| タイトル |
-
en
Chemical evidence for the origin of the cold water belt along the northeastern coast of Hokkaido
|
| 作成者 |
|
| アクセス権 |
open access |
| 権利情報 |
-
en
The final publication is available at link.springer.com
|
| 主題 |
-
Other
en
Cold water belt
-
Other
en
Okhotsk Sea
-
Other
en
Japan Sea
-
Other
en
Chemical components
-
Other
en
Hydrographic data
-
NDC
660
|
| 内容注記 |
-
Abstract
en
In the southwestern Okhotsk Sea, the cold water belt (CWB) is frequently observed on satellite images offshore of the Soya Warm Current flowing along the northeastern coast of Hokkaido, Japan, during summertime. It has been speculated that the CWB is upwelling cold water that originates from either subsurface water of the Japan Sea off Sakhalin or bottom water of the Okhotsk Sea. Hydrographic and chemical observations (nutrients, humic-type fluorescence intensity, and iron) were conducted in the northern Japan Sea and southwestern Okhotsk Sea in early summer 2011 to clarify the origin of the CWB. Temperature-salinity relationships, vertical distributions of chemical components, profiles of chemical components against density, and the (NO3 + NO2)/PO4 relationship confirm that water in the CWB predominantly originates from Japan Sea subsurface water.
|
| 出版者 |
en
Springer
|
| 日付 |
|
| 言語 |
|
| 資源タイプ |
journal article |
| 出版タイプ |
AM |
| 資源識別子 |
HDL
http://hdl.handle.net/2115/59630
|
| 関連 |
-
isVersionOf
DOI
https://doi.org/10.1007/s10872-014-0239-3
|
| 収録誌情報 |
-
-
PISSN
0916-8370
-
NCID
AA00704803
-
en
Journal of Oceanography
-
巻70
号4
開始ページ377
終了ページ387
|
| ファイル |
|
| コンテンツ更新日時 |
2023-07-26 |
