梅雨前線の季節進行は黄海の暖まり方次第
Our paper showing that
"the seasonal migration of the Baiu frontal zone depends on
the warming in the marine surface layer of the Yellow Sea"
has been accepted on 30 January 2013.
”梅雨前線の季節進行は黄海の暖まり方次第”
であることを示した茂木と万田さんの論文が
2013年1月30日に受理されました．
You can see our results on Youtube too.
これまでも学会発表の動画などでお伝えしてきた内容です．
MOTEKI Qoosaku, and Atsuyoshi MANDA, 2013,
"Seasonal migration of the Baiu frontal zone
over the East China Sea:
Sea surface temperature effect"
This work is supported by
the Japanese Ministry of Education,
Culture, Sports, Science and Technology (MEXT)
through a Grant-in-Aid for Scientific Research
in Innovative Areas:
A "hot spot" in the climate system.
の一環として，中緯度海洋変動が気候系に与える影響とその仕組みを
調べたものです．
短い論文ですが，結構イケてる仮説を提示した
独自性には自信があるので，掲載されたら是非，
チェックしてみて下さいませ(・∀・)
Acknowledgements & References:
We are inspired by the following papers and
personal communications.
We deeply appreciate and respect the works.
僕らの仕事は，下記の論文などに強く影響を受けて，
仕上げることができました．
心からの感謝と敬意を表します．
Miyama Toru et al. 2013:
"A striking early-summer event of
a convective rainband persistent
along the warm Kuroshio in the East China Sea."
Tellus A, Vol. 64, DOI 10.3402/Tellusa.V64i0.18962
Yasumasa Miyazawa et al. 2009:
"Water Mass Variability in the
Western North Pacific Detected in a 15-Year
Eddy Resolving Ocean Reanalysis."
J Oceanogr, 65(6), 737-756.
Takeaki Sampe and S-P Xie, 2010:
"Large-Scale Dynamics of the Meiyu-Baiu Rainband:
Environmental Forcing by the Westerly Jet."
J. Climate, 23(1), 113-134.
and so on.
