Results 221 to 230 of about 17,552 (267)

Rainfall microphysical characteristics observed in the Jakarta flood events. [PDF]

open access: yesSci Rep
Renggono F   +13 more
europepmc   +1 more source

Rising dengue risk with increasing El Niño-Southern Oscillation amplitude and teleconnections. [PDF]

open access: yesNat Commun
Tian Y   +21 more
europepmc   +1 more source

The influence of the quasi-biennial oscillation on the Madden–Julian oscillation

Nature Reviews Earth & Environment, 2021
Z. Martin   +7 more
semanticscholar   +3 more sources

Madden–Julian oscillation changes under anthropogenic warming

Nature Climate Change, 2018
The Madden–Julian oscillation (MJO) produces a region of enhanced precipitation that travels eastwards along the Equator in a 40–50 day cycle, perturbing tropical and high-latitude winds, and thereby modulating extreme weather events such as flooding, hurricanes and heat waves.
E. Maloney, Á. Adames, Hien X. Bui
semanticscholar   +2 more sources

Exceptionally Persistent Madden‐Julian Oscillation Activity Contributes to the Extreme 2020 East Asian Summer Monsoon Rainfall

Geophysical Research Letters, 2021
During June–July 2020, the record‐breaking flooding in the recent four decades struck the plum rain belt over China, Japan, and Korea. Concurrent with this persistent heavy rainfall, pronounced Indian Ocean basin warming (IOBW) was observed, following ...
Wenjun Zhang   +5 more
semanticscholar   +1 more source

Prediction of the Madden–Julian Oscillation: A Review

Journal of Climate, 2018
There has been an accelerating interest in forecasting the weather and climate within the subseasonal time range. The Madden–Julian oscillation (MJO), an organized envelope of tropical convection, is recognized as one of the leading sources of ...
Hye-Mi Kim, F. Vitart, D. Waliser
semanticscholar   +1 more source

Madden Julian Oscillation

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
openaire   +1 more source

Moisture Modes and the Madden–Julian Oscillation

Journal of Climate, 2009
AbstractMoisture 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
openaire   +1 more source

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