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General Circulation of the Atmosphere
Current Weather/Dorian Update Finish Temperature Wind Essentials Idealized Global Circulation Seasonal and Regional Modification For Monday: Read Chapter 5: pp Reminder: Exam I on Friday (9/13)! Review Sheet is posted on AsUlearn.
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Discussion Where are the coldest places in the world in January? Why?
Where are the coldest places in the world in July? Why? What locations have the greatest Annual Temperature Range?
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Chapter 4, Figure 4.29 Labeled
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Coldest Village on Earth
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Chapter 4, Figure 4.30 Labeled
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Chapter 4, Figure 4.31 Labeled
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Chapter 4, Figure 4.32 Labeled
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What is Wind?
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Pressure Gradient Figure 6.7
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Coriolis Force Chapter 5, Figure 5.8 Labeled
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Coriolis Force Figure 6.9
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Chapter 5, Figure 5.9 Labeled
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Energy Budget by Latitude
Figure 4.13
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Idealized Global Circulation Model
ITCZ – Inter-Tropical Convergence Zone STHP – Sub-Tropical High Pressure SPLP – Sub-Polar Low Pressure PHP – Polar High Pressure
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Seasonal Patterns Location of the sun’s noon-time vertical rays (i.e., where the sun is directly overhead) helps to control the position of the ITCZ Northern Hemisphere summer, ITCZ and all of the wind and pressure belts migrate to the north North Hemisphere winter, ITCZ and all of the wind and pressure belts migrate to the south
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Chapter 5, Unnumbered Figure 1, Page 130 Labeled
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Chapter 5, Unnumbered Figure 1, Page 131 Labeled
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General Atmospheric Circulation
Figure 6.12
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General Atmospheric Circulation
Figure 6.12
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Global Barometric Pressure
Figure 6.10
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Global Barometric Pressure
Figure 6.10
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June–July ITCZ Figure 6.11
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Rossby Waves Giant meanders in upper-level wind patterns: can range from small to large (zonal to meridional flow) Figure 6.16
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Location of Polar Front and Sub-Polar Low Pressure
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March 13, 1993
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Chapter 5, Figure 5.19 Labeled
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Chapter 5, Figure 5.18 Labeled
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Monsoonal Winds Figure 6.20
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Major Ocean Currents Figure 6.21
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