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Wednesday/Thursday 1/221/23/2014 Atmosphere and Weather Unit Agenda: Layers of the Atmosphere *Notes: Layers of the Atmosphere Biogeochemical Cycles Carbon Cycle Nitrogen Cycle Water Cycle *Goldilocks Lab and Write up due Friday 1/17/2014 for 40 Points Weather So the FINAL EXAM in May will cover… Biogeochemical Processes Weather Ecology Atmospheric Processes – The Water (Hydrological) Cycle • Moisture: – Most water in atmosphere comes from oceans – Most precipitation falling over land its way back to oceans – 2/3 of the water in the oceans evaporates back to the atmosphere in the Water Cycle Atmospheric Processes – The Water (Hydrological) Cycle • Heat: – Oceans hold & are a source of heat – Ocean currents transfer heat toward the North & South Poles (convection). – This transfer of heat toward the poles contributes to different types of weather & climates. Energy Heat Transfer Most of the energy that reaches Earth comes from the sun (solar energy) What happens to the solar energy when it reaches Earth? ◦ First reaches Earth’s atmosphere Some gets absorbed by gases, such as ozone (O3) & water vapor (H2O) greenhouse gases ◦ Some gets reflected space by surface ◦ Some gets absorbed masses or back to clouds & Earth’s by land oceans Energy Heat Transfer Processes • Solar/heat energy gets transferred between Earth’s surface & atmosphere by – Conduction – Convection – Radiation Energy Heat Transfer Processes Conduction – process by which heat energy is transmitted through direct contact with neighboring molecules ◦ Air & water are poor heat energy conductors of ◦ Most conduction occurs at surface During the day, solar the Earth’s Heat energy is then the the surface Earth’s energy heats surface conducted to molecules of air just above Energy Heat Transfer Processes • Convection – process by which heat energy is transmitted by transporting groups of molecules from one place to another – Can occur in fluids, such as air & water Energy Heat Transfer Processes • Convection – – Which molecules are moving are more spread apart? air? faster & Hot air or cold • Heated molecules move faster & more spread apart compared to less heated (cooler) molecules • Warmer air masses are therefore less dense (less molecules in a space) • Therefore, warmer air masses rise • Cooler air masses are more dense (more molecules in a space), so they fall back toward the Earth’s surface Energy Heat Transfer Processes • Convection – – Cycle of rising warm air & sinking cold air – convection cell • Distribute heat & from poles moisture equator toward the • Create large wind patterns • Produce & transport large storm systems (I.e, hurricanes) Energy Heat Transfer Processes Radiation – process by which heat energy is transferred by electromagnetic waves ◦ What are the forms of electromagnetic radiation? ◦ Which form of EM radiation has the longest wavelength? ◦ Which form of EM radiation has the shortest wavelength? ◦ What does the wavelength of radiation tell us about a form of radiation? ◦ Which form of EM radiation has more energy, radio waves or gamma rays? ◦ What form of EM radiation from the sun affects humans the most? ◦ Is this the only form of EM radiation that reaches the Earth’s surface?