Summary of "Proses Terjadinya Petir"

Lightning formation

  1. Clouds: Lightning formation begins in cumulonimbus (rain) clouds where ice crystals form.
  2. Charge separation: Initially neutral ice crystals gain charge through collisions and rubbing caused by wind.
  3. Charge sorting: Heavier ice and graupel tend to become negatively charged and collect in the lower part of the cloud; lighter particles become positively charged and rise to the upper cloud.
  4. Ground charging: The ground becomes positively charged relative to the negatively charged cloud base.
  5. Discharge: When the potential difference overcomes air’s insulating threshold, negative charge discharges toward the ground, producing a bright flash (lightning) and a rapid pressure wave heard as thunder.

Types of lightning

Lightning monitoring (BMKG)

Reported benefits (as presented)

Note: These are claims presented in the source material; the magnitude and net environmental/health effects vary and are subject to scientific context.

Impacts and hazards

Safety recommendations

Researchers / sources featured

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Science and Nature


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