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Published byMelinda James Modified over 9 years ago
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The Atmosphere Earth Science Mr. Barry
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Atmospheric Composition The atmosphere is mainly Oxygen (21%) and Nitrogen (78%) Other major gases include Argon, Hydrogen, Carbon Dioxide (CO 2 ) and water vapor This balance of gases is critical to life on Earth
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Key Atmospheric Gases Water Vapor – Source of clouds, major step in the water cycle – Anywhere from 0-4% of the atmosphere depending on the water cycle Carbon Dioxide – Less than 1% of the atmosphere Ozone – O 3 exists in small quantities, absorbs ultraviolet (UV) radiation from the sun
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Atmospheric Layers Characteristics of the atmosphere vary by layer as you move away from the Earth Layers of the atmosphere (bottom to top): – 1. Troposphere – 2. Stratosphere – 3. Mesosphere – 4. Thermosphere – 5. Exosphere
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Separation of Layers Each of the different layers of the atmosphere have very different characteristics They are separated by “-pauses” – Tropopause (Troposphere & Stratosphere) – Stratopause (Stratosphere & Mesosphere) – Mesopause (Mesosphere & Thermosphere) – Thermopause (Thermosphere & Exosphere)
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Temperature Variation in the Atmosphere
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Heat Transfer Heat is the energy transfer from one object to another because of a difference in temperature Temperature is a measure of the average energy of the individual atoms/molecules in a substance
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Types of Heat Transfer
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Radiation Radiation: transfer of energy through waves
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Solar Radiation & The Earth 3 results of solar radiation hitting the Earth: – 1. Energy is absorbed by an object – 2. Energy travels through an object – 3. Energy is reflected by an object
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Conduction & Convection Conduction: transfer of heat energy through a solid object – Blacksmith heating metal to change its shape Convection: transfer of heat energy through movement of a liquid or gas – Boiling Water (States of Matter Lab)
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Heat Transfer in the Atmosphere
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