JET STREAM LOW PRESSURE LAND BREEZE FROM AREAS OF HIGH PRESSURE TO LOW PRESSURE HIGH PRESSURE AREAS FOUND AT 30 DEGREES LATITUDE DIFFERENCES IN AIR PRESSURE THE SUN WESTERLIES LIGHT TO NO WINDS TO BLOW LOW PRESSURE AREAS AROUND THE EQUATOR CONVECTION CELL SEA BREEZE HORSE LATITUDES DOLDRUMS Coriolis Effect POLAR EASTERLIES GLOBAL WINDS FORM BETWEEN HOT AND COLD AIR MASSES MOUNTAIN BREEZE UNEQUALLY HEATS THE EARTH VALLEY BREEZE STRONG WINDS BLOW LOCAL WINDS HIGH PRESSURE JET STREAM LOW PRESSURE LAND BREEZE FROM AREAS OF HIGH PRESSURE TO LOW PRESSURE HIGH PRESSURE AREAS FOUND AT 30 DEGREES LATITUDE DIFFERENCES IN AIR PRESSURE THE SUN WESTERLIES LIGHT TO NO WINDS TO BLOW LOW PRESSURE AREAS AROUND THE EQUATOR CONVECTION CELL SEA BREEZE HORSE LATITUDES DOLDRUMS Coriolis Effect POLAR EASTERLIES GLOBAL WINDS FORM BETWEEN HOT AND COLD AIR MASSES MOUNTAIN BREEZE UNEQUALLY HEATS THE EARTH VALLEY BREEZE STRONG WINDS BLOW LOCAL WINDS HIGH PRESSURE
(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.
JET STREAM
LOW PRESSURE
LAND BREEZE
FROM AREAS OF HIGH PRESSURE TO LOW PRESSURE
HIGH PRESSURE AREAS FOUND AT 30 DEGREES LATITUDE
DIFFERENCES IN AIR PRESSURE
THE
SUN
WESTERLIES
LIGHT TO NO WINDS TO BLOW
LOW PRESSURE AREAS AROUND THE EQUATOR
CONVECTION
CELL
SEA BREEZE
HORSE LATITUDES
DOLDRUMS
Coriolis Effect
POLAR EASTERLIES
GLOBAL WINDS
FORM BETWEEN HOT AND COLD AIR MASSES
MOUNTAIN BREEZE
UNEQUALLY HEATS THE EARTH
VALLEY BREEZE
STRONG WINDS BLOW
LOCAL WINDS
HIGH PRESSURE