Phytoplankton productivity in the western subarctic gyre of the North Pacific in early summer 2006

2011 ◽  
Vol 67 (3) ◽  
pp. 295-303 ◽  
Author(s):  
Tetsuichi Fujiki ◽  
Kazuhiko Matsumoto ◽  
Shuichi Watanabe ◽  
Takuji Hosaka ◽  
Toshiro Saino
2014 ◽  
Vol 70 (1) ◽  
pp. 91-103 ◽  
Author(s):  
Yuichi Nosaka ◽  
Tomonori Isada ◽  
Isao Kudo ◽  
Hiroaki Saito ◽  
Hiroshi Hattori ◽  
...  

Author(s):  
Hiroshi Kuroda ◽  
Satoshi Suyama ◽  
Hiroomi Miyamoto ◽  
Takashi Setou ◽  
Takuya Nakanowatari

2014 ◽  
Vol 59 (3) ◽  
pp. 887-900 ◽  
Author(s):  
Tetsuichi Fujiki ◽  
Kazuhiko Matsumoto ◽  
Yoshihisa Mino ◽  
Kosei Sasaoka ◽  
Masahide Wakita ◽  
...  

2014 ◽  
Vol 70 (3) ◽  
pp. 211-223 ◽  
Author(s):  
Sachihiko Itoh ◽  
Ichiro Yasuda ◽  
Hiromichi Ueno ◽  
Toshio Suga ◽  
Shigeho Kakehi

2021 ◽  
Vol 34 (2) ◽  
pp. 495-507
Author(s):  
Kenta Kawasaki ◽  
Yoshihiro Tachibana ◽  
Tetsu Nakamura ◽  
Koji Yamazaki

AbstractSummertime temperatures in marginal seas are, in general, colder than on the surrounding continent because of the large contrast in heat capacity between the land and the ocean. The Okhotsk Sea, which is covered by sea ice until early summer, is much colder than the surrounding continent in summer. The Okhotsk Sea is thus located in an area with one of the largest temperature contrasts of all the marginal seas in summertime midlatitudes. Cooled air over the Okhotsk Sea may have an impact on remote summer climates, such as by serving as the source of cold-air advection that results in a poor crop harvest in Japan. Here, we examine the role of the Okhotsk Sea on the early summer climate of the western part of the North Pacific through an ideal numerical experiment by artificially changing the model’s default oceanic condition in the Okhotsk Sea to a condition of land cover. Simulation results reveal that the presence of the Okhotsk Sea increases precipitation of the baiu/mei-yu front through strengthening of the northward moisture flux at the western edge of an intensified North Pacific subtropical high. The Okhotsk influence farther extends toward western North America to which the strengthened jet stream with a storm track extends. This remote influence is achievable through feedback from a transient eddy anomaly that is activated by the surface temperature gradient between the cold Okhotsk Sea and the warm Pacific Ocean. The findings imply that the existence of the Okhotsk Sea strengthens the East Asian summer monsoons.


2011 ◽  
Vol 67 (3) ◽  
pp. 281-293 ◽  
Author(s):  
Sachihiko Itoh ◽  
Yugo Shimizu ◽  
Shin-ichi Ito ◽  
Ichiro Yasuda

2019 ◽  
Vol 617-618 ◽  
pp. 221-244 ◽  
Author(s):  
MR Baker ◽  
ME Matta ◽  
M Beaulieu ◽  
N Paris ◽  
S Huber ◽  
...  

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