Knowra Climate change in Indonesia Climate change in Indonesia Climate change in Indonesia is the long-term warming and shifting of climate conditions across the archipelago, including changing rainfall, rising seas, and altered extreme-weather risks.
Jakarta land subsidence : The gradual sinking of land in and around Jakarta, caused by groundwater extraction, construction loads, and natural geological processes. Subsidence compounds rising seas and worsens flooding in Indonesia’s largest coastal city.
Indian Ocean Dipole : A climate pattern involving changing sea-surface temperature contrasts between the western and eastern tropical Indian Ocean. Its positive phase often suppresses Indonesian rainfall and can compound drought conditions.
Nationally Determined Contribution : A country’s stated climate commitments under the Paris Agreement, including targets and planned actions. Indonesia’s submission sets out mitigation targets and adaptation priorities.
Deforestation in Indonesia : The conversion or loss of Indonesian forest, driven by activities including agriculture, logging, mining, and infrastructure. Forest loss releases stored carbon and can alter local rainfall and temperature.
Climate models : Mathematical representations of the climate system used to simulate past, present, and possible future climate conditions. Models differ in regional rainfall projections, affecting local planning across the archipelago.
Peatland fires in Indonesia : Fires in drained or degraded Indonesian peatlands that release smoke and large quantities of stored carbon. Drought and heat can intensify fires, while fire emissions further warm the climate.
Indonesian Throughflow : The system of ocean currents that carries water from the Pacific through Indonesian seas into the Indian Ocean. These currents connect regional ocean heat transport with climate conditions around the archipelago.
Renewable energy in Indonesia : The use of replenishing energy sources, such as geothermal, hydropower, solar, and wind, in Indonesia. Expanding low-carbon power can reduce emissions from a fossil-fuel-dependent energy system.
Peatland drainage : The removal of water from peat soils, commonly through canals, to enable cultivation or other land uses. Drainage exposes carbon-rich peat to oxidation and makes it more vulnerable to fire.
Climate tipping point : A threshold beyond which a small additional change can trigger a large, potentially self-reinforcing shift in a climate system. The stability of tropical forests and peatlands matters for Indonesia’s carbon stores and ecosystems.
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