Topic 2 - EQ4 Flashcards
Why does a contrast have to be drawn between active and relict glacial and periglacial landscapes found in (high) polar latitudes and high altitudes?
Whereas nearly all of the former can be classified as true wilderness as they are remote, possess a harsh physical environment and carry little or no population , except for small groups of indigenous people or groups exploiting their resources short term,the latter relict areas are often more densely populated as they provide many more opportunities for economic development and employment, for example farming, forestry and tourism.
How do the qualities of the wilderness provide opportunities for spiritual refreshment?
They provide spiritual refreshment and enjoyment for many travellers and explorers who wish to experience pristine, almost wholly natural environments and almost always untouched by humans. Wildernesses have inspired an enormous range of people to write, paint and communicate their feelings and experiences - for example wilderness poets such as Robert W Service from Alaska, polar explorer John Muir or the legendary David Attenborough.
How have some areas of wilderness lost their pristine quality?
Relict environments of the summits of Snowdon or the.Cairngorms, both reached by mountain railways, only have elements of pristine quality; they have lost their innate remoteness to large quantities of tourists.
Why are wilderness areas, such as polar environments, hold value due to scientific reasons?
Environmentalists and ecologists would point this out about wilderness areas.
-They need to maintain a gene pool of wild organisms to ensure the maintenance of genetic variety.
-The need to retain wilderness so that animal communities can remain in their natural environment, for example providing sanctuary for the migratory bird and anima, communities of the Alaskan North Slope.
-To use wholly natural communities that still exist as a control system for comparison with exploited, mismanaged areas elsewhere.
What do scientists use the Arctic and Antarctic polar environments for?
Both artic and Antarctic polar environments have become ‘living labs’ for scientists. They have both similarities and significant differences in their research programmes.
How do people benefit from goods and services provided by glacial environments?
Millions of people, who live far from any mountains, benefit from a wide range of goods and services provided by glacial environments, both relict and active. These include supplies of pure mountain water, timber (usually coniferous woodland), hydroelectric power for their homes, as well as the opportunity to enjoy beautiful mountain environments such as the Alps or Himalayas for recreation and leisure.
About 8% of the worlds population live in polar and mountainous and upland areas, many of which have been glaciated in the past or still contain some glaciers albeit mostly diminishing in volume.
How do glacial environments hold economic value for farming?
Within mountainous regions in developing nations, there may be limited transport links and access to essential supplies and markets may be poor; employment opportunities can also be limited. In countries such as Nepal, Bolivia, Ethiopia, the highlands are largely inhabited by indigenous communities who gain their living from subsistence farming. In Bolivia 70% of the population lives in the High Andes, growing crops such as potatoes, quinoa and beans to feed themselves, as well as rearing llamas and alpacas, yet they earn only 30% of the country’s GDP. Almost all of the 60% of Bolivias population that live below the poverty line are indigenous Indians living in the Altiplano of the Hugh Andes. The development of internet and mobile phones, leapfrogging old technology of landlines and cables, has revolutionised their lives, providing many opportunities for cottage industries such as weaving and knitting co-operatives, and eco-tourism.
What is farming like in glaciated countries in developed areas?
In Alpine areas in developed countries, the agriculture in upland glaciated regions is primarily pastoral because of the above average precipitation, rugged terrain with steep slopes and stony, shallow soils, which together make cultivation difficult. In the truly Alpine areas transhumance is a traditional pattern of livestock management; the farming system takes advantage of the seasonal climate cycle - I’m summer animals are grazed at high altitudes on Alpine meadows, which become free from snow and provide high-quality grass. At the same time the grass in the valley bottom can be made into hay for winter feed. In the snowy winters the animals are brought down and housed near the farm houses and are fed on hay or graze the lower pastures.
How do glaciated landscapes provide economic value through forestry?
Depending on farm prices and the degree of government support systems (such as EU rural payments), hill farming is an increasing struggle in many regions and uplands are now increasingly used for forestry (silviculture). In the UK this is carried out by the Forestry Commission and private investors, with the main type of tree being non-native, quick growing conifers, such as Sitka spruce, grown for softwood timber, wood pulp and even paper. Conifers tolerate harsh climates and acidic soils that would not even be suitable for other land uses.
What is silviculture?
The planting of trees for commercial forestry
How do glacial environments provide economical value through mining and quarrying?
Glacial erosion plays an important role in removing regolith (loose overlying soil) and vegetation to expose economically valuable rocks. In many active or relict areas there are mines and quarries of mineral deposits are ores, as well as rocks such as skates as many of the glaciated mountains are made from igneous and metamorphic rocks. In lowland areas, outwash deposits from the Pleistocene Ice Sheets provide a very important source of sand and gravel for the building industry, pre-sorted by meltwater into sands and gravels to be sold as aggregates, making them very useful for making concrete.
How do glacial environments provide economic value through hydroelectricity?
HEP is a major use of water derived from glaciers. Both Norway and New Zealand derive over 90% of their electricity from this source. In most cases either a natural ribbon lake or dam and reservoir in a glaciated valley provide the HEP. Switzerland has over 500 HEP stations, producing some 70% of its electricity. Clearly HEP is a renewable ‘green’ source, although there are issues with both the reliability of the water supply and environmental concerns over damming of rivers. In mountain settlements in developing nations, such as Nepal or Bolivia, micro-hydros can revolutionise the quality of life in many villages.
Background info on Antarctica….
Antarctica was designated a continent of peace and science as a result of the 1959 Antarctic Treaty and subsequent protocols. In the International Polar Year of 2008-09, the UN Environment Programme reports that 60 countries and more than 10,000 researchers took part in scientific research there costing over $1.5billion.
What are some of the planned/ongoing researches by international Antarctic Scientists?
-Understanding global change - past, present and future by looking at ice cores.
-Researching ‘life on the edge’ to explore how ecosystems cope with intensely harsh conditions.
-Investigating subglacial Lake Vostok and other lakes beneath the ice sheet.
-Developing sustainable food webs in the Southern Ocean ecosystem. In particular, looking at changing impacts on the various tropic levels such as the decline in krill, key component of the Antarctic marine food web.
-Studying the earths upper atmosphere and its links to the lower atmosphere and the earths climate - taking advantage of unpolluted atmosphere above the continent.
-Understanding how the Antarctic ice is melting, in terms of scale and pace, using satellites and field data.
How do glaciated environments provide economic value through tourism?
-The industry has seen tremendous growth in recent decades, which has bought many economic benefits to mountain regions.
-Visitors are attracted to scenery or present day and relict glacial landscapes.
-A huge range of activities are also possible: hill walking, climbing, mountaineering and skiing. These have led to whole regions capitalising on their tourist potential.
-Glaciated regions are increasingly visited for the glaciers themselves, which puts pressure on some very fragile landscape.
Why must the economic value of any mountain tourism require careful management?
The benefits require careful management so that they are not outweighed by environmental costs to the scenery and to the culture of the local people. It’s a very fine balance. So much depends on the fragility of the landscape and the nature and intensity of the economic activities.
How do glacial and periglacial landscapes hold ecological and environmental value?
They make a very significant contribution to the world’s life support systems. Approximately 75%of all the freshwater of the world is locked up in ice - so glaciers contain nearly 2% of water overall. Glacially eroded valleys in many mountainous regions for, natural hollows for water collection, forming ribbon lakes, or can be dammed for reservoirs, for example in the English Lake District.
Why are glaciers a valuable source of water for irrigation?
They produce most water in the late spring and summer, which is often the hot, dry season when other sources dry up. For example, in the USA the Arapaho Glacier currently produces about 260 million gallons of drinking water per day for the city of Boulder, Colorado, as well as irrigating huge areas of crops such as fruit and grapes. Glaciers have a very cool and beautiful image and this is used to promote sales of bottled water.
Being composed of freshwater, icebergs also offer a potential water resource, but there are numerous complications even in their potential use.
How is permafrost and tundra useful for soil carbon storage?
The extensive areas of permafrost and tundra peat are major areas for soil carbon storage . Currently the Arctic lands remain a weak carbon sink, meaning that more carbon is added each year than is lost. However, as permafrost melts as a result of positive feedback within the climate warming process, ancient carbon being released, especially via methane emissions, thus upsetting the balance in the system.
What are carbon sinks?
These are a natural or artificial reservoir that absorbs more carbon than it releases, leading to carbon accumulation.
What is biodiversity?
This is a measure of the variety of organisms present at a particular location
What is primary productivity?
This is the rate at which energy is converted by photosynthesis; it has a major influence on the level of biodiversity.
What does permafrost cause to soil’s fragility?
The presence of permafrost in most areas in the soil increases their fragility. In the lower Arctic latitudes (around 70 to 75°N) there is a continuous cover of ground vegetation, with sedges and mosses in the wetter hollows and scattered dwarf trees on the lower ridges. Elsewhere heaths, grasses and rapidly flowering plants flourish. At higher latitudes 75 to 80 °N) and higher altitudes, polar desert conditions prevail, but a small range of plants survive in favourable sheltered locations such as the purple saxifrage and arctic poppy.
How do tundra plants have to adapt?
They have to adapt to low temperatures, drying winds and snow blasts in winter blizzards. The system has low biodiversity and low primary productivity and the low nutrient content of the Arctic soils, leading to very weak nutrient cycling in dynamic equilibrium with the underlying permafrost, so any melting will have dramatic effects.