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Access Geography Unit 3 Lesson 2 Hydrology
Today’s objectives ,[object Object],[object Object],[object Object],[object Object]
Why study physical systems? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Energy from the Sun ,[object Object],[object Object],[object Object],[object Object],[object Object]
The energy balance
The Hydrological System: Water on Earth ,[object Object],[object Object],[object Object],[object Object]
2. The Miracle of Water ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
3. Water Availability & Use ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
4. Distribution: Water Stores
Hydrology ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Before we can understand the Hydrological cycle we need to understand a little about weather
So it is hotter at the equator but why???
Where on earth receives the most year round sunshine to provide good growing conditions? 1) Distance the sun’s rays have to travel through the atmosphere Equator Sun  Rays Longer Distance Shorter Distance
2) The curvature of the earth
3) The sun´s rays have to travel through thicker atmosphere at the poles Thinner atmosphere  Thicker atmosphere
What causes it to rain? 1) The sun heats up the sea.  This causes water to be evaporated (made into a gas called water vapour). 2) The warm air full of water vapour rises high into the sky.  Because it is so warm it is very light, that’s why it rises. 3) The higher up the air gets, the colder it gets as well.  This makes the water vapour condense (turn back to liquid) and form clouds. 4) These clouds eventually drop all of the water in them as rain. This type of rain is called CONVECTIONAL rain
The UK is affected by a number of different air masses.  Air masses are huge blocks of air at different temperatures.  Some of the air masses are  warm  and some of the air masses are  cold .
But air masses at different temperatures DO NOT like one another so they won’t mix together.  Birmingham is affected by cold air coming down from the north and warm air coming up from the south. The junction between these two different air masses is called a  front  so when they cause it to rain it is called  FRONTAL RAIN .
But if they won’t mix, what happens when they meet?
Its fair to assume then, that the final type of rainfall will also follow the same process.  But what is it that is  causing  the air to rise? A FEW CLUES Name:  RELIEF rainfall
Meet Reggie, the RELIEF RAIN raindrop Reggie  is a gas flying in the air  (water vapour)  but when he meets a hill he has to climb over it.  It gets very cold near the top of the hill as he is so high and Reggie changes from a gas to a liquid and settles into some clouds  (condensation).   When lots of Reggie’s friends arrive in the cloud it is too cramped to stay so some of them fall back to earth as relief rainfall  (precipitation).
The Hydrological Cycle
Hydrological Cycle Matching Resurgence Overland Flow (surface runoff Ground water flow Infiltration Surface water storage Percolation Transpiration Isolation Precipitation Atmospheric Store Snowmelt Saturated zone (aquifer) evaporation Soil moisture Ocean store Base flow Atmospheric condensation Water table Volcanic water Ice cap storage Human activities Interception Stream runoff Impervious bedrock Reabsorbed by plants
The Drainage Basin ,[object Object],[object Object],[object Object],[object Object]
Drainage Patterns ,[object Object],[object Object],[object Object],[object Object],[object Object]
Nested Basins ,[object Object],[object Object],[object Object],[object Object]

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Lesson 2 hydrology

  • 1. Access Geography Unit 3 Lesson 2 Hydrology
  • 2.
  • 3.
  • 4.
  • 6.
  • 7.
  • 8.
  • 10.
  • 11. Before we can understand the Hydrological cycle we need to understand a little about weather
  • 12. So it is hotter at the equator but why???
  • 13. Where on earth receives the most year round sunshine to provide good growing conditions? 1) Distance the sun’s rays have to travel through the atmosphere Equator Sun Rays Longer Distance Shorter Distance
  • 14. 2) The curvature of the earth
  • 15. 3) The sun´s rays have to travel through thicker atmosphere at the poles Thinner atmosphere Thicker atmosphere
  • 16. What causes it to rain? 1) The sun heats up the sea. This causes water to be evaporated (made into a gas called water vapour). 2) The warm air full of water vapour rises high into the sky. Because it is so warm it is very light, that’s why it rises. 3) The higher up the air gets, the colder it gets as well. This makes the water vapour condense (turn back to liquid) and form clouds. 4) These clouds eventually drop all of the water in them as rain. This type of rain is called CONVECTIONAL rain
  • 17. The UK is affected by a number of different air masses. Air masses are huge blocks of air at different temperatures. Some of the air masses are warm and some of the air masses are cold .
  • 18. But air masses at different temperatures DO NOT like one another so they won’t mix together. Birmingham is affected by cold air coming down from the north and warm air coming up from the south. The junction between these two different air masses is called a front so when they cause it to rain it is called FRONTAL RAIN .
  • 19. But if they won’t mix, what happens when they meet?
  • 20. Its fair to assume then, that the final type of rainfall will also follow the same process. But what is it that is causing the air to rise? A FEW CLUES Name: RELIEF rainfall
  • 21. Meet Reggie, the RELIEF RAIN raindrop Reggie is a gas flying in the air (water vapour) but when he meets a hill he has to climb over it. It gets very cold near the top of the hill as he is so high and Reggie changes from a gas to a liquid and settles into some clouds (condensation). When lots of Reggie’s friends arrive in the cloud it is too cramped to stay so some of them fall back to earth as relief rainfall (precipitation).
  • 23. Hydrological Cycle Matching Resurgence Overland Flow (surface runoff Ground water flow Infiltration Surface water storage Percolation Transpiration Isolation Precipitation Atmospheric Store Snowmelt Saturated zone (aquifer) evaporation Soil moisture Ocean store Base flow Atmospheric condensation Water table Volcanic water Ice cap storage Human activities Interception Stream runoff Impervious bedrock Reabsorbed by plants
  • 24.
  • 25.
  • 26.