On the Relationship Between the Marine Cold Air Outbreak M Parameter and Low-Level Cloud Heights in the Midlatitudes

Focusing on conditions of subsidence when low clouds are present, ground-based observations in both the North Atlantic and the Southern Ocean reveal strong relationships between cloud boundary (base and top heights) and different measures of lower tropospheric instability. The difference in potentia...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Naud, Catherine M., Booth, James F., Lamer, Katia, Marchand, Roger, Protat, Alain, McFarquhar, Greg M.
Language:unknown
Published: 2021
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1802938
https://www.osti.gov/biblio/1802938
https://doi.org/10.1029/2020jd032465
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spelling ftosti:oai:osti.gov:1802938 2023-07-30T04:05:20+02:00 On the Relationship Between the Marine Cold Air Outbreak M Parameter and Low-Level Cloud Heights in the Midlatitudes Naud, Catherine M. Booth, James F. Lamer, Katia Marchand, Roger Protat, Alain McFarquhar, Greg M. 2021-08-16 application/pdf http://www.osti.gov/servlets/purl/1802938 https://www.osti.gov/biblio/1802938 https://doi.org/10.1029/2020jd032465 unknown http://www.osti.gov/servlets/purl/1802938 https://www.osti.gov/biblio/1802938 https://doi.org/10.1029/2020jd032465 doi:10.1029/2020jd032465 54 ENVIRONMENTAL SCIENCES 2021 ftosti https://doi.org/10.1029/2020jd032465 2023-07-11T10:04:50Z Focusing on conditions of subsidence when low clouds are present, ground-based observations in both the North Atlantic and the Southern Ocean reveal strong relationships between cloud boundary (base and top heights) and different measures of lower tropospheric instability. The difference in potential temperature between the surface and 800 hPa (a metric called M) provides a stronger relationship than measures of inversion strength such as the lower tropospheric stability and estimated inversion strength. This is because (1) inversion strength itself does not correlate well with cloud boundaries, and (2) M contains information that appears important for cloud boundaries. These include the surface forcing through the use of sea surface rather than near-surface air temperature and an upper level close to the real cloud top. These results expand upon previous work on the importance of M as a predictor of cloud morphology. However, important differences are found in low-cloud conditions for the North Atlantic as compared to the Southern Ocean (for a given value of M): stronger inversions, deeper boundary layers, and much larger sea level pressures. Therefore, the relationship between cloud boundaries and M differs between the two regions. A general circulation model provides similar relationships as observed between M and both cloud top height and temperature but tends to place clouds higher and at colder temperatures than observed for a given M. This might cause issues with the representation of precipitation, cloud cover and radiation in the Southern Ocean. Other/Unknown Material North Atlantic Southern Ocean SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Southern Ocean Journal of Geophysical Research: Atmospheres 125 13
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
Naud, Catherine M.
Booth, James F.
Lamer, Katia
Marchand, Roger
Protat, Alain
McFarquhar, Greg M.
On the Relationship Between the Marine Cold Air Outbreak M Parameter and Low-Level Cloud Heights in the Midlatitudes
topic_facet 54 ENVIRONMENTAL SCIENCES
description Focusing on conditions of subsidence when low clouds are present, ground-based observations in both the North Atlantic and the Southern Ocean reveal strong relationships between cloud boundary (base and top heights) and different measures of lower tropospheric instability. The difference in potential temperature between the surface and 800 hPa (a metric called M) provides a stronger relationship than measures of inversion strength such as the lower tropospheric stability and estimated inversion strength. This is because (1) inversion strength itself does not correlate well with cloud boundaries, and (2) M contains information that appears important for cloud boundaries. These include the surface forcing through the use of sea surface rather than near-surface air temperature and an upper level close to the real cloud top. These results expand upon previous work on the importance of M as a predictor of cloud morphology. However, important differences are found in low-cloud conditions for the North Atlantic as compared to the Southern Ocean (for a given value of M): stronger inversions, deeper boundary layers, and much larger sea level pressures. Therefore, the relationship between cloud boundaries and M differs between the two regions. A general circulation model provides similar relationships as observed between M and both cloud top height and temperature but tends to place clouds higher and at colder temperatures than observed for a given M. This might cause issues with the representation of precipitation, cloud cover and radiation in the Southern Ocean.
author Naud, Catherine M.
Booth, James F.
Lamer, Katia
Marchand, Roger
Protat, Alain
McFarquhar, Greg M.
author_facet Naud, Catherine M.
Booth, James F.
Lamer, Katia
Marchand, Roger
Protat, Alain
McFarquhar, Greg M.
author_sort Naud, Catherine M.
title On the Relationship Between the Marine Cold Air Outbreak M Parameter and Low-Level Cloud Heights in the Midlatitudes
title_short On the Relationship Between the Marine Cold Air Outbreak M Parameter and Low-Level Cloud Heights in the Midlatitudes
title_full On the Relationship Between the Marine Cold Air Outbreak M Parameter and Low-Level Cloud Heights in the Midlatitudes
title_fullStr On the Relationship Between the Marine Cold Air Outbreak M Parameter and Low-Level Cloud Heights in the Midlatitudes
title_full_unstemmed On the Relationship Between the Marine Cold Air Outbreak M Parameter and Low-Level Cloud Heights in the Midlatitudes
title_sort on the relationship between the marine cold air outbreak m parameter and low-level cloud heights in the midlatitudes
publishDate 2021
url http://www.osti.gov/servlets/purl/1802938
https://www.osti.gov/biblio/1802938
https://doi.org/10.1029/2020jd032465
geographic Southern Ocean
geographic_facet Southern Ocean
genre North Atlantic
Southern Ocean
genre_facet North Atlantic
Southern Ocean
op_relation http://www.osti.gov/servlets/purl/1802938
https://www.osti.gov/biblio/1802938
https://doi.org/10.1029/2020jd032465
doi:10.1029/2020jd032465
op_doi https://doi.org/10.1029/2020jd032465
container_title Journal of Geophysical Research: Atmospheres
container_volume 125
container_issue 13
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