Factors affecting climate
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Transcript of Factors affecting climate
LAMECOWS
Factors Affecting Climate
L is for Latitude
LatitudeLatitude The farther away from the Equator, The farther away from the Equator,
the colder the climate becomes. the colder the climate becomes.
Low
Mid
Mid
Cold
Warm
Hot
Warm
Cold
High
High
Tropic of Cancer
Equator
Tropic of Capricorn
From which From which latitude zone were latitude zone were
these pictures these pictures taken?taken?
Rainforest
Deciduous Trees
Tundra
Steppe
Tropical Grasslands
Marine West Coast
L is for Latitude
A is for Air Pressure
Air PressureAir Pressure Air pressure is caused by the unequal Air pressure is caused by the unequal
heating of earth’s surface.heating of earth’s surface.
1. Low pressure is warm, moist air. It 1. Low pressure is warm, moist air. It raises and forms clouds. raises and forms clouds.
2. High pressure is cold, dry air.2. High pressure is cold, dry air.
It sinks and creates clear skies.It sinks and creates clear skies.
L is for Latitude
A is for Air Pressure
M is for Mountain Barriers
Mountain BarriersMountain Barriers Mountain Barriers create a phenomenon Mountain Barriers create a phenomenon
called the Orographic Effect or called the Orographic Effect or Rainshadow.Rainshadow.
The rainshadow helps create deserts The rainshadow helps create deserts
Ex. Sierra Nevada mountains in CA Ex. Sierra Nevada mountains in CA receive nice amounts of precipitation, receive nice amounts of precipitation, Las Vegas, NV is in the rainshadow Las Vegas, NV is in the rainshadow creating a desert climate.creating a desert climate.
Rainshadow EffectRainshadow Effect
Windward Side Leeward side
‘Wet’ side ‘Dry’ side
This rainshadow region in India was createdby the presence of the Western Ghats mountain
range, which block the monsoon(seasonal) winds from the west.
L is for Latitude
A is for Air Pressure
M is for Mountain Barriers
E is for Elevation
Based on the location of Quito, Ecuador, what type of climate do you think it should have?
What about Guayaquil, Ecuador?
Quito, EcuadorQuito, Ecuador
JanJan FebFeb MarMar AprApr MayMay JuneJune JulyJuly AugAug SeptSept OctOct NovNov DecDec
5858 5858 5858 5959 5858 5858 5858 5858 5858 5858 5858 5858
JanJan FebFeb MarMar AprApr MayMay JuneJune JulyJuly AugAug SeptSept OctOct NovNov DecDec
8181 8181 8282 8282 8181 7878 7777 7777 7878 7878 7979 8181
Guayaquil, Ecuador
ElevationElevation As elevation increases, temperature As elevation increases, temperature
decreases. decreases.
1. For every thousand feet the 1. For every thousand feet the
temperature drops 3.6°F temperature drops 3.6°F In a highlands climate, lower elevation In a highlands climate, lower elevation
means more vegetationmeans more vegetation
L is for Latitude
A is for Air Pressure
M is for Mountain Barriers
E is for Elevation
C is for Continental Location
Continental LocationContinental Location
Large bodies of water are slower to Large bodies of water are slower to heat and cool than land. heat and cool than land.
As a result, water temps. remain As a result, water temps. remain stable, and land temps. change stable, and land temps. change frequently .frequently .
Coastlines have Coastlines have stablestable temperatures. temperatures. Interior of continent has Interior of continent has extremeextreme
temperatures (hotter and colder)temperatures (hotter and colder)
High/Low Temperatures for Donna High/Low Temperatures for Donna and South Padre Island and South Padre Island
December Monthly Temperatures69 67
48 52
01020304050607080
Donna SPI
Deg
rees
High Temperature
Low Temperature
High/Low Temperatures for High/Low Temperatures for Donna and South Padre Island Donna and South Padre Island
August Temperatures
9689
74 77
0
20
40
60
80
100
120
Donna SPI
Deg
rees High
TemperatureLowTemperatures
L is for Latitude
A is for Air Pressure
M is for Mountain Barriers
E is for Elevation
C is for Continental Location
O is for Ocean Currents
Ocean CurrentsOcean Currents Ocean currents are giant rivers of sea Ocean currents are giant rivers of sea
water flowing within oceans.water flowing within oceans.
Ocean currents flow in circular paths:Ocean currents flow in circular paths:
1. Warm currents carry water from low 1. Warm currents carry water from low to high latitudes. These make land to high latitudes. These make land nearby warmer.nearby warmer.
2. Cool currents carry water from high 2. Cool currents carry water from high to low latitudes. These make land to low latitudes. These make land nearby colder.nearby colder.
Ocean Current MapOcean Current Map
L is for Latitude
A is for Air Pressure
M is for Mountain Barriers
E is for Elevation
C is for Continental Location
O is for Ocean Currents
W is for Wind Belts
Wind BeltsWind Belts
Wind is the movement of air from Wind is the movement of air from high pressure to low pressure (like high pressure to low pressure (like when you poke a hole in a tire.)when you poke a hole in a tire.)
1. Trade Winds1. Trade Winds
2. Westerlies2. Westerlies
3. Polar Winds3. Polar Winds
Wind Belt MapWind Belt Map
L is for Latitude
A is for Air Pressure
M is for Mountain Barriers
E is for Elevation
C is for Continental Location
O is for Ocean Currents
W is for Wind Belts
S is for Storms
StormsStorms Occur during Occur during low pressurelow pressure
conditions.conditions. Storm fronts occurs when two air Storm fronts occurs when two air
masses with different temperatures masses with different temperatures meet. (cold meets warm)meet. (cold meets warm)
1. Thunderstorms 1. Thunderstorms
2. Tornadoes 2. Tornadoes
3. Hurricanes3. Hurricanes