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Science Not yet confirmed elsewhere1 publisher 3 min read Published

Kalimantan's fires: El Nino is the multiplier, the drained peat is the base rate

NASA FIRMS counts show a sharp August spike across five provinces. A published study puts El Nino's megafire effect at roughly 2.7x, and severe fires still happen without it.

The Scientist · Science desk

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What happened

  • MODIS via FIRMS counted roughly 5,206 thermal anomaly pixels across Kalimantan on Aug. 18, 2026, equal to 520,600 hectares of observation area.
  • VIIRS detections for Aug. 1-18 were led by West Kalimantan with 82,728 pixels, ahead of Central Kalimantan's 34,105 and East Kalimantan's 20,686.
  • The authors stress that the resulting 2.24 million hectare pixel-area total is not a burn scar measurement.
  • A study in npj Natural Hazards puts El Nino's effect on Kalimantan megafire risk at roughly 2.7 times, while severe fires occur in every ENSO phase.

Why it matters

  • What it costs cost Whoever holds the plantation drainage licences does not receive the invoice; Indonesian GDP does, at 1.9% of it in 2015.
  • What it limits constraint An ENSO forecast cannot serve as a fire-risk forecast while the peat stays drained: rain restores flow but not storage, and the retention loss is described as nearly irreversible over decades.
  • Who has to decide decision Calling this weather funds haze advisories and firefighting; calling it drainage funds canal blocking and licence review. The all-ENSO-phase evidence narrows which of the two is defensible.
  • Who's exposed exposure Smoke crossing into neighbouring countries turns the hydrology of Kalimantan's peat into a diplomatic exposure rather than a provincial land management file.

Start with the arithmetic the pixel totals hide. Add the five provincial VIIRS counts and you get 159,278 detections over 18 days [16], an average of about 8,850 a day [19], with West Kalimantan alone supplying 52% of them [17]. One VIIRS pixel at 375 metres a side covers 14.06 hectares, which is how those detections turn into the 2.24 million hectare figure [14]. The authors say plainly it is not burned area [8], and the size of that caveat deserves stating in local terms: 2.24 million hectares is close to half of all the peatland in Kalimantan [15]. Sensor choice moves the number as much as fire does. A MODIS pixel covers 100 hectares, about seven times a VIIRS pixel [20], which is why one day of MODIS detections converts to 520,600 hectares of observation area [6].

What the detections do locate is where the water stopped being held. Peat forms under waterlogged conditions and resists burning as long as the water table stays high [9]. Canals cut to clear peat for plantations removed that condition [1]. Soil holds moisture through its structure, organic matter, porosity and groundwater level, and once those are disturbed a short dry spell behaves like a long one [2]. According to the analysis, pulpwood and oil palm expansion is what cost Borneo that retention capacity, and the loss has been nearly irreversible for decades [3].

That reading is what makes the 2.7 figure from the npj Natural Hazards study a multiplier and not a cause [10]. A multiplier needs something to act on. The same study notes severe fires continue across all ENSO phases, La Nina included [10], so the quantity being amplified is not zero when the Pacific is neutral or cool. El Nino sets the year. Drainage sets the level.

The cost record points the same way. The World Bank put 2015 losses at US$16.1 billion, about 1.9% of Indonesian GDP [11], and 2019 at US$5.2 billion, about 0.5% [12]. In dollars, 2015 was 3.1 times 2019; as a share of the economy, 3.8 times [18]. Both bills were presented to the same degraded landscape, and the recurring pattern across 1997-98, 2015 and 2019 was drought arriving on ground already prepared for it [13]. The variable that swung between those two years was rainfall, which no ministry controls. The variable that persisted was the water table, and the canals that lowered it were dug on purpose [1].

That is the practical asymmetry in this data. Smoke is now choking residential areas and drifting across borders [4], and the near-real-time counts will fall when the rains come, because thermal anomalies track flame rather than the condition underneath it. Storage capacity in 4.5 million hectares of peat [9] will not recover on the same schedule.

What to watch

  • Whether daily VIIRS counts keep climbing past mid-August as the dry season runs on, or flatten before the rains.

Clarity's read

What the record supports and how the coverage leans. The claims behind it follow.

Reality

Evidence58
Adoption38
Hype gap+12
Incentives55
Confidence52
Why these scores

Claim ledger

Ranked by verification strength, evidence, and original report placement.

  1. [1]

    Drainage networks constructed to clear peatlands for plantations have upended the water balance that keeps peat resilient.

  2. [2]

    Soil structure, organic matter, porosity, groundwater levels and vegetation cover determine how long moisture remains after rain stops; when these functions are disrupted, landscapes become hypersensitive to dry spells.

  3. [3]

    Major fires happen when dry weather meets a Bornean landscape that has lost its natural capacity to retain water because of the expansion of industrial plantations such as pulpwood and oil palm, a loss described as nearly irreversible for decades.

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Sources

1 independent publisher whose own reporting we read for this story.

  1. phys.org

    1 article · August 24, 2026

    Borneo forest fires spike again: Why El Niño isn't the sole culprit

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