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Rapid Melting of Turkiye’s Mount Cilo Glaciers

Why in the News ?

Mountain glaciers on Cilo Mountain, the second-largest glacier zone in southeastern Turkey, are experiencing rapid melting of glaciers due to climate change impact. Experts warn that nearly 50% of ice cover has disappeared over the past four decades, intensifying heatwaves and drought. This melting of alpine glaciers is part of a broader trend affecting water resources and contributing to sea level rise globally, necessitating improved water resource management strategies and attention to groundwater availability.

Glacier Retreat Observed on Mount Cilo:

Cilo Mountain, at 4,135 meters, lies in Hakkari province near the Iraq border.

● It holds Turkiye’s second-largest glacier system, after Mount Ararat.

Kemal Ozdemir, a local mountain guide, noted that visible glacier chunks now float downstream, showing accelerated melt and increased glacial meltwater.

● Areas once permanently ice-capped are now bare rock and grass, reflecting rapid warming and changes in local microclimates.

Waterfalls are flowing more intensely, signalling rapid glacial melt feeding streams and potentially forming meltwater lakes in the alpine watershed.

Impact of Climate Change in Turkiye

Human-induced global warming has intensified heatwaves and droughts across southeastern Turkey.

● The country recently recorded a historic high of 50.5°C.

● The melting rate has exceeded scientific predictions, alarming researchers involved in world glacier monitoring efforts and glacier database maintenance.

Geographer Onur Satir from Yuzuncu Yil University states that nearly half the glacier mass has vanished in 40 years, highlighting the need for an updated glacier inventory.

● Melting glaciers disrupt water availability, threaten biodiversity, and risk natural disasters like floods, impacting overall ecosystem integrity and alpine springs.

About Glaciers and Climate Change :

Glaciers are critical freshwater reservoirs, regulating river systems and climate, influencing groundwater recharge and surface runoff patterns in the alpine watershed.

● Their retreat is a key climate indicator, monitored by global bodies like the UN and IPCC using advanced techniques such as environmental isotopes and carbon isotopes analysis.

● According to the UN, many world glaciers may not survive this century, a stark contrast to conditions during the Little Ice Age.

● Melting glaciers contribute to sea level rise and alter weather patterns, affecting hydrogeological processes and potentially leading to coastal erosion.

Glacier monitoring and preservation efforts need international cooperation and strong climate policies, including international outreach programs.

● The melting of mountain glaciers is not just a local issue but part of the broader climate crisis affecting alpine communities worldwide, from the Andes Mountains to Glacier National Park.

● The process of iceberg calving in tidewater glaciers is accelerating, further contributing to ice mass loss and sea level rise.

Mount Kenya: Key Facts
Location: Situated in Central Kenya, East Africa.
Coordinates: Lies at 0°9′S 37°18′E, close to the Equator.
Elevation: Rises to 5,199 meters (17,057 feet); Africa’s second-highest peak after Mount Kilimanjaro.
Geological Type: An extinct stratovolcano, formed over 3 million years ago.
Glacial Coverage: Once had extensive glaciers, now shrinking rapidly due to climate change.
Protected Area: Enclosed within Mount Kenya National Park, a UNESCO World Heritage Site.
Flora: Hosts unique alpine vegetation, including Afro-alpine moorlands and giant lobelias.
Fauna: Inhabited by elephants, buffaloes, leopards, and endemic species like the Mount Kenya mole shrew.
Significance: Acts as a water tower for millions and holds cultural and ecological importance.
Tourism: A hub for trekking, mountaineering, and ecotourism, drawing nature lovers and adventure seekers globally.