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What happens to the ocean surface gravity waves when ENSO and MJO phases combine during the extended boreal winter? [期刊论文]
Climate Dynamics, 2020-01-01, 54 (2020-03-04
Godoi V.A.;  de Andrade F.M.;  Durrant T.H.;  Torres Júnior A.R.
View/Download:11/0
 
Modelling the role of Atlantic air–sea interaction in the impact of Madden–Julian Oscillation on South American climate [期刊论文]
International Journal of Climatology, 2019-01-01, 39 (2
Barreiro M.;  Sitz L.;  de Mello S.;  Franco R.F.;  Renom M.;  Farneti R.
View/Download:28/0
 
Interactions between intraseasonal and diurnal variability of precipitation in the South Central Pacific: The case of a small high island, Tahiti, French Polynesia [期刊论文]
International Journal of Climatology, 2019-01-01, 39 (2
Hopuare M.;  Guglielmino M.;  Ortega P.
View/Download:18/0
 
Regional-scale ocean wave variability associated with El Niño–Southern Oscillation-Madden-Julian Oscillation combined activity [期刊论文]
International Journal of Climatology, 2019-01-01, 39 (1
Godoi V.A.;  de Andrade F.M.;  Bryan K.R.;  Gorman R.M.
View/Download:32/0
 
全球变化背景下北半球冬季 MJO传播的年代际变化 [期刊论文]
大气科学, 2019-01-01, 43 (1) : 803-814
修军艺;  温敏;  王遵娅;  张人禾
View/Download:5/0
 
全球变化背景下北半球冬季 MJO传播的年代际变化 [期刊论文]
大气科学, 2019-01-01, 43 (1) : 155-170
修军艺;  温敏;  王遵娅;  张人禾
View/Download:7/0
 
The role of SST variability in the simulation of the MJO [期刊论文]
Climate Dynamics, 2018-01-01, 51 (2018-07-08
Stan C.
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Intrinsic precursors and timescale of the tropical Indian Ocean Dipole: insights from partially decoupled numerical experiment [期刊论文]
Climate Dynamics, 2018-01-01, 51 (4
Crétat J.;  Terray P.;  Masson S.;  Sooraj K.P.
View/Download:37/0
 
Predictability of CFSv2 in the tropical Indo-Pacific region, at daily and subseasonal time scales [期刊论文]
Climate Dynamics, 2018-01-01, 50 (2018-11-12
Krishnamurthy V.
View/Download:4/0
 
Planetary scale selection of the Madden–Julian Oscillation in an air-sea coupled dynamic moisture model [期刊论文]
Climate Dynamics, 2018-01-01, 50 (2018-09-10
Wei Y.;  Liu F.;  Mu M.;  Ren H.-L.
View/Download:50/0
 

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