The Water cycle EQ2 Flashcards
(43 cards)
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)
What is atmospheric circulation?
The global atmospheric circulation model is based on cells. These cells are regions where the air moves from low pressure to high pressure. There are three cells in each hemisphere. On either side of the equator is the Hadley cell, with the Ferrell cell next and then the Polar cell at the top and bottom of the planet.
Australia case study: Drought
From 1997-2009 a drought in Australia took place.
- El Nino events in 2002-2003, 2004-2005, and 2006-2007 led to especially low rainfall in South-East Australia.
- Australia has a naturally low rainfall due to the 30* South high-pressure belt that passes through it.
- Scientists think that climate change may be increasing global temperatures and changing rainfall patterns: temperatures were higher than normal during this period, resulting in more water evaporating than normal; and weather fronts that normally bring rain to South-East Australia to move further South, causing annual rainfall totals to be lower.
- The drought caused vegetation loss and soil erosion which lead to rivers and lakes suffering from outbreaks of toxic algae.
- Farmers’ incomes fell leading to over 100,000 people losing their jobs.
- Livestock died - the number of sheep in Australia fell by around 8 million during 2002-2003.
- Crop yields fell and crops that rely on irrigation were badly affected e.g rice production fell to just 2% of pre-drought totals and lead to increased food prices.
Brazil case study: Drought
In 2014-2015, high-pressure systems diverted moist air further North, causing heavy rains in Bolivia and Paraguay but dry air over Brazil.
- Water rationing for 4 million people.
- Brazil relies heavily on HEP for its power, so the drought caused power cuts.
- Increased groundwater abstraction.
- A vast number of illegal wells.
- In fact, 70% of wells are illegal. Illegal wells are shallower and polluted.
- The Arabica Coffee bean crop was reduced, which drove global coffee prices up 50%.
- By 2015, main reservoirs had reached 5% of their capacity.
The Aral Sea case study: Human causes of drought
The Aral Sea has progressively shrunk due to evaporation and lack of recharge by rivers. Before the Aral Sea received 2060km^3 of fresh water per year from rivers and by the early 1980s, it received none. By 2007, the Aral Sea shrunk by 10% of its original size and increased from about 1% dissolved salt to about 10% of dissolved salt.
- This has caused a variety of respiratory illnesses including tuberculosis as well as dust storms.
The Sahel case study: Drought risk from human activity
Since the 1970s, the Sahel has experienced drought conditions on a regular basis. This is down to physical and human factors:
- Overgrazing and deforestation on marginal land can lead to desertification. With less vegetation there is less transpiration and evaporation from the soil, causing less rainfall.
- Changes in surrounding ocean temperature – the temperatures of the south Atlantic and Indian Oceans increased, with a smaller temperature gap between land and ocean, and monsoon rains were reduced.
- Some scientists believe climate change has reduced rainfall or made it less predictable.
- With less food being grown and an increase in demand, food prices increase.
- Increased soil erosion makes the land less fertile, creating a long-term issue for the farming community.
- Encouraging farmers to grow drought-resistant crops.
Improving knowledge and understanding of droughts across the region by launching the Africa Climate Exchange - Seasonal rivers and water holes dry up, so organisms which live in them or rely on them for water may die.
- Vegetation dies causing animals depending on it for food or shelter to perish or migrate.
What are the human causes of drought?
Overgrazing: With less vegetation there is less transpiration and evaporation from the soil, causing less rainfall.
Deforestation: With less vegetation, changes in soil conditions through compaction and reduced soil moisture and soil retention.
Climate change: Warmer temperatures enhance evaporation, which reduces surface water and dries out soils and vegetation. This makes periods with low precipitation drier than they would be in cooler conditions. Climate change is also altering the timing of water availability.
What is surface water flooding?
Flooding occurs when intense rainfall has insufficient time to infiltrate the soil, so flows overland.