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| Holocene variability of East Asian summer monsoon as viewed from the speleothem δ18O records in central China [期刊论文]
Earth and Planetary Science Letters, 2021-01-01, 558
Cai Y.; Cheng X.; Ma L.; Mao R.; Breitenbach S.F.M.; Zhang H.; Xue G.; Cheng H.; Edwards R.L.; An Z.
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| Amplified tropical Pacific rainfall variability related to background SST warming [期刊论文]
Climate Dynamics, 2020-01-01, 54 (2020-03-04
Sun N.; Zhou T.; Chen X.; Endo H.; Kitoh A.; Wu B.
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| Challenges in predicting and simulating summer rainfall in the eastern China [期刊论文]
Climate Dynamics, 2019-01-01, 52 (2019-03-04
Liang P.; Hu Z.-Z.; Liu Y.; Yuan X.; Li X.; Jiang X.
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| Relative roles of dynamic and thermodynamic processes in causing positive and negative global mean SST trends during the past 100 years [期刊论文]
DYNAMICS OF ATMOSPHERES AND OCEANS, 2019-01-01, 86) : 18-32
Li, Zhibo; Liu, Jia; Li, Tim; Sun, Ying
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| EnOI-IAU Initialization Scheme Designed for Decadal Climate Prediction System IAP-DecPreS [期刊论文]
Journal of Advances in Modeling Earth Systems, 2018-01-01, 10 (2
Wu B; , Zhou T; , Zheng F
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| Inter-decadal variation of the Tropical Atlantic-Korea (TA-K) teleconnection pattern during boreal summer season [期刊论文]
Climate Dynamics, 2018-01-01, 51 (2018-07-08
Ham Y.-G.; Hwang Y.J.; Lim Y.-K.; Kwon M.
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| Early summer southern China rainfall variability and its oceanic drivers [期刊论文]
Climate Dynamics, 2018-01-01, 50 (2018-11-12
Li W.; Ren H.-C.; Zuo J.; Ren H.-L.
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| Nonlinear interactions between the Amazon River basin and the Tropical North Atlantic at interannual timescales [期刊论文]
Climate Dynamics, 2018-01-01, 50 (2018-07-08
Builes-Jaramillo A.; Marwan N.; Poveda G.; Kurths J.
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| A warming tropical central Pacific dries the lower stratosphere [期刊论文]
Climate Dynamics, 2018-01-01, 50 (2018-07-08
Ding Q.; Fu Q.
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| Recent interdecadal shift in the relationship between Northeast China’s winter precipitation and the North Atlantic and Indian Oceans [期刊论文]
Climate Dynamics, 2018-01-01, 50 (2018-03-04
Tingting H.; Shengping H.; Xin H.; Huijun W.
View/Download：10/0
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