• LOGIN
    Login with username and password
Repository logo

BORIS Portal

Bern Open Repository and Information System

  • Publications
  • Theses
  • Research Data
  • Projects
  • Organizations
  • Researchers
  • More
  • Collections
  • Statistics
  • LOGIN
    Login with username and password
Repository logo
Unibern.ch
  1. Home
  2. Publications
  3. A climatological analysis of high-precipitation events in Dronning Maud Land, Antarctica, and associated large-scale atmospheric conditions

A climatological analysis of high-precipitation events in Dronning Maud Land, Antarctica, and associated large-scale atmospheric conditions

Details
Files
DOI
10.7892/boris.60014
Publisher DOI
10.1002/2014JD022259
Abstract
The link between high precipitation in Dronning Maud Land (DML), Antarctica, and the large-scale atmospheric circulation is investigated using ERA-Interim data for 1979–2009. High-precipitation events are analyzed at Halvfarryggen situated in the coastal region of DML and at Kohnen Station located in its interior. This study further includes a comprehensive comparison of high precipitation in ERA-Interim with precipitation data from the Antarctic Mesoscale Prediction System (AMPS) and snow accumulation measurements from automatic weather stations (AWSs), with the limitations of such a comparison being discussed. The ERA-Interim and AMPS precipitation data agree very well. However, the correspondence between high precipitation in ERA-Interim and high snow accumulation at the AWSs is relatively weak. High-precipitation events at both Halvfarryggen and Kohnen are typically associated with amplified upper level waves. This large-scale atmospheric flow pattern is preceded by the downstream development of a Rossby wave train from the eastern South Pacific several days before the precipitation event. At the surface, a cyclone located over the Weddell Sea is the main synoptic ingredient for high precipitation both at Halvfarryggen and at Kohnen. A blocking anticyclone downstream is not a requirement for high precipitation per se, but a larger share of blocking occurrences during the highest-precipitation days in DML suggests that these blocks strengthen the vertically integrated water vapor transport (IVT) into DML. A strong link between high precipitation and the IVT perpendicular to the local orography suggests that IVT could be used as a “proxy” for high precipitation, in particular over DML's interior.
Date Issued
2014
Publication Type
Article
Subject(s)
500 Science > 550 Earth sciences & geology
900 History > 910 Geography & travel
500 Science > 530 Physics
Language(s)
en
Author(s)
Welker, Christoph Simon  
Oeschger Centre for Climate Change Research (OCCR)  
Geographisches Institut der Universität Bern (GIUB)  
Romppainen-Martius, Olivia  
Geographisches Institut der Universität Bern (GIUB)  
Oeschger Centre for Climate Change Research (OCCR)  
Froidevaux, Paul Arnaud  
Geographisches Institut der Universität Bern (GIUB)  
Oeschger Centre for Climate Change Research (OCCR)  
Reijmer, Carleen H.
Fischer, Hubertus  
Physikalisches Institut, Klima- und Umweltphysik (KUP)  
Additional Credits
Oeschger Centre for Climate Change Research (OCCR)  
Geographisches Institut der Universität Bern (GIUB)  
Physikalisches Institut, Klima- und Umweltphysik (KUP)  
Journal
Journal of Geophysical Research: Atmospheres
Publisher
American Geophysical Union
ISSN
2169-897X
Access(Rights)
open.access
Show full item
BORIS Portal
Bern Open Repository and Information System
Build: 0eaa7c [ 7.08. 11:06]
Explore
  • Projects
  • Funding
  • Publications
  • Research Data
  • Organizations
  • Researchers
  • Audiovisual Material
  • Software & other digital items
  • Events
More
  • About BORIS Portal
  • BORIS Portal & Open Science
  • Send Feedback
  • Cookie settings
  • Service Policy
Follow us on
  • Mastodon
  • YouTube
  • LinkedIn
UniBe logo
Repository logo COAR Notify