Surface-based observations of cold-air outbreak clouds during the COMBLE field campaign

<p>Cold-air outbreaks (CAOs) are characterized by extreme air–sea energy exchanges and low-level convective clouds over large areas in the high-latitude oceans. As such, CAOs are an important component of the Earth's climate system. The CAOs in the Marine Boundary Layer Experiment (COMBLE...

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Main Authors: Z. Mages, P. Kollias, Z. Zhu, E. P. Luke
Format: Article
Language:English
Published: Copernicus Publications 2023-03-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/23/3561/2023/acp-23-3561-2023.pdf
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author Z. Mages
P. Kollias
P. Kollias
Z. Zhu
E. P. Luke
author_facet Z. Mages
P. Kollias
P. Kollias
Z. Zhu
E. P. Luke
author_sort Z. Mages
collection DOAJ
description <p>Cold-air outbreaks (CAOs) are characterized by extreme air–sea energy exchanges and low-level convective clouds over large areas in the high-latitude oceans. As such, CAOs are an important component of the Earth's climate system. The CAOs in the Marine Boundary Layer Experiment (COMBLE) deployment of the US Department of Energy Atmospheric Radiation Measurement (ARM) Mobile Facility (AMF) provided the first comprehensive view of CAOs using a suite of ground-based observations at the northern coast of Norway. Here, cloud and precipitation observations from 13 CAO cases during COMBLE are analyzed. A vertical air motion retrieval technique is applied to the Ka-band ARM Zenith-pointing Radar (KAZR) observations. The CAO cumulus clouds are characterized by strong updrafts with magnitudes between 2–8 m s<span class="inline-formula"><sup>−1</sup></span>, vertical extents of 1–3 km, and horizontal scales of 0.25–3 km. A strong relationship between our vertical air velocity retrievals and liquid water path (LWP) measurements is found. The LWP measurements exceed 1 kg m<span class="inline-formula"><sup>−2</sup></span> in strong updraft areas, and the vertical extent of the updraft correlates well with the LWP values. The CAO cumulus clouds exhibit eddy dissipation rate values between 10<span class="inline-formula"><sup>−3</sup></span> and 10<span class="inline-formula"><sup>−2</sup></span> m<span class="inline-formula"><sup>2</sup></span> s<span class="inline-formula"><sup>−3</sup></span> in the lowest 10 km of the atmosphere, and using a radar Doppler spectra technique, evidence of secondary ice production is found during one of the cases.</p>
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spelling doaj.art-6e1caa6046ce4721a7ea2728a36f42142023-03-22T11:39:10ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242023-03-01233561357410.5194/acp-23-3561-2023Surface-based observations of cold-air outbreak clouds during the COMBLE field campaignZ. Mages0P. Kollias1P. Kollias2Z. Zhu3E. P. Luke4School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY, USASchool of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY, USAEnvironmental and Climate Sciences Dept., Brookhaven National Laboratory, Upton, NY, USAEnvironmental and Climate Sciences Dept., Brookhaven National Laboratory, Upton, NY, USAEnvironmental and Climate Sciences Dept., Brookhaven National Laboratory, Upton, NY, USA<p>Cold-air outbreaks (CAOs) are characterized by extreme air–sea energy exchanges and low-level convective clouds over large areas in the high-latitude oceans. As such, CAOs are an important component of the Earth's climate system. The CAOs in the Marine Boundary Layer Experiment (COMBLE) deployment of the US Department of Energy Atmospheric Radiation Measurement (ARM) Mobile Facility (AMF) provided the first comprehensive view of CAOs using a suite of ground-based observations at the northern coast of Norway. Here, cloud and precipitation observations from 13 CAO cases during COMBLE are analyzed. A vertical air motion retrieval technique is applied to the Ka-band ARM Zenith-pointing Radar (KAZR) observations. The CAO cumulus clouds are characterized by strong updrafts with magnitudes between 2–8 m s<span class="inline-formula"><sup>−1</sup></span>, vertical extents of 1–3 km, and horizontal scales of 0.25–3 km. A strong relationship between our vertical air velocity retrievals and liquid water path (LWP) measurements is found. The LWP measurements exceed 1 kg m<span class="inline-formula"><sup>−2</sup></span> in strong updraft areas, and the vertical extent of the updraft correlates well with the LWP values. The CAO cumulus clouds exhibit eddy dissipation rate values between 10<span class="inline-formula"><sup>−3</sup></span> and 10<span class="inline-formula"><sup>−2</sup></span> m<span class="inline-formula"><sup>2</sup></span> s<span class="inline-formula"><sup>−3</sup></span> in the lowest 10 km of the atmosphere, and using a radar Doppler spectra technique, evidence of secondary ice production is found during one of the cases.</p>https://acp.copernicus.org/articles/23/3561/2023/acp-23-3561-2023.pdf
spellingShingle Z. Mages
P. Kollias
P. Kollias
Z. Zhu
E. P. Luke
Surface-based observations of cold-air outbreak clouds during the COMBLE field campaign
Atmospheric Chemistry and Physics
title Surface-based observations of cold-air outbreak clouds during the COMBLE field campaign
title_full Surface-based observations of cold-air outbreak clouds during the COMBLE field campaign
title_fullStr Surface-based observations of cold-air outbreak clouds during the COMBLE field campaign
title_full_unstemmed Surface-based observations of cold-air outbreak clouds during the COMBLE field campaign
title_short Surface-based observations of cold-air outbreak clouds during the COMBLE field campaign
title_sort surface based observations of cold air outbreak clouds during the comble field campaign
url https://acp.copernicus.org/articles/23/3561/2023/acp-23-3561-2023.pdf
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AT zzhu surfacebasedobservationsofcoldairoutbreakcloudsduringthecomblefieldcampaign
AT epluke surfacebasedobservationsofcoldairoutbreakcloudsduringthecomblefieldcampaign