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| Diversity of the Pacific-Japan Pattern among CMIP5 Models: Role of SST Anomalies and Atmospheric Mean Flow [期刊论文]
Journal of Climate, 2018-01-01, 31 (17
Gong H.; Wang L.; Chen W.; Wu R.; Huang G.; Nath D.
 View/Download：30/0
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| Multidecadal fluctuation of the wintertime Arctic Oscillation pattern and its implication [期刊论文]
Journal of Climate, 2018-01-01, 31 (14
Gong H.; Wang L.; Chen W.; Nath D.
View/Download：32/0
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| Origins of biases in CMIP5 models simulating northwest pacific summertime atmospheric circulation anomalies during the decaying phase of ENSO [期刊论文]
Journal of Climate, 2018-01-01, 31 (14
Tao W.; Huang G.; Wu R.; Hu K.; Wang P.; Gong H.
View/Download：26/0
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| Large-scale pattern of the diurnal temperature range changes over East Asia and Australia in boreal winter: A perspective of atmospheric circulation [期刊论文]
Journal of Climate, 2018-01-01, 31 (7
Liu L.; Guo J.; Chen W.; Wu R.; Wang L.; Gong H.; Xue W.; Li J.
View/Download：19/0
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| Diverse relationship between ENSO and the northwest pacific summer climate among CMIP5 models: Dependence on the enso decay pace [期刊论文]
Journal of Climate, 2017-01-01, 30 (1
Jiang W.; Huang G.; Hu K.; Wu R.; Gong H.; Chen X.; Tao W.
View/Download：25/0
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| Trends in the frequency of high relative humidity over China: 1979-2012 [期刊论文]
Journal of Climate, 2015-01-01, 28 (24
Mao R.; Gong D.-Y.; Zhao T.; Wang W.; Yang J.
View/Download：17/0
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| A new upper-level circulation index for the East Asian summer monsoon variability [期刊论文]
Journal of Climate, 2015-01-01, 28 (24
Zhao G.; Huang G.; Wu R.; Tao W.; Gong H.; Qu X.; Hu K.
View/Download：21/0
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| Diverse influences of ENSO on the East Asian-western Pacific winter climate tied to different ENSO properties in CMIP5 models [期刊论文]
Journal of Climate, 2015-01-01, 28 (6
Gong H.; Wang L.; Chen W.; Nath D.; Huang G.; Tao W.
View/Download：1/0
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| The climatology and interannual variability of the East Asian winter Monsoon in CMIP5 models [期刊论文]
Journal of Climate, 2014-01-01, 27 (4
Gong H.; Wang L.; Chen W.; Wu R.; Wei K.; Cui X.
View/Download：5/0
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