Skip to main content

ETHNOS_APP

Home • Search • Journals • List 0

Zonal shift in the cold airmass stream of the East Asian winter monsoon

Bibliographic Data

ID15544613
AuthorsQian Liu (0000-0001-7603-2146, Sun Yat-sen University), Guixing Chen (0000-0002-3112-0668, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), corresponding author)
Year2021
Volume16
Issue12
Pages124028-124028
Publication date2021-11-05
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ac36f5
OpenAlexW3213645590
LanguageEN
References cited29

The East Asian winter monsoon (EAWM) exhibits long-term variations in intensity and spatial pattern, though the latter one is less understood. To investigate the long-term spatial variations of the EAWM and their possible causes, we propose a new position index of the EAWM by quantifying the low-level East Asian stream (EAS) of cold airmass in the Lagrangian sense. Based on the new-defined index, we find that the EAS undergoes an evident zonal shift between two channels over the land and coast. At interdecadal timescale, the peak location of the EAS is displaced eastward, with an increasing southward cold airmass flux at the coast since the mid-1960s. The interannual shift of the EAS presents not only the zonal oscillation of peak location between two channels but also the width changes of coastal channel over the northwestern Pacific. These shifts in the EAS are related to the strength changes of two source cold airmass streams from Siberia or Bering Sea, which are associated with the phase changes in the upper-tropospheric atmospheric teleconnections. At interdecadal timescale, the phase change in the North Atlantic Oscillation modulates the zonal shift in the EAS via the East Atlantic-West Russia teleconnection. At interannual timescale, the Pacific/North American teleconnection becomes the dominant factor altering the zonal shift and width change of the EAS

Climatology · East Asia · East Asian Monsoon · El Niño Southern Oscillation · Geography · Jet (fluid · Jet stream · Monsoon · North Atlantic oscillation · Rainband · Siberian High · Teleconnection · Tropical cyclone · Climate variability and models · Environmental Science · Meteorological Phenomena and Simulations · Oceanographic and Atmospheric Processes · Geology

  • A Formulation of a Phase-Independent Wave-Activity Flux for Stationary and Migratory Quasigeostrophic Eddies on a Zonally Varying Basic Flow

    Koutarou Takaya, Hisashi Nakamura•Journal of the Atmospheric Sciences•2001

  • The JRA-55 Reanalysis

    Open Access•Shinya Kobayashi, Yukinari OTA et al.•Journal of the Meteorological…•2015

  • Robust warming over East Asia during the boreal winter monsoon and its possible causes

    Open Access•Sun‐Seon Lee, Seon‐Hwa Kim et al.•Environmental Research Letters•2013

Citation velocityhistorical
Highly citedNo

Tools

Open DOIOpen Access
Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae