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  1. F300 宇宙地球環境研究所
  2. F300a 雑誌掲載論文
  3. 学術雑誌

Frontolysis by surface heat flux in the eastern Japan Sea: importance of mixed layer depth

http://hdl.handle.net/2237/00030583
http://hdl.handle.net/2237/00030583
2b0d685a-3c2f-43ab-aa26-caeabe2f5924
名前 / ファイル ライセンス アクション
Manuscript(re-re-revise)_fin.pdf Manuscript(re-re-revise)_fin (4.8 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2019-08-08
タイトル
タイトル Frontolysis by surface heat flux in the eastern Japan Sea: importance of mixed layer depth
言語 en
著者 Ohishi, Shun

× Ohishi, Shun

WEKO 92887

en Ohishi, Shun

Search repository
Aiki, Hidenori

× Aiki, Hidenori

WEKO 92888

en Aiki, Hidenori

Search repository
Tozuka, Tomoki

× Tozuka, Tomoki

WEKO 92889

en Tozuka, Tomoki

Search repository
Cronin, Meghan F.

× Cronin, Meghan F.

WEKO 92890

en Cronin, Meghan F.

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
権利
言語 en
権利情報 “This is a post-peer-review, pre-copyedit version of an article published in [Journal of Oceanography]. The final authenticated version is available online at: http://dx.doi.org/10.1007/s10872-018-0502-0”.
キーワード
主題Scheme Other
主題 Frontolysis
キーワード
主題Scheme Other
主題 Mixed layer processes
キーワード
主題Scheme Other
主題 Entrainment
キーワード
主題Scheme Other
主題 Japan Sea
キーワード
主題Scheme Other
主題 Sea surface temperature front
抄録
内容記述 Frontolysis mechanisms by which surface heat flux relaxes the sea surface temperature (SST) front in the eastern Japan Sea (JS) are investigated in detail using observational datasets. On the warm southern side of the front, larger air–sea specific humidity and temperature differences induce stronger turbulent heat release compared to the cool northern side. As a result, stronger wintertime cooling and weaker summertime warming occur south of the front, and the meridional gradient in the surface net heat flux (NHF) tends to relax the SST front throughout the year. In the mixed-layer deepening phase (September–January), a higher entrainment velocity occurs on the warm southern side because of weaker stratification. Since the resulting thicker mixed layer on the southern side is less sensitive to surface cooling, the mixed layer depth (MLD) gradient damps the frontolysis by the NHF gradient. In the shoaling phase (April–June), a deeper mixed layer south of the front is caused by the weaker warming and reduced sensitivity of the thicker mixed layer to a shoaling effect by shortwave radiation. Owing to weaker sensitivity of the thicker mixed layer on the southern side to surface warming, the MLD gradient enhances the frontolysis by the NHF gradient. Therefore, it is shown that the mixed layer processes cause seasonality of weaker (stronger) frontolysis by surface heat fluxes, damping (enhancing) the frontolysis by the NHF gradient in winter (summer). This study reveals unique features of the frontolysis in the eastern JS compared with the Agulhas Return Current and Kuroshio Extension regions.
言語 en
内容記述タイプ Abstract
内容記述
内容記述 ファイル公開:2020/06/01
言語 ja
内容記述タイプ Other
出版者
言語 en
出版者 Springer
言語
言語 eng
資源タイプ
資源タイプresource http://purl.org/coar/resource_type/c_6501
タイプ journal article
出版タイプ
出版タイプ AM
出版タイプResource http://purl.org/coar/version/c_ab4af688f83e57aa
DOI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 https://doi.org/10.1007/s10872-018-0502-0
ISSN(print)
収録物識別子タイプ PISSN
収録物識別子 0916-8370
書誌情報 en : Journal of Oceanography

巻 75, 号 3, p. 283-297, 発行日 2019-06
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