barometric differences and the respective as follows: winds with their mean directions and velocities ; but traveis more slowly than the globe itself, rotating from ‘*The air above the equator being gradually heated, west to east, a current from the east is generated. This we may mention that there… … wind on all oceans ; the equatorial calms, their irregu- the surface a current of ‘cold air rushing toward the lar distribution on the northern and southern hemi- current combines with e to form the ordinary north- warmer spaces, the velocity of which depends upon the sphere, and on the three…
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