Geography: Water cycle, water insecurity Flashcards
Name an input of the hydrological cycle
land precipitation
name some stores in the hydrological cycle (3)
rivers/lakes
ocean
atmosphere
name 3 flows in the hydrological cycle
ocean to land water vapour transport
surface flow
groundwater flow
name 3 outputs of the hydrological cycle
ocean evaporation
ocean precipitation
evaporation/transporation
what is a drainage basin?
an area of land drained by a river and its tributaries, seprated from other drainage basins by a ridge of land called a watershed.
which physical factors affect drainage basin flows? explain each
- interception: leaves and vegetation intercept rainfall. this can result in more evaporation, dry leaves and shoots can also absorb and store precipitation.
- direct runoff (overland flow): the ground becomes saturated, forcing rainwater to run off the surface. this quickly delivers water to river channels.
- infiltration and throughflow: infiltration is the movement of water downwards through the soil. the rate of infiltration depends on the amount of water already in the soil. it can then flow downwards towards a river through the soil.
- percolation and groundwater flow: percolation is the movement of water through permeable rocks. groundwater flow happens as water travels through rocks in the ground.
which human factors affect the drainage basin? explain each
- deforestation: less roots in the soil makes it less permeable, less water can be stored there as a result.
- Urbanisation: more man-made materials such as concrete are impermeable. this increases surface runoff.
- reservoirs: interrupt the travel of water. delays flows through a drainage basin and adds to the amount of water lost through evaporation.
What is potential evapotranspiration?
the maximum amount of water that can be lost through evapotranspiration in an endless supply of water in surface water stores.
what is economic water insecurity?
when water resources are available but there’s insufficient capital to meet the demand.
what is a storm hydrograph?
shows change in a river’s discharge at a given point on a river over a short period of time.
what are the 4 types of drought?
- meteorological
- agricultural
- hydrological
- socio-economic
why are the sub-tropics more affected by drought than anywhere else?
intense solar radiation at the equator warms the air, causing convection. the subtropical high pressure zone forms when hot air from the equator rises and forms a belt of high pressure. this results in clear skies and dry, hot temperatures.
what does a river regime show?
the annual variation in the discharge of a river
what are the causes of drought in the Sahel?
- deficiency of rain
- the monsoon is patchy and irregular
- monsoon weakened as there’s no temperature difference between the land and sea.
how do humans increase drought risk?
- irrigation
- over abstraction
- deforestation
- climate change
what are the differences between simple and complex river regimes?
SIMPLE REGIMES: river experiences seasonally high discharge, followed by low discharge
COMPLEX REGIMES: larger rivers cross several different relief and climatic zones, and therefore experience the effects of these events.
what is the ITCZ?
a belt of low atmospheric pressure located around the equator.
what is soil moisture recharge?
when water is added to soil following a period of soil moisture defecit.
what are the general processes taking place on the atmospheric circulation model?
- The most intense sunlight hits the equator, causing air to heat up and rise.
- This forms an area of low pressure at the equator.
- Air rises and moves away from the equator, the air then falls and moves back towards the equator, forming trade winds.
- At the equator, air moves in Hadley cells.
- Trade winds meet at the ITCZ to cause alternating wet and dry conditions at the tropics.
- It also means that the equator has dry, arid conditions.
- Warmer air moves towards the polar front, cools and falls at the poles, air then begins to move back towards the equator in the polar cells.
What are the causes of drought in the Sahel?
- deficiency of rain
- monsoon is patchy and irregular.
- change in temp. of surrounding oceans means that the monsoon remains south.
- ENSO can produce a cold atlantic current which reduces evaporation, results in less evaporation.