controlled environment, cannot tell you ake, so you can imagine ties t confront meteorologists o predict sucions in a spinning, windy, large-scale world.

    because  from tributed, differences inair pressure arise on t. Air can’t abide t rusrying to equalizetrying to keep to areas of lo; tank—and tently tpressured air s to get someplace else), and ter ter the wind blows.

    Incidentally,  t accumulate, groially, so a  ten times stronger tty miles an  a imes stronger—and  mucructive.

    Introduce several million tons of air to tor effect and t can be exceedinglyenergetic. A tropical y-four ion like Britain or France uses in a year.

    tmospo seek equilibrium  suspected by Edmonded upon in teentury by on George  rising and falling columns of air tended toproduce “cells” (kno in ter all, Englised a linkbetions of air t give us our trade tecave-Gaspard de Coriolis, ails of teractions in 1835, andt t. (Coriolis’s otinction at to introduceercoolers, ly.) t a brisk1,041 miles an  tor, toe slopes offconsiderably, to about 600 miles an ance. t . If you are on tor tocarry you quite a distance—about 40,000 kilometers—to get you back to t. If youstand beside travel only a fe to complete arevolution, yet in bot takes ty-four o get you back to where you began.

    t follo t to tor ter you must be spinning.

    t explains o tance, seem to curve to t in to t in t. tandard o envision to imagine yourself at ter of a large carousel and tossing a ball tosomeone positioned o