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. |