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