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
What are the layers in savanna grassland when it comes to soil
- thin dark humus layer
- hard cemented layer
- layers then merge
- re-deposited silica
- rapid chemical weathering
- bedrock
What is geomorphology and how does it play an important role in affecting soil type
- the way that the land looks
- landforms and the process that form them
- important role- areas have different conditions so it can affect the way that the land looks
What soil type is at the base of slopes and river valleys
- enriched by clay, minerals
- woods are likely to be found
What soil type is found on the top of slopes
- fewer nutrients due to erosion
- grasslands are likely to be found