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VARIATION OF EURASIAN SNOW COVER EXTENT AND NORTHERN HEMISPHERE SURFACE AIR TEMPERATURE
https://doi.org/10.15094/00003723
https://doi.org/10.15094/000037232b6fd583-56fc-4567-a025-eef92d56e282
名前 / ファイル | ライセンス | アクション |
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KJ00002409952 (86.3 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1992-02-01 | |||||
タイトル | ||||||
タイトル | VARIATION OF EURASIAN SNOW COVER EXTENT AND NORTHERN HEMISPHERE SURFACE AIR TEMPERATURE | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003723 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
記事種別(英) | ||||||
en | ||||||
ABSTRACT | ||||||
論文名よみ | ||||||
その他のタイトル | VARIATION OF EURASIAN SNOW COVER EXTENT AND NORTHERN HEMISPHERE SURFACE AIR TEMPERATURE | |||||
著者名よみ |
モリナガ, ユキ
× モリナガ, ユキ× ヤスナリ, テツゾウ× マスダ, コウイチ |
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著者名(英) |
MORINAGA, Yuki
× MORINAGA, Yuki× YASUNARI, Tetsuzo× MASUDA, Kooiti |
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著者所属(英) | ||||||
en | ||||||
Institute of Geoscience, University of Tsukuba | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Geoscience, University of Tsukuba | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth and Planetary Physics, University of Tokyo | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Correlations between the snow cover extent and northern hemisphere mean surface air temperature (P. D. JONES et al. : J. Appl. Meteorol., 25,161,1986) were analyzed for 1967-1987. Snow cover extent in Central Asia (35-65°E, 25-70°N), which correlates better with the interannual variation of snow cover extent over the whole continent than that in other regions, was chosen to represent the Eurasian snow cover (October, December, February and April). For snow cover extent data, the NOAA/NESDIS Northern Hemisphere Snow and Ice Chart was used. Negative correlations were found between the NHT in late summer to autumn (r=-0.67 for September) and the October snow cover extent. The so-called Eurasian Pattern (J. M. WALLACE and D. S. GUTZLER : Mon. Weather Rev., 109,784,1981) detected in the atmospheric circulation (500mb) in autumn seems to be largely responsible both for the large extent of snow cover and the low NHT. Positive correlations were found between the April snow cover extent and the NHT in the following winter to autumn period (r=0.72 for January). On the other hand, two other relations are found. 1) Negative correlations between April snow cover in central Asia and the following Indian summer monsoon rainfall (r=-0.52). 2) Negative correlation between April snow cover extent and the sea water temperature of the western tropical Pacific the following January (T. YASUNARI and Y. SEKI : submitted to J. Meteorol. Soc. Jpn., 1991). These three correlations may indicate that these lag correlations show a possible link among Eurasian snow cover, tropical sea surface temperature (SST) and NHT. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10756213 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 巻 5, p. 185, 発行日 1992-02 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |