Open AccessClimatology of Polar Lows over the Sea of Japan Using the JRA-55 Reanalysis
Author(s) -
Wataru Yanase,
Hiroshi Niino,
Shunichi Watanabe,
Kevin I. Hodges,
Matthias Zahn,
Thomas Spengler,
И.А. Гурвич
Publication year - 2016
Publication title -
journal of climate
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.315
H-Index - 287
eISSN - 1520-0442
pISSN - 0894-8755
DOI - 10.1175/jcli-d-15-0291.1
Subject(s) - extratropical cyclone , climatology , geology , baroclinity , polar , troposphere , cyclone (programming language) , zonal flow (plasma) , cyclogenesis , westerlies , trough (economics) , physics , astronomy , field programmable gate array , computer science , computer hardware , economics , macroeconomics , plasma , quantum mechanics , tokamak
Polar lows are intense meso-α-scale cyclones that develop over the oceans poleward of the main baroclinic zone. A number of previous studies have reported polar low formation over the Sea of Japan within the East Asian winter monsoon. To understand the climatology of polar lows over the Sea of Japan, a tracking algorithm for polar lows is applied to the recent JRA-55 reanalysis. The polar low tracking is applied to 36 cold seasons (October–March) from October 1979 to March 2015. The polar lows over the Sea of Japan reach their maximum intensity on the southeastern side of the midline between the Japanese islands and the Asian continent. Consistent with previous case studies, composite analysis demonstrates that the polar low development is associated with the enhanced northerly flow on the western side of a synoptic-scale extratropical cyclone, with the cold trough in the midtroposphere and with increased heat fluxes from the sea surface. Furthermore, the present climatological study has revealed two dominant directions of motion of the polar lows: southward and eastward. Southward-moving polar lows are steered by a strong northerly flow in the lower troposphere, which is enhanced on the western side of synoptic-scale extratropical cyclones, while the eastward-moving polar lows occur within a planetary-scale westerly flow in the midlatitudes. Thus, the direction of polar low motion reflects the difference in planetary- and synoptic-scale conditions