Exam 24: The Oceans, Atmosphere, and Climatic Effects
Exam 1: Patterns of Motion and Equilibrium94 Questions
Exam 2: Newtons Laws of Motion109 Questions
Exam 3: Momentum and Energy128 Questions
Exam 4: Gravity, Projectiles, and Satellites114 Questions
Exam 5: Fluid Mechanics120 Questions
Exam 6: Thermal Energy and Thermodynamics100 Questions
Exam 7: Heat Transfer and Change of Phase115 Questions
Exam 8: Static and Current Electricity144 Questions
Exam 9: Magnetism and Electromagnetic Induction105 Questions
Exam 10: Waves and Sound120 Questions
Exam 11: Light146 Questions
Exam 12: Atoms and the Periodic Table128 Questions
Exam 13: The Atomic Nucleus and Radioactivity124 Questions
Exam 14: Elements of Chemistry49 Questions
Exam 15: How Atoms Bond and Molecules Attract150 Questions
Exam 16: Mixtures141 Questions
Exam 17: How Chemicals React118 Questions
Exam 18: Two Classes of Chemical Reactions182 Questions
Exam 19: Organic Compounds98 Questions
Exam 20: Rocks and Minerals170 Questions
Exam 21: Plate Tectonics and Earths Interior175 Questions
Exam 22: Shaping Earths Surface175 Questions
Exam 23: Geologic Timereading the Rock Record145 Questions
Exam 24: The Oceans, Atmosphere, and Climatic Effects172 Questions
Exam 25: Driving Forces of Weather145 Questions
Exam 26: The Solar System87 Questions
Exam 27: Stars and Galaxies84 Questions
Exam 28: The Structure of Space and Time55 Questions
Exam 29: Prologue: the Nature of Science22 Questions
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What is the polar front and how does it influence the development of the polar jet stream?
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The polar front is where cool, polar air meets warm, tropical air. The temperature difference between these two air masses creates a steep temperature and pressure gradient that intensifies high altitude wind speeds. The polar jet is strongest during the winter as the polar front migrates to lower latitudes. In summer, the jet stream is weaker as the polar front migrates to higher latitudes.
Temperature increases with altitude in the
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The extremely hot temperature of the thermosphere has very little significance because
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In the Northern Hemisphere, air rushing into a low-pressure region
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Going from continental land toward the deep ocean basin, the continental margin consists of the
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A strong temperature gradient contributes to steep pressure gradients and this can create very strong
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Fresh water enters the ocean by runoff from stream and rivers,
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The atmosphere is divided into several layers. The troposphere is the
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Compared with equatorial open ocean waters, open ocean water in the northern Pacific
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