Summary: Winds on Upper-Level Charts

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<strong>Summary</strong>: <strong>Winds</strong> on Surface Maps

L

PGF

wind

CF

H

Basically the same deal at the ground, but......because of friction,

the winds cross the isobars towards lower pressure.

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<strong>Summary</strong>: <strong>Winds</strong> on Surface Maps L PGF wind CF H Basically the same deal at the ground, but......because of friction, the winds cross the isobars towards lower pressure.

.....so maybe something like this L schematic winds on a surface map, converging towards low pressure

Page 1 and 2: Summary: W
Page 3 and 4: Summary: W
Page 5 and 6: Which point has the bigger wind
Page 7 and 8: Which point has the bigger wind PGF
Page 9 and 10: Which point has the bigger wind PGF
Page 11: Summary: W
Page 15 and 16: Schematic showing winds in balance
Page 17 and 18: Surface Convergence and Rising Air
Page 19 and 20: As air converges into a low center,

Summary: Winds on Upper-Level Charts

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