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The East Asian winter monsoon is characterized by a strong east–west surface pressure gradient and the outbreak of cold air around Japan. It causes heavy snowfall in the Sea of Japan side of the Japanese Islands. Meanwhile, fine weather prevails ov
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d33dc77e17fe1499f41f7da1e7d954fc
https://doi.org/10.5194/cp-2021-33
https://doi.org/10.5194/cp-2021-33
