Glaciers: Case Studies Flashcards

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1
Q

Zermatt, Switzerland: Sustainable ski resort

A
  • Receives over 2million visitors each year
  • Creates huge demand for energy and water resources
  • Demand for further urbanisation
  • Increase noise and vehicle pollution
  • Zermatt marketed as sustainable ski resort
  • Town is car free, waste water is collected and reused and hotels and businesses use solar/geothermal energy
  • Company responsible for development in area have invested 1million swiss francs into environmental projects
  • Proposal for tower on Matterhorn (mountain) and new car park in Zermatt would have resulted in 9000m3 of forest being cut down for construction
  • WWF denied this proposal, showing that more can be done, such as restricting future construction and tourist numbers
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2
Q

The Alpine Convention:

A

-International treaty between Alpine countries and European Union
-Aim is to achieve sustainable development in the Alps by protecting the natural environment, while promoting economic growth
-Has to balance needs of 14million residents and 120million tourists
-Entered into force in 1995
-Consists of a number of protocols that need to be put in place to achieve sustainability
-Not all parties have ratified every protocol, e.g. Switzerland
-Protocols include:
Renewable energy, tourism, sustainable development and conservation of nature and landscape protection

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3
Q

Greenland Climate Change:

A
  • Losing ice 7x faster than in 1990s
  • 7cm ocean rise expected by end of century from Greenland alone
  • Threatens millions in low lying coastal regions
  • Roughly 1billion live less than 10m above current high-tides, with 250million under 1m
  • Greenland seen 0.75*C rise in just the past decade
  • Lost 3.8million tonnes of ice since start of study period
  • This is equivalent to 10.6mm sea level rise
  • Losing ice via surface melting and calving
  • Even in the ice sheet interior of Jakobshavn glacier, temperatures of 0*C were reached (highest ever recorded)
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4
Q

Iceland: Outburst Floods

A
  • Are particularly frequent due to volcanic activity
  • Generates both meltwater beneath glaciers and acts as a trigger for ice instability
  • When lake reaches critical size, it forces through subglacial tunnels
  • Total discharge range between 0.5 and 3.5km3 every 3 to 6 years
  • 1996 eruption of one volcano broke through ice and melted a large quantity of water, causing a glacial outburst flood that caused US$15million infrastructure damage (Nov. 5th)
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5
Q

Sagarmatha National Park: Deforestation

A

-Caused by farming, firewood for fuel, clearing areas for roads, reservoirs, etc.
-Less than 30% of Nepal’s forests remain
Consequences include:
-Exposure of soil= nutrients washed away= infertile land
-More exposed soil=increased erosion=increased landslide risk
-Disruption of water cycle- less infiltration/interception
-Less CO2 taken in from atmosphere

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6
Q

Sagarmatha National Park, Nepal: Tourism

A

-Boosted economy, improved standards of living, better healthcare, education and infrastructure
-Largely in hands of Sherpa people
Consequences:
-Water pollution
-Footpath erosion and illegal trails
-Poor waste disposal
-Increase demand for forest products/ new infrastructure
-Changes to Sherpa way of life

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7
Q

Himalayan Glacier Retreat + Avalanches:

A
  • In 2013, found that Himalayan glaciers shrunk 13% in last 50 years
  • Creates consequences for farming and hydropower generation downstream
  • Glacial retreat causes the growth of lakes dammed by glacial debris
  • Natural dams broken by avalanches and earthquakes, leading to catastrophic flooding
  • In August 1985, glacial outburst flood led to 10-15m high surge of water that destroyed the Namche Hydropower Project
  • In April 2015, 7.8M earthquake struck Nepal, triggering several large avalanches on and round M. Everest
  • One swept into South Base Camp, killing 22 people, including 10 Sherpas
  • Areas in Peru and Bolivia covered by glaciers shrank by 25% over the last 30 years
  • Around 85% of the Himalayan glaciers are in rapid retreat
  • In 1949 in Tajikistan glaciers covered 18,500km2 of land by 2012 they covered only 11,000km2 (38% decrease)
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8
Q

Sagarmatha National Park, Nepal: Future Management

A
  • Establishing plant nurseries to re establish forests on hill slopes and reduce erosion
  • Setting up projects, including schools, hospitals and bridges
  • Banning goats in certain areas to protect vegetation
  • Using kerosene for fuel instead of deforesting large areas of forest
  • Building micro HEP stations for local use
  • Limiting major development projects
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9
Q

Arctic/Antarctic Tourism:

A

-Polar tourism becoming much more accessible that it was in the Victorian Era
-Annual figures have doubled since 1990s
-1million tourists annually became 2million in 2014
-Greenland tourism up 400% since 2004
-Main issue is landing sites (nearly 200) which could spread damage to uninhabited pristine areas
-Tourist numbers have become too large and need to be limited
Some environmental impacts include:
-Wildlife disturbance
-Litter/waste/fuel spills
-Removing historic artefacts
-Disruption of important research
-Increase GHG emissions in these areas

