Number of the records: 1  

Spatial changes in two major modes of atmospheric circulation variability during the 20th century

  1. 1.
    0580719 - ÚFA 2024 RIV CZ eng J - Journal Article
    Piskala, V. - Huth, Radan
    Spatial changes in two major modes of atmospheric circulation variability during the 20th century.
    Geografie. Roč. 128, č. 4 (2023), s. 379-396. ISSN 1212-0014. E-ISSN 2571-421X
    R&D Projects: GA ČR(CZ) GA17-07043S
    Institutional support: RVO:68378289
    Keywords : teleconnections * North Atlantic Oscillation * Pacific/North American Pattern * atmospheric circulation * modes of variability
    OECD category: Meteorology and atmospheric sciences
    Impact factor: 0.9, year: 2022
    Method of publishing: Open access
    https://geografie.cz/media/pdf/geografie.2023.017.pdf

    This study presents the time development of two major modes of atmospheric circulation variability in the Northern Hemisphere, the North Atlantic Oscillation (NAO) and the Pacific/North American Pattern (PNA), during the 20th century. We employ 500 hPa winter monthly means of the long-term reanalysis 20CR, which cover the 1871-2011 period. We use a moving Principal Component Analysis calculated for 40-year periods with a one-year step. The spatial structure of NAO is well developed and stable during the whole 20th century using the ensemble mean. However, substantial changes in PNA pattern occur during the late 19th century. Its centres are weaker and smaller, except the centre over the northern Pacific Ocean, which is stronger and larger in the early period. However, these changes are not visible when using ensemble members. Therefore, we suggest that these shifts do not reflect real changes in the atmosphere but are produced by the reanalysis and statistical method itself.
    Permanent Link: https://hdl.handle.net/11104/0349477

     
    FileDownloadSizeCommentaryVersionAccess
    0580719_Geografie_Huth_2023.pdf26.8 MBPublisher’s postprintrequire
     
Number of the records: 1  

  This site uses cookies to make them easier to browse. Learn more about how we use cookies.