Short And Long Term Influences On Hydrological System Flashcards

1
Q

Name four types of drought

A

Meteorological drought
Agriculture drought
Hydrological drought
Socio-economic drought

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2
Q

Define meteorological drought

A

Occurs when long term precipitation trend is below the long term average. This type of drought is region specific to its atmospheric conditions

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3
Q

Define agricultural drought

A

When there is insufficient soil moisture to meet the demands of crops at a particular time. Can be caused by water shortage, evapotranspiration, reduced groundwater supply. Usually occurs after a meteorological drought.

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4
Q

Define hydrological drought

A

When there are deficiencies in sub/surface water supplies (rivers, groundwater) to meet the needs of vegetation. Originates because a lack of precip

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5
Q

Define socio-economic drought

A

When water demand for social purposes exceeds water availability. Result from lack of precip or exploitation of water supplies

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6
Q

Define ITCZ

A

Intertropical convergence zone

A belt of low atmospheric pressure around the equator.
Here air rises due to intense heating from sun causing high evaporation (ocean). Causing alternating wet season

Example: Africa Sahel lower humidity=less evap. High pressure blocks ITCZ (wet season) could cause a drought

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7
Q

Define mid latitude blocking cyclones

A

Occurs in mid latitudes
Anticyclone forms (area of high pressure) where air descends to ground causing the increase in pressure.
Anticyclones brings stable conditions able to block low pressure systems from the west up to two weeks. Multiple blocking anticyclones can cause drought

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8
Q

Define El-niño southern oscillation ENSO cycles

A

Naturally occurring phenomenon that involves movement of a mass of warm water in Pacific. Because the changes in surface trade winds, atmospheric circulation and ocean currents.

Causing cooler ocean to replace warmer ocean= less evap and precip leading to drought

Naturally occurs every seven years

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9
Q

Name the three physical causes of drought

A

Intertropical convergence zone
Mid latitude blocking anticyclones
El Niño southern oscillation cycles

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10
Q

Examples of human activities that increase drought risk

A

Over abstraction of groundwater- causes water deficit
Building reservoirs/water transfer- alters natural course/hydrological cycle (China, 600 rovers dried up)
Deforestation- reduced vegetation cover reducing evapotranspiration levels
Overgrazing- removal of vegetation changes soil conditions reducing infiltration increasing runoff and decreasing soil moisture content

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11
Q

Case study: Sahel region

A

Vast arid region across 11 African countries. Regular droughts

Most severe drought 2011-12 causes:

Air pollution generated by EU/USA cashed atmospheric cooling changing global heat and circulation. So tropical rains didn’t arrive=drought

Higher sea surface temperatures caused by global warming. Rain bearing winds fail when sea temperatures are warmer over Sahel

El Niño event could increase water stress in western sahel

Sahel has one of highest poverty rates and lowest development levels. High pop growth from 2.5-4%

Over cultivated land causes desertification increasing vulnerability to drought

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12
Q

Case study: Millennium Drought

A

Southern Eastern Australia 1997-2009 (longest drought)
Annual rainfall 97-09 12.4% below 20th century mean
El nino events in 2002-03 and 2006/07 partly responsible. Estimated for 80% of rainfall decline in Australia.

Ridge of high pressure also blocked depression reducing rainfall

Global warming intensifies sea surface temperature

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13
Q

Impact of drought on a wetland ecosystem

A

Wetland- area of land saturated with water permanently/seasonally (Everglades)

Supply of water reduced, flooded areas shrink/dry up causing progressive loss of habitat

Soil moisture reduces, extended period leads to soil erosion (loss of nutrients)

Aquatic species decline

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14
Q

Meteorological causes of flooding

A

Flash flooding due to thunderstorms/tropical storms. 2013 Island of Sardinia flash floods killed 18 people $1.14 billion damage

Mid-latitude depressions causes flooding in UK, each depression brings rain. Multiple depression cause flooding, as grounds already saturated

Monsoons (seasonal change in direction of prevailing winds) India Sri Lanka warm climate with torrential rain because of the ITZ moving north. Myanmar caused 103 deaths and affected 1mill+

Snow melt from mountain areas. Red River North Dakota USA

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14
Q

Impact of drought on forest ecosystems

A

Forests are valuable due to their ecological function/services/regulation of hydrological cycle

Species become less resilient to droughts and take years to recover

foliage loss/increase number of pests (hot conditions= pine bark bettle attacks USA) causing major ecosystem changes

Forest important for carbon sequestration, average 0.73 tonnes of carbon per hectare per year

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14
Q

Human causes of flooding

A

Deforestation- reduced interception/evapotrans causing greater runoffs/flashy hydrographs

Intensive crop growing-soil is exposed more susceptible to erosion (wind/water) increasing sediment load in rivers

Urbanisation- increase of impermeable surfaces and draining system decreasing lag time

Floodplain drainage- floodplain used for agriculture/urban meaning natural drainage is at a lower capacity

Flood management/hard engineering- designed to reduce frequency of flooding it can cause worse impacts downstream in unprotected areas (Carlisle)

14
Q

Potential impacts for UK of climate change in 2050

A

Short droughts more frequent
Sea level rise between 0.4-1m by 2100
Decrease in recharge of groundwater supplies
Cold water species decrease
More intensive downpours

14
Q

Case study: Storm Desmond

A

2015
more than a month’s rainfall in one day, most rivers exceeded highest ever recorded levels
341.1mm of rain in 24 hours
Caused by low pressure system, already saturated ground and steep landscape

5,200 homes affected 40 schools closures

15
Q
A