24/7 monitoring of 13 glacial lakes underway in Uttarakhand due to GLOF threat, starting with Vasundhara Tal
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Aaj Tak
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24/7 monitoring of 13 glacial lakes underway in Uttarakhand due to GLOF threat, starting with Vasundhara Tal

An early warning system is being installed in the Chamoli district of Uttarakhand state to monitor the threat of Glacial Lake Outburst Floods (GLOFs) originating from the Vasundhara Tal glacial lake. This installation is the first of its kind placed on a glacial lake in Uttarakhand. Its purpose is to continuously track the water level in the lake and any changes in the surrounding terrain.

This campaign is being conducted under the supervision of the Uttarakhand State Disaster Management Authority (USDMA) and will last until October 15th. For this, a team of scientists and technical experts traveled from Dehradun to Vasundhara Tal. The group includes specialists from the Central Building Research Institute (CBRI) in Roorkee and the Wadi Institute of High Altitude Geology in Dehradun. Military personnel from SDRF, NDRF, and ITBP have also joined the team.

Vasundhara Tal is one of 13 glacial lakes classified by the National Disaster Management Authority (NDMA) and technical institutions as high-risk lakes. A sudden release of a large volume of water from a glacial lake can cause severe flooding in downstream areas. It is because of this danger that observation of these lakes is being intensified.

GLOF, or Glacial Lake Outburst Flood, occurs when water from a lake near a glacier suddenly bursts out. This can lead to very rapid water movement downstream and create a flood threat. Meltwater accumulates in glacial lakes. The risk increases if there is intense snowmelt or heavy rainfall, which leads to an increase in the lake's water level. Furthermore, changes to the ice or earthen dam holding the lake, or landslides, also increase the danger.

The system being installed at Vasundhara Tal will use sensors, satellite communication, and real-time data monitoring. Sensors will collect information about the condition of the lake and its surroundings. This data will be constantly monitored to promptly detect any significant changes in the lake. Since mobile and conventional communication methods are often unavailable in the Himalayan high-altitude regions, satellite data transmission will be extremely useful. This will allow scientists and administrators to monitor the lake's condition remotely.

According to data from the National Remote Sensing Centre (NRSC) for 2023, 344 glacial lakes have been identified in Uttarakhand, of which 13 are classified as high-risk lakes. Six of these are in Pithoragarh, four in Chamoli, and one each in Bagheshwar, Tihri, and Uttarkashi. Six of these 13 lakes have undergone bathymetric surveys. These include Saraswati Tal and Vasundhara Tal in Chamoli, Kedartal and Mabang, and Pyungru and Sukti Yankti in Pithoragarh. This survey provides information about the lake's depth and the volume of water it contains.

The work initiated at Vasundhara Tal is part of a plan to enhance monitoring of Uttarakhand's glacial lakes. The state government plans to strengthen similar systems in high-altitude areas in collaboration with scientific institutions, experts, and disaster management agencies. This will help in timely understanding of changes occurring in the glacial lakes. If a risk situation arises in any lake, the relevant departments will receive advance information, providing more time to take necessary measures.

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NASA study indicates Arctic thaw season stabilized after decades of advance
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NASA study indicates Arctic thaw season stabilized after decades of advance

A study conducted by NASA, and published in the journal Communications Earth & Environment, revealed that the period of sea ice melt in the Arctic, which had been extending over several decades, appears to have reached a point of stability starting in 2010. The analysis was based on satellite observation data collected between 1979 and 2023.

The research demonstrated that currently, the Arctic melt season lasts approximately 40 days longer compared to 1979. However, most of this accumulated increase occurred before 2010; since then, the average duration has remained relatively constant, despite showing large annual variations.

Scientists monitored both the start of the thaw in spring and the return of freezing in autumn. The investigation pointed out that the change in the season's duration was primarily due to freezing occurring later in the year, and not due to an earlier start to the spring thaw.

Linette Boisvert, a sea ice scientist at NASA's Goddard Space Flight Center and co-author of the study, explained to Phys.org that previously there was a greater amount of multiyear ice that resisted summer heat. Currently, with the ice being thinner and in smaller quantities, variability has increased significantly.

Climate Implications and Future Concerns

The findings do not suggest that global climate changes have stopped impacting the Arctic. The region continues to warm at a rate almost four times higher than the global average, and the remaining sea ice is visibly thinner than in past decades.

Therefore, the study suggests that the Arctic may have entered a new phase, where specific annual climate patterns exert greater influence on the length of the melt season. However, researchers warn that this apparent stabilization may be temporary.

There is still thick ice present throughout the year north of Greenland and in the Canadian Arctic Archipelago. If this ice continues to become thinner, a new phase of acceleration in sea ice loss may emerge, extending the melt season again. Researchers emphasize the continued need for satellite observations of Arctic sea ice and the energy balance governing its growth and melting, as it is not yet clear whether this stabilization represents a permanent change or merely a pause before a new cycle of accelerated transformation.

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