densityLOCALWINDSHIGHPRESSUREAREASFOUND AT 30DEGREESLATITUDEHORSELATITUDESSEABREEZETHESUNDOLDRUMSdewpointDIFFERENCESIN AIRPRESSUREcumulonimbuscloudsgreenhouseeffectbarometerslingpsychrometerprecipitationCoriolisEffectCONVECTIONCELLPOLAREASTERLIESconductionultravioletraysLANDBREEZEcirruscloudswatervaporand dustJETSTREAMLOWPRESSUREAREASAROUND THEEQUATORGLOBALWINDSrelativehumidityprevailingwesterliesanemometerFROM AREASOF HIGHPRESSURETO LOWPRESSUREdensityLOCALWINDSHIGHPRESSUREAREASFOUND AT 30DEGREESLATITUDEHORSELATITUDESSEABREEZETHESUNDOLDRUMSdewpointDIFFERENCESIN AIRPRESSUREcumulonimbuscloudsgreenhouseeffectbarometerslingpsychrometerprecipitationCoriolisEffectCONVECTIONCELLPOLAREASTERLIESconductionultravioletraysLANDBREEZEcirruscloudswatervaporand dustJETSTREAMLOWPRESSUREAREASAROUND THEEQUATORGLOBALWINDSrelativehumidityprevailingwesterliesanemometerFROM AREASOF HIGHPRESSURETO LOWPRESSURE

Wind Bingo - Call List

(Print) Use this randomly generated list as your call list when playing the game. 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.


1
B
2
I
3
N
4
I
5
G
6
G
7
N
8
B
9
G
10
O
11
O
12
I
13
N
14
O
15
B
16
B
17
O
18
N
19
I
20
B
21
G
22
O
23
I
24
B
25
G
26
G
27
I
28
N
29
O
  1. B-density
  2. I-LOCAL WINDS
  3. N-HIGH PRESSURE AREