Transcript Climate
Bell Quiz
1. The Earth has seasons because it
A) Is closer to the sun in the summer than
the winter.
B) Has a tilted axis
C) Has a moon
D) Has chemicals that cause the air to warm
or cool depending upon what time of the
year it is.
2. What is the angle of the tilt of the Earth?
A) 35˚
B) 23.5 ˚
C) 15.5 ˚
D) 55.3 ˚
3. The earth is closest to the sun when?
A) Spring
B) Summer
C) Fall
D) Winter
4. The longest day of the year occurs
when?
A) Spring
B) Summer
C) Fall
D) Winter
5. Why do we have daylight savings?
A) Phases of the moon
B) Orbit around the sun
C) Someone suggested the idea
D) International time clocks don’t match
Climate
Transfer of heat
Radiation
Conduction
Convection
Conduction – Transfer of heat through
direct contact
Example Lizard sitting on a rock
Metal/plastic plate demo - They are the same
temperature, but the metal plate feels colder because it is
transferring heat from your hand through conduction.
Convection – Transfer of
heat through the movement
of a fluid (liquid or gas)
Examples : blowing on your
food to cool it down,
convectional oven, sea
breezes
Convection currents – warm
air rises and cools air sinks
Reasons for climate change
Latitude
Earth on an Axis
Topography
Latitude
Affects the amounts of solar radiation per
unit area. Earth is tilted on an axis. 23.5˚
Angle of insolation : Angle at which the
sun’s radiation hits earth.
link
Earth on an axis: 23.5˚
Causes the seasons; tilt of the earth.
Summer solstice
June 22-23 – N Hemisphere tilted toward
the sun.
Receives the most direct sun
Warm temps even though we are furthest
away from the sun
Longest day of the year
September Equinox (autumn)
September 22-23
Equator faces the sun directly
All areas of the earth experience 12 hours
of daylight and 12 hours of darknesss
Winter Solstice
December 22-23
Southern Hemisphere tilted toward the sun
Earth is closest to the sun, but Northern
half is cold; less solar radiation
Shortest day of the year
March Equinox (Spring)
March 20-21
Solar radiation equal in both hemispheres
link
Love, Stargirl
Daylight Savings
Ben Franklin - link
States not observed – Hawaii, Arizona
Allows longer daylight in the summer
Topography
Near Water – specific heat
Rain Shadow
1. Tropical
High Temperature and Rainfall
Places near the equator
2. Dry Climate
30% of crust
Vegetation and rainfall scarce
Deserts
3. Mild
Humid subtropical, marine west coast,
Mediterranean
4. Continental
Midwest, great lakes, sub arctic
5. Polar
Cold, Arctic, Antarctic
6. High Elevation
High Mountains
Andes, Himalayas
Lung Adjustments
Microclimates
Localized climate that differs from the
main regional climate
North Side vs. South Side of the building
Climate Change
Ice Age
Natural Causes
Human Impact
ICE AGE
Global cooling –
Earth’s cycles back and forth from ice
ages to warm climate every 10,000 years.
Natural Causes
Orbit Changes
Earth’s wobble
Solar activity
Volcanoes
Orbital Changes
Wobble – every
21,000-100,000
years reverses
seasons
Milankovitch
theory
Volcanoes
Human Impact
CO2 – fossil fuels
Urbanization
Deforestation
Greenhouse effect
Natural heating of the earth’s surface
caused by atmospheric gases.
Radiation is trapped in atmosphere
increasing temperature overall on Earth.
Global Warming
Trend in the rise of global temperatures
Nature vs. nuture
Ozone Depletion
O3 – is being
depleted by
CFC’s which
cause more
radiation to
enter the
atmosphere.
Ozone Hole
Measuring climate change
1. Fossil Record
2. Ice Cores
3. Sea Floor Sediments
4. Tree Rings
Fossil Record
Fossils found in Antarctica indicating once
was a warmer climate
Ice Cores
Measures the concentration of gases in
the ice.
Sea Floor Sediments
Concentration of O18 in the shells of
microorganisms
Tree Rings
Ring Width
measured
Wet years have
larger rings
whereas dry years
the rings are closer
together.
Oxygen Bar
Montreal Protocol
Aerosol Cans