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A machine learning model that outperforms conventional global subseasonal forecast models. [PDF]
Nat CommunChen L +11 more
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Vertical structure and occurrence patterns of the cross-equatorial northerly surge under different ENSO and MJO phases. [PDF]
Sci RepMoteki Q.
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Unraveling the role of the western North Pacific circulation anomaly in modulating Indian summer monsoon rainfall variability beyond ENSO. [PDF]
Sci RepSon JH +4 more
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Frequent floods in the Yangtze River basin linked to a shifted Indian Ocean wave regime. [PDF]
Nat CommunDasgupta P +5 more
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Identifying Priority Habitat for Conservation of the Australian Bustard Under Climate Change Scenarios. [PDF]
Ecol EvolLamichhane S, Shephard J, Fleming PA.
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Global asymmetries in the moisture origins of atmospheric river precipitation
Crespo-Otero A +5 more
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Reviews of Geophysics, 2005
The Madden‐Julian Oscillation (MJO) is the dominant component of the intraseasonal (30–90 days) variability in the tropical atmosphere. It consists of large‐scale coupled patterns in atmospheric circulation and deep convection, with coherent signals in many other variables, all propagating eastward slowly (∼5 m s−1) through the portion of the Indian ...
Chidong Zhang
exaly +2 more sources
The Madden‐Julian Oscillation (MJO) is the dominant component of the intraseasonal (30–90 days) variability in the tropical atmosphere. It consists of large‐scale coupled patterns in atmospheric circulation and deep convection, with coherent signals in many other variables, all propagating eastward slowly (∼5 m s−1) through the portion of the Indian ...
Chidong Zhang
exaly +2 more sources
2013
The Madden Julian Oscillation, often abbreviated as MJO, is a major feature of the tropical circulation. It manifests as quasi-periodic fluctuations in the sea level pressure and wind structure, and consequently – in the sea surface temperature, convection and rainfall. The time scale of the phenomenon is, on average, about 30–60 days.
T. N. Krishnamurti +2 more
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The Madden Julian Oscillation, often abbreviated as MJO, is a major feature of the tropical circulation. It manifests as quasi-periodic fluctuations in the sea level pressure and wind structure, and consequently – in the sea surface temperature, convection and rainfall. The time scale of the phenomenon is, on average, about 30–60 days.
T. N. Krishnamurti +2 more
openaire +1 more source
Moisture Modes and the Madden–Julian Oscillation
Journal of Climate, 2009AbstractMoisture mode instability is thought to occur in the tropical oceanic atmosphere when precipitation is a strongly increasing function of saturation fraction (precipitable water divided by saturated precipitable water) and when convection acts to increase the saturation fraction.
Raymond, David J., Fuchs, Željka
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