CLIMATE

Day vs. Night

 Earth

rotates

on it’s axis (24 hours). Results in day and night

Seasons

 Earth

revolves

around the Sun (orbits 365 days).

Results in seasons



Cloud Cover

Cloud Cover:   Nightly cloud cover will result in less temperature range (like a blanket) Without cloud cover, heat escapes (at night), but temperature range is very high (hot days, cold nights…the desert)

Differences in Day Length

The tilt of the earth

’

s axis combined with the earth

’

s rotation in orbit around the sun results in different day lengths. The difference?

•In June

: because of the tilt on the earth's axis giving it longer days. , the north pole points towards the sun and receives more hours of exposure to the sun hence

•In December

: because of the tilt on the earth's axis, points away from the sun and receives fewer hours of exposure to the sun hence giving it shorter days.

the north pole SUN

JUNE DECEMBER

SEASONS

 The

tilt

on the earth's axis and;  The

revolution

of the earth around the sun  These two features of the earth-sun relationship mean that different latitudes on earth receive different directness of light at different times.

Equinox and Solstice

  Solstice:   sun is directly over head @ 12 noon on 23.5º North or South; occurs Dec 21 & June 21  longest day of the year & shortest day of the year. Equinox:  sun is directly over head @ 12 noon on the equator;   occurs Sept. 21 & March 21 equal length of night and day everywhere on earth.

Tropics vs. The Poles

    The tropics are located between 23.5˚ north and 23.5˚ south (Cancer and Capricorn)

The further you move away from the tropics the more severe the seasons. The length of day varies more the further you move from the equator.

When light hits the earth towards the poles it is on a severe angle which decreases the intensity of heat.

How the Sun hits the Earth

Greenhouse Effect

     A good thing? In moderation of course; moderates our temperatures Without we would have extreme variation of temperatures between day and night

Atmosphere reflects and absorbs about 50% of radiant energy Without atmosphere, planets have nothing to hold heat in (like the glass in a greenhouse… consequently the nights are not as cool)

Latitude and Temperature

   The closer we get to the equator, the warmer it gets “

The further south one goes the warmer it gets

”

(FALSE). Once we went far enough south to go past the equator the temperatures would start getting colder again.

As latitude increases, temperature decreases

Other Factors

   

Prevailing Winds

Regular, predictable, normal wind direction. They are caused by global convection cells in the earth's atmosphere.

Ocean Currents

The biggest factor besides the sun. If the water is warm, the temperatures will be more moderate.   

Altitude

the higher the altitude, the cooler it will be.

Rate is about 1˚ per 100m

Altitude

WIND



Winds Blow From High Pressure to Low Pressure

   Any real examples of this at work?

Air inside a balloon balloon).

. If left untied the air will escape the high pressure of the balloon and create a wind blowing from high pressure (inside the balloon) to relatively low pressure (outside the

High and low pressures in the earth ’ s atmosphere are responsible for wind.

High vs. Low Pressure

 Low Pressure: Usually a result of “ heating ”  High Pressure: Usually a result of “ cooling ”

Sea Breeze/Land Breeze

 What heats faster; land or water?

 When do things warm or cool over the course of 24 hours?

   

During the day the land heats much faster than the water; Consequently the air over the land heats and rises ( low the air over the water/sea is relatively high ; pressure) while Wind blows from the high pressure to the low pressure Hence the name 'sea breeze'—the wind is blowing off the sea.

During the Day

Convection Cells

 The global

convection cells

are created because of the differential heating of the earth's surface.  Alternating high and low pressure belts result from the convection cells.  You want real results?

Convection Cells

The results?



Every desert in the world is found at a similar latitude



Every rainforest of the world is found at a similar latitude.



Coincidence?

Types of Rain

 1.

2.

3.

Three types of rainfall: Relief Rain Convectional Frontal / Cyclonic Rain

Rain. Period.

 hot air rises  warm moisture-laden air cools at higher altitude  cool air holds less moisture;  consequently clouds condense and rain falls.

Relief Rainfall

    Moisture laden air blows off the sea; Air is forced up by mountains (high relief) Most rain falls on the windward side of the relief Leeward side is often in a dry rain shadow because the moisture has all been lost.

Relief Rainfall

Convectional Rainfall

 Usually occurs in hot areas like tropics or continental summer (Winnipeg thunderstorms)  sun heats the earth causing large amounts of water to evaporate  Then what?  Remember RAIN.PERIOD. Check it out!

Convectional Rainfall

Frontal / Cyclonic Rainfall

 Warm moist air meets cold air  Warm air is less dense & is forced up over the cooler, more dense air  Then What? 

Fall/spring/some summer Winnipeg rains

Frontal Rainfall

Ocean Currents

 Permanent horizontal movement of surface water (the top 100m)  It is unusually cold or warm , when compared with the surrounding water  Analogy:  Sun =CEO of climate  Ocean Currents =BOSS of climate

Where do they go?

