Once-a-century rains that have pounded the Indian state of Kerala and displaced 1.3 million people are in line with the predictions of climate scientists, who warn that worse is to come if global warming continues unabated.
The monsoon rains on which farmers in the southwestern state depend for their food and livelihoods last week dumped two-and-a-half times the normal amount of water across the state, Indian meteorologists said.
It is difficult to attribute any single extreme weather event — such as the Kerala flooding — to climate change, said Roxy Mathew Koll, a climate scientist at the Indian Institute of Tropical Meteorology in Pashan, near Mumbai.
Photo: Bloomberg
At the same time, “our recent research shows a threefold increase in widespread extreme rains from 1950 to last year, leading to large-scale flooding,” he told reporters.
Across India, flooding caused by heavy monsoon rainfall claimed 69,000 lives and left 17 million people without homes over the same period, according to a study he coauthored, which was published in October last year in Nature Communications.
In Kerala, all 35 of the state’s major reservoirs were brimming with rain water by Aug. 10, forcing local authorities to open the sluice gates on the Idukki Dam for the first time in 26 years.
“These floods that we are seeing in Kerala right now are basically in line with climate projections,” said Kira Vinke, a scientist at the Potsdam Institute for Climate Impact Research in Germany.
“If we continue with current levels of emissions — which is not unlikely — we will have unmanageable risks,” she told reporters.
The weather patterns behind these destructive downpours are well understood, even if the fingerprint of global warming is still difficult to distinguish from what scientists call “natural variability,” she added.
Rapid warming in the Arabian Sea and nearby landmasses causes monsoon winds to fluctuate and intensify for short spans of three to four days, Koll said, adding that during those periods, moisture from the Arabian Sea is dumped inland.
“Over the last decade, due to climate change, the overheating of landmass leads to the intensification of monsoon rainfalls in central and southern India,” said Elena Surovyatkina, a professor at the Russian Academy of Sciences and senior scientist at Potsdam Institute for Climate Impact Research.
The changes observed so far have occurred after an increase in the Earth’s average surface temperature of only 1°C above pre-industrial levels, she said.
On current trends, India’s average annual temperature is set to rise 1.5°C to 3°C compared with that benchmark by 2050, a World Bank report titled South Asia’s Hotspots said.
“If no corrective measures are taken, changing rainfall patterns and rising temperatures will cost India 2.8 percent of its GDP and will drag down living standards of half its population by 2050,” the World Bank said in a statement.
The 196-nation Paris climate treaty calls for capping global warming at “well below” 2°C — at 1.5°C if possible — but voluntary national pledges to reduce greenhouse gas emissions, even if respected, would still see temperatures rise at least 3°C.
Flooding is not the only problem that India’s burgeoning — and highly vulnerable — population would face as a consequence of global warming.
“What we will see with climate change in India is that the wet season is going to be wetter and the dry season drier,” Vinki said. “Already we are observing that the monsoon is becoming harder to predict with traditional methods.”
If human-generated carbon emissions continue unabated, some regions in northeast India could literally become unlivable by the end of the century due to a deadly combination of heat and humidity during heatwaves, research has shown.
Large swathes of south Asia, including the Ganges-Brahmaputra Basin, could indeed approach the threshold for survivability outdoors.
Meanwhile, coastal cities are especially vulnerable to sea-level rise, driven by melting ice sheets and expanding ocean water, on the one hand, and subsidence due to over-development and the depletion of water tables, on the other.
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