Tropical Climates Flashcards

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1
Q

Describe the Walker Circulation

A

Point to have:

  • Easterly trade winds moving warm water from the Eastern to Western Pacific
  • Pooling of warm water at the Western coast drives the thermocline downwards
  • Low pressure conditions created, as warm air above the water rises
  • In the east, cold water wells up after warm water migrates to the west
  • Easterly trade winds form the north-flowing Peruvian current
  • Rising air over the Western Pacific feeds return airflow, closing and strengthening the circulation
  • Subsidence resulted in the East
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2
Q

Describe El Nino

A
  • Walker circulation has broken down
  • Easterly trade winds weaken or reverses such that wind flows from the West to the East
  • Warm water pools at the Eastern coast, causing low pressure conditions and a wet season
  • Cold water in the Western Pacific reduces evaporation, encouraging drier conditions
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3
Q

El Nino statistics

A
  • Peru saw 2500mm of rain in a 6-month period, 300 times the average
  • Eastern Australia endured the worst drought in 1982, losing $2000million in agriculture
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4
Q

Statistics for the Af climate type

A

Singapore - Annual Temperature Range: 25-32 degrees Diurnal Temperature Range: 25-33 degrees
Rainfall: 2340mm a year
Kisangani, Congo - Average rainfall: 1804mm
Average Temperature: 25.4 degrees

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5
Q

Statistics for the Am climate type:

A
Cochin, India: Annual temperature range of 3.3 degrees, total of almost 3000mm of rainfall in a year
Western Ghats (Gujarat) - less than 400mm a year
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6
Q

Statistics for the Aw climate type:

A

Lagos, Nigeria: Average rainfall of 1780mm, average temperature 26.7 degrees

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7
Q

Statistics for the BSh climate type:

A

Kayes, Mali - Annual temperature of 74 cm, 10.7 degree range annually

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8
Q

Statistics for the BWh climate type:

A

Atacama desert, Chile - Annual rainfall of 15mm, diurnal temperature range of up to 35 degrees

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9
Q

Describe the African monsoon (January)

A
  • ITCZ migrates southwards (Capricorn)
  • African continent loses heat faster than the surrounding Atlantic Ocean
  • Winds blow out of Africa into the Gulf of Guinea and Atlantic Ocean
  • Majority of landmass experiences dry spell because north east trade winds (harmattan) dominate most of West Africa, and they are dry and dusty
  • Outliers include coastal zones as the southwest monsoon brings rain when it travels onshore to converge at the ITCZ
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10
Q

Describe the African monsoon (July)

A
  • ITCZ migrates northwards (Cancer)
  • Landmass gains heat faster than the Atlantic Ocean, creating a low pressure area over Western Africa
  • Thermal capacity of water is higher, air over it is colder, denser and sets up high pressure area
  • South east trade winds cross the equator and are deflected to become South West monsoon winds
  • Blows over the hot landmass and facilitates convective uplift
  • Convergence uplift takes place at the ITCZ when northeast trade winds and southwest monsoon winds converge
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