Lecture 5: Drought Flashcards

1
Q

What is drought?

A

A drought occurs when there is not enough rainfall to support human or agricultural needs

There are various causes, both human and natural and they interact

It is a weather-related hazard that can develop slowly

Drought is difficult to prevent & can cause crop failure, famine, death, fires & land degradation

Preparedness can help us to cope with the consequences

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2
Q

Meteorological Drought

A

reduced rainfall compared to the norm for the same place and time of year (e.g. rainfall in Spain in 1990s).

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3
Q

Hydrological Drought

A

the effect of low rainfall on water levels in rivers, reservoirs, lakes and aquifers.
Hydrological droughts usually appear some time after meteorological droughts (e.g. reservoir levels in Spain).

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4
Q

Agricultural Drought

A

when there is not enough water available for a particular crop to grow at a particular time. This drought doesn’t depend only in the amount of rainfall, but also on the correct use of that water(e.g. crop growth in Spain).

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5
Q

Socio-economic Drought

A

Socio-economic drought occurs when the demand for an economic good exceeds supply as a result of a weather-related shortfall in water supply.

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6
Q

Causes of drought- natural/physical

A

Changes in circulation patterns brought about by normal seasonality, inter-annual or decadal variability, or changes to sunspots, sea surface temperatures, periodic events e.g. ENSO lead to:
Less rain: dominance of high pressure systems (no convection) or wind carrying dry continental air masses (reduced moisture in atmos) brings less rain for a period
More heat= more evaporation

Significant change in land surface (e.g. land cover) lead to changes in albedo, ET and cloud generation

Climate change: A long-term change in climate brings less rain and/or higher temperatures either seasonally or annually

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7
Q

Causes of drought- human causes

A

Over-population: many people living in an area and using more water than can be provided reliably

Over-cultivation: more agriculture than can be sustained during the dry years

Over-extraction: use of stores at a faster rate than they can be replenished e.g. for irrigation

Inefficient use – pollution or wastage of water

Degradation of soil and landscape leading to reduced capacity of soil/ecosystems to provide water to agriculture or urban populations

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8
Q

circulation- drought 1988

A

In 1988, a strong high-pressure system stalled over the central United States. Winds circled the high pressure ridge, pushing air south over the Midwest. This pattern essentially cut off moist air that would otherwise have flowed north from the Gulf of Mexico.

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9
Q

circulation- floods 1993

A

In 1993, pulses of moist air moved into the Midwest throughout the summer. Air moved around a high-pressure system in the Southeastern United States (where drought dominated), drawing moisture from the Gulf into the Midwest. The moist air brought flood-inducing rain.

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10
Q

Albedo

A

Land cover-> climate feedbacks
Land surface affects albedo and thus net radiation at the surface
Land surface affects partitioning between latent and sensible heat
⇓Veg = ⇑Albedo = ⇓LE and ⇑H = ⇓clouds = ⇓rainfall = ⇓Veg

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11
Q

Consequences of drought

A

Ecological/environmental – impacts on terrestrial and aquatic habitats

Agricultural –crop declines, failures

Water supply e.g. reduced water storage for dry season (lake Mead SW USA)

Humanitarian e.g loss of livelihood, migration, malnutrition

Off-site and further impacts (e.g. dust, fire, navigation)

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12
Q

Dust

A

Aviation
Infrastructure and transport
Respiratory health
Manufacturing

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13
Q

Ethiopia drought 2006

A

Sahel region, drought conditions since 1985

(Drought of 1984-1985 = 1 million deaths)

Causes = natural climatic causes (low precipitation), human causes (desertification, overpopulation, over-cultivation)

GDP per capita $110, life expectancy 43yrs
2006 event = affected 2.7million people

UNICEF donated $50million to water aid projects

Consequences = famine, chronic poverty, migration, disease, 46% of cattle died, debt

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14
Q

Australia drought, 2006

A

Extremely low rainfall season (lowest rain since 1900) across southern Australia

River Murray dried up in places (Murray-Darling Austalia’s most impt. Agric. Area, with vast irrigation)

Triggered by ‘El Nino’ weather event – which caused excessively low rainfall

Human causes = poor use of water resources

Consequences: 6 million sheep died in 2 years, temporary migrations, improvements to water resource use
Floods in 2010-2011

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