Vertical and horizontal structures of the North Pacific subtropical gyre axis

Verfasser / Beitragende:
[Masafumi Kimizuka, Fumiaki Kobashi, Atsushi Kubokawa, Naoto Iwasaka]
Ort, Verlag, Jahr:
2015
Enthalten in:
Journal of Oceanography, 71/4(2015-08-01), 409-425
Format:
Artikel (online)
ID: 605455457
LEADER caa a22 4500
001 605455457
003 CHVBK
005 20210128100212.0
007 cr unu---uuuuu
008 210128e20150801xx s 000 0 eng
024 7 0 |a 10.1007/s10872-015-0301-9  |2 doi 
035 |a (NATIONALLICENCE)springer-10.1007/s10872-015-0301-9 
245 0 0 |a Vertical and horizontal structures of the North Pacific subtropical gyre axis  |h [Elektronische Daten]  |c [Masafumi Kimizuka, Fumiaki Kobashi, Atsushi Kubokawa, Naoto Iwasaka] 
520 3 |a Mean structures of the North Pacific subtropical gyre are investigated using Argo float observations and several wind stress products, with a particular focus on the gyre axis, which is defined as a large-scale boundary between eastward motions on the northern part of the subtropical gyre and westward motions on the southern part. Structures of the gyre axis are different between the regions east and west of about 180°. In the west, the gyre axis is affected by the strong Kuroshio Extension jet, showing discrepancy with features expected from the Sverdrup balance and ventilated thermocline theory. In the east, depth-integrated geostrophic circulation displays the two gyre axes at about 25°N and 30°N in association with a local cyclonic wind stress curl anomaly. It is expected from the Sverdrup balance that the two gyre axes would extend to the west across the subtropical gyre, but the actual geostrophic circulation exhibits only one gyre axis around 30°N to the west. The vertical structure of the subtropical gyre exhibits a remarkable northward shift of the gyre axis with depth in the east, consistent with the southward decrease in the thickness of density layers around the gyre axis, while the northward shift is less obvious in the west, where the gyre axis lies along the southern flank of the Kuroshio Extension. The gyre shift is relatively smaller in the central mode water (CMW) layer due to the horizontal uniformity of the CMW, suggesting a dynamic effect of the CMW on large-scale circulations of the subtropical gyre. 
540 |a The Oceanographic Society of Japan and Springer Japan, 2015 
690 7 |a North Pacific subtropical gyre  |2 nationallicence 
690 7 |a Wind-driven circulation  |2 nationallicence 
690 7 |a Gyre axis  |2 nationallicence 
690 7 |a Sverdrup balance  |2 nationallicence 
690 7 |a Ventilated thermocline theory  |2 nationallicence 
700 1 |a Kimizuka  |D Masafumi  |u Graduate School of Marine Science and Technology, Tokyo University of Marine Science and Technology, Etchujima 2-1-6, 135-8533, Koto-Ku, Tokyo, Japan  |4 aut 
700 1 |a Kobashi  |D Fumiaki  |u Graduate School of Marine Science and Technology, Tokyo University of Marine Science and Technology, Etchujima 2-1-6, 135-8533, Koto-Ku, Tokyo, Japan  |4 aut 
700 1 |a Kubokawa  |D Atsushi  |u Faculty of Environmental Earth Science, Hokkaido University, Sapporo, Japan  |4 aut 
700 1 |a Iwasaka  |D Naoto  |u Graduate School of Marine Science and Technology, Tokyo University of Marine Science and Technology, Etchujima 2-1-6, 135-8533, Koto-Ku, Tokyo, Japan  |4 aut 
773 0 |t Journal of Oceanography  |d Springer Japan  |g 71/4(2015-08-01), 409-425  |x 0916-8370  |q 71:4<409  |1 2015  |2 71  |o 10872 
856 4 0 |u https://doi.org/10.1007/s10872-015-0301-9  |q text/html  |z Onlinezugriff via DOI 
898 |a BK010053  |b XK010053  |c XK010000 
900 7 |a Metadata rights reserved  |b Springer special CC-BY-NC licence  |2 nationallicence 
908 |D 1  |a research-article  |2 jats 
949 |B NATIONALLICENCE  |F NATIONALLICENCE  |b NL-springer 
950 |B NATIONALLICENCE  |P 856  |E 40  |u https://doi.org/10.1007/s10872-015-0301-9  |q text/html  |z Onlinezugriff via DOI 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Kimizuka  |D Masafumi  |u Graduate School of Marine Science and Technology, Tokyo University of Marine Science and Technology, Etchujima 2-1-6, 135-8533, Koto-Ku, Tokyo, Japan  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Kobashi  |D Fumiaki  |u Graduate School of Marine Science and Technology, Tokyo University of Marine Science and Technology, Etchujima 2-1-6, 135-8533, Koto-Ku, Tokyo, Japan  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Kubokawa  |D Atsushi  |u Faculty of Environmental Earth Science, Hokkaido University, Sapporo, Japan  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Iwasaka  |D Naoto  |u Graduate School of Marine Science and Technology, Tokyo University of Marine Science and Technology, Etchujima 2-1-6, 135-8533, Koto-Ku, Tokyo, Japan  |4 aut 
950 |B NATIONALLICENCE  |P 773  |E 0-  |t Journal of Oceanography  |d Springer Japan  |g 71/4(2015-08-01), 409-425  |x 0916-8370  |q 71:4<409  |1 2015  |2 71  |o 10872