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In the western Pacific, global warming makes the storm-track stronger and the westerly jet weaker, closely related to the leading mode of the storm-track variability. Much projection onto the leading mode is also realized for the global warming response in the Western Hemisphere; the storm-track is suppressed along with weaker zonal wind there at least in this model. It is therefore found that there are two types of interannual variability of storm-tracks (one for the western Pacific and the other for the Western Hemisphere), both mostly explain the global warming response."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420282801201770496","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80422450"},{"@type":"NRID","@value":"1000080422450"},{"@type":"ORCID","@value":"0000-0002-1693-1024"},{"@type":"NRID","@value":"9000414746025"},{"@type":"NRID","@value":"9000415146159"},{"@type":"NRID","@value":"9000345292748"},{"@type":"NRID","@value":"9000399765019"},{"@type":"NRID","@value":"9000398808425"},{"@type":"NRID","@value":"9000257827233"},{"@type":"NRID","@value":"9000399936662"},{"@type":"NRID","@value":"9000399528048"},{"@type":"NRID","@value":"9000326649840"},{"@type":"NRID","@value":"9000404664206"},{"@type":"NRID","@value":"9000411566753"},{"@type":"NRID","@value":"9000283621213"},{"@type":"NRID","@value":"9000414223589"},{"@type":"NRID","@value":"9000405666045"},{"@type":"NRID","@value":"9000244879599"},{"@type":"NRID","@value":"9000399765135"},{"@type":"NRID","@value":"9000410958892"},{"@type":"NRID","@value":"9000238038314"},{"@type":"NRID","@value":"9000315141606"},{"@type":"NRID","@value":"9000283593286"},{"@type":"NRID","@value":"9000283593508"},{"@type":"NRID","@value":"9000403163173"},{"@type":"NRID","@value":"9000411524336"},{"@type":"NRID","@value":"9000266899000"},{"@type":"NRID","@value":"9000257768423"},{"@type":"NRID","@value":"9000363502569"},{"@type":"NRID","@value":"9000297476356"},{"@type":"NRID","@value":"9000375859378"},{"@type":"NRID","@value":"9000363500193"},{"@type":"NRID","@value":"9000257767416"},{"@type":"NRID","@value":"9000351090870"},{"@type":"NRID","@value":"9000239881409"},{"@type":"NRID","@value":"9000412162920"},{"@type":"NRID","@value":"9000399538815"},{"@type":"NRID","@value":"9000326657003"},{"@type":"NRID","@value":"9000237782066"},{"@type":"NRID","@value":"9000411102314"},{"@type":"NRID","@value":"9000402233616"},{"@type":"NRID","@value":"9000399252237"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/inaz"}],"foaf:name":[{"@language":"en","@value":"Inatsu 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Pacific Storm Track Activity and East Asian Winter Monsoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993423336448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Unified Three-Dimensional Instability Theory of the Onset of Blocking and Cyclogenesis"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995074510336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An Idealized Model Study Relevant to the Dynamics of the Midwinter Minimum of the Pacific Storm Track"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996101870720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Barotropic Effects on Atmospheric Storm Tracks"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505733504","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reproducibility and Future Projection of the Midwinter Storm-Track Activity over the Far East in the CMIP3 Climate Models in Relation to \"Haru-Ichiban\" over Japan"},{"@value":"Notes and correspondence: Reproducibility and future projection of the midwinter storm-track activity over the Far East in the CMIP3 climate models in relation to \"Haru-Ichiban\" over Japan"},{"@value":"Reproducibility and Future Projection of the Midwinter Storm-Track Activity over the Far East in the CMIP3 Climate Models in Relation to \"Haru-Ichiban\" over Japan(<Special Edition>Evaluations of CMIP3 Model Performance for Various Atmospheric and Oceanic Phenomena, Part I)"},{"@value":"Reproducibility and future projection of the midwinter stormtrack activity over the Far East in the CMIP3 climate models in relation to the occurrence of the first spring storm (Haru-Ichiban) over Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680198668032","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Soil-Frost Depth Change in Eastern Hokkaido under +2 K-World Climate 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