2022
DOI: 10.1007/s44195-022-00016-0
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The impact of El Niño southern oscillation and Indian Ocean Dipole on the burned area in Indonesia

Abstract: Land and forest fire have been identified as one of the main problems contributing to forest biodiversity and Global Warming and well known as the phenomenon affected by El Niño Southern Oscillation (ENSO) and Indian Ocean Dipole (IOD). The total burned area becomes higher when either El Niño or positive IOD occur. This research aims to analyze and quantify the direct correlation of the Niño 3.4 and difference between west and east pole of IOD sea surface temperature anomaly (SSTA) to the burned area in Indone… Show more

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Cited by 19 publications
(13 citation statements)
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“…It is important to note that we did not analyze other important drivers such as El Nino Southern Oscillation (ENSO) in SEA, which is a limitation. Specific to ENSO in the region and Indonesia, it was shown to be a drought-inducing agent that, combined with human drivers, affects fires spatially and temporally 62 64 . Analysis of ENSO in relation to fires requires separation of land and sea-side domains separately for ENSO impacts, including lagged-correlations.…”
Section: Discussionmentioning
confidence: 99%
“…It is important to note that we did not analyze other important drivers such as El Nino Southern Oscillation (ENSO) in SEA, which is a limitation. Specific to ENSO in the region and Indonesia, it was shown to be a drought-inducing agent that, combined with human drivers, affects fires spatially and temporally 62 64 . Analysis of ENSO in relation to fires requires separation of land and sea-side domains separately for ENSO impacts, including lagged-correlations.…”
Section: Discussionmentioning
confidence: 99%
“…A positive IOD phase features anomalously warm sea surface temperature (SST) in the western Indian Ocean and cold SST in the east, and the zonal warm-cold pattern is reversed during its negative phase. IOD events alter ocean and atmospheric circulation patterns 3 5 and the associated precipitation anomalies cause substantial impact on Indian Ocean-rim countries, such as droughts and floods in Australia 6 , 7 , Southeast Asia 8 10 , the Indian continent 11 , 12 , and East Africa 13 , wildfires in southeast Australia 14 and Indonesia 9 , coral reef dieback in western Sumatra 15 , and malaria outbreaks in East Africa 16 .…”
Section: Introductionmentioning
confidence: 99%
“…ENSO, IOD, and PDO are the main external climatic factors of tropical regions [15], [21]. Previous studies have investigated the relationship between these climate factors and IMR and discovered that ENSO, IOD and PDO are the most significant drivers of IMR variability [17], [22]- [24]. Additionally, they illustrated the impact of circulation and Indo-Pacific SST on IMR variability in order to elucidate the mechanism.…”
Section: Introductionmentioning
confidence: 99%