semi-transparent to greenhouse gases, most notably water vapour. Here we show how temperature and humidity control CRE through competing influences between the mid- and far-infrared. At constant relative humidity, CRE does not decrease with increasing temperature/absolute humidity as expected, but rather is found to be approximately constant for temperatures characteristic of the Arctic. This stability is disrupted if relative humidity varies. Our findings explain observed seasonal and regional variability in Arctic CRE of order 10Wm 2 . With the physical properties of Arctic clouds held constant, we calculate recent increases in CRE of 1–5Wm 2 in autumn and winter, which are projected to reach 5–15Wm 2 by 2050, implying increased sensitivity of the surface to clouds.
author Cox, Christopher J.
Walden, Von P.
Rowe, Penny M.
Shupe, Matthew D.
author_facet Cox, Christopher J.
Walden, Von P.
Rowe, Penny M.
Shupe, Matthew D.
author_sort Cox, Christopher J.
title Humidity trends imply increased sensitivity to clouds in a warming Arctic
title_short Humidity trends imply increased sensitivity to clouds in a warming Arctic
title_full Humidity trends imply increased sensitivity to clouds in a warming Arctic
title_fullStr Humidity trends imply increased sensitivity to clouds in a warming Arctic
title_full_unstemmed Humidity trends imply increased sensitivity to clouds in a warming Arctic
title_sort humidity trends imply increased sensitivity to clouds in a warming arctic
publishDate 2023
url http://www.osti.gov/servlets/purl/1240604
https://www.osti.gov/biblio/1240604
https://doi.org/10.1038/ncomms10117
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_relation http://www.osti.gov/servlets/purl/1240604
https://www.osti.gov/biblio/1240604
https://doi.org/10.1038/ncomms10117
doi:10.1038/ncomms10117
op_doi https://doi.org/10.1038/ncomms10117
container_title Nature Communications
container_volume 6
container_issue 1
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