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10
Q

The Lake District: Tourism

A
  • 16million tourists each year
  • Landscape and ecology under threat
  • Walking, climbing and camping leads to footpath erosion, trampling and littering
  • Local economy benefits greatly, where in 2014, visitors contributed £1.1billion
  • Tourism provides 16,000 jobs in the National Park
  • Exposed soil washed away by heavy rain, which can wash away nutrients and make the soil infertile
  • Therefore, the fragile ecosystem is most under threat from tourism
  • Climate change likely to worsen problem due to an increase in non native species, greater risk of extreme weather events and migration of certain habitat upwards
  • Environment becoming more fragile
  • Walkers are destroying vegetation and compacting the soil, leading to a reduction in infiltration
  • Caused localised flooding as well as exposing the soil so that it is being easily washed away in heavy rain, reducing its fertility`
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11
Q

Farming in Bolivia:

A
  • In countries such as Nepal, Bolivia and Ethiopia, the highlands are largely inhabited by indigenous communities who gain their living from subsistence farming
  • In Bolivia 70% of people live in the High Andes, growing crops to feed themselves, however only earn 30% of the country’s GDP
  • Almost all of the 60% living below the poverty line are Indigenous Mestizo population living in the High Andes
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12
Q

HEP as economic value of glaciated landscapes:

A
  • HEP is a major use of water derived from glaciers
  • Both Norway and New Zealand derive over 90% of their electricity from this source from either a natural ribbon lake or a dam/reservoir in a glaciated valley provide HEP
  • Switzerland has over 600 HEP stations producing 70% of its electricity
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13
Q

Effect of global warming on river discharge:

A
  • Summer months discharge is highest
  • Decrease in the long term as most glaciers have melted
  • Will increase in short term as more meltwater will drain downstream
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14
Q

Effect of global warming on sediment yield:

A
  • Decrease in winter
  • Increase in summer as ablation is highest which will release trapped sediment
  • Short term increase but long term increase as few glaciers left so less sediment release
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15
Q

Effect of global warming on water quality:

A
  • Lower volume of water, worse water quality in long term

- Increased sediment means water increasingly cloudy and sediment laden

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16
Q

Biodiversity in Low Arctic Latitudes:

A
  • Continuous of low ground vegetation, such as sedges, mosses in the wetter holloes and scattered dwarf trees
  • Elsewhere, heaths, grasses and rapidly flowering plants flourish
  • High biodiversity here
  • Will be lost if these areas are not protected
17
Q

Biodiversity in Higher Arctic Latitudes:

A
  • Polar desert conditions prevail
  • Small range of plants survive in sheltered locations such as the purple saxifrage and the arctic poppy
  • Not found anywhere else and they will be lost if not protected
18
Q

How long does the growing season last in the Arctic?

A

3 months

19
Q

What is the average temperature during growing season?

A

Rise to 12*C

20
Q

What happens during the Summer in the Arctic?

A
  • Surface layer of permafrost begins to melt to form bogs and shallow lakes
  • Attract insects and in turn attract migrating birds
  • Supports variety of larger animals such as Arctic Fox, grey wolves, snow geese and musk oxen
21
Q

What happens during Winter in the Arctic?

A
  • Temperature fall well below freezing
  • Plants must survive under the snow and be prepared to re emerge and flower quickly once temperature rise again in spring
  • Many animal hibernate
22
Q

What role do glaciated landscapes play in the water cycle?

A
  • Store approximately 75% of world’s freshwater
  • Glaciers store only 2%, most of it is stored in the ice sheets
  • During summer months, meltwater serves as a water source for settlements downstream creating storage in lakes and rivers
  • The Alps known as the ‘water towers of Europe’ and transport 216km3 of water a year to nearby regions
  • Meltwater used for drinking water and HEP
23
Q

What role do glaciated landscapes play in the carbon cycle?

A
  • Extensive areas of permafrost and tundra peat are major areas for soil carbon and methane storage
  • As much as 14% of Earth’s carbon is stored in the permafrost
  • Currently Arctic acts as a carbon sink due to the limited rate of decomposition
  • However, melting of permafrost creates a positive feedback loop
  • Polar sea ice reduced by global warming due to the dark oceans absorbing more solar radiation due to less white ice sheets to reflect heat (Albedo effect). Increasing warming of oceans further reduces Albedo effect
  • Lower levels of snow cover increase areas of bare rock exposed to solar radiation. Heat absorption from sun increases, leading to increased temperatures and snowmelt
  • Could turn Arctic into carbon source
  • Some scientist claim melting of permafrost wont be an issue as new growing vegetation will use the carbon before it can be released into the soil
  • New vegetation can then take in carbon for photosynthesis