日本銀行金融研究所所蔵藩札資料番号：ⅢAエドa1-46-2-102(1)科学研究費助成事業（研究成果公開促進費）で電子化を実施データベースの名称：藩札等に関する統合データベース課題番号：18HP8038藩札の利用に関するお問い合わせ：藩札画像の転載（出版物・HP等）に際しては、日本銀行貨幣博物館への申請手続きが必要です。詳しくは貨幣博物館ホームページ（http://www.imes.boj.or.jp/cm/service/）をご覧ください

Ahumada-Sempoal, Miguel Ángel

Cruzado, Antonio

Ocean Science Discussions

13 páginas, 18 figuras, 1 tabla.The Princeton Ocean Model – POM (Blumberg
and Mellor, 1987) has been implemented in the Northwestern
Mediterranean nested (in one-way off-line mode) to a general circulation model of the Mediterranean Sea – OGCM
(Pinardi and Masetti, 2000; Demirov and Pinardi, 2002)
in order to investigate if this model conﬁguration is capable of reproducing the major features of the circulation as
known from observations and to improve what has been
made by previous numerical modeling works. According to
the model results, the large-scale cyclonic circulation in the
northern part of the Northwestern Mediterranean is, at least
in the upper layers, less coherent in winter and spring than
in summer and autumn. Furthermore, there is evidence that
the mesoscale structure (eddies and meanders) is, during all
year, a signiﬁcant dynamic characteristic in this region of the
Mediterranean Sea. Finally, concerning the circulation in the
lower layers, the model results have conﬁrmed that Levantine
Intermediate Water (LIW) and Western Mediterranean Deep
Water (WMDW) follow essentially a cyclonic path during all
year.M. Ahumada was supported by the Universidad del Mar
and the Secretar´ıa de Educacion P ´ ublica (SEP) of Mexico through ´
the PROMEP program.Peer reviewe

Digital.CSIC

Ocean Science

Modeling of the circulation in the northwestern Mediterranean sea with the princeton ocean model.

日本銀行金融研究所所蔵藩札
資料番号：ⅢAエドa1-46-2-102(1)
科学研究費助成事業（研究成果公開促進費）で電子化を実施
データベースの名称：藩札等に関する統合データベース
課題番号：18HP8038
藩札の利用に関するお問い合わせ：
藩札画像の転載（出版物・HP等）に際しては、日本銀行貨幣博物館への申請手続きが必要です。
詳しくは貨幣博物館ホームページ（http://www.imes.boj.or.jp/cm/service/）をご覧ください。datase

Waseda University Repository

出雲国  松江藩札  銭2貫文

The Princeton Ocean Model – POM (Blumberg and Mellor, 1987) has been implemented
in the Northwestern Mediterranean nested (in one-way off-line mode) to a general
circulation model of the Mediterranean Sea – OGCM (Pinardi and Masetti, 2000;
5 Demirov and Pinardi, 2002) in order to investigate if this model configuration is capable
of reproducing the major features of the circulation as known from observations and to
improve what has been made by previous numerical modeling works. According to the
model results, the large-scale cyclonic circulation in the northern part of the Northwestern
Mediterranean is, at least in the upper layers, less coherent in winter and spring
10 than in summer and autumn. Furthermore, there is evidence that the mesoscale structure
(eddies and meanders) is, during all year, a significant dynamic characteristic in
this region of the Mediterranean Sea. Finally, concerning the circulation in the lower
layers has been confirmed that the Levantine Intermediate Water and the Western
Mediterranean Deep Water follow essentially a cyclonic path during all year.Peer reviewe

出雲国松江藩札銭2貫文

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出雲国 松江藩札 銭2貫文

Abstract

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Waseda University Repository

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出雲国松江藩札銭2貫文