© Oxford University Press 2009 Quit Part 7 Global warming─Are humans responsible 7.2 7.2 What is the What is the normal normal global global distribution distribution pattern pattern of of temperature? temperature? Part B Part B
Mar 26, 2015
© Oxford University Press 2009 Quit
Part 7 Global warming─Are humans responsible?
7.27.2 What is the normal What is the normal global distributionglobal distribution pattern of pattern of temperature?temperature?
Part BPart B
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Earth’s surface Heated earth’s surface
Insolation
Radiation
Long wave
radiation
Conduction Convection
How is insolation related to the global distribution of temperature?How is energy transferred into the atmosphere?
When the earth’s surface is heated up, it releases heat energy and warms the air
above through three ways.
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When is the insolation the highest?When is the insolation the highest?When does the ground receive no
insolation?When does the ground receive no
insolation?
What is the relationship between insolation and air temperature?
The more the insolation, the ( higher / lower ) the air temperature.Air temperature is controlled by __________.insolation
At noon.Between
sunset and sunrise.
Maximum insolation
No insolation
No insolation
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Around 16-17°C
Around 27-28°C
What is the world distribution pattern of temperatures? What is the July
temperature of London and Hong Kong?
What is the July temperature of London
and Hong Kong?
What is the January temperature of London
and Hong Kong?
What is the January temperature of London
and Hong Kong?
Around 3°C
20°C
( Hong Kong / London ) has a higher temperature in both July and January.
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What is the world distribution pattern of temperatures?
( Low- / Mid- ) latitude region
( Low- / Mid- ) latitude
region
What regions are London and Hong Kong located at?
What regions are London and Hong Kong located at?
What conclusion can you draw from
this?
What conclusion can you draw from
this?
Temperature ( decreases / increases ) with increasing latitude.Temperature is ( lower / higher ) in lower-latitude regions.
1 Air temperature is higher in low-latitude regions
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2 Temperature variation over latitude is more marked in winter in the Northern Hemisphere
The ( Northern / Southern ) Hemisphere has a closely-
spaced pattern of isotherms in January.
It means temperature variation over latitude
is more marked in winter in the Northern
Hemisphere.
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2 Temperature variation over latitude is more marked in winter in the Northern Hemisphere
JanuaryJuly
Moscow: ____°CJerusalem: ____°CDifference: ____°C
152914
Moscow: ____°CJerusalem: ____°CDifference: ____°C
-151530
Let’s look at the temperatures of Moscow and Jerusalem.
The two cities have a larger temperature difference in
( summer / winter ).
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July
What are the temperatures of Places A and B which are at the same
latitude?
What are the temperatures of Places A and B which are at the same
latitude?
Place A: ____°CPlace B: ____°C
Difference: ____°C
8124 January
Place A: ____°CPlace B: ____°C
Difference: ____°C
0-3434
3 Places at the same latitude may have different air temperatures
What conclusion can you draw from this?
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January
3 Places at the same latitude may have different air temperatures
July
The isotherms in mid-latitudes in the Southern Hemisphere are roughly
parallel to the latitudes. Why?
The isotherms in mid-latitudes in the Southern Hemisphere are roughly
parallel to the latitudes. Why?
It is because most of the area there is covered by sea. The changes in
temperature are relatively ( small / large ).
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4 There is a seasonal pattern of air temperature
0
July
Compare the difference of temperatures of
Tokyo and Sydney in July and January
respectively.
Temperature in July (°C)
Tokyo
Sydney
Temperature in January (°C)
24
13
January
0°
8
21
In July, it is ( summer / winter ) in the Northern Hemisphere and ( summer / winter ) in the Southern Hemisphere.In January, it is winter in the Northern Hemisphere and summer in the Southern Hemisphere.
25
20
15
10
5
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How is insolation related to the global distribution of temperature?What are the factors affecting temperature patterns?
Factors affecting temperature patterns
Insolation Land and sea
Winds Ocean currents
Aspect Altitude Cloud cover
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How is insolation related to the global distribution of temperature?What are the factors affecting temperature patterns?
Land and sea
Winds Ocean currents
Aspect Altitude Cloud cover
Factors affecting temperature patterns
Insolation The more the insolation received, the ( lower /
higher ) the air temperature.
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2 Land and seaJuly
January
Moscow:15°C
Place A (over the sea): 8°C
Place A (over the sea): -6°C
Moscow: -15°C
A
A
Why are there different
temperatures at places at the same latitude?
Why are there different
temperatures at places at the same latitude?
In July, Moscow is ( colder / hotter ) than Place A.In January, Moscow is ( colder / hotter ) than Place A.
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2 Land and sea
8°CLand absorbs heat more quickly
15°C
Sea loses heat more slowly
-6°CLand loses heat more quickly
-15°C
Heat can be transferred quickly through the land by __________. Hence, the land absorbs and loses heat quickly.
