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VICGeographySyllabus dot point

What is causing the loss of ice and snow cover, and what are the impacts on people and the environment?

the processes and human activities causing the melting of ice and snow cover as a form of land cover change, and the impacts of and responses to this change

A VCE Geography Unit 3 answer on melting ice and snow as land cover change: the warming processes driving it, environmental and human impacts, and responses, using the Arctic sea ice and Greenland ice sheet as case studies.

Generated by Claude Opus 4.76 min answer

Reviewed by: AI editorial process; not yet individually human-reviewed

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What this dot point is asking

VCAA wants you to treat the loss of ice and snow as a change in land cover, explain the process that drives it, evaluate the impacts on people and the environment, and assess responses. You need at least one located case study supported with data.

What this land cover change is

Ice and snow cover includes sea ice, ice sheets, glaciers, permafrost and seasonal snow. As global temperatures rise, this bright white cover melts and is replaced by darker ocean, rock or tundra. Because ice and snow cover changes with the seasons and over decades, geographers measure it by extent (area) and by volume or thickness.

Causes: the human activities driving the melt

  • Burning fossil fuels for electricity, transport and industry releases carbon dioxide, the main driver of the enhanced greenhouse effect that warms the planet.
  • Deforestation and land clearing add carbon and remove a carbon sink, intensifying warming.
  • Agriculture releases methane and nitrous oxide, powerful greenhouse gases.
  • The albedo feedback is the key amplifying process: white ice reflects most sunlight, but once it melts the exposed dark ocean or land absorbs far more heat, warming the area further and melting still more ice. This is a self-reinforcing loop.

Case study: Arctic sea ice and the Greenland ice sheet

The Arctic is warming several times faster than the global average, a pattern known as Arctic amplification. September sea ice extent, measured at the end of the summer melt, has declined sharply over recent decades, and the ice that remains is younger and thinner. The Greenland ice sheet, the largest body of land ice in the Northern Hemisphere, is losing mass as surface melting and faster glacier flow outpace winter snowfall.

Impacts on the environment

Melting ice raises global sea levels, because land ice that melts into the ocean adds water that was previously locked away. It destroys habitat for ice-dependent species such as polar bears, seals and walruses. Thawing permafrost releases stored carbon and methane, adding to warming. Loss of bright ice reduces the planet's reflectivity, so more solar energy is absorbed, accelerating global temperature rise.

Impacts on people

Rising seas threaten low-lying coasts and island nations with flooding and saltwater intrusion. Indigenous Arctic peoples such as the Inuit lose sea ice they rely on for hunting and travel, undermining traditional livelihoods. Thawing permafrost cracks roads, pipelines and buildings across Alaska, Canada and Siberia. Loss of seasonal snowpack in mountain ranges reduces meltwater that millions of people depend on for drinking water and irrigation.

Responses to melting ice

  • Cutting greenhouse gas emissions through the Paris Agreement and national targets addresses the root cause, since the melt is driven by global warming.
  • Renewable energy and energy efficiency reduce the fossil fuel emissions causing warming.
  • Monitoring by satellites such as NASA's GRACE and ICESat missions tracks ice loss so responses can be targeted.
  • Adaptation measures, including sea walls, managed retreat and relocating infrastructure off thawing permafrost, manage impacts that warming has already made unavoidable.

Exam-style practice questions

Practice questions written in the style of VCAA exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.

2023 VCAA10 marksDiscuss the impacts of melting ice sheets and glaciers on economic activity and social conditions at a selected location you have studied this year.
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For 10 marks you need a precise location and a discussion (causes, consequences and significance) of impacts on both economic activity and social conditions, with supporting detail. Aim to develop two or three impacts of each type and weigh their significance.

Using the Arctic and Greenland: "As the Greenland ice sheet and Arctic sea ice melt, economic activity is affected in mixed ways. New shipping routes such as the Northwest Passage open for part of the year, and retreating ice exposes minerals and oil for extraction, creating economic opportunity. However, thawing permafrost cracks roads, airstrips and pipelines, raising maintenance and rebuilding costs across Alaska and northern Canada.

"Social conditions are also affected. Indigenous Arctic peoples such as the Inuit rely on stable sea ice for hunting seals and for travel between communities. As the ice becomes thinner and less predictable, traditional hunting becomes dangerous and food insecurity rises, eroding culture and wellbeing. Coastal villages face relocation as erosion accelerates."

A high-band answer reaches a judgement, for example that the social and cultural costs to Indigenous communities outweigh the short-term economic gains, and uses the location's data throughout.

2025 VCAA5 marksa. Identify the approximate compass direction of the flow of the main body of the Fjallsjökull Glacier (1 mark). b. State the approximate length of the Fjallsjökull Glacier in 1890 and in 2010, as shown in Figure 2d (2 marks). c. Distinguish between a glacier and an ice sheet (2 marks).
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This 5 mark data question tests map and graph skills plus a key definition. Parts a and b are read directly from the data book figures, so the exact figures depend on the supplied map and cross-section; the method is what matters.

Part a (1 mark): give a compass direction read from the north arrow and the direction the glacier tongue points, for example "south-east".

Part b (2 marks): read the glacier length off the cross-section for each year, showing it has shortened, for example roughly 14 km in 1890 reducing to roughly 11 km in 2010 (state the values the figure shows for 1 mark each). The expected pattern is clear retreat over the period.

Part c (2 marks): "A glacier is a relatively confined mass of ice that forms in mountains or valleys and flows slowly downslope under gravity. An ice sheet is a far larger, continental-scale mass of ice, more than 50,000 square kilometres, that spreads outward in all directions and covers the underlying land, as in Antarctica and Greenland." One mark for each clearly contrasted feature, such as size and how the ice moves.

2025 VCAA10 marks'The application of geospatial technology has done little to effectively assess and manage rates of melting ice sheets and glaciers.' Evaluate this statement with reference to one selected location.
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For 10 marks you must evaluate the statement, meaning argue both for and against it with reference to a named location, then reach a judgement. The statement is deliberately negative, so a strong answer largely disagrees while acknowledging limits.

Against the statement (geospatial technology is effective): "At Greenland and the Arctic, satellite remote sensing such as NASA's GRACE gravity mission and ICESat laser altimetry has accurately measured ice mass loss and thinning over time, while satellite imagery tracks sea ice extent each September. This data has been essential for assessing the rate of melting and for informing climate models and policy."

For the statement (limitations): "However, geospatial technology only monitors the melt; it does not by itself manage or slow it, because the underlying cause is global greenhouse gas emissions, which require political and economic responses. Coverage gaps, cost and cloud interference can also limit data quality."

Judgement: "On balance the statement is largely incorrect for assessment, where geospatial technology has been highly effective, but partly correct for management, since monitoring alone cannot reduce melting without emissions cuts."