Climate.

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Presentation transcript:

Climate

What is Climate? Yearlong average of weather patterns over an area

What are greenhouse gases? These are gases that allow for our environment to be suitable to live The gases include: Water vapor, Carbon dioxide, Methane and Nitrogen

Human Impact on Greenhouse Gases Brainstorm:

“THINK AIR MASS LOCATIONS” Koppen Classification System Uses mean monthly and annual values of amounts of moisture and temperature “THINK AIR MASS LOCATIONS”

Köppen Climate Classification System Most commonly used system Uses mean monthly and annual values of temperature and precipitation Five Principal Groups Humid Tropical Humid Mid-Latitude Dry Highland Polar

a little rain and a huge daily temperature range ( ) Group Description Humid Tropical high temperatures year round and for their large amount of year round rain. Humid Mid- Latitude land/water differences play a large part. These climates have warm,dry summers and cool, wet winters. Dry a little rain and a huge daily temperature range ( ) Highland Total precipitation is not very high and seasonal temperatures vary widely. Polar These climates are part of areas where permanent ice

Group Location Example Humid Tropical Humid Mid- Latitude Dry Highland Polar

Factors that Affect Climate Latitude Elevation Topography Water Bodies Global Winds Vegetation

Factor #1: Latitude As latitude increases, the intensity of solar energy decreases Three Zones Tropical Temperate Polar

The Zones Zone 1: Tropical Zone Region between the Tropic of Cancer (23.5ºN) and the Tropic of Capricorn (23.5ºS) Warm Year Round

Zone 3: Polar Zone Zone 2: Temperate Zone Region between 23.5ºN/S and 66.5ºN/s of the equator Hot Summers Cold Winters Zone 3: Polar Zone Region from 66.5ºN/S of the equator to the poles Very cold temperature year round

Factor #2: Elevation Higher the elevation is, the colder the climate Elevation determines amount of precipitation it receive

Factor #3: Topography Land features affect amount of precipitation that falls over an area Mountains cause a rain shadow event One side has cool, wet air One side has warm, dry air

Factor #4: Water Bodies Large bodies of water (lakes & oceans) have an important effect on the temperature of an area. Temperature of the water body influences the temperature of the air above.

Factor #5: Global Winds Winds distribute heat and moisture around the Earth Warm air moves to the poles Cold air moves to the equator

Factor #6: Vegetation Affects both temperature and precipitation Influence how much of the sun’s energy is absorbed and how quickly it is released Precipitation When plants release water vapor from its leaves into the air (transpiration)

CLIMOGRAPHS what scientists create to show a particular location's average temperature and precipitation during the year.

CLIMOGRAPHS

Natural Processes that Change Climate Volcanic Eruption Ocean Circulation Solar Activity Earth’s Motions

Volcanic Eruption The presence of volcanic ash, dust and aerosols in the air increase the amount of solar radiation that is reflected back into space. Causes Earth’s lower atmosphere to cool

Solar Activity Formation of sunspots appear to correspond with warm periods in Europe and North America 11 year cycle

CO2 Fluctuations Changes in plant growth rates CO2 levels fall during the growing season and rise in the winter

Carbon “Sinks” CO2 is absorbed by the ocean and forms carbonic acid. Decrease in the ocean’s pH levels in the ocean. Coral Reefs: High levels of CO2 negatively affects corals photosynthesis 50% of coral reefs have been destroyed Ocean Acidification

Human Impact on Climate Change Burning Fossil Fuels Humans have added more greenhouse gases to the atmosphere in the past 200 years by burning fossil fuels Major Gases: Water Vapor and Carbon Dioxide

Human Impact on Climate Change Deforestation Plants remove carbon dioxide from the atmosphere during photosynthesis When large areas of vegetation are cleared, carbon dioxide, a greenhouse gas, remains in the atmosphere

Human Impact on Climate Change The Greenhouse Effect is a natural warming of both Earth’s lower atmosphere and surface Makes life as we know it possible Burning fossil fuels and deforestation by humans have affected this process in the last 200 years

Climate Change As a result of increases in Carbon Dioxide (CO2) as well as other greenhouse gases, global temperatures have increased Affects weather and climates

Hottest Years Since 1980, the Earth has had 19 of its 20 hottest years on record 2010 2005 2009 2007 2006 1998 2002 2003 2001 1997

Antarctica Melting If all of the ice in the glaciers of Antarctica melts, the oceans will rise