2017
DOI: 10.1063/1.4987095
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Evolution of 2015/2016 El Niño and its impact on Indonesia

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Cited by 17 publications
(16 citation statements)
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“…A coupled ocean-atmosphere mode, namely an El Niño event (cooler waters and higher primary production), took place in the tropical Pacific Ocean during 2012 and 2015-2016, which might have influenced Lombok waters through the Indonesian Throughflow that passes through the Lombok Strait. In 2012, the El Niño occurred in August and September and was categorized as a weak El Niño [23], while in 2015, the El Niño event started to develop from April to May 2015, reached its maximum between November and December 2015, and finished in April-May 2016 [24]. This event had an El Niño index of 3.4 and was classified as a strong event [25], one of the strongest events recorded during the last two decades [24].…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…A coupled ocean-atmosphere mode, namely an El Niño event (cooler waters and higher primary production), took place in the tropical Pacific Ocean during 2012 and 2015-2016, which might have influenced Lombok waters through the Indonesian Throughflow that passes through the Lombok Strait. In 2012, the El Niño occurred in August and September and was categorized as a weak El Niño [23], while in 2015, the El Niño event started to develop from April to May 2015, reached its maximum between November and December 2015, and finished in April-May 2016 [24]. This event had an El Niño index of 3.4 and was classified as a strong event [25], one of the strongest events recorded during the last two decades [24].…”
Section: Discussionmentioning
confidence: 99%
“…In 2012, the El Niño occurred in August and September and was categorized as a weak El Niño [23], while in 2015, the El Niño event started to develop from April to May 2015, reached its maximum between November and December 2015, and finished in April-May 2016 [24]. This event had an El Niño index of 3.4 and was classified as a strong event [25], one of the strongest events recorded during the last two decades [24]. During El Niño events, it is likely that the water movement from Makassar Strait has lower flow [26], thus it could have influenced the upwelling level in the coastal waters of Lombok and Sumbawa waters because cold water with higher productivity in deep water flows to the surface.…”
Section: Discussionmentioning
confidence: 99%
“…A remarkable feature was observed in 2015 when a strong El Niño event took place in the tropical Pacific, an anomalous chl-a concentration was observed in the entire GoT and its surrounding region (Figure 4.M1-M7). Note that the peak of chl-a anomaly was observed at the end of development phase of the 2015/2016 El Niño event in September 2015 until the early peak phase of the event in October-November 2015 (Iskandar et al 2017). The chl-a concentration was rapidly reduced in December 2105 before the termination of the 2015/2016 El Niño event.…”
Section: Year-to-year Variationsmentioning
confidence: 93%
“…During 1997 and 2015, the strong El Niño and pIOD events occurred, leading to a significant decrease in precipitation over the Indonesian region including the South Sumatra (Iskandar et al, 2017a). It can be noted that the El Niño and pIOD events in 1997 and 2015 were similar in intensity; however, the number of hotspots in 2015 were more extensive than those in 1997.…”
Section: Resultsmentioning
confidence: 95%
“…In September up to October, hotspots became more extensive in the study area as the humidity and precipitation decreased more significantly. According to Iskandar et al (2017a), a large number of hotspots existed one month prior to the peak of 2015 El Niño. It is important to note that the 2015 pIOD event ended bit earlier than the typical pIOD event.…”
Section: Resultsmentioning
confidence: 99%