The Water cycle EQ2 Flashcards
What is the UN definition of a drought?
An extended period - a season, a year or several years of deficient rainfall relative to the statistical multiyear average for a season.
What are the types of droughts?
- Meteorological
- Agricultural
- Hydrological
- Socio- economic
What is a meteorological drought?
Meteorological drought is defined usually on the basis of the degree of dryness (in comparison to some “normal” or average amount) and the duration of the dry period. Definitions of meteorological drought must be considered as region specific since the atmospheric conditions that result in deficiencies of precipitation are highly variable from region to region.
What is an agricultural drought?
Agricultural Drought refers to the impacts on agriculture by factors such as rainfall deficits, soil water deficits, reduced ground water, or reservoir levels needed for irrigation.
What is a hydrological drought?
Hydrological drought is associated with the effects of periods of precipitation (including snowfall) shortfalls on surface or subsurface water supply (i.e., streamflow, reservoir and lake levels, groundwater). The frequency and severity of hydrological drought is often defined on a watershed or river basin scale. Although all droughts originate with a deficiency of precipitation, hydrologists are more concerned with how this deficiency plays out through the hydrologic system. Hydrological droughts are usually out of phase with or lag the occurrence of meteorological and agricultural droughts.
What is a famine drought?
A humanitarian crisis in which the widespread failure of agricultural systems leads to food shortages and famines
Food deficit:
- loss of natural vegetation
- increased risk of wild fires
- wind blown soil erosion
- desertification
What is positive feedback?
cyclical sequence of events that amplifies an impact.
What is negative feedback?
cyclical sequence of events that dampens down or neutralises an impact.
What are the major features of meteorological drought?
What are the major features of hydrological drought?
What are the major features of agricultural drought?
What are the major features of famine drought?
Deficit: Rainfall - Low precipitation, high temperatures, strong winds
Deficit: Streamflow - Low soil moisture, little percolation and groundwater recharge.
Deficit: Soil moisture - Plant water stress reduced biomass.
Deficit: Food - loss of natural vegetation, and desertification.
List the droughts in order of severity.
- Meteorological
- Hydrological
- Agricultural
- Famine
What are El Nino southern oscillation cycles (ENSO)?
What are teleconnections?
- The trade wind pattern is disrupted - it may slacken or even reverse and this has a knock-on effect on the ocean currents
- The air circulation loop reversed
When this happens, cool water normally found along the coast of Peru is replaced by warmer water. At the same time, the area of warmer water further west, near Australia and Indonesia, is replaced by cooler water.
El Niño events usually occur every 3-7 years, and usually last for 18 months. El Niño events seem to trigger very dry conditions throughout the world, usually in the second year. For example, the monsoon rains in India and South East Asia often fail.
The way that changes in sea temperatures in the Eastern Pacific is linked to changes in precipitation and climate generally across the rest of the globe.
What is La nina?
La Niña events may sometimes, but not always, follow an El Niño event. They involve the build-up of cooler-than-usual subsurface water in the tropical part of the Pacific. This situation can lead to severe drought conditions, particularly on the western coast of South America.
- Very strong air circulation and very warm water moving east-west.
What are the physical causes of drought?
- ENSO
- El Nina
- Blocking anti-cyclones
- Failure of seasonal rainfalls
Causes of droughts - failure of seasonal rainfall
Some areas get low pressure for half the year and high pressure for the other half e.g rain, then dry.
But sometimes the switch between the two doesn’t happen so they wait for low pressure (rain) but it doesn’t come.
Causes of droughts - mid-latitude blocking anticyclones
- Low latitudes get monsoons but mid-latitude get blocking anticyclones (high-pressure weather systems).
- Normally mid-latitudes get alternating low pressure (depressions) and high pressure (anticyclones) over days:
- Sometimes an anticyclone gets stuck over a mid-latitude stopping low pressure (rain) from entering. If this happens over a long time it causes a drought.
- Droughts in the UK develop over a year when blocking anticyclones are more common than usual. Dry winters mean a lack of groundwater recharge so the following summer has more of an impact.
What is the ITCZ?
A low-pressure belt of rising air along the equator fed by the convergence of Northeast and Southeast trade winds.
What are the stages of ITCZ?
- Intense solar radiation at the Equator warms the air which rises, cools and condenses to form clouds and rain.
- Air moves away from the Equator it cools and sinks in a belt of high pressure and hot dry conditions.
- Air returns to ground levels and moves back towards the equator forming trade winds.
- Trade winds meet at ITCZ where warm air rises, cools and condenses and creates convection rainfall
Position of ITCZ changes with seasons (north in June-August & South in Dec-Feb – this creates alternating wet and dry seasons in the tropics)