2018
DOI: 10.1088/1755-1315/129/1/012001
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Water table depth fluctuations during ENSO phenomenon on different tropical peat swamp forest land covers in Katingan, Indonesia

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Cited by 8 publications
(6 citation statements)
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“…This study linear with the previous findings that 2016 was recorded as the heaviest transmission in Bali Province (16). El Nino Southern Oscillation (ENSO) by the end of 2015, followed by the La Nina 2016 event, could be the underlying condition that brought the high intensity of rainfall (17).…”
Section: Discussionsupporting
confidence: 91%
“…This study linear with the previous findings that 2016 was recorded as the heaviest transmission in Bali Province (16). El Nino Southern Oscillation (ENSO) by the end of 2015, followed by the La Nina 2016 event, could be the underlying condition that brought the high intensity of rainfall (17).…”
Section: Discussionsupporting
confidence: 91%
“…The highest peak of DF incidence in January 2016 might be related to an El Nino Southern Oscillation (ENSO) event. The strong El Niño event that reached its peak in November 2015 caused an extensive and longer dry season with elevated sea surface temperature (SST) . It was followed by a light La Niña in 2016, when the rainy season started earlier and lasted longer.…”
Section: Discussionmentioning
confidence: 99%
“…It was followed by a light La Niña in 2016, when the rainy season started earlier and lasted longer. The ENSO event also influenced inter-annual rainfall variability [44], with Sumatra, Kalimantan and Malaysia being most affected [45]. This phenomenon is similar to ENSO 1992-2001 [46] and was also recorded in Taiwan in 2016 [47][48][49][50].…”
Section: Variablesmentioning
confidence: 91%
“…Limited available land in mineral soil for plantation expansion has transferred the land demand to peatland, causing deforestation and adding pressures to the peat ecosystem (Boer 2016; Uda et al 2018;Nurrochmat et al 2020). The pressure from land demand, exacerbated by the building of canals to make peatland feasible for dryland cultivation, has led to the peatland becoming increasingly exposed to the aerobic environment (Hooijer et al 2006;Carlson et al 2015) and thus more susceptible to peat fires (Wösten et al 2006;Putra et al 2008;Taufik et al 2017), which could worsen with climate change (Osaki et al 2016;Cobb et al 2017;Rossita et al 2018). It has been reported that under massive peat degradation, the peat ecosystem could lose its capacity to provide ES as carbon flux dynamics shift (Hooijer et al 2010;Gunawan et al 2016;Hirano et al 2016).…”
Section: Introductionmentioning
confidence: 99%