Raspodjela tlaka zraka duž merdijana 100° i 180°
Item
Title (Dublin Core)
hrv
Raspodjela tlaka zraka duž merdijana 100° i 180°
eng
Profiles of mean sea-level pressure along the 100th meridian east and 180th meridian
Description (Dublin Core)
eng
The presented profiles of the mean sea-level pressure in high latitudes (including the North and the South Pole) are based on the observed data. In this way in the cold part of the year on the northern hemisphere along the 180th meridian it has been possible to note that the highest air pressure is not centered at the North Pole but about 15° to the south. It is the effect of influence of Islandic minimum, so that the air pressure in the Northern Pacific is still on the rise. In summer because of strong thermal influence of Asia, it is demonstrated that the subtropical high-pressure belt over that part of the northern hemisphere does not exist at all.
Creator (Dublin Core)
Filipčić, Anita
Subject (Dublin Core)
hrv
tlak zraka; geografska dužina
eng
air pressure; longitude
Publisher (Dublin Core)
Andrija Mohorovicic Geophysical Institute
Date (Dublin Core)
1991
Type (Dublin Core)
text
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
https://hrcak.srce.hr/20638
hrv
https://hrcak.srce.hr/file/32496
Source (Dublin Core)
Geofizika
ISSN 0352-3659 (Print)
ISSN 1846-6346 (Online)
Volume 8
Issue 1
Language (Dublin Core)
hrv
Rights (Dublin Core)
info:eu-repo/semantics/openAccess
All manuscripts published on-line are subject to Creative Commons Attribution-NonCommercial 4.0 International License which permits users to read, download, copy, redistribute, print, search, or link to the full texts of these articles in any medium or format. Also, users can remix, transform and build upon the material, provided the original work is properly cited and any changes properly indicated. They may not use the material for commercial purposes.
By submitting a manuscript, the author accepts the application of the Creative Commons Attribution-NonCommercial 4.0 International License.
By submitting a manuscript, the author accepts the application of the Creative Commons Attribution-NonCommercial 4.0 International License.