Variabilitas Suhu di Samudera India Pada Saat Indian Ocean Dipole Positif Tahun 2006
The Indian Ocean Dipole (IOD) is a phenomenon of ocean and atmosphere interaction characterized by differences in sea surface temperature between the eastern (90oE-110oE and 10oS-0oN) and western (50oE-70oE and 10oS-10oN) of Indian Ocean.
Johan, Septi
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Nationwide monthly burned area monitoring in Indonesia using Sentinel-2. [PDF]
Gaveau DLA, Descals A, Salim MA.
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Global climate mode resonance due to rapidly intensifying El NiƱo-Southern Oscillation. [PDF]
Stuecker MF +8 more
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Towards developing an operational Indian ocean dipole warning system for Southeast Asia. [PDF]
Jain S +5 more
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Summer warming in the East Antarctic interior triggered by southern Indian Ocean warming. [PDF]
Kurita N +7 more
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Influence of global climate modes on wildfire occurrence in the contiguous United States under recent and future climates. [PDF]
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Seasonal predictability of an indicator of mass coral bleaching between the Pacific ocean and the East China sea with a large ensemble climate model. [PDF]
Doi T, Yasunaka S, Kurihara H.
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Coral growth records 20<sup>th</sup> Century sea-level acceleration and climatic variability in the Indian Ocean. [PDF]
Kench PS +5 more
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Miocene African topography induces decoupling of Somali Jet and South Asian summer monsoon rainfall. [PDF]
Han Z +5 more
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Enhanced global extreme droughts driven by the Indian Ocean and Pacific Ocean on decadal timescales. [PDF]
Xu Y, Guan X, Huang J, Jin S, Jin Z.
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