5.4A Flashcards

1
Q

What are the courses of drought

A

The courses of drought, both meteorological and hydrological:
short-term precipitation deficit, longer term trends, and ENSO
cycles

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2
Q

When does water stress occur

A

When water demand > available amount

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3
Q

What does water stress lead to

A
  • deterioration of fresh water resources
  • in terms of quantity (aquifer over-exploitation, dry rivers, etc.)
  • and quality (eutrophication, organic matter pollution, saline intrusion, etc.).
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4
Q

Define meterological drought

A

shortfall or deficiency of water over an extended period, usually at least a season.
- long term precip is much lower than normal but depends on whether evapotranspiration is high

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5
Q

define hydrological drought

A

0 reduced stream flow, lowered groundwater levels and reduced water stores.
- deficiencies in surafce and subsurface water
- starts with lack of rain but takes a while for that to affect water flow

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6
Q

Normal conditions in pacific basin

A
  • In a non-El niño year, the trade winds blow from east to west along the equator
  • The air pushes the warm water westerwards
  • Thermocline, upwelling,
  • Warm, moist air rises, cools and condenses, forming rain clouds
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7
Q

Conditions in pacific basin during an el nino event

A
  • The trade wind pattern is disrupted - it may slacken or even reverse and this has a knock-on effect on the ocean currents
  • Air circulation loop reversed
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8
Q

What happens as a result of el nino

A
  • cool water normally found along the coast of Peru is replaced by warmer wate
  • area of warmer water further west, near Australia and Indonesia, is replaced by cooler water.
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9
Q

How often does el nino occur and what is its duration

A
  • every 3-7yrs
  • last 18 months
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10
Q

What is el nino

A
  • El Nino is the change in water body patterns within the Southern hemisphere, leading to unusual weather conditions.
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11
Q

What else does El nino trigger

A

ENSO can also trigger extremely dry conditions in areas South & South-East
Asia, Eastern Australia and North-East Brazil.
- In South Asia, ENSO can weaken the annual monsoon.

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12
Q

Describe normal pacific basin conditions

A
  • rising warm moist air gives heavy rainfall in west
  • high altitude air flow west
  • descending waring air gives dry conditions
  • surface flow from trade winds blowing from east to west
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13
Q

Describe el nino process

A
  • high altitude air flow from east to west
  • so rising air in the east gives heavy rainfall on pacific coast from peru to cali
  • descending air warms to give dry conditions in west
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14
Q

simplified types of drought

A
  • Meteorological drought – when the 0 amount of precipitation received in a specific area is less than the average.
  • Hydrological drought – when reduced precipitation impacts on water supply, eg there is decreased streamflow, soil moisture, reservoir and lake levels, and groundwater
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15
Q
A
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