Chapter 18 Vocabulary Flashcards
Pressure tendency
a low moving toward or away by falling or rising pressure
wind
horizontal movement of air due to pressure differences caused by solar heating
Pressure Gradient Force (PGF)
has both magnitude and direction and is the driving force of wind. Measured on weather maps and shown as isobars
steep gradient
high speed & closely packed isobars
Coriolis effect
freely moving objects turn to the right of their apparent direction of motion in the northern hemisphere and to the left in the southern hemisphere; a product of the rotating earth
jet stream wind effects
geostrophic winds paralleling isobars several kilometers above the earth. Jet stream is a fast moving river of air from 75-150 mph moving west to east. One is situated over the polar front and sometimes splits into two jet streams, a northern and a southern branch
cyclones
low pressure centers; winds blow inward and counterclockwise around a low pile up and rise (convergence) and diverge at high altitude and perpetuate itself. If upper air divergence increases the low may intensify
anticyclones
high pressure with surface divergence; balanced by high altitude convergence and produces adiabatic heating of the air and tendency to clear conditions
List the five basic assumptions
- hot air rises; 2. pressure flows from high to low; 3. warm air can hold more moisture than cold air; 4. pressure decreases in the atmosphere as altitude increases; 5. Coriolis effect
sea breeze
develops as air over land heats and rises, pulling in cooler air from the water beginning about noon