Tropical Climates Flashcards
Describe the Walker Circulation
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
Describe El Nino
- 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
El Nino statistics
- 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
Statistics for the Af climate type
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
Statistics for the Am climate type:
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
Statistics for the Aw climate type:
Lagos, Nigeria: Average rainfall of 1780mm, average temperature 26.7 degrees
Statistics for the BSh climate type:
Kayes, Mali - Annual temperature of 74 cm, 10.7 degree range annually
Statistics for the BWh climate type:
Atacama desert, Chile - Annual rainfall of 15mm, diurnal temperature range of up to 35 degrees
Describe the African monsoon (January)
- 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
Describe the African monsoon (July)
- 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