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