DECREASE OF SEA ICE PRODUCTION IN THE OKHOTSK SEA CAUSES WEAKENING OF OVERTURNING IN THE NORTHWESTERN NORTH

It is known that North Pacific Intermediate Water (NPIW), characterized by a salinity minimum at 26.8σθ, is a major water mass at the intermediate level of the North Pacific (e.g., Reid, 1965). Figure 1 shows the distribution of potential temperature on the 27.0σθ isopycnal

Bibliographic Details
Main Authors: Ohshima Kay I, Nakanowatari T, Wakatsuchi M
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Okhotsk
Pacific
okhotsk sea
Sea ice
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.132
http://www.chikyu.ac.jp/AMORE/2006proceeding-no.4/03.oshima-seaice-15-23.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.519.132
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.519.132 2023-05-15T17:52:35+02:00 DECREASE OF SEA ICE PRODUCTION IN THE OKHOTSK SEA CAUSES WEAKENING OF OVERTURNING IN THE NORTHWESTERN NORTH Ohshima Kay I Nakanowatari T Wakatsuchi M The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.132 http://www.chikyu.ac.jp/AMORE/2006proceeding-no.4/03.oshima-seaice-15-23.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.132 http://www.chikyu.ac.jp/AMORE/2006proceeding-no.4/03.oshima-seaice-15-23.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.chikyu.ac.jp/AMORE/2006proceeding-no.4/03.oshima-seaice-15-23.pdf text ftciteseerx 2016-01-08T10:00:09Z It is known that North Pacific Intermediate Water (NPIW), characterized by a salinity minimum at 26.8σθ, is a major water mass at the intermediate level of the North Pacific (e.g., Reid, 1965). Figure 1 shows the distribution of potential temperature on the 27.0σθ isopycnal Text okhotsk sea Sea ice Unknown Okhotsk Pacific
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description It is known that North Pacific Intermediate Water (NPIW), characterized by a salinity minimum at 26.8σθ, is a major water mass at the intermediate level of the North Pacific (e.g., Reid, 1965). Figure 1 shows the distribution of potential temperature on the 27.0σθ isopycnal
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Ohshima Kay I
Nakanowatari T
Wakatsuchi M
spellingShingle Ohshima Kay I
Nakanowatari T
Wakatsuchi M
DECREASE OF SEA ICE PRODUCTION IN THE OKHOTSK SEA CAUSES WEAKENING OF OVERTURNING IN THE NORTHWESTERN NORTH
author_facet Ohshima Kay I
Nakanowatari T
Wakatsuchi M
author_sort Ohshima Kay I
title DECREASE OF SEA ICE PRODUCTION IN THE OKHOTSK SEA CAUSES WEAKENING OF OVERTURNING IN THE NORTHWESTERN NORTH
title_short DECREASE OF SEA ICE PRODUCTION IN THE OKHOTSK SEA CAUSES WEAKENING OF OVERTURNING IN THE NORTHWESTERN NORTH
title_full DECREASE OF SEA ICE PRODUCTION IN THE OKHOTSK SEA CAUSES WEAKENING OF OVERTURNING IN THE NORTHWESTERN NORTH
title_fullStr DECREASE OF SEA ICE PRODUCTION IN THE OKHOTSK SEA CAUSES WEAKENING OF OVERTURNING IN THE NORTHWESTERN NORTH
title_full_unstemmed DECREASE OF SEA ICE PRODUCTION IN THE OKHOTSK SEA CAUSES WEAKENING OF OVERTURNING IN THE NORTHWESTERN NORTH
title_sort decrease of sea ice production in the okhotsk sea causes weakening of overturning in the northwestern north
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.132
http://www.chikyu.ac.jp/AMORE/2006proceeding-no.4/03.oshima-seaice-15-23.pdf
geographic Okhotsk
Pacific
geographic_facet Okhotsk
Pacific
genre okhotsk sea
Sea ice
genre_facet okhotsk sea
Sea ice
op_source http://www.chikyu.ac.jp/AMORE/2006proceeding-no.4/03.oshima-seaice-15-23.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.132
http://www.chikyu.ac.jp/AMORE/2006proceeding-no.4/03.oshima-seaice-15-23.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766160179243515904

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