The water in oceans is heated by __________. As oceans are large bodies of water, it takes time to transfer the heat. Hence, oceans absorb and lose heat slowly.
conduction
convection
Sea absorbs heat more slowly
Place A
Place A
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2 Land and sea Annual range of temperatureCopenhagen: 18°CMoscow: 30°C
( Copenhagen / Moscow ) has a smaller annual range of temperature.
Copenhagen is located at the coast. _______ help regulate the temperature along coastal areas.
Oceans
Maritime climate:Mild winters and cool summers
Continental climate:Cold winters and hot / warm summers
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2 Land and sea
Annual range of temperature
What characteristics do you notice about the distribution of annual range of temperature?
What characteristics do you notice about the distribution of annual range of temperature?
Annual range of temperature( decreases / increases ) as the latitude increases;( decreases / increases ) with the distance from the sea.
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How do winds affect the
temperature of a place?
How do winds affect the
temperature of a place?
3 WindsThis is the seasonal pattern of winds in Hong Kong:
Hong Kong
Winter
Hong Kong
Cold northerly winds blowing from the cold inland areas of the mainland
Some places receive onshore winds in winter. The warm onshore winds from the sea help raise the winter temperature there.
South-easterly winds blowing from the Pacific Ocean
Summer
Temperature in Hong Kong (
/ )
Temperature in Hong Kong (
/ )
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4 Ocean currentsOcean currents are seawater flowing along fixed routes.They are divided into warm currents and cold currents.
Warm currents flow from equatorial
areas to polar areas
Cold currents flow from polar areas to
equatorial areas
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4 Ocean currents
How do ocean currents affect the
temperatures of the places lying along
their paths?
How do ocean currents affect the
temperatures of the places lying along
their paths?
Warm ocean currents originate from areas where the water is warm.
Warm ocean currents originate from areas where the water is warm.
The air above the currents becomes ( cold / warm ).
The air above the currents becomes ( cold / warm ).
Places lying along the paths of warm ocean
currents have ( lower / higher ) temperatures.
Places lying along the paths of warm ocean
currents have ( lower / higher ) temperatures.
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4 Ocean currents Cold ocean currents originate from areas where the water is cold.
Cold ocean currents originate from areas where the water is cold.The air above
the currents becomes cold.
The air above the currents
becomes cold.
Places lying along the paths of cold ocean currents have
lower temperatures.
Places lying along the paths of cold ocean currents have
lower temperatures.
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4 Ocean currents
Glasgow Nain
Located at similar latitudes, both Glasgow and Nain are affected by
ocean currents.
What do you notice about the relationship between the type of ocean current and mean temperatures in
July and January of Glasgow and Nain?
What do you notice about the relationship between the type of ocean current and mean temperatures in
July and January of Glasgow and Nain?
Ocean currentMean temperature
in JulyMean temperature
in January
Glasgow
Nain
North Atlantic Drift
( cold / warm ) current
Labrador Current
( cold / warm ) current
17°C
( lower / higher ) temperature
8.2°C
( lower / higher ) temperature
5°C
( lower / higher ) temperature
-21.7°C
( lower / higher ) temperature
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5 AspectAspect refers to the direction a slope faces in relation to the sun.
Sun’s rays strike at a larger angle on south-facing slopes
Sun’s rays strike at a smaller angle on north-facing slopes
South-facing slopes receive ( less / more ) insolation per unit area
North-facing slopes receive less insolation per unit area
Northern Hemisphere What is the situation in
the Southern Hemisphere? What is the situation in
the Southern Hemisphere?
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6 Altitude
Denser air
Heat loss
_____________, ______ and _______________ in the atmosphere absorb long wave radiation and keep the air warm
Water vapour dustcarbon dioxide
Less dense air
Heat released from the earth’s surface is stored in the air
Heat loss
Less dense air absorbs ( less / more ) heat
Air becomes less dense with increasing altitude. Heat loss is faster and thus the air temperature ( falls / rises ).
The average rate of decrease in air temperature with height is 6°C per 1,000
metres. This is known as the ________________________.environmental lapse rate
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7 Cloud cover
Earth’s surface Earth’s surface
With cloud cover Without cloud cover
Insolation
Direct reflection
Place A Place B
Daytime
A large part of the insolation reaches the
earth’s surface
Only part of the insolation reaches the
earth’s surface
Which area would have a lower temperature?
Which area would have a lower temperature?
Insolation
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7 Cloud cover
Night time
Which area has a larger daily range of temperature?
Which area has a larger daily range of temperature?
Earth’s surface Earth’s surface
With cloud cover Without cloud cover
The warmth is kept
The warmth is lost
Only a small part of the radiation is released back to space
A large part of the radiation is blocked by the clouds
A large part of the radiation would be
released back to space
Place A Place B
Longwave radiation
Longwave radiation
Some radiation is absorbed by clouds