Drylands Flashcards
What is aridity?
- The main characteristic of deserts and drylands
- Means lack of available water
Are drylands always hot?
- No
- Winters are cold – winter snowfall can be an important precipitation source
- Clear cloudless skies cause high diumal range - range between temp
What is the moisture balance like in drylands?
- Net negative moisture balance
- Evapotranspiration > precipitation
- P/PET ratio is below 0.5
- This ratio is a measurement of potential stress from lack of water
What are hyper arid areas?
- True deserts
- P/PET less than 0.05
- Central Sahara, Arabian
- Periods more than 12 months with no rainfall
What are arid areas?
- P/PET between 0.05 and 0.2
- Central Australia and fringes of Sahara
What are semi arid areas?
- P/PET between 0.2 and 0.5
- Western interior of North America
What are dry-subhumid areas?
- P/PET between 0.5 and 0.65
- Added to classification by UNEP because subject to drought
- Southern Russia, Canadian Prairies
Outline precipitation variation in drylands
- All dry lands subject to large year to year precipitation variations
- High inter-annual rainfall variation is common
- All regions are drought susceptible
What are the 4 main locations of dry lands
1) Sub tropical regions - stable depending air with high pressure belts
2) Interior continental regions - far from oceans
3) Lee of mountain zones - rain shadow effects
4) Certain western effect of land masses - cold ocean currents suppress sea-surface evaporation
What factors control drylands rock weathering?
- Bare rock surfaces = exposure
- High diurnal temp ranges – thermal weathering
- Excess of evapotranspiration – salt weathering
- Different salts have different susceptibilities
What weathering landforms are formed in drylands?
- Honeycomb weathering features
- Cracked ephemeral drylands lakes - playas
Why can water be effective in drylands?
- Rainfall events are frequently intensive
- Short bursts of rainfall transport high yields of sediment
- Little vegetation cover causes high run off
- However, infiltration capacities can be high in sandy sediments
What is channel flow like in drylands?
- Usually in short duration and irregular
- Localised nature of drylands rainfall events
- Localised high infiltration in unsaturated conditions
What are the flow features of a channel in drylands?
- Irregular and unpredictable
- High event to event variability
- High water losses through evaporation and stream bed
- Peaked hydrograph
- High velocity
What are the geomorphic and ecological implications of the flow features in drylands?
- Wide channels, short distance changes in channel
- Systems can change rapidly
- High sediment loads