Meltwater

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Kinney Run looking downstream in Spring 2015
Cavell Glacier with Crevices and Annual Rings
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Meltwater MOSAiC
Fryxellsee Opt
Melting glacier (Skaftafellsjökull)

Meltwater is a term used to describe water that has melted from snow or ice, including glaciers, icebergs, and frozen ground (permafrost). It plays a crucial role in the hydrological cycle, influencing water availability, ecosystems, and climate change impacts. Meltwater is significant in both natural and human-modified landscapes, affecting agriculture, water resources, and flood management.

Formation and Sources[edit | edit source]

Meltwater is primarily formed during the spring and summer months when temperatures rise above freezing, causing snow and ice to melt. This process can be accelerated by direct sunlight, warm air temperatures, rainfall, and other factors such as black carbon deposits on snow and ice, which increase absorption of sunlight. In glacial environments, meltwater can also be produced at the glacier base due to geothermal heat and the pressure-induced melting point depression.

Pathways and Processes[edit | edit source]

Once formed, meltwater can take various pathways. It can percolate through snow (a process known as meltwater percolation), refreezing and forming ice lenses that contribute to the snowpack's metamorphism. Meltwater can also flow over the surface of glaciers, entering crevasses and moulins, eventually reaching the glacier's base. This subglacial meltwater plays a critical role in glacier dynamics, influencing glacial motion through lubrication of the bed.

In the broader landscape, meltwater contributes to river flows, recharges groundwater systems, and can create temporary or permanent lakes. Meltwater runoff is a critical source of fresh water in many regions, particularly those downstream of major mountain ranges like the Himalayas and the Andes, where it supports millions of people.

Impacts and Importance[edit | edit source]

Meltwater is a key factor in flood generation, particularly in regions prone to rapid snowmelt events and glacial lake outburst floods (GLOFs). These floods can have devastating effects on communities, infrastructure, and agriculture. Conversely, meltwater is also a vital resource, supporting irrigation, hydropower, and potable water supply in various parts of the world.

The study of meltwater is important for understanding climate change impacts. Glaciers and snow cover are sensitive indicators of climate change, with meltwater patterns providing clues about shifts in temperature and precipitation. Changes in meltwater flow can affect sea level rise, water security, and ecosystem health.

Challenges and Management[edit | edit source]

Managing meltwater resources in the face of climate change and increasing human demand is a significant challenge. Strategies include the development of sustainable water management practices, construction of infrastructure to control flood risks, and adaptation measures for communities dependent on meltwater.

In the context of global warming, the retreat of glaciers and changes in snowpack are altering meltwater regimes, with implications for water availability and risk management. Understanding and predicting these changes require ongoing research and monitoring.

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Contributors: Prab R. Tumpati, MD