February 4, 2008

Compare the forecasted 500 mb map (given as a handout) with the actual 500 mb map for Monday morning, February 4.

Review Geostrophic wind.

Apply PGF, CF, and Newton’s laws to explain curved flow on upper air charts (gradient wind)

n Gradient winds consider the more general case of upper level air flow when the height contours are curved.

n Gradient winds move parallel to the height contours

o Because the motion follows a curved path, there must be a net force acting on the air, since the direction of motion is changing. In this case the PGF and CF are not in balance. For curved flow, the net force is inward toward the center of curvature. This inward force is called the centripetal force.

n Show Figure 6.18 from textbook. This shows the forces that act on the air as it flows around closed lows and closed highs on upper air maps. (Again the figure shows upper air isobars rather than height contours).

o Notice that for either a close upper high or a closed upper low, the net force must be directed inward in order for the air to curve.

o The same thing must happen when air flows through a trough or a ridge. It follows a curved path, so the net force must be directed in toward the center of curvature.

§ Draw a simple picture of this during lecture.

End Quiz #1 Material

Frictional Force / Wind direction on surface maps

n Frictional Force (FF)

o Air moving along the ground is slowed by friction. Thus, the frictional force always acts in the direction opposite to the wind flow.

Apply CF, PGF, and FF to explain wind direction on surface maps

n Draw a diagram with parallel isobars to show surface wind direction

o FF acts opposite to the wind direction, slowing it

o Slower wind results in a weaker CF

o The weaker CF is not able to balance the PGF as it does on upper air maps

o The result: surface winds do not blow parallel to the isobars, but are directed slightly across the isobars toward lower pressure.

§ Over land areas, a good rule of thumb is that the wind direction makes an angle of about 30° with the isobars. This angle is generally smaller over the oceans because the frictional drag (and FF) is less over water.

n Draw diagrams showing the air flow around closed surface high and surface low pressure areas and look at figure 6.20 in textbook.