Where would you expect cool currents to start from?

Where would you expect warm currents to start from?

How do currents create balance in the world?

Warm and Cold Currents

     

Cold ocean currents: move water towards the equator.

For example the Humbolt or Peru Current carries cold water from Antarctica toward the equator. Another example is the Labrador Current which carries cold water from the Arctic Ocean.

Warm ocean currents: Move water away from warm equatorial regions.

For example the Gulf Stream moves warm water from the Gulf of Mexico northeast toward England. Another good example is the Japanese current which moves warm water from Japan northeast towards Vancouver.

Ocean Currents & the Affect on Climate



Affect of cold ocean currents

Cools the summer temperature; Reduces precipitation; cooler air holds less moisture. 

Affect of warm ocean currents

Warms the winter temperature; Increases precipitation; warmer air holds more moisture. El Nino

Continentality



Temperature range

region. : the difference between the highest and the lowest average monthly temperatures of a

 What helps creates this range in this case?

Proximity to ocean (or larger body of water)  

Large or high temperature range : extremes of temperature, hot summer, cold winter (Winnipeg). Small or low temperature range : moderated temperature, warm summer, cool winter (Victoria)

Continental vs. Maritime Climates

   

As distance from the ocean increases,

annual temperature range increases.

Continental climates experience greater extremes of temperature than coastal climates at the same latitude. The plains region of Saskatchewan, for example, experience a continental climate. The winter temperatures are very cold, and the summer temperatures are fairly hot. Range could be from: -40

°

to 40

°

C Close to the ocean, Victoria experiences a much more moderate climate. Range is from: -5

°

hot in the summer. to 25

°

. Not too cold, but at the same time, not too

Climate Graphs

 Give us a yearly climate snap-shot of a given place  Temperature will always be shown with a line graph  Precipitation will always be shown with bar graphs

 Scotland….

Maritime



Winnipeg

Continental

Tropical Climates

 All Tropical Climates have average temperatures over 18˚C every day  All Tropical climates can be divided into:

a) Tropical Wet b) Tropical Wet and Dry



Almost all of the tropical wet / wet & dry climates located between the tropic of cancer and the tropic of Capricorn

(23.5˚ N and S).

are

Tropical Wet Climate

Tropical Wet : heavy rain all year due to hot temp & resulting convectional rain .

Tropical Wet and Dry Climate

Tropical Wet& Dry : very heavy summer rain & very dry winter due to seasonal shift in prevailing winds. (monsoon regions)

Dry Climates

 All Dry climates receive less than 500mm precipitation annually.  Dry Climates can be divided into: a) Arid b) Semi-Arid 

more evaporation than precipitation = water deficit.



There is little vegetation & it is often windy

Arid or Desert Climates

 Arid Climates: occur mostly between 10-30˚N & 10-30˚S and receive 10-250mm rain annually.

Semi-Arid Climate

 Semi-arid Climates: are transition zones between Desert & Forest. They receive 250-500mm rain annually which is often enough to support grasses but not forests.

Temperate Climates

    

Usually in higher latitudes (above 30˚ N and S) Temperate Climates can be divided into: a)Temperate Mild Climates

hemispheres occur in both

b)Temperate Cold Climates

only occur in the northern Hemisphere. (Winnipeg) The distinguishing feature on a climate graph is the temperature line ( yearly average Temp .)

Temperate Climates

 

Temperate Mild Winter

  Temperature varies with seasons Mid Latitudes   Mild winter Summer temperatures vary but winters are warmer than –3ºC

Temperate Cold Winter

 Temperature varies with seasons    Mid-high Latitudes cold winters Summer temperatures vary but winters are colder than –3ºC

Temperate Climate

Polar Climates

 Polar climates are distinguished by their extremely low winter temperatures and low summer temperatures.  Polar Climates can be divided into:  Tundra : summer temperature never above 10˚C  Ice Caps : summer's average monthly temperature is never above 0˚C

Polar Climate

?

?

?

?

?

Monsoons

 A sudden wet season in the tropics “ rainy ” . Notice the difference between the annual rainfall of some places directly influenced by monsoons

India’s Monsoons

India’s Monsoons

India

’

s Winter Monsoon

 Continental Asia cools & high atmospheric pressure results;   Very little rain or dry season results because the wind is blowing over dry land and does not pick up moisture.

India

’

s Summer Monsoon

 Wind blows southward towards the low pressure over Indian ocean; Continental Asia heats up & low atmospheric pressure results;   Wind blows northward towards the low pressure over India; Tremendous rains result because the wind is blowing over the warm Indian Ocean.

India’s Monsoons

Affect on People

   Tourism in the tropics is very important. During monsoons, travel is not safe, even prohibited in some cases (Malaysia ’ s East Coast) Severe flooding Economy suffers (fishing, tourism, etc.)