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Global And Local Winds

Published on Nov 18, 2015

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PRESENTATION OUTLINE

1.

H.A.T

HUMIDITY, ALTITUDE, TEMPATURE.
2.

GLOBAL WINDS

FORMED BY THE UNEVEN HEATING AND THE EARTH'S ROTATION
3.

CORIOLIS EFFECT

MOVEMENT OF LARGE AIR MASSES DUE TO THE EARTH'S ROTATION
Photo by mliu92
4.

MAJOR TYPES OF GLOBAL WINDS

POLOR EASTERLIES, PREVAILING WESTERLIES, TRADE WINDS, AND JET STREAM.
5.

DOLDRUMS

DOLDRUMS ARE ON THE EQUATOR WHERE THERE IS LITTLE TO NO WIND
Photo by vabellon
6.

HORSE LATITUDES

AT 30 DEGREES N. AND S. LITTLE WIND HERE SO THEY WOULD THROW THE HORSES OVER BOARD.
7.

SEA, LAND, BREEZES

WE HAVE THESE BREEZES BECAUSE THE LAND HEATS FASTER THAN THE WATER
8.

MOUNTAIN AND VALLY BREEZES

THIS HAPPENS BECAUSE ONE IS WARMER THAN THE OTHER ONE.

Thomas Milne