YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of Climate
    • View Item
    •   YE&T Library
    • AMS
    • Journal of Climate
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    Atmospheric Patterns over the Antarctic Peninsula

    Source: Journal of Climate:;2018:;volume 031:;issue 009::page 3597
    Author:
    Gonzalez, Sergi
    ,
    Vasallo, Francisco
    ,
    Recio-Blitz, Cayetana
    ,
    Guijarro, José A.
    ,
    Riesco, Jesús
    DOI: 10.1175/JCLI-D-17-0598.1
    Publisher: American Meteorological Society
    Abstract: AbstractUsing clustering analysis for the sea level pressure field of the ERA-Interim reanalysis between 1979 and 2016, five synoptic pressure patterns have been obtained for the Drake area and Antarctic Peninsula (AP) region (45°?75°S, 20°?120°W), and the resulting daily series has been made available to the scientific community. The five patterns have been named according to their most important features as follows: low over the Weddell Sea (LWS), low over the Amundsen and Bellingshausen Seas (LAB), low over the Drake Passage (LDP), zonal flow over the Drake Passage (ZDP), and ridge over the Antarctic Peninsula (RAP). Each atmospheric pattern is described after analyzing its development and evolution. A frequency analysis shows that the five atmospheric patterns present a similar annual frequency but a large seasonal variability. The transitions from one pattern to another tend to follow a cycle in which synoptic atmospheric waves are displaced eastward by a quarter wavelength. Four of the five atmospheric patterns (all except RAP) are very influenced by the southern annular mode (SAM); however, only LAB and LWS are influenced to some degree by ENSO. The occurrence of the LAB pattern presents a positive trend showing agreement with other studies that indicate an enhancement of the Amundsen?Bellingshausen Seas low. Finally, atmospheric circulation patterns have been related to the airmass advection and precipitation in Livingston Island, showing the potential application for studying the changes in the surface mass balance on the AP cryosphere.
    • Download: (1005.Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Statistics

      Atmospheric Patterns over the Antarctic Peninsula

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4262259
    Collections
    • Journal of Climate

    Show full item record

    contributor authorGonzalez, Sergi
    contributor authorVasallo, Francisco
    contributor authorRecio-Blitz, Cayetana
    contributor authorGuijarro, José A.
    contributor authorRiesco, Jesús
    date accessioned2019-09-19T10:09:53Z
    date available2019-09-19T10:09:53Z
    date copyright1/22/2018 12:00:00 AM
    date issued2018
    identifier otherjcli-d-17-0598.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4262259
    description abstractAbstractUsing clustering analysis for the sea level pressure field of the ERA-Interim reanalysis between 1979 and 2016, five synoptic pressure patterns have been obtained for the Drake area and Antarctic Peninsula (AP) region (45°?75°S, 20°?120°W), and the resulting daily series has been made available to the scientific community. The five patterns have been named according to their most important features as follows: low over the Weddell Sea (LWS), low over the Amundsen and Bellingshausen Seas (LAB), low over the Drake Passage (LDP), zonal flow over the Drake Passage (ZDP), and ridge over the Antarctic Peninsula (RAP). Each atmospheric pattern is described after analyzing its development and evolution. A frequency analysis shows that the five atmospheric patterns present a similar annual frequency but a large seasonal variability. The transitions from one pattern to another tend to follow a cycle in which synoptic atmospheric waves are displaced eastward by a quarter wavelength. Four of the five atmospheric patterns (all except RAP) are very influenced by the southern annular mode (SAM); however, only LAB and LWS are influenced to some degree by ENSO. The occurrence of the LAB pattern presents a positive trend showing agreement with other studies that indicate an enhancement of the Amundsen?Bellingshausen Seas low. Finally, atmospheric circulation patterns have been related to the airmass advection and precipitation in Livingston Island, showing the potential application for studying the changes in the surface mass balance on the AP cryosphere.
    publisherAmerican Meteorological Society
    titleAtmospheric Patterns over the Antarctic Peninsula
    typeJournal Paper
    journal volume31
    journal issue9
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-17-0598.1
    journal fristpage3597
    journal lastpage3608
    treeJournal of Climate:;2018:;volume 031:;issue 009
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian