Alpine Area Flashcards
altitude
alpine refers to areas above the tree line (climatic limit of tree growth - where the mean temperature of the warmest month is less than 11 degrees C) and below the snow line (zone of permanent snow cover)
latitude + altitude
the tree line decreases approximately 110 m in altitude for each additional 1 degree of latitude from the equator
New Guinea highlands (6 degrees S) has a treeline of 3700m VS
NSW (36 degrees S) has a tree line at 1850m
size
the largest and highest area of mountain lands occur in the himalaya-tibet region (reaching 8848m in altitude and covering an area of 600 000km2) the alpine zone extends from 3200m - 4200m
continuity
the largest contiguous area of alpine extends along the Andes (7200km long) from Peru (treeline = 4300m) to Chile (treeline = 1600m)
term = islands in the sky which makes them vulnerable
significant areas of alpine to namedrop
Europe: The Alps, Pyrenees Asia: Caucasus, Urals Highlands of New Guinea Southern Alps of NZ East Africa Highlands
spatial patterns and dimensions of Australia
size: sub alpine and alpine areas occupy 11 200km2 of Aus. True alpine areas occupy only 250km2 (0.003% of Aus)
latitude/altitude: Australian alps 36 degrees S, 1850m
spatial patterns and dimensions of Kosciusko National Park
Location: southern end of Great Dividing range in the Aus Alps, 350km SW of Sydney.
Latitude: 35-37S, 145-149E
Size: covers 100km2 (40% of Aus alpine ecosystem)
Continuity: it is the largest continuous zone of alpine vegetation in Australia
Has Australia’s highest mountain, Mt Kosciusko (2228m tall)
Atmosphere
- temperature decreases by 6.5C per km increase in altitude
- alpine area has a continuous snow cover for >4 months of the year (June - September)
- 10 frost free days per year on Mt K
- the treeline has risen 40m
Hydrosphere
- orographic rainfall: produced when moist air is lifted as it moves over a mountain range –> resulting in a dense and moist Western fall and sparse dry East Planes
- weak glaciation has produced features (Blue Lake) with long periods of erosion leaving exposed granite boulder fields
- peri glacial processes of freezing and thawing results in weathered rock and porous, skeletal soil which can be easily eroded (nutrients loss)
Lithosphere
- soil development is slow
- dominant soil type = alpine humus soils (shallow skeletal soil) which are low in nutrients due to slow rates of decomposition
- nutrients transported out of the soil profile by water (leaching) increasing acidity
- low temperatures, leaching, frosts, strong winds and slow regrowth makes soil vulnerable
- exposed soil open to agents of erosion due to slow plant growth
Process to form plateau
- uplift over 40 years
- glaciation
- plateau is dissected due oto erosion, forming islands in the sky, small, fragmented ecosystems
Wetlands
- bogs and fens allow for slow release of snow melt to streams and rivers during summer
- maintain water during winter with sphagnum moss, storing 20x their weight in water
- permanently wet, providing unique habitats for threatened terrestrial and semi-aquatic species such as the southern corroboree frog
Plant community and adapting
- growing season is too short to sustain trees
- short life cycle of rapid growth
- flowering and seed production (surviving winter as a seed)
Types
Tall alpine herbfield: covers 65% of alpine area. Found on well drained slopes, most resilient
Other species: snow grass, silver snow daisy, mountain celery, billy buttons
Windswept feldmark: grows in the most severe conditions on ridges with little soil
Rock heath: warmth and wind shelter of boulders. WOody shrubs with a slow growth rate.
Bog: sphagnum moss and candle heath
Ecological succession
- 204 species of native flowering plants (21 endemic)
- low energy
- nutrient limitations of soil = slow growth = high vulnerability
- increasing frequency of natural stresses (bushfires)