Synoptic Drivers of Atmospheric River Induced Precipitation Near Dronning Maud Land, Antarctica
Abstract
Abstract Atmospheric rivers (ARs) that reach the Antarctic Ice Sheet (AIS) transport anomalous moisture from lower latitudes and can impact the AIS via extreme precipitation and increased downward longwave radiation. ARs contribute significantly to the interannual variability of precipitation over the AIS and thus are likely to play a key role in understanding future changes in the surface mass balance of the AIS. Dronning Maud Land (DML) is one of four maxima in AR frequency over coastal East Antarctica, with AR precipitation explaining 77% of the interannual variability in precipitation for this region. We employ a 16‐node self‐organizing map (SOM) trained with MERRA‐2 sea‐level pressure anomalies to identify synoptic‐scale environments associated with landfalling ARs in and around DML. Node composites of atmospheric variables reveal common drivers of precipitation associated with ARs reaching DML including anomalous high‐low surface pressure couplets, anomalously high integrated water vapor, and coastal barrier jets. Using a quasi‐geostrophic framework, we find that upward vertical motion associated with the occlusion process of attendant cyclones dominates atmospheric lift in AR environments. We further identify mechanisms that explain the variability in AR precipitation intensity across nodes, such as the lift associated with the occlusion process of attendant cyclones and themore »
- Authors:
-
- Univ. of Colorado, Boulder, CO (United States)
- National Center for Atmospheric Research (NCAR), Boulder, CO (United States)
- Publication Date:
- Research Org.:
- University Corporation for Atmospheric Research (UCAR), Boulder, CO (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC), Biological and Environmental Research (BER)
- OSTI Identifier:
- 1970355
- Alternate Identifier(s):
- OSTI ID: 1972740
- Grant/Contract Number:
- SC0022070; DE‐SC0022070
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Geophysical Research: Atmospheres
- Additional Journal Information:
- Journal Volume: 128; Journal Issue: 7; Journal ID: ISSN 2169-897X
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES
Citation Formats
Baiman, Rebecca, Winters, Andrew C., Lenaerts, Jan, and Shields, Christine A. Synoptic Drivers of Atmospheric River Induced Precipitation Near Dronning Maud Land, Antarctica. United States: N. p., 2023.
Web. doi:10.1029/2022jd037859.
Baiman, Rebecca, Winters, Andrew C., Lenaerts, Jan, & Shields, Christine A. Synoptic Drivers of Atmospheric River Induced Precipitation Near Dronning Maud Land, Antarctica. United States. https://doi.org/10.1029/2022jd037859
Baiman, Rebecca, Winters, Andrew C., Lenaerts, Jan, and Shields, Christine A. Sat .
"Synoptic Drivers of Atmospheric River Induced Precipitation Near Dronning Maud Land, Antarctica". United States. https://doi.org/10.1029/2022jd037859. https://www.osti.gov/servlets/purl/1970355.
@article{osti_1970355,
title = {Synoptic Drivers of Atmospheric River Induced Precipitation Near Dronning Maud Land, Antarctica},
author = {Baiman, Rebecca and Winters, Andrew C. and Lenaerts, Jan and Shields, Christine A.},
abstractNote = {Abstract Atmospheric rivers (ARs) that reach the Antarctic Ice Sheet (AIS) transport anomalous moisture from lower latitudes and can impact the AIS via extreme precipitation and increased downward longwave radiation. ARs contribute significantly to the interannual variability of precipitation over the AIS and thus are likely to play a key role in understanding future changes in the surface mass balance of the AIS. Dronning Maud Land (DML) is one of four maxima in AR frequency over coastal East Antarctica, with AR precipitation explaining 77% of the interannual variability in precipitation for this region. We employ a 16‐node self‐organizing map (SOM) trained with MERRA‐2 sea‐level pressure anomalies to identify synoptic‐scale environments associated with landfalling ARs in and around DML. Node composites of atmospheric variables reveal common drivers of precipitation associated with ARs reaching DML including anomalous high‐low surface pressure couplets, anomalously high integrated water vapor, and coastal barrier jets. Using a quasi‐geostrophic framework, we find that upward vertical motion associated with the occlusion process of attendant cyclones dominates atmospheric lift in AR environments. We further identify mechanisms that explain the variability in AR precipitation intensity across nodes, such as the lift associated with the occlusion process of attendant cyclones and the spatial coincidence of ascent induced by the occlusion process and frontogenesis. The latter suggests that ARs making landfall during the mature phase of cyclogenesis result in higher precipitation intensity compared to landfalling ARs that occur during the occluded phase.},
doi = {10.1029/2022jd037859},
journal = {Journal of Geophysical Research: Atmospheres},
number = 7,
volume = 128,
place = {United States},
year = {Sat Mar 25 00:00:00 EDT 2023},
month = {Sat Mar 25 00:00:00 EDT 2023}
}
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