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Insights on sources and formation mechanisms of liquid-bearing clouds over MosaiC examined from a Lagrangian framework

Bibliographic Data

ID19568445
AuthorsIsrael Silber (0000-0001-6588-2145, Pennsylvania State University), Matthew D Shupe (0000-0002-0973-9982, Cooperative Institute for Research in Environmental Sciences)
Year2022
Volume10
Issue1
Publication date2022-03-16
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.1525/elementa.2021.000071
OpenAlexW4225109020
LanguageEN
Citations received1
References cited79

Understanding Arctic stratiform liquid-bearing cloud life cycles and properly representing these life cycles in models is crucial for evaluations of cloud feedbacks as well as the faithfulness of climate projections for this rapidly warming region. Examination of cloud life cycles typically requires analyses of cloud evolution and origins on short time scales, on the order of hours to several days. Measurements from the recent Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition provide a unique view of the current state of the central Arctic over an annual cycle. Here, we use the MOSAiC radiosonde measurements to detect liquid-bearing cloud layers over full atmospheric columns and to examine the cloud-generating air masses’ properties. We perform 5-day (120 h) back-trajectory calculations for every detected cloud and cluster them using a unique set of variables extracted from these trajectories informed by ERA5 reanalysis data. This clustering method enables us to separate between the air mass source regions such as ice-covered Arctic and midlatitude open water. We find that moisture intrusions into the central Arctic typically result in multilayer liquid-bearing cloud structures and that more than half of multilayer profiles include overlying liquid-bearing clouds originating in different types of air masses. Finally, we conclude that Arctic cloud formation via prolonged radiative cooling of elevated stable subsaturated air masses circulating over the Arctic can occur frequently (up to 20% of detected clouds in the sounding data set) and may lead to a significant impact of ensuing clouds on the surface energy budget, including net surface warming in some cases

Air mass (solar energy) · Arctic · Atmospheric sciences · Climatology · Cloud computing · Cloud top · Depth sounding · Geography · Lidar · Liquid water content · Meteorology · Middle latitudes · Physics · Radiosonde · Remote sensing · Atmospheric aerosols and clouds · Atmospheric chemistry and aerosols · Climate variability and models · Computer Science · Environmental Science · Geology · Oceanography

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Citations per year0.25
Citation span2022 - 2022 (1)
Highly citedNo

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