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Climate and Climate Change
Chapter 25
Temperature and Precipitation
• Climates describe by average
temperature and precipitation
• Yearly average temperature range
• Precipitation - months with greatest
amount focused on
Global Wind Patterns
• Solar energy (or lack of) cause pooling of
either warm, less dense air (equator) or cold
dense air w/ high pressure (poles)
• These differences in air pressure create
winds
• Air close to the equator (the doldrums) air
rises and cools and water vapor condenses
causing greater amounts of precipitation
• The amount fof precipitation decreases then,
as you increase in latitude
Climates and Latitude
• 20 - 30 degrees - subtropical highs (air
sinks, warms and dries) with little
precip.
• 45-60 degrees - mid latitudes - polar air
and warm tropical air meet, causing
greater precip.
• Above 60 degrees - cold and dry
Heat Absorption
• Land heats faster than water (which is moving
and mixing constantly, changing the
temperature)
• Specific Heat is higher for water - meaning
that it takes greater energy to raise 1 g of
water 1 degree - meaning too, that the water
will hold onto heat a longer time.
• This difference in land and water
heating/cooling rates also contributes to
precip. And winds
El Nino Oscillation (ENSO)
• Cycle of changing wind and water-current
patterns in the Pacific
• El Nino the warm water phase of the cycle
causes temperatures along the west coast of
South America to rise, causing the interaction
of the ocean and atmosphere to change
• Typhoons, cyclones, and floods are common
during the El Nino cycle
• Cool water phase is called El Nina
Special Circumstances
• Rain Shadows
– Air that moves up a mountain slope
condenses as it cools, causing
precipitation
– As that same air moves over the mountain
range and moves down along its slope the
air compresses and warms, causing dry
hot conditions
– Deserts
Climate Zones
Tropical
Climates

High Temp,
high rainfall

Equator

Rainforest,
desert,
Savanna
Middle
Latitude

Moderate
0-60 degrees
Temp. range, north
varying precip. 0-60 degrees
south

Polar Climates Can have

60-80 degrees
Climate CHange
• Page 641, table 1
• Understanding Isotopes
– Atoms of the same elements that have the
same number of protons, but a different
number of neutrons
– Indicate change - temp increases, O 18
decreases, temp. decreases, O16
increases
Just the Facts

Climate Change
Plate Tectonics
Volcanic Activity

Orbital Changes
Tilt of the Earth

Human Activity
Increased Emissions
Latitude
• The higher the latitude the smaller the angle
of the sun’s rays hitting the Earth
• The smaller the angle the less solar energy
received and the lower the temperature
• Less range of temperatures influences the
amount of varying heat on the Earth, thus
changing the winds/precipition
• The longer the daylight the greater the
amount of solar energy and higher
temperatures - the equator has constant
warm temperatures due to direct sun rays

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Climate

  • 1. Climate and Climate Change Chapter 25
  • 2. Temperature and Precipitation • Climates describe by average temperature and precipitation • Yearly average temperature range • Precipitation - months with greatest amount focused on
  • 3. Global Wind Patterns • Solar energy (or lack of) cause pooling of either warm, less dense air (equator) or cold dense air w/ high pressure (poles) • These differences in air pressure create winds • Air close to the equator (the doldrums) air rises and cools and water vapor condenses causing greater amounts of precipitation • The amount fof precipitation decreases then, as you increase in latitude
  • 4. Climates and Latitude • 20 - 30 degrees - subtropical highs (air sinks, warms and dries) with little precip. • 45-60 degrees - mid latitudes - polar air and warm tropical air meet, causing greater precip. • Above 60 degrees - cold and dry
  • 5. Heat Absorption • Land heats faster than water (which is moving and mixing constantly, changing the temperature) • Specific Heat is higher for water - meaning that it takes greater energy to raise 1 g of water 1 degree - meaning too, that the water will hold onto heat a longer time. • This difference in land and water heating/cooling rates also contributes to precip. And winds
  • 6. El Nino Oscillation (ENSO) • Cycle of changing wind and water-current patterns in the Pacific • El Nino the warm water phase of the cycle causes temperatures along the west coast of South America to rise, causing the interaction of the ocean and atmosphere to change • Typhoons, cyclones, and floods are common during the El Nino cycle • Cool water phase is called El Nina
  • 7. Special Circumstances • Rain Shadows – Air that moves up a mountain slope condenses as it cools, causing precipitation – As that same air moves over the mountain range and moves down along its slope the air compresses and warms, causing dry hot conditions – Deserts
  • 8. Climate Zones Tropical Climates High Temp, high rainfall Equator Rainforest, desert, Savanna Middle Latitude Moderate 0-60 degrees Temp. range, north varying precip. 0-60 degrees south Polar Climates Can have 60-80 degrees
  • 9. Climate CHange • Page 641, table 1 • Understanding Isotopes – Atoms of the same elements that have the same number of protons, but a different number of neutrons – Indicate change - temp increases, O 18 decreases, temp. decreases, O16 increases
  • 10. Just the Facts Climate Change Plate Tectonics Volcanic Activity Orbital Changes Tilt of the Earth Human Activity Increased Emissions
  • 11. Latitude • The higher the latitude the smaller the angle of the sun’s rays hitting the Earth • The smaller the angle the less solar energy received and the lower the temperature • Less range of temperatures influences the amount of varying heat on the Earth, thus changing the winds/precipition • The longer the daylight the greater the amount of solar energy and higher temperatures - the equator has constant warm temperatures due to direct sun rays