Statistics on the currents in the seas adjacent to Japan.

Statistics on the currents in the seas adjacent to Japan have been carried out with use of approx. eighty thousand GEK data observed from 1953 to 1970. The statistics have been conducted for the vector mean, scalar mean, maximum velocity, stability and standard deviation in three statistical periods, the periods in which the large meander of the Kuroshio off Kishu and Enshu-nada is both absent and present, the overall period from 1953 to 1970. Although the detailed characteristics can be seen from the statistical atlases attached, the comprehensive characters of each statistical element in each region, and the relationships among them, are described. In general, the distributional pattern of each element is similar to each other, especially in the region of the Kuroshio. The variability,defined as (standard deviation) / (stability), of the Kuroshio propagates from west to east, and is larger in the period when the large meander is absent than in the period of its presence. A characteristic linear relationship between vector mean and scalar mean is significant in each region, and the other relationships between each element, except the maximum velocity, can be introduced from this basic relationship.

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Bibliographic Details
Main Authors: Nitani, Hideo, Yoshida, Shozo, Okumoto, Jun, Nakamura, Hiromi
Format: Journal Contribution biblioteca
Language:Japanese
Published: 1979
Online Access:http://hdl.handle.net/1834/16304
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id dig-aquadocs-1834-16304
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spelling dig-aquadocs-1834-163042021-05-19T06:55:12Z Statistics on the currents in the seas adjacent to Japan. Nitani, Hideo Yoshida, Shozo Okumoto, Jun Nakamura, Hiromi Statistics on the currents in the seas adjacent to Japan have been carried out with use of approx. eighty thousand GEK data observed from 1953 to 1970. The statistics have been conducted for the vector mean, scalar mean, maximum velocity, stability and standard deviation in three statistical periods, the periods in which the large meander of the Kuroshio off Kishu and Enshu-nada is both absent and present, the overall period from 1953 to 1970. Although the detailed characteristics can be seen from the statistical atlases attached, the comprehensive characters of each statistical element in each region, and the relationships among them, are described. In general, the distributional pattern of each element is similar to each other, especially in the region of the Kuroshio. The variability,defined as (standard deviation) / (stability), of the Kuroshio propagates from west to east, and is larger in the period when the large meander is absent than in the period of its presence. A characteristic linear relationship between vector mean and scalar mean is significant in each region, and the other relationships between each element, except the maximum velocity, can be introduced from this basic relationship. Published 2020-02-16T15:44:34Z 2020-02-16T15:44:34Z 1979 Journal Contribution Refereed http://hdl.handle.net/1834/16304 ja https://www1.kaiho.mlit.go.jp/GIJUTSUKOKUSAI/KENKYU/report/rhr14/rhr14-04.pdf pp.57-91
institution UNESCO
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-aquadocs
tag biblioteca
region Europa del Oeste
libraryname Repositorio AQUADOCS
language Japanese
description Statistics on the currents in the seas adjacent to Japan have been carried out with use of approx. eighty thousand GEK data observed from 1953 to 1970. The statistics have been conducted for the vector mean, scalar mean, maximum velocity, stability and standard deviation in three statistical periods, the periods in which the large meander of the Kuroshio off Kishu and Enshu-nada is both absent and present, the overall period from 1953 to 1970. Although the detailed characteristics can be seen from the statistical atlases attached, the comprehensive characters of each statistical element in each region, and the relationships among them, are described. In general, the distributional pattern of each element is similar to each other, especially in the region of the Kuroshio. The variability,defined as (standard deviation) / (stability), of the Kuroshio propagates from west to east, and is larger in the period when the large meander is absent than in the period of its presence. A characteristic linear relationship between vector mean and scalar mean is significant in each region, and the other relationships between each element, except the maximum velocity, can be introduced from this basic relationship.
format Journal Contribution
author Nitani, Hideo
Yoshida, Shozo
Okumoto, Jun
Nakamura, Hiromi
spellingShingle Nitani, Hideo
Yoshida, Shozo
Okumoto, Jun
Nakamura, Hiromi
Statistics on the currents in the seas adjacent to Japan.
author_facet Nitani, Hideo
Yoshida, Shozo
Okumoto, Jun
Nakamura, Hiromi
author_sort Nitani, Hideo
title Statistics on the currents in the seas adjacent to Japan.
title_short Statistics on the currents in the seas adjacent to Japan.
title_full Statistics on the currents in the seas adjacent to Japan.
title_fullStr Statistics on the currents in the seas adjacent to Japan.
title_full_unstemmed Statistics on the currents in the seas adjacent to Japan.
title_sort statistics on the currents in the seas adjacent to japan.
publishDate 1979
url http://hdl.handle.net/1834/16304
work_keys_str_mv AT nitanihideo statisticsonthecurrentsintheseasadjacenttojapan
AT yoshidashozo statisticsonthecurrentsintheseasadjacenttojapan
AT okumotojun statisticsonthecurrentsintheseasadjacenttojapan
AT nakamurahiromi statisticsonthecurrentsintheseasadjacenttojapan
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