DIFFERENCES IN AIR PRESSURE WESTERLIES LOW PRESSURE HIGH PRESSURE AREAS FOUND AT 30 DEGREES LATITUDE POLAR EASTERLIES MOUNTAIN BREEZE LOW PRESSURE AREAS AROUND THE EQUATOR LIGHT TO NO WINDS TO BLOW HIGH PRESSURE CONVECTION CELL DOLDRUMS VALLEY BREEZE JET STREAM LOCAL WINDS STRONG WINDS BLOW Free! THE SUN Coriolis Effect FROM AREAS OF HIGH PRESSURE TO LOW PRESSURE UNEQUALLY HEATS THE EARTH LAND BREEZE GLOBAL WINDS FORM BETWEEN HOT AND COLD AIR MASSES HORSE LATITUDES SEA BREEZE DIFFERENCES IN AIR PRESSURE WESTERLIES LOW PRESSURE HIGH PRESSURE AREAS FOUND AT 30 DEGREES LATITUDE POLAR EASTERLIES MOUNTAIN BREEZE LOW PRESSURE AREAS AROUND THE EQUATOR LIGHT TO NO WINDS TO BLOW HIGH PRESSURE CONVECTION CELL DOLDRUMS VALLEY BREEZE JET STREAM LOCAL WINDS STRONG WINDS BLOW Free! THE SUN Coriolis Effect FROM AREAS OF HIGH PRESSURE TO LOW PRESSURE UNEQUALLY HEATS THE EARTH LAND BREEZE GLOBAL WINDS FORM BETWEEN HOT AND COLD AIR MASSES HORSE LATITUDES SEA BREEZE
(Print) Use this randomly generated list as your call list when playing the game. There is no need to say the BINGO column name. Place some kind of mark (like an X, a checkmark, a dot, tally mark, etc) on each cell as you announce it, to keep track. You can also cut out each item, place them in a bag and pull words from the bag.
DIFFERENCES IN AIR PRESSURE
WESTERLIES
LOW PRESSURE
HIGH PRESSURE AREAS FOUND AT 30 DEGREES LATITUDE
POLAR EASTERLIES
MOUNTAIN BREEZE
LOW PRESSURE AREAS AROUND THE EQUATOR
LIGHT TO NO WINDS TO BLOW
HIGH PRESSURE
CONVECTION
CELL
DOLDRUMS
VALLEY BREEZE
JET STREAM
LOCAL WINDS
STRONG WINDS BLOW
Free!
THE
SUN
Coriolis Effect
FROM AREAS OF HIGH PRESSURE TO LOW PRESSURE
UNEQUALLY HEATS THE EARTH
LAND BREEZE
GLOBAL WINDS
FORM BETWEEN HOT AND COLD AIR MASSES
HORSE LATITUDES
SEA BREEZE