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