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| The key role of ozone-depleting substances in weakening the walker circulation in the second half of the twentieth century [期刊论文]
Journal of Climate, 2019-01-01, 32 (5
Polvani L.M.; Bellomo K.
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| Historical forcings as main drivers of the Atlantic multidecadal variability in the CESM large ensemble [期刊论文]
Climate Dynamics, 2018-01-01, 50 (2018-09-10
Bellomo K.; Murphy L.N.; Cane M.A.; Clement A.C.; Polvani L.M.
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| The role of historical forcings in simulating the observed Atlantic multidecadal oscillation [期刊论文]
Geophysical Research Letters, 2017-01-01, 44 (5
Murphy L.N.; Bellomo K.; Cane M.; Clement A.
View/Download：1/0
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| Low-pass filtering, heat flux, and Atlantic multidecadal variability [期刊论文]
Journal of Climate, 2017-01-01, 30 (18
Cane M.A.; Clement A.C.; Murphy L.N.; Bellomo K.
View/Download：13/0
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| New observational evidence for a positive cloud feedback that amplifies the Atlantic Multidecadal Oscillation [期刊论文]
Geophysical Research Letters, 2016-01-01, 43 (18
Bellomo K.; Clement A.C.; Murphy L.N.; Polvani L.M.; Cane M.A.
View/Download：24/0
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| Amplification of El Nino by cloud longwave coupling to atmospheric circulation [期刊论文]
Nature Geoscience, 2016-01-01, 9 (2
Radel G.; Mauritsen T.; Stevens B.; Dommenget D.; Matei D.; Bellomo K.; Clement A.
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| Evidence for weakening of the Walker circulation from cloud observations [期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (18
Bellomo K.; Clement A.C.
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| The influence of cloud feedbacks on equatorial atlantic variability [期刊论文]
Journal of Climate, 2015-01-01, 28 (7
Bellomo K.; Clement A.C.; Mauritsen T.; Rädel G.; Stevens B.
View/Download：1/0
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| Observational and model estimates of cloud amount feedback over the Indian and Pacific oceans [期刊论文]
Journal of Climate, 2014-01-01, 27 (2
Bellomo K.; Clement A.C.; Norris J.R.; Soden B.J.
View/Download：1/0
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| Simulating the role of subtropical stratocumulus clouds in driving Pacific climate variability [期刊论文]
Journal of Climate, 2014-01-01, 27 (13
Bellomo K.; Clement A.; Mauritsen T.; Rädel G.; Stevens B.
View/Download：10/0
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