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World environment day: Rise in temperature caused faster snowmelt in March, April

Pratibha Chauhan Shimla, June 5 Even as there has been an increase of 19.47 per cent in the total area under snowfall during the last winter as compared to 18 per cent decline in 2019-20, the abrupt rise in temperature...
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Pratibha Chauhan

Shimla, June 5

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Even as there has been an increase of 19.47 per cent in the total area under snowfall during the last winter as compared to 18 per cent decline in 2019-20, the abrupt rise in temperature in March-April at various basins has resulted in the accelerated glacial melting as compared to the previous years.

The mapping of the seasonal snow in various river basins of the Chenab, the Beas, the Ravi, the Satluj, the Spiti and the Baspa through satellite imagery has indicated that the unusually warm March and April this year had resulted in glaciers melting at a faster pace and reduction in snow cover by 19-25 per cent as compared to 4-10 per cent during March-April 2021.

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“The spatial distribution of snow from October to April and its mapping is important to understand the contribution of snow in different catchments to sustain the hydrology of the river basins,” said Lalit Jain, Member Secretary, Council for Environment, Science and Technology.

The early onset of winters and snow in October-November resulted in more area under snow but early summers too have contributed in accelerated glacial melting. The temperature in April had been almost seven to eight degrees higher than normal this year.

In the Chenab basin, the rise in temperature was 1.3°C, 8.3°C and 3°C in March, April and May. Similarly, the increase was 2.3°C, 6.1°C and 3.5°C in March, April and May in Chamba and Dalhousie falling in the Ravi basin.

The unusually high temperature in April, March and May was also witnessed in the Beas basin with the maximum temperature being higher by 3°C , 7.3°C and 5°C in the three months. In the Satluj basin too, the rise in the maximum temperature was 2.8°C. 8.2°C and 2.9°C in these months.

While the Chenab and Ravi basins exhibited negative snow trends, the Satluj and Beas basins showed positive trends. This could have been attributed to the fact that Chenab and Ravi basins are adjacent to the Pir Panjal ranges and must have controlled the western disturbances. On the other hand, the Satluj and Beas basins are on the south and southeastern side, reflecting a positive trend.

Basin wise the percentage area that will meet the water requirement at the end of April was 66 per cent in case of the Chenab, 36 per cent in case of the Beas, 21 per cent in case of the Ravi and 33 per cent in case of the Satluj during ablation season, which is after May.

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