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+ 3 Express Pure Geog: Types of Climate 28 th March 2012 Reconsolidation Arman Alluwie TP2 SHSS
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Page 1: Full Geography Secondary 3 Express- Weather and Climate 5

Arman Alluwie TP2 SHSS

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3 Express Pure Geog:Types of Climate28th March 2012Reconsolidation

Page 2: Full Geography Secondary 3 Express- Weather and Climate 5

Arman Alluwie TP2 SHSS

2+What did we learn last lesson?Climograph Climatic Graph

graph of average temperatures and average rainfall for a place over the twelve months of a year

drawn by reference to data presented in a climatic table

Page 3: Full Geography Secondary 3 Express- Weather and Climate 5

Arman Alluwie TP2 SHSS

3+Climograph:Inferring Climate

Page 4: Full Geography Secondary 3 Express- Weather and Climate 5

4+What did we learn last lesson?

Expert Group Learning

After completion of case study, Expert A, B, C, D will come together to form a Learning Group

Arman Alluwie TP2 SHSS

Each Learning Group works on one final assignment

Page 5: Full Geography Secondary 3 Express- Weather and Climate 5

Arman Alluwie TP2 SHSS

5+Getting to Know Me:

Return all Getting to Know Me worksheets privately

The map

Page 6: Full Geography Secondary 3 Express- Weather and Climate 5

Arman Alluwie TP2 SHSS

6+How is Weather different from Climate? Weather refers to the conditions of the

atmosphere at a specific place over a relatively short period of time, whereas climate refers to the average atmospheric conditions over a specific place over a considerable period of time, usually 30 to 35 years.

Page 7: Full Geography Secondary 3 Express- Weather and Climate 5

Arman Alluwie TP2 SHSS

7+How is Weather different from Climate? Must be written in full prose

Either choose specific characteristics or use conjunctions of contrast eg. while, but etc.

Weather refers to the conditions of the atmosphere at a specific place over a relatively short period of time, whereas climate refers to the average atmospheric conditions over a specific place over a considerable period of time, usually 30 to 35 years.

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Evaporation a process where water from water bodies is

converted into water vapor as the Earth’s surface is heated up

Relative Humidity Increases as the amount of water vapor in the air

increases

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Condensation process in which cooled water vapour changes into

water droplets

Relative Humidity increasing and approaching saturation point

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Saturation air is carrying the maximum amount of water vapour

it can hold at that temperature

Relative Humidity 100 per cent

Arman Alluwie TP2 SHSS

*but shouldn’t the rising air reach saturationpoint before condensation? -> pg 96

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Page 12: Full Geography Secondary 3 Express- Weather and Climate 5

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12+Questions

What are the characteristics of relief rain?

How does a typhoon occur?

How is lighting formed?

Where is the saturation level? Are HDBs considered high relief? Why doesn’t the land feel cold when warm air rises?

Why does it rain when its bright and sunny?

Page 13: Full Geography Secondary 3 Express- Weather and Climate 5

Arman Alluwie TP2 SHSS

13+Relative Humidity:Varies with Location

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Page 18: Full Geography Secondary 3 Express- Weather and Climate 5

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18+“Condo Fog”

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Precipitation water falling from the atmosphere onto the Earth’s

surface

Relative Humidity Decreases, water vapour has condensed and thus its

amount has reduced

*do not mention temperature changes