Synoptic climatology associated with extreme snowfall events in Sapporo city of northern Japan

Abstract Synoptic‐scale atmospheric circulations are crucial for extreme snowfall events. On the basis of topmost 100 snowfall intensity days in Sapporo, Hokkaido, Japan over winter seasons from 1992 to 2011, this study uses principal component analysis and K‐means clustering to characterize synopti...

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Published in:Atmospheric Science Letters
Main Authors: Farukh, M. A., Yamada, Tomohito J.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2014
Subjects:
Online Access:http://dx.doi.org/10.1002/asl2.497
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spelling crwiley:10.1002/asl2.497 2024-09-15T17:36:28+00:00 Synoptic climatology associated with extreme snowfall events in Sapporo city of northern Japan Farukh, M. A. Yamada, Tomohito J. 2014 http://dx.doi.org/10.1002/asl2.497 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl2.497 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl2.497 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Atmospheric Science Letters volume 15, issue 4, page 259-265 ISSN 1530-261X 1530-261X journal-article 2014 crwiley https://doi.org/10.1002/asl2.497 2024-08-09T04:26:58Z Abstract Synoptic‐scale atmospheric circulations are crucial for extreme snowfall events. On the basis of topmost 100 snowfall intensity days in Sapporo, Hokkaido, Japan over winter seasons from 1992 to 2011, this study uses principal component analysis and K‐means clustering to characterize synoptic circulation patterns. Composite maps were constructed for sea‐level pressure, 850 hPa moisture and wind field, and 500 hPa geopotential height. The circulation patterns of the topmost seven snowfall events were triggered by the advection of very cold airmass from eastern Siberia, anomalously huge moisture with northerly strong wind, active and stationary Aleutian low, and 500 hPa deep cold‐core low over the southern Hokkaido . Article in Journal/Newspaper aleutian low Siberia Wiley Online Library Atmospheric Science Letters 15 4 259 265
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Synoptic‐scale atmospheric circulations are crucial for extreme snowfall events. On the basis of topmost 100 snowfall intensity days in Sapporo, Hokkaido, Japan over winter seasons from 1992 to 2011, this study uses principal component analysis and K‐means clustering to characterize synoptic circulation patterns. Composite maps were constructed for sea‐level pressure, 850 hPa moisture and wind field, and 500 hPa geopotential height. The circulation patterns of the topmost seven snowfall events were triggered by the advection of very cold airmass from eastern Siberia, anomalously huge moisture with northerly strong wind, active and stationary Aleutian low, and 500 hPa deep cold‐core low over the southern Hokkaido .
format Article in Journal/Newspaper
author Farukh, M. A.
Yamada, Tomohito J.
spellingShingle Farukh, M. A.
Yamada, Tomohito J.
Synoptic climatology associated with extreme snowfall events in Sapporo city of northern Japan
author_facet Farukh, M. A.
Yamada, Tomohito J.
author_sort Farukh, M. A.
title Synoptic climatology associated with extreme snowfall events in Sapporo city of northern Japan
title_short Synoptic climatology associated with extreme snowfall events in Sapporo city of northern Japan
title_full Synoptic climatology associated with extreme snowfall events in Sapporo city of northern Japan
title_fullStr Synoptic climatology associated with extreme snowfall events in Sapporo city of northern Japan
title_full_unstemmed Synoptic climatology associated with extreme snowfall events in Sapporo city of northern Japan
title_sort synoptic climatology associated with extreme snowfall events in sapporo city of northern japan
publisher Wiley
publishDate 2014
url http://dx.doi.org/10.1002/asl2.497
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl2.497
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl2.497
genre aleutian low
Siberia
genre_facet aleutian low
Siberia
op_source Atmospheric Science Letters
volume 15, issue 4, page 259-265
ISSN 1530-261X 1530-261X
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/asl2.497
container_title Atmospheric Science Letters
container_volume 15
container_issue 4
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