Author
Listed:
- H. Mitsudera
(Hokkaido University)
- T. Miyama
(Japan Agency for Marine-Earth Science and Technology)
- H. Nishigaki
(Oita Univeristy)
- T. Nakanowatari
(National Institute of Polar Research)
- H. Nishikawa
(Hokkaido University)
- T. Nakamura
(Hokkaido University)
- T. Wagawa
(Japan Fisheries Research and Education Agency)
- R. Furue
(Japan Agency for Marine-Earth Science and Technology)
- Y. Fujii
(Japan Meteorological Agency)
- S. Ito
(The University of Tokyo)
Abstract
Sea surface temperature (SST) fronts in mid- to high-latitude oceans have significant impacts on extratropical atmospheric circulations and climate. In the western subarctic Pacific, sharp SST fronts form between the cold subarctic water and the recently found quasi-stationary jets that advect warm waters originating in the Kuroshio northeastward. Here we present a new mechanism of the jet formation paying attention to the propagation of baroclinic Rossby waves that is deflected by eddy-driven barotropic flows over bottom rises, although their height is low (~500 m) compared with the depth of the North Pacific Ocean (~6000 m). Steered by the barotropic flows, Rossby waves bring a thicker upper layer from the subtropical gyre and a thinner upper layer from the subarctic gyre, thereby creating a thickness jump, hence a surface jet, where they converge. This study reveals an overlooked role of low-rise bottom topography in regulating SST anomalies in subpolar oceans.
Suggested Citation
H. Mitsudera & T. Miyama & H. Nishigaki & T. Nakanowatari & H. Nishikawa & T. Nakamura & T. Wagawa & R. Furue & Y. Fujii & S. Ito, 2018.
"Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets,"
Nature Communications, Nature, vol. 9(1), pages 1-11, December.
Handle:
RePEc:nat:natcom:v:9:y:2018:i:1:d:10.1038_s41467-018-03526-z
DOI: 10.1038/s41467-018-03526-z
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