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The Atmosphere: Structure and Temperature What is Meteorology?  The study of weather, climate, and atmospheric processes How Does Weather differ from Climate?   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 Composition of the Atmosphere  Main Components Nitrogen – 78%  Oxygen – 21%  CO2 < 1%  Argon < 1%  What is the significance of Water Vapor?  Water vapor - source of all clouds and precipitation. Ozone 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 • Human Influences and Primary Pollutants    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 Pollutions: not emitted directly into air (agriculture) Primary Pollutants and Sources  Primary Pollutants      Carbon monoxides Nitrogen oxides Volatile Organics Sulfur oxides Particulate matter Sources     Transportation Stationary Source Fuel Combustion Industrial Processes Solid Waste Pressure and Temperature Changes   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. Layers of the Atmosphere  The Troposphere - the bottom layer     Temperature decreases with an increase in altitude. Where weather occurs Tropopause: boundary of the troposphere The Stratosphere     Above the troposphere Temperature remains constant, then gradually starts to increase Contains the ozone layer Stratopause: boundary of the stratosphere  The Mesosphere     Above the stratosphere Temperature decreases with height Mesopause: boundary of the mesosphere The Thermosphere: Upper layer of the atmosphere  Temperature increase with height   Auroras occur here Fades into space Heating the Atmosphere Heat: the energy transferred from one object to another because of a direct difference in their temperature  Temperature: measure of the amount of heat  Ways Heat Can be Transferred  Heat transfer from HOT to COLD objects  Conduction The transfer of heat through matter by molecular activity  Transfer by touching   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  What Happens to Solar Radiation? Reflection vs. Scattering  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.  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  Why Do Temperatures Vary?  Factors: Heating of land  Heating of water  Altitude  Geographic position  Cloud cover  Ocean currents  Land and Water Temperatures Land heats and cools more rapidly and to higher temperatures than water  Water – heats up longer and will retain the heat longer  Albedo 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 World Distribution and Temperatures Isotherms - lines on a weather map that connect points that have the same temperatures
 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                            