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Predicting the severity of spurious “double ITCZ” problem in CMIP5 coupled models from AMIP simulations [期刊论文]
Geophysical Research Letters, 2017-01-01, 44 (3
Xiang B.;  Zhao M.;  Held I.M.;  Golaz J.-C.
View/Download:36/0
 
Seasonal and regional variations in extreme precipitation event frequency using CMIP5 [期刊论文]
Geophysical Research Letters, 2016-01-01, 43 (10
Janssen E.;  Sriver R.L.;  Wuebbles D.J.;  Kunkel K.E.
View/Download:2/0
 
Past- and present-day Madden-Julian Oscillation in CNRM-CM5 [期刊论文]
Geophysical Research Letters, 2016-01-01, 43 (8
Song E.-J.;  Seo K.-H.
View/Download:25/0
 
Winter warming and summer monsoon reduction after volcanic eruptions in Coupled Model Intercomparison Project 5 (CMIP5) simulations [期刊论文]
Geophysical Research Letters, 2016-01-01, 43 (20
Zambri B.;  Robock A.
View/Download:19/0
 
Double ITCZ in Coupled Ocean-Atmosphere Models: From CMIP3 to CMIP5 [期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (20
Zhang X.;  Liu H.;  Zhang M.
View/Download:14/0
 
Assessment of future changes in water availability and aridity [期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (13
Greve P.;  Seneviratne S.I.
View/Download:0/0
 
Increases in the annual range of soil water storage at northern middle and high latitudes under global warming [期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (10
Wu W.-Y.;  Lan C.-W.;  Lo M.-H.;  Reager J.T.;  Famiglietti J.S.
View/Download:38/0
 
Can the CMIP5 models represent winter frontal precipitation? [期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (20
Catto J.L.;  Jakob C.;  Nicholls N.
View/Download:11/0
 
Robust Sahel drought due to the Interdecadal Pacific Oscillation in CMIP5 simulations [期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (4
Villamayor J.;  Mohino E.
View/Download:0/0
 
Sensitivity of terrestrial precipitation trends to the structural evolution of sea surface temperatures [期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (4
Anderson B.T.;  Lintner B.R.;  Langenbrunner B.;  Neelin J.D.;  Hawkins E.;  Syktus J.
View/Download:21/0
 

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