Meliput cuaca ekstrem dan perubahan iklim

The document serves as a journalistic guide to 'event attribution', the scientific method used to determine if and to what extent climate change influenced a specific extreme weather event. It warns against common reporting errors—such as ignoring climate change, claiming it as the sole cause without evidence, or over-caution in reporting heatwaves—and provides specific scientific guidance on heatwaves, floods, droughts, wildfires, tropical cyclones, and heavy snowfall.

• Event attribution studies use climate models to compare the modern world (influenced by human activity) with a simulated 'natural world' without human emissions to calculate how much more likely or intense an extreme event became due to global warming.
• Heatwaves are the most straightforward events to attribute; every heatwave globally is now more likely and more intense due to human-induced climate change.
• Extreme rainfall has become more frequent and intense in most parts of the world since the 1950s due to the 'Clausius-Clapeyron' relationship, where warmer air holds more moisture (approximately 7% more per 1ºC).
• Climate change increases drought risk primarily through increased evaporation and more sporadic, intense rainfall that fails to maintain soil moisture, with high-confidence links in Central and East Asia, Southern Australia, the Mediterranean, Southern Africa, and Western North America.
• While the total number of tropical cyclones per year is not increasing globally, climate change has increased the frequency of the strongest and most destructive storms (Categories 3-5), increased their rainfall, and raised storm surges via sea-level rise.
• Wildfire risk is increasing in areas where heat and drought trends overlap, with clearly attributable increases in probability and burned area in Southern Europe, Northern Eurasia, the United States, and Australia.
• Extreme cold events have decreased in likelihood and intensity worldwide, though heavy snowfall remains highly uncertain and difficult to simulate, with possible intensity increases only in high-latitude regions like Northern Asia, North America, and Greenland.

APA

Clarke, B., & Otto, F. (n.d.). Meliput cuaca ekstrem dan perubahan iklim. World Weather Attribution. http://www.worldweatherattribution.org/wp-content/uploads/WWA_GuideIN_2111_Final.pdf

Chicago

Clarke, Ben, and Friederike Otto. Meliput cuaca ekstrem dan perubahan iklim. World Weather Attribution, n.d. http://www.worldweatherattribution.org/wp-content/uploads/WWA_GuideIN_2111_Final.pdf.

Wikipedia

{{cite report |last1=Clarke |first1=Ben |last2=Otto |first2=Friederike |title=Meliput cuaca ekstrem dan perubahan iklim |publisher=World Weather Attribution |url=http://www.worldweatherattribution.org/wp-content/uploads/WWA_GuideIN_2111_Final.pdf |access-date=23 October 2026 |via=Climate Insights Directory}}

BibTeX

@techreport{clarkendmeliput, author = {Clarke, Ben and Otto, Friederike}, title = {{Meliput cuaca ekstrem dan perubahan iklim}}, institution = {World Weather Attribution}, url = {http://www.worldweatherattribution.org/wp-content/uploads/WWA_GuideIN_2111_Final.pdf}, urldate = {2026-10-23}, note = {Indexed by Climate Insights Directory} }