Short-Long term variations hydrological cycle. Flashcards
Define Drought.
Extended period (Season, year, several years) of deficient relative to the statistical multi year average for a region.
What four catagories cause droughts?
Socio-economic drought, Hydrological drought, Agriculture drought, meteorological drought.
Define Socio-economic drought.
And what causes it?
Occurs when water demand is higher than water avaliability. Can be caused by lack of precipitation or by human overuse of water sources.
Define Hydrological drought.
And what causes it?
This happens when when the amount of surface area and subsurface water (rivers, groundwater ect.)is deficient. Caused by lack of precipitation.
When do Hydrological droughts usually occur?
After meteorological and agricultural droughts.
Define Agricultural drought.
And what causes it.
When there is not enough soil moisture to allow enough crops to grow. It is caused by precipitation shortages, changes in rates of evapotranspiration and reduced groundwater levels.
Define Meteorological drought.
And what effects it.
When long-term precipitation is lower than normal. It changes for different regions as it is affected by the atmospheric conditions.
Describe a normal Non-El Niño year.
- Trade winds blow equator-wise and westwards across tropical pacific.
- Winds blow towards warm water of western Pacific.
- As water heats the atmosphere, convectional uplift occurs.
- Trade wind pushes warm air westwards. Along the East coast of Peru, shallow position of thermoline allows winds to pull up water from below.
- Cause upwelling of nutrient-rich cold water creating optimum fishing conditions.
- The pressure of the trade winds results in sea levels in Australasiabeing 50cm higher than Peru, sea temperature being 8°C higher.
- The Walker loop returns air.
Describe an El-Niño year.
- Trade winds in Western Pacific weaken and die.
- May be a reverse direction of flow.
- Piled-up water in West moves back east leading to Peru sea levels 30cm rise.
- Region of rising air moves East with associated convectional uplift. Upper air disturbances distort the path of jet streams which can lead to teleconnections all around the world.
- Eastern Pacific Ocean becomes 6-8°C warmer. The El Niño effect overiddes cold northbound Humboldt current, thus breaking the food chain. Lack of phtoplankton results in reduction in fish numbers, which in turn affects fish eating birds on the Galapagos Islands.
- Conditions are calmer across the whole Pacific.
Describe a La Niña year.
- Extremerly strong trade winds.
- Trade winds push warm water westwards giving a sea level up to 1m higher in Indonesia and the Philippines.
- Low pressure develops with very strong convectional cuplft as very warm water heats the atmosphere. Leads to heavy rain in southeast Asia.
- Increase in the equatorial undercurrent and very strong upwelling of cold water off Peru results in strong high pressure and extreme drought. This can be a major problem in the already semi-arid areas of Northern Chile and Peru.
What were the 2014-16 El Niño’s impacts on Australia?
- Drying influence of event was contradicted by warm temperatures in Indian Ocean leading to above average rainfall in Western Australia, New South Wales and eastern Victoria.
- Spring 2015 it reversed and Indian Ocean started to help El Nino, meant limited crop growth, third driest spring ever.
- Lack of heavy rains in North and West meant reduced downtime for mining.
- Fewer clouds and less tropical rain contributed to most severe coral bleaching event for the Great Barrier Reef ever recorded.
- Heat and low rainfall brought Australian bushfire season in 2015-16, 125 fires recorded in Victoria and Tasmania during October.
- Dry conditions also started fires from dry lightning in January 2016, damaged Tasmanian world heritage area.
What were the 2014-16 El Niño’s impacts on Africa?
- El Nino 2014-16 boosted 2015 short rains season from October-december. Increasign rainfall in east Africa.
- Multiple countries including, Lesotho, Swaziland and Zimbabwe declared national states of emergency.
- March 2016 Southern African Community declares a regional drought disaster.
Tell the card about the Case study for Human influences on drought in the Sahel region of Africa. In regards to Sahel’s features that make in vulnerable to drought.
The Sahal region is a vast semi-arid region of the Southern edge if the Sahara. It goes from Mauritania to Eritrea and houses some of the poorest developing countries in the world.
- Sahel = drought sensitive as it occupies a transitional climate zone. In normal conditions mean annual rainfall is all concentrated in the Summer. Varies from 100mm on edge of Sahara to 800mm on Southern Margins.
- Annually, there is huge variability on the Saharan fringe. On tropical seas warm sea surface temperatures create strong convectional uplift. This weakens West African monsoons and contributes to the Sahel drought.
Case study. What human influences increase drought in the Sahel region of Africa?
1999-2000 there was an Ethiopian > Enitrean drought and 10 million people needed famine assistance.
Drought’s impact was increased by socio-economic conditions like environmental degradation by overgrazing by Nomadic tribes. Also deforestation for feul wood and rural poverty.
Rural population density increased so population growth outstripped food production.
Etheopia and Enitrea were at war which blocked people’s access to food.
Case Study. Drought in Australia. What are the two main types of drought in Australia?
- Serious deficiency - Rainfall totals within 10% of value’s record for at least 3 months.
- Severe deficiency - Rainfall totals within the lowest 5% of values on record for at least 3 months.
Case study. Drought in Australia. How much of Australia is usually affected per year?
30% is usuallly affected per year.