5.4 Deficits within the hydrological cycle result from physical processes but can have significant impacts Flashcards
Meteorological drought -
Shortfalls in precipitation as a result of short - term variability or longer term trends, increasing the duration of dry periods.
The precipitation deficiency is usually combined with high temperatures, winds and strong sun.
Agricultural drought -
Some farming practices such as over grazing can onset the causes of agricultural drought leading to a lack of soil moisture and soil water availability. Effects of plant growth and biomass.
Hydrological drought -
Associated with reduced stream flow and groundwater because of reduced rates of precipitation and high rates of evaporation. Can result in decreased water supplies for urban areas as there is reduced access for storage of lakes which lead to marked salinisation and poorer water quality.
Affects of hydrological drought in Northen-East Brazil -
Rural areas. Where there are no rivers and they depend on seasonal rainfall for reservoirs and ponds leaves many rural dwellers with little access to water leading to the decrease of water quality and resulting in ill health and water insecurity.
Famine drought -
All these 3 types of drought cause famine drought, leads to widespread failure of agricultural systems, food shortages with economic and environmental impacts. Malnutrition effects.
ENSO cycle affects on the demanding population -
As populations grow and become wealthier their demand for water also increases, while this occurs there can be natural variability in a climate which can cause a temporary decline in supply with no replenished stores this can be brought about by an ENSO cycles.
What does ENSO stand for?
El Niño - southern Oscilation
ENSO 1. Changes of water
Conditions of an El Niño event when cooler water for example along the coast of Peru is replaced by warmer water, at the same time the warmer of Australia and Indonesia further west is replaced by cooler water.
How often for El Niño events?
Occur every 3-7 and last for about 18 months
El Nino 2. The effects of changing water -
This can trigger very dry conditions throughout the world, usually in the second year especially in South East Asia, in India El Nino always leads to a relatively weak monsoon rain.
El Nino Events 1-3 -
- Trade winds die in the Western Pacific
- May even be a reverse of direction of flow
- The piled up water in the west moves back east, leading to a 30cm rise in Peru
El Nino Events 4-6
- The region of rising air moves east with the associated convectional uplift.
- Therefore the eastern Pacific ocean becomes 6-8 degrees warmer, breaks the food chain.
- Conditions are calmer across the whole Pacific
La Nina Events 1-4 -
- Extremely strong trade winds
- The trade winds push warm water westwards
- Low pressure develops with strong convectional uplift as the warm water heats the atmosphere, leads to heavy rainfall in south east Asia
- Results in strong high pressure and extreme drought and can be a problem in the already semi- arid environments in Chile and Peru
Human Influences on drought - Sahel region
Human factors do not necessarily cause drought but act like positive feedback loop making it worse, for example the drought impacts were increased by socio-economic impacts due to worsening degradation of deforestation and overgrazing. Also rural populations have increased for example the population had double every 20-30 years. So population had outstripped food production in those years and agriculture was mainly rainfed making the drought worse for agricultural benefits. This doesn’t help in certain seasons due to 85% of their annual rainfall coming in the summer months.
Desertification -
Land degradation in semi-arid dry areas resulting from various factors including human activities.