Met112lecture4 - San Jose State University

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MET 112 Global Climate Change - Lecture 4

Controls on Climate

Dr. Eugene Cordero

San Jose State University

Outline

 Energy balance: a latitudinal perspective

 Seasons

 Atmospheric circulation; quick view

 Climate game

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Definitions

 Insolation – Incoming solar radiation

 Solstice – day of the year when the sun shines directly over 23.5

°S or 23.5°N

 Equinox – days of the year when the sun shines directly over the equator

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Sun angle

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Sun angle (2)

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What influences incoming solar energy?

 The Sun’s angle of incidence:

– Lower sun angle, less incoming energy

– Higher sun angle, more incoming energy

 Length of time the Sun shines each day:

– Summer season, more sun hours

– Winter season, less sun hours

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Why do we have seasons?

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What month do you think this graph represents?

a) December b) March c) June d) September

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What month do you think this graph represents?

0 of 70

1. December

2. March

3. June

4. September

0% 0% 0% 0%

D ec em be r

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M ar ch

S ep te m be r

Ju ne

12

Review questions

 On June 21 st , at what latitude is the sun directly overhead at noon?

 On September 22 nd , at what latitude is the sun directly overhead at noon?

 How many hours of daylight are present at the

South Pole on February 20 th ?

 Where would you expect to have longer days;

45 ° N on June 21 st or 50 °S on Dec 21 st ?

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On June 21 st , at what latitude is the sun directly overhead at noon?

1. Equator (0)

2. 23.5

°N

3. 23.5

°S

4. 90 °N (north pole)

5. 90 °S (south pole)

0 of 70

0% 0% 0% 0% 0%

E qu at or

(0

)

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.5

°N

23

.5

°S

90

°N

(n or th

p ol e)

90

°S

(s ou th

p ol e)

16

Where would you expect to have longer days;

45 ° N on June 21 st or 50 °S on Dec 21 st ?

1. 45 °N

2. 50 °S

3. They are the same

4. Impossible to tell

0 of 70

0% 0% 0% 0%

C ho ic e

O ne

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C ho ic e

Tw o

C ho ic e

Th re e

C ho ic e

Fo ur

17

On September 22 nd , at what latitude is the sun directly overhead at noon?

1. Equator (0)

2. 23.5

°N

3. 23.5

°S

4. 90 °N (north pole)

5. 90 °S (south pole)

0 of 70

0% 0% 0% 0% 0%

E qu at or

(0

)

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23

.5

°N

23

.5

°S

90

°N

(n or th

p ol e)

90

°S

(s ou th

p ol e)

18

How many hours of daylight are present at the South Pole on February 20 th ?

1. 0 hours

2. 6 hours

3. 12 hours

4. 18 hours

5. 24 hours

0 of 70

0% 0% 0% 0% 0%

0 ho ur s

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6 ho ur s

12

h ou rs

18

h ou rs

24

h ou rs

19

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Earth’s energy: latitudinal perspective

 A majority of the sun’s energy enters the Earth system in the tropics.

 The tropics thus becomes quite warm, while the poles relatively cool.

 The atmosphere attempts to bring the tropics and high latitude into equilibrium

– Weather systems ultimately act to bring warm air to higher latitudes and cold air to lower latitudes.

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Annual Surface Temperature

Questions

 Indicate the warmest and coldest areas of the

Earth.

 Consider the temperature at 60N latitude.

Indicate on the map the coldest and warmest places at 60N.

 What is the temperature difference between these locations

 What factors might explain this temperature difference?

 Why is there not a similar difference seen at 60S?

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Annual Surface Temperature

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Climate controls:

Latitude/Mountains

 Latitude

– Higher latitude climates are generally

(cooler/warmer)

– Lower latitudes climates are generally

(cooler/warmer)

 Mountains

– Higher altitudes climate are generally

(cooler/warmer): cooler temperatures

– Windward side of mountains are generally

(cooler/warmer) and (wetter/drier), than leeward side

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Climate controls:

Latitude/Mountains

 Latitude

– Higher latitude climates are generally

(cooler/warmer)

– Lower latitudes climates are generally

(cooler/warmer)

 Mountains

– Higher altitudes climate are generally

(cooler/warmer): cooler temperatures

– Windward side of mountains are generally

(cooler/warmer) and (wetter/drier), than leeward side

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Controls on Climate

 Seasonal temperature and precipitation patters are generally attributable to:

 Latitude

 Mountains and highlands

 Land and water location

 Prevailing winds

 Pressure and wind systems

 Ocean currents

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Controls on Climate: Oceans

 Ocean Temperatures

– Coasts of continents are affected by ocean temperatures: Generally less temperature extremes compared to interior of continents

– Cold oceans: generally produce cooler/drier conditions

– Warm oceans: generally produce more warm/humid conditions

31

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Cold ocean

Warm ocean

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Dry

Humid

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Controls on Climate: Pressure systems

 Rising and sinking motion associated with low and high pressure affects climate

 Areas where pressure seasonally low,

Tropics: rainy

 Areas where pressure seasonally high,

Subtropical high (30N/3OS): warm and dry

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January Average sea-level Pressure and surface wind pattern

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July Average sea-level Pressure and surface wind pattern

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A_B_D_ let’s check out clicker id’s out

1. E Q U

2. I E B

3. E L O

4. O U W

0 of 70

0% 0% 0% 0%

E

Q

U

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I E

B

E

L

O

O

U

W

41

Climate Game

Names ___________________________

 Match the city with the corresponding climatology by indicating the appropriate letter

 Sacramento, California (38 °N) _____________

 Phoenix, Arizona (33 °N) _____________

 Denver, Colorado (40 °N) _____________

 Iquitos, Peru (4 °S)

 Mobile, Alabama (30 °N)

 Winnipeg, Canada (50 °N)

 Fairbanks, Alaska (65 °N)

_____________

_____________

_____________

_____________

City A

1. Sacramento, California

2. Phoenix, Arizona

3. Denver, Colorado

67%

4. Iquitos, Peru

5. Mobile, Alabama

14%

6. Winnipeg, Canada

7% 7%

0%

2% 2%

7. Fairbanks, Alaska

S ac ra m en to

, C al ifo

P rn ia rizo ho en ix

, A

D en ve r, na

C ol or ad o

Iq ui to s,

P er u

M ob ile

, A la

W in ni ba m a pe g,

C an ad a

Fa irb an ks

, A la sk a

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City B

1. Sacramento, California

2. Phoenix, Arizona

3. Denver, Colorado

72%

4. Iquitos, Peru

5. Mobile, Alabama

6. Winnipeg, Canada 14%

12%

0%

2%

0% 0% 7. Fairbanks, Alaska

S ac ra m en to

, C al ifo

P rn ia rizo ho en ix

, A

D en ve r, na

C ol or ad o

Iq ui to s,

P er u

M ob ile

, A la

W in ni ba m a pe g,

C an ad a

Fa irb an ks

, A la sk a

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City C

1. Sacramento, California

2. Phoenix, Arizona

3. Denver, Colorado

67%

4. Iquitos, Peru

5. Mobile, Alabama

19%

6. Winnipeg, Canada

7%

5%

0%

2%

0% 7. Fairbanks, Alaska

S ac ra m en to

, C al ifo

P rn ia rizo ho en ix

, A

D en ve r, na

C ol or ad o

Iq ui to s,

P er u

M ob ile

, A la

W in ni ba m a pe g,

C an ad a

Fa irb an ks

, A la sk a

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City D

1. Sacramento, California

2. Phoenix, Arizona

3. Denver, Colorado

84%

4. Iquitos, Peru

5. Mobile, Alabama

6. Winnipeg, Canada

9%

4%

0% 0% 0%

2%

7. Fairbanks, Alaska

S ac ra m en to

, C al ifo

P rn ia rizo ho en ix

, A

D en ve r, na

C ol or ad o

Iq ui to s,

P er u

M ob ile

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W in ni ba m a pe g,

C an ad a

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, A la sk a

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City E

1. Sacramento, California

2. Phoenix, Arizona

3. Denver, Colorado

47%

4. Iquitos, Peru

20%

5. Mobile, Alabama

13%

9% 6. Winnipeg, Canada

7%

4%

0% 7. Fairbanks, Alaska

S ac ra m en to

, C al ifo

P rn ia rizo ho en ix

, A

D en ve r, na

C ol or ad o

Iq ui to s,

P er u

M ob ile

, A la

W in ni ba m a pe g,

C an ad a

Fa irb an ks

, A la sk a

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City F

1. Sacramento, California

2. Phoenix, Arizona

3. Denver, Colorado

83%

4. Iquitos, Peru

5. Mobile, Alabama

6. Winnipeg, Canada

5% 5% 5%

0%

2%

0% 7. Fairbanks, Alaska

S ac ra m en to

, C al ifo

P rn ia rizo ho en ix

, A

D en ve r, na

C ol or ad o

Iq ui to s,

P er u

M ob ile

, A la

W in ni ba m a pe g,

C an ad a

Fa irb an ks

, A la sk a

MET 112 Global Climate Change

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