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AAMP98観測期間中のレーダー観測
https://doi.org/10.15094/00009219
https://doi.org/10.15094/0000921927016d0f-0bad-4f2c-9811-39486315df19
名前 / ファイル | ライセンス | アクション |
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KJ00000139343 (232.4 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2002-06-01 | |||||
タイトル | ||||||
タイトル | AAMP98観測期間中のレーダー観測 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Characteristics of radar echo during AAMP98 | |||||
言語 | ||||||
言語 | jpn | |||||
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 | 10.15094/00009219 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | AAMP98 カンソク キカン チュウ ノ レーダー カンソク | |||||
著者名(日) |
小西, 啓之
× 小西, 啓之× 和田, 誠× 塩原, 匡貴 |
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著者名(英) |
Konishi, Hiroyuki
× Konishi, Hiroyuki× Wada, Makoto× Shiobara, Masataka |
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著者所属(日) | ||||||
大阪教育大学/国立極地研究所/国立極地研究所 | ||||||
著者所属(英) | ||||||
en | ||||||
Osaka Kyoiku University/National Institute of Polar Research/National Institute of Polar Research | ||||||
抄録(日) | ||||||
内容記述タイプ | Other | |||||
内容記述 | AAMP期間中を含む1997年12月 から1998年3月のNy-Alesundの冬季の雲の特徴をレーダーエコーから分類した.その結果,降水エコー出現頻度は,気温の高低とよく対応し,気温が高くなると降水エコーの出現頻度は,50%近くになった. 観測期間平均の降水エコー出現頻度は23%であった. また,降水エコーが層状性であるか対流性であるかを調べた結果,層状性の降水エコーが全体の64%を占めた. この割合は,気温が低下すると大きくなり,平均気温 が-20℃より低かった2月には,80%を越えた. AAMP期間中は,マイクロパルスライダー(MPL)による雲エコーとの比較も行った. レーダーによる降水エコーの出現頻度は15% と少なかったが,雲エコーの出現頻度は70%もあり,降水域と雲域に大きな差があることが示唆された. |
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抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Precipitation clouds were classified by vertical pointing radar data measured at Ny-Alesund, Arctic from December 1997 to March 1998 including the AAMP period. The results show that the apparent radar echo frequency averaged 23% over the period and increased to roughly 50% in a warmer period. The ratio of apparent time between layer and convective clouds was 64% to 36%. The propotion of layer clouds increased in the colder period and exceeded 80% in February when the averaged temperature at the ground was lower than - 20°C. The radar echo data were also compared with Micro-pulse Lidar (MPL) data during the AAMP period. The apparent MPL echo frequency reached 70%; on the other hand, that of the radar echo was 15%. The results suggest that the area of clouds was much larger than that of precipitation. |
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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 en : Antarctic Record 巻 46, 号 1A, p. 280-286, 発行日 2002-06 |
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国際十進分類法 | ||||||
主題Scheme | UDC | |||||
主題 | 551.5 |