Results 11 to 20 of about 3,114 (254)
Years of the Maritime Continent [PDF]
Geophysical Research Letters, 2020 Abstract Years of the Maritime Continent (YMC) is a multiyear international program with participants from over 15 countries. Its overarching goal is to expedite the progress toward improving understanding and prediction of the local oceanic and atmospheric multiscale variability of the Indo‐Pacific Maritime Continent (MC) and its ...
Kunio Yoneyama, Chidong Zhang
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The progression of the boreal winter monsoon through the western Maritime Continent as differentiated by ENSO phase [PDF]
Advances in Geosciences, 2016 The impact of global ENSO on the regional monsoon onset over the Maritime Continent is examined, using satellite-derived scatterometer surface winds over the sea channel from the South China Sea, through the Karimata Strait into the Java Sea. An index
S.-Y. Lee, J. L. McBride
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Change in Salinity of Indonesian Upper Water in the Southeastern Indian Ocean during Argo Period
Heliyon, 2022 The change in salinity of Indonesian Upper Water (IUW) in the Indian Ocean has been examined during 2004–2020 based on the Argo product. Monthly salinity fields reveal a contrast of IUW salinity changes between two time periods (2004–2013 and 2014–2020 ...
Mochamad Riza Iskandar, Toshio Suga
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Wet and Dry Cold Surges Over the Maritime Continent
Journal of Geophysical Research: Atmospheres, 2022 AbstractCold surges are synoptic weather systems that occur over the Maritime Continent during the boreal winter. They are characterized by the strengthening of prevailing low‐level northerly to north‐easterly winds, temperature falls of a few degrees over several days, and in some cases, heavy prolonged rainfall and flooding.
Isaac Tan +4 more
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Island Rainfall Enhancement in the Maritime Continent
Geophysical Research Letters, 2020 AbstractThe hypothesis that the islands of the Maritime Continent (MC) enhance total rainfall and time‐mean upward motion is tested using a convection‐permitting regional model. Sensitivity experiments with the islands removed greatly diminish both rainfall and upward motion, supporting the hypothesis.
James H. Ruppert, Xingchao Chen
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Active and weakening MJO events in the Maritime Continent [PDF]
Climate Dynamics, 2021 AbstractTo better understand the Madden–Julian Oscillation (MJO) in the Maritime Continent (MC), events from 1980 to 2019 were classified as active or weakening according to propagation characteristics and amplitude changes in two leading indices, the Real-time Multivariate MJO (RMM) index and Outgoing Longwave Radiation (OLR) MJO Index (OMI).
Bradford S. Barrett +3 more
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Scale Interactions between the MJO and the Western Maritime Continent [PDF]
Journal of Climate, 2016 Abstract State-of-the-art regional climate model simulations that are able to resolve key mesoscale circulations are used, for the first time, to understand the interaction between the large-scale convective environment of the MJO and processes governing the strong diurnal cycle over the islands of the Maritime Continent (MC). Convection
Birch, CE +6 more
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Precipitation regime changes in the maritime continent [PDF]
, 2022 This thesis focuses on changes in the precipitation regime in the Maritime Continent. The Maritime Continent is the region between the Indian and Pacific oceans consisting of the Indonesian and Philippine archipelagos and countless other smaller islands. The Maritime Continent connects the Indian and Pacific oceans and plays a crucial role in the world’
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Gaoyuan qixiang, 2022 Snow cover over the Qinghai-Xizang Plateau （QXP） is an important physical factor that affects the Asian monsoon system through atmospheric circulation.The boreal summer intraseasonal oscillation （BSISO， including a 30~60-day BSISO mode named BSISO1 and a
Yanchao CAO, Xiaochun WANG
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The Indo‐Pacific Maritime Continent Barrier Effect on MJO Ensemble Prediction
Geophysical Research Letters, 2023 The barrier effect of the Indo‐Pacific Maritime Continent (MC) on the Austral summertime Madden‐Julian Oscillation (MJO) is explored using retrospective forecasts from subseasonal‐to‐seasonal (S2S) prediction models.
S. Abhik, Chidong Zhang, Harry H. Hendon
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