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期刊论文 [17]
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Seasonally-dependent impact of easterly wind bursts on the development of El Niño events
[期刊论文]
Climate Dynamics, 2019-01-01,
Fan H.
;
Huang B.
;
Yang S.
;
Li Z.
;
Deng K.
View/Download:27/0
Air–sea fluxes in a climate model using hourly coupling between the atmospheric and the oceanic components
[期刊论文]
Climate Dynamics, 2017-01-01, 48 (2017-09-10
Tian F.
;
von Storch J.-S.
;
Hertwig E.
View/Download:3/0
Phase locking of equatorial Atlantic variability through the seasonal migration of the ITCZ
[期刊论文]
Climate Dynamics, 2017-01-01, 48 (2017-11-12
Richter I.
;
Xie S.-P.
;
Morioka Y.
;
Doi T.
;
Taguchi B.
;
Behera S.
View/Download:41/0
Roles of energy conservation and climate feedback in Bjerknes compensation: a coupled modeling study
[期刊论文]
Climate Dynamics, 2017-01-01, 49 (2017-05-06
Dai H.
;
Yang H.
;
Yin J.
View/Download:11/0
Modulation of Bjerknes feedback on the decadal variations in ENSO predictability
[期刊论文]
Geophysical Research Letters, 2016-01-01, 43 (24
Zheng F.
;
Fang X.-H.
;
Zhu J.
;
Yu J.-Y.
;
Li X.-C.
View/Download:45/0
Strong and moderate nonlinear El Niño regimes
[期刊论文]
Climate Dynamics, 2016-01-01, 46 (2017-05-06
Takahashi K.
;
Dewitte B.
View/Download:0/0
The Bjerknes feedback in the tropical Atlantic in CMIP5 models
[期刊论文]
Climate Dynamics, 2016-01-01, 47 (2017-07-08
Deppenmeier A.-L.
;
Haarsma R.J.
;
Hazeleger W.
View/Download:18/0
Assessment of the simulation of Indian Ocean Dipole in the CESM—Impacts of atmospheric physics and model resolution
[期刊论文]
Journal of Advances in Modeling Earth Systems, 2016-01-01, 8 (4
Yao Z
;
, Tang Y
;
, Chen D
;
, Zhou L
;
, Li X
;
, Lian T
;
, Ul Islam S
View/Download:8/0
Feedback processes responsible for El Niño-La Niña amplitude asymmetry
[期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (13
Im S.-H.
;
An S.-I.
;
Kim S.T.
;
Jin F.-F.
View/Download:21/0
A possible explanation on the changes in the spatial structure of ENSO from CMIP3 to CMIP5
[期刊论文]
Geophysical Research Letters, 2014-01-01, 41 (1
Yeh S.-W.
;
Ham Y.-G.
;
Kirtman B.P.
View/Download:12/0
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