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CLIMATE. A region’s “general” weather conditions as established over a long period of time is known as climate. Climate is defined by two weather variables: temperature and atmospheric moisture . Lincoln, NE ~ 40˚N. Providence, RI ~ 40˚N. - PowerPoint PPT Presentation
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A region’s “general” weather conditions as established over a long period of time is known as climate.
Climate is defined by two weather variables: temperature and atmospheric moisture.
Lincoln, NE ~ 40˚N Providence, RI ~ 40˚N
“How is it possible that two locations at the same latitude can experience different climates?”
CLIMATE
Climate Regions
P = Annual Precipitation (moisture)PET = Potential Evapotranspiration (temperature)
ARIDP < PET
HUMIDP > PET
SUB-HUMIDSEMI-ARID
P ≅ PET
Factors Affecting Climate
Latitude
Large Bodies
of Water
Planetary Winds and Pressure
Belts
Vegetation Cloud
Cover
Ocean Currents
Elevation
Mountains
Climate Change due to Latitude The Earth receives maximum intensity and fairly consistent duration of insolation between 23 ½ ˚N and 23 ½ ˚S during its revolution around the
Sun.
Annual temperatures tend to be high and there is a minimal variation in temperature throughout
the year.
Latitudes north of 23 ½ ˚N and latitudes south of 23 ½ ˚S never receive direct
insolation and the duration of insolation fluctuates.
Annual temperatures tend to vary over a wide range seasonally.
Climate Change due to Latitude The location of pressure belts will alter the moisture conditions at
certain latitudes.
Low
Low
Low
High
High
Low pressure belts (convergence) are
known for rising air, cloud development and precipitation.
Humid-like climate
High pressure belts (divergence) are
known for descending air, few clouds and
lack of precipitation.
Arid-like climate
Climate Change due to Large Bodies of Water
Land tends to heat up and cool down more quickly than water (due to specific heat).
The temperature of a location near a large body of water will be moderated by its presence near the water (MARINE CLIMATE)
The temperatures of locations far away from large bodies of water are not affected by the presence of water (CONTINENTAL CLIMATE).
Providence, RI(MARINE CLIMATE)
The Atlantic Ocean helps to moderate the temperature of
the city.
Cooler summers and warmer
winters.
A narrow annual temperature range.
Lincoln, NE(CONTINENTAL
CLIMATE)
There is no large body of water nearby
to moderate the temperature of the
city.
Hot summers and Cold winters.
A wide annual temperature range.
Climate Change due to Prevailing Winds
Prevailing winds are generated by the convergence/divergence of air near pressure
belts and due to the Coriolis Effect.
Southern California is much “more of a marine climate” (more moderate
climate )due to the southwesterly winds blowing off the Pacific Ocean.
Storm track moving westward pick up moisture over the Great Lakes. Cities in northwestern New York
experience “lake effect” snows and rains due to this movement (more humid climate).
Climate Change due to Ocean Currents
Surface ocean temperatures are a
reflection of the amount of insolation
received.
Warm ocean currents tend to move away from the equator.
Warm ocean currents create warm, humid conditions for coastal
locations.
Cool ocean currents tend to move towards
the equator. Cool ocean currents create cool, drier conditions for coastal locations.
RT = Pg. 4
Some parts of Europe (Ireland, Iceland, England) may be more humid and a bit warmer during certain times of the year due to their presence near warm ocean currents.
The location and pathway of
ocean currents will change as the amount of
insolation received by
certain parts of the oceans
changes during Earth’s
revolution.
Climate Change due to Elevation
Elevation
Air
Tem
pera
ture
ElevationCh
ance
of
Prec
ipita
tion
Generally speaking…..
As air rises it expands and cools.
Higher elevations are less likely to be affected by greenhouse gases and the infrared radiation being absorbed by
them.
As air rises its temperature drops as does its capacity to hold water vapor. Dewpoint temperature is
reached, clouds form and precipitation follows.
Climate Change due to Mountains “The Orographic Effect”
WINDWARD LEEWARD
As prevailing winds move up the mountain:
1. Air rises, expands, and cools.2. Dewpoint is reached; clouds form
due to condensation.3. Precipitation occurs.
As prevailing winds move down the mountain:
1. Air descends, compresses, and warms.2. Air temperature is too high for
dewpoint to be reached.3. Little to no precipitation occurs.
Cool and humid Warm and arid
Climate Change due to Vegetation The vegetation of a region is determined by its climate.
Arid Humid
When the vegetation of a region is removed, the climate will change.
The destruction of this forest will cause the climate to change:
1. More insolation reaches the soil2. Temperatures rise3. Increase in greenhouse gases4. Less infiltration of water into the soil
UrbanizationDeforestation
Climate Change due to Cloud Cover
Areas that are prone to cloudy skies often experience
climatic change:
1. Less insolation strikes the earth’s surface.
2. Slight drop in temperature.
3. Clouds absorb and reflect insolation back into space.
“How come the equator is NOT the warmest spot on Earth’s surface? Where is the warmest place?”
Ecuadorian Beach, South America ~ 0˚ latitude (equator)
The equator is NOT the warmest spot on Earth due to the uplift of air from the low
pressure belt. This will lead to cloud formation and
precipitation.
The warmest place on Earth would be at the high pressure belts (30˚ N and S) where air is descending and there is a lack
of clouds.