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期刊论文 [7]
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jet stream [5]
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Two-stage evolution of glacial-period Asian monsoon circulation by shifts of westerly jet streams and changes of North American ice sheets
[期刊论文]
Earth Science Reviews, 2021-01-01, 215
Wang H.
;
Zhou W.
;
Shu P.
;
Hong B.
;
An Z.
View/Download:16/0
Westerly jet stream controlled climate change mode since the Last Glacial Maximum in the northern Qinghai-Tibet Plateau
[期刊论文]
Earth and Planetary Science Letters, 2020-01-01, 549
Li Y.
;
Peng S.
;
Liu H.
;
Zhang X.
;
Ye W.
;
Han Q.
;
Zhang Y.
;
Xu L.
;
Li Y.
View/Download:13/0
Coupled ocean and atmospheric changes during Greenland stadial 1 in southwestern Europe
[期刊论文]
QUATERNARY SCIENCE REVIEWS, 2019-01-01, 212) : 108-120
Naughton, F.
;
Costas, S.
;
Comes, S. D.
;
Desprat, S.
;
Rodrigues, T.
;
Goni, M. F. Sanchez
;
Renssen, H.
;
Trigo, R.
;
Bronk-Ramsey, C.
;
Oliveira, D.
;
Salgueiro, E.
;
Voelker, A. H. L.
;
Abrantes, F.
View/Download:40/0
Amplified contiguous United States summer rainfall variability induced by East Asian monsoon interdecadal change
[期刊论文]
Climate Dynamics, 2018-01-01, 50 (2018-09-10
Zhu Z.
;
Li T.
View/Download:13/0
Multi-centennial-scale changes in East Asian typhoon frequency during the mid-Holocene
[期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2017-01-01, 476
Katsuki K.
;
Yang D.-Y.
;
Lim J.
;
Lee J.-Y.
;
Asahi H.
;
Han M.
View/Download:35/0
Thermodynamic and dynamic influences in the Far East-Okhotsk region on stagnant Meiyu-Baiu
[期刊论文]
Journal of Geophysical Research: Atmospheres, 2017-01-01, 122 (14
Wu C.-H.
View/Download:4/0
Reconstructing atmospheric circulation over southern New Zealand: Establishment of modern westerly airflow 5500 years ago and implications for Southern Hemisphere Holocene climate change
[期刊论文]
Quaternary Science Reviews, 2017-01-01, 159
Turney C.S.M.
;
Wilmshurst J.M.
;
Jones R.T.
;
Wood J.R.
;
Palmer J.G.
;
Hogg A.G.
;
Fenwick P.
;
Crowley S.F.
;
Privat K.
;
Thomas Z.
View/Download:31/0
AGS-PRF: Wave-mean Flow Interactions in a Moist and Warmer Atmosphere
[项目]
Ray Yamada
View/Download:0/0
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