The Biome Of One Tropical Region Flashcards
What is the tropical biome that we have studied
Tropical savanna grasslands
What are Savannas and give some facts
- areas of tropical grasslands that can occur with or without trees and shrubs
- cover 1/4 of the worlds land surface
- found between rainforests and desserts
- depend on an inter-relationship between plants, animals and the physical environment
- these areas are under increasing pressure from human activity
Features of a savanna grassland
- associated with continental interiors and develop where temperatures are high
- precipitation is low
- seasonal drought is common
Location of savanna grasslands
- occur in a broad band 5-15* north and south of the equator
- found between tropical rainforests and hot desserts
- occupy 65% of Africa’s land area
- other locations include Australia, South America and India
Climate of a savanna grassland
- lies close enough to the equator to experience high temperatures throughout the year
- climate varies across the Savanna
- towards the rainforest belt there is more rainforest to support tree growth
- towards the dessert belt only grasses occur
What is the mean temperature in a savanna grassland
- about 20* throughout the year
- highest reaching 36*
- 11-13 hours of daylight
What is the rainfall like in a savanna grassland
- total rainfall can range between 600mm-2000mm
How long is their prolonged drought and what does it do
- Lasting at least 5 months
- increases potential for seasonal outbreaks of fire
- creates a cycle of water surplus/deficiency
- linked to annual wet/dry seasons
- drier cooler season has high temperatures and evapotranspiration
Formation of the ITCZ rainfall belt
- inter- tropical convergence zone
- forms as a result of intense solar heating
- warm air can hold more water vapour than cool
- when air on the surface is heated it can hold large quantities of water vapour that has been evaporated from the surface
- as air rises and cools it’s less able to hold water vapour
- some of that water vapour condenses to form water droplets
- if the air continues to rise condensation continues to add to the size of the water droplets
- thick clouds form leading to rain
- called convection rainfall
ITCZ continued
- the heating is so intense and the convection currents are so strong
- dominate the climate of the whole tropical region
- air rises and cools and brings rain
- cooler air flows pole wards away from the equator
- at 30* from the equator the cooled air starts to sink back to the surface
- as the air sinks it warms again due to compression
- be chase the air has lost its moisture the warming process is more rapid than the cooling
- areas of hot , high-pressure air formed at about 30* north and south of the equator
Movement of ITCZ
- sun appears overhead at the equator on the 21st of March and September
- during summer in the northern hemisphere the sun appears to migrate north of the equator
- northern winter appears to migrate south
- overhead sun migrates and so does the ITCZ
Example of movement of ITCZ
- Kano
- ## one season a year when the sun is overhead and the ITCZ dominates the area and brings intense rainfall
What is the soil moisture budget
- the combined pattern of rainfall and temperature
What happens during the wet season in the soil moisture budget
- may to September
- usually an excess of rainfall
- over evaporation
- plenty of water available for plant growth
What happens during the dry season in the soil moisture budget
- excess of evaporation from over precipitation
- so little water percolates down through the soil
- some is drawn back to the surface where it then evaporates so little percolates
- evaporation combined with water being used by plants, steadily reduces the soils store of moisture until it is dry
- from this point on there is no moisture so plants stop growing and enter a dormant period
The situation in East Africa
- West Africa has two areas of tropical grassland
- one north and south of the equator
- the grassland spreads right across the equator and there is no area of rainforest
Savanna grassland soils
- closely linked with climate and tend to reflect the local seasonal rainfall pattern
- soils in the savanna are commonly leached
- similar to soils of the rainforest but are not as intensely weathered
What happens to the soils during the wet season
- excess of precipitation
- over potential evapotranspiration
- this results in leaching of soluble materials and small particles will be taken down through the soil
- these soils are deposited deep within the soil
What happens to the soil during the dry season
- evapotranspiration is less than precipitation
- silica and iron compounds are carried up through the soil and precipitated close to the surface
What is another word for horizon in soils
Layer