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The study of weather, climate, and atmospheric processes
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Weather is constantly changing, and it refers to the state of the atmosphere at any given time and place Climate is based on observations of weather that have been collected over many years to help describe a place or region 3
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Main Components CO2 < 1% Argon < 1% DRAW GRAPH Nitrogen – 78%
Oxygen – 21% CO2 < 1% Argon < 1% DRAW GRAPH 4
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Water vapor - source of all clouds and precipitation.
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• Ozone is a form of oxygen that combines three oxygen atoms into each molecule (O3)
• Ozone filters and absorbs harmful UV radiation by the sun OZONE VIDEO 6
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Primary Pollution: emitted directly from identifiable sources
Air pollution is airborne particles and gases that occur in concentrations large enough to endanger the health of organisms Primary Pollution: emitted directly from identifiable sources Secondary Pollution: not emitted directly into air (agriculture) 7
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Sources Primary Pollutants Carbon monoxides Nitrogen oxides
Volatile Organics Sulfur oxides Particulate matter Sources Transportation Stationary Source Fuel Combustion Industrial Processes Solid Waste 8
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The atmosphere rapidly thins as you travel away from Earth until there are too few gas molecules to detect. Pressure Changes As you increase in altitude, or travel away from Earth, pressure decreases Temperature Changes As you increase in altitude in the Troposphere the temperature decreases. 10
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The atmosphere is divided into four layers based on temperature:
Troposphere Stratosphere Mesosphere Thermosphere
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The bottom layer Temperature decreases with an increase in altitude.
Where weather occurs Tropopause: boundary of the troposphere 13
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Above the troposphere Temperature remains constant, then gradually starts to increase Contains the ozone layer Stratopause: boundary of the stratosphere
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Above the stratosphere Temperature decreases with height
Mesopause: boundary of the mesosphere 15
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Upper layer of the atmosphere
Temperature increase with height Auroras occur here Fades into space Why do you think temperatures increase in this layer?
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Factors: Heating of land Heating of water Altitude Geographic position
Cloud cover Ocean currents 18
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Water – heats up longer and will retain the heat longer
Land heats and cools more rapidly and to higher temperatures than water Water – heats up longer and will retain the heat longer 19
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The higher the altitude the lower the temperatures.
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Albedo Daylight Cloud Cover Nighttime Cloud Cover
the fraction of total radiation that is reflected by any surface. Daylight Cloud Cover Clouds reflect solar radiation back to space Temperatures are lower than on a clear day Nighttime Cloud Cover Clouds absorb radiation from land and reradiates some of it back to Earth Temperatures are higher than on a clear night 21
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As you move away from the equator the temperature drops
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Isotherms - lines on a weather map that connect points that have the same temperatures
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Temperature: measure of the amount of heat
Heat: the energy transferred from one object to another because of a direct difference in their temperature Temperature: measure of the amount of heat 24
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Heat transfer from HOT to COLD objects
Conduction The transfer of heat through matter by molecular activity Transfer by touching 25
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Convection The transfer of heat by a mass movement or circulation within a substance Radiation Travels out in all directions Solar energy reaches earth by radiation 26
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Reflection occurs when light bounces off an object. 30 % of all radiation is reflected back to space Scattering produces a larger number of rays that travel in many directions. 28
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Absorption: 50 % of the solar energy that strikes the top of the atmosphere reaches the Earth’s surface 20% is absorbed in the clouds 30% is reflected back to space 29
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Windward - is the direction upwind from the point of reference
Leeward- is the direction downwind from the point of reference 30
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Rotation: spinning of the Earth about its axis (24 hours)
Revolution : movement of Earth in its orbit around the sun ( days) The tilt of Earth’s axis causes seasons Spins on its axis at a speed of 113,000 km/hr Axis points to the North Star (Polaris) 31
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Seasons are caused by the tilting of the earth on its axis
When the Earth is tilted towards the Sun – warmer seasons When the Earth is tilted away from the Sun – cooler seasons 32
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Solstice: The length of daylight and nighttime are different
Summer Solstice: June 21 or 22 First day of summer Longest daylight hour of the year Winter Solstice: December 21 or 22 First day of winter Shortest daylight hours of the year 33
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Equinox Sun rays directly over the equator
Daylight and nighttime length are the same Autumnal Equinox September 22 or 23 First day of fall Spring Equinox March 21 or 22 First day of spring 34
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