Shillong, Sept. 21 -- Meghalaya's Mawsynram and Cherrapunji, among the world's wettest places, are facing a growing drought risk as climate change brings heavier rain, fewer rainy days and rising temperatures, a new study has found.

The study, published in Theoretical and Applied Climatology recently, analysed projected climate and hydrological data for the state and adjoining areas for the period 1981-2100 to understand the apparent paradox of increasing rainfall intensity alongside rising drought vulnerability.

Researchers Ashesh Rudra Paul and Pankaj Kumar Roy found that rainfall is becoming concentrated in intense spells, while light rain and the number of rainy days are declining.

The study recorded an increase in the Simple Daily Intensity Index (SDII), with a maximum local rise of 0.08 mm per day per year.

The number of rainy days, meanwhile, declined by an average 0.40 days per year. SDII is a climate index that measures the average amount of rainfall on a "wet day" over a specific period, usually given in millimeters per day (mm/day).

"Contrary to the conventional expectation that increased precipitation alleviates drought," the researchers said, the findings showed "a clear tendency toward elevated drought risk" in Meghalaya.

The changing rainfall pattern is particularly significant for Meghalaya because of its steep terrain and shallow soils, the researchers said. Intense rain causes rapid surface runoff instead of being absorbed into the soil, reducing groundwater recharge. As a result, large amounts of monsoon rain may not translate into enough water being available during drier months.

"Such rainfall concentration enhances surface runoff and reduces infiltration," the study said.

Rising temperatures are adding to the pressure by increasing evapotranspiration, or water loss from soil, vegetation and other surfaces. Minimum temperatures were found to be rising by as much as 0.08 degrees Celsius per year.

The researchers said higher temperatures increase atmospheric water demand and accelerate soil-moisture loss during rain-free periods.

To assess drought, the researchers used the Standardised Precipitation Evapotranspiration Index, or SPEI, at a three-month timescale. The analysis indicated an increasing frequency and intensity of moderate, severe and extreme drought events, particularly under the high-emission SSP585 scenario.

Published by HT Digital Content Services with permission from Millennium Post.