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みずほ観測拠点における水蒸気量観測
https://doi.org/10.15094/00007978
https://doi.org/10.15094/000079783b8d2b5c-7af4-413e-82e5-729af08fbb77
名前 / ファイル | ライセンス | アクション |
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KJ00002477038 (1.4 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1978-03-01 | |||||
タイトル | ||||||
タイトル | みずほ観測拠点における水蒸気量観測 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Atmospheric Water Vapor Measurements at Mizuho Camp, East Antarctica in 1976-1977 | |||||
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 | 10.15094/00007978 | |||||
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(日) | ||||||
研究論文 | ||||||
記事種別(英) | ||||||
en | ||||||
Scientific Paper | ||||||
論文名よみ | ||||||
その他のタイトル | ミズホ カンソク キョテン ニオケル スイジョウキ リョウ カンソク | |||||
著者名(日) |
西尾, 文彦
× 西尾, 文彦 |
|||||
著者名(英) |
NISHIO, Fumihiko
× NISHIO, Fumihiko |
|||||
著者所属(日) | ||||||
国立極地研究所 | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(日) | ||||||
内容記述タイプ | Other | |||||
内容記述 | 1976年11月30日から1977年1月21日まで,みずほ観測拠点において水蒸気量の測定を行った.測定期間中,相対湿度は30~80%の値を示し,低気圧の影響を受けている期間は,斜面下降風に支配されている気象状況のときよりも高い相対湿度が観測された.水蒸気量が測定された気温範囲は,-6.5℃から-22.8℃であった.水蒸気量の測定結果から,この測定期間中の雪面からの昇華量が計算された.計算結果は雪尺測定による消耗量の2~3倍になった. | |||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The measurement of air humidity at the height of 1.5 meters above the snow surface was made at Mizuho Camp, East Antarctica, several times a day during the summer in 1976-1977, with the Karl Fisher method and the Assmann ventilated psychrometer method. The values of air humidity obtained by these two methods agreed within approximately 5% error. Water vapor pressure was estimated from the air humidity at temperatures between -6.5 and -22.8℃. The water vapor pressure obtained showed daily variation similar to air temperature. During the measurement no supersaturation of water vapor with respect to ice was detected and no ice fog was observed. The relative air humidity was between 30 and 80%. It was lower under a condition of predominant katabatic winds than under an influence of cyclones. The daily mean amount of sublimation estimated from the water vapor pressure obtained was between 1.3 and 1.9 millimeters per day and it was nearly two or three times larger than the amount of sublimation obtained by a direct measurement, snow stake measurement. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00181831 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00857289 | |||||
書誌情報 |
南極資料 巻 61, p. 1-10, 発行日 1978-03 |
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国際十進分類法 | ||||||
主題Scheme | UDC | |||||
主題 | 551.5 | |||||
出版者 | ||||||
出版者 | 国立極地研究所 |