| Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
| 公開日 |
1991-05-01 |
| タイトル |
|
|
タイトル |
A NOTE ON WATER EXCHANGE UNDER FAST ICE IN LUTZOW-HOLM BAY, ANTARCTICA |
| 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 |
10.15094/00003644 |
|
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) |
| 著者名(英) |
OHSHIMA, Kay I.
ONO, Nobuo
TAKIZAWA, Takatoshi
USHIO, Shuki
|
| 著者所属(英) |
|
|
言語 |
en |
|
値 |
Institute of Low Temperature Science, Hokkaido University |
| 著者所属(英) |
|
|
言語 |
en |
|
値 |
Institute of Low Temperature Science, Hokkaido University |
| 著者所属(英) |
|
|
言語 |
en |
|
値 |
Institute of Low Temperature Science, Hokkaido University |
| 著者所属(英) |
|
|
言語 |
en |
|
値 |
Institute of Low Temperature Science, Hokkaido University |
| 抄録(英) |
|
|
内容記述タイプ |
Other |
|
内容記述 |
Under coastal fast ice in the Ongul Strait near Syowa Station, Antarctica, warmer, more saline, and oxygen-poorer water appears in mid-depth and deep layers from winter to spring every year. This water is explained as a result of mixing between Circumpolar Deep Water (CDW) and Winter Water (WW). This water becomes more like CDW and more homogenized with time from winter to spring, and in December a mixing ratio of 1 : 3-1 : 4 for CDW to WW is required to explain the properties of the homogenized water. It is inferred that the CDW comes along the glacial troughs. Transport of CDW results in a significant amount of heat supply into the water under fast ice. |
| 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 4,
p. 74-80,
発行日 1991-05
|
| 出版者 |
|
|
出版者 |
National Institute of Polar Research |
KJ00000767847 (962.0 kB)
.png)
