urce:

| Back |    
  Refer back to this page  
     
  Examiner advice:
~ Students may refer to one climatic type from either a tropical or temperate region. These notes apply to the TROPICAL CONTINENTAL (Savanna) Type Climate of West Africa.
~ Reference should be made to temperature, precipitation, winds and pressure change. It would be pleasing to see some supporting statistics in relation to temperature and precipitation changes, but if not students must use qualified descriptive statements.
 
     
  Christian - the Lion  
 

 

 
  Source: http://www.youtube.com/watch?v=HjWtRYaxmWM  
     
  Savanna - Grassland (Kenya)  
 

 

 
  Source: http://www.youtube.com/watch?v=chCFUw4uZgA  
     
  Lake Chad  
 

 

 
  Source: http://www.youtube.com/watch?v=4Np7u53hdH8  
     
  Examiner's Notes about Tropical continental (Savanna) Climate  
  Savanna Type – 5-20 degrees latitude either side of the Equatorial belt
As insolation is high, high temperatures prevail all the year
– 35 to 25 degrees centigrade
– this climate type is distinguished by a hot wet and a cooler dry season
– humidity highest in the wet season
– evaporation rates remain high during the cooler dry season. Rainfall occurrence is associated with the movement of the ITCZ zone towards the tropic in association with the apparent movement of the overhead sun’s position
– as this occurs low pressure prevails with moist in blowing winds and rising air currents leading to convection rainfall during the hot season
– amounts are most reliable towards the equatorial latitudes averaging 800 mms.
– becoming less reliable towards the hot desert margins averaging 300 to 400 mms. (In some years persistence of high pressure over the outer margins of the Savanna e.g. the Sahel zone prevents the ITCZ and in blowing moist winds from extending into these marginal areas leading to drought conditions. The variation from the normal seasonal weather patterns is partly linked to deviations in the path of Jet Streams in the higher atmosphere. Global warming is a further contributory factor. Refer back to this page
The cooler dry season in the savanna belt occurs as high pressure and dry out blowing winds prevail when the overhead sun and ITCZ move away to extend beyond the Equator towards the other tropics. Refer back to this page
 
     
  Climate graph for Kano, Nigeria  
 

 
     
  Climate in the region around Kano in Nigeria.  
  Mean annual rainfall ranges from over 1,000mm in the extreme south to a little less than 800mm in the extreme north. The rains last for three to five months. Mean temperature ranges from 26*C  to 33*C.

There are four seasons:
~ a dry and cool season,
Kaka, (mid-November to February), marked by cool and dry weather plus occasional dusty haze:
~ the dry and hot season,
Bazara (March to mid-May) when temperatures climb up to 40*C and which is a transition period between the harmattan (dry wind) and the wet season;
~ the wet and warm season,
Damina (mid-May to September), is the proper wet season when the lowest diurnal temperature is recorded;
~ a dry warm season,
Rani (October to mid-November) marked by high humidity and high temperature second to Bazara in hotness.

Can you match this description to the climate graph above?

 
  Source: http://www.onlinenigeria.com/links/kanoadv.asp?blurb=281  
     
  Rainfall variation with RELIEF in NE Nigeria (Komodugu-Yobe Drainage Basin)  
 

The mean annual rainfall ranges from over 1,000 mm in the upstream Basement Complex area to approximately 400 mm in the middle part of the basin and less than 300 mm near Lake Chad. However, climatic variability has resulted in these mean annual rainfall values being unrepresentative for different periods. Hess et al. (1995) calculated an average decline in annual rainfall of 8 mm yr-1 between 1961-90 for the north-eastern arid zone of Nigeria (i.e. the middle and lower part of the basin). Since the mid-1990s the decreasing trend in annual rainfall seems to have been reversed.
Source: http://www.kyb-project.net/_products/200511-pre_water_audit_KYB.pdf

 
   
  The main factor affecting rainfall amount is latitude - the south is wetter and rainfall decreases northwards towards the desert. Seasonal shift of the ITCZ factor.  
     
  Climate Stations in West Africa  
  The hyperlink below lets you visit a site where you can click on different town and see the climate graphs. The problem is that the rainfall scale varies from graph to graph and this makes visual comparison difficult. Look at Makurdi, Jos, Kano, Magaria, Zinder, Agadez and Tamanrasset - a transect roughly from South to North starting in mid-Nigeria. What happens to the amount and seasonality of rainfall and why?  
  Source: http://en.allmetsat.com/climate/niger.php?code=65046  
     
     
  Multiple-Choice Quiz: Savanna Climate  
 

 
     
     
  Video: Nigeria - Tale of two families.  
     
     
  Essays:  
 

JAN 2010 Q.7 Account for the distinctive characteristics of one climatic type chosen from either a tropical or a temperate region. Theme 1.3 [25]

 
   

Click here for larger version

 
  Resource made with http://classtools.net/widgets/turningPage_8/MyzfJ.htm  
Legacy Describe and explain the seasonal variations in your chosen climatic region [20] June 2009  
Specification    
  With reference to your chosen climatic region, explain the formation of low pressure systems and describe their associated weather patterns. [20] January 2009  
     
  Describe and account for the distinctive climatic characteristics of your chosen climatic region. [20] June 2008  
     
  Explain how high and low pressure systems create distinctive weather patterns in your chosen region. [20] January 2008  
     
  Describe and account for the distinctive climatic characterisdtics of your chosen climatic region. [20] June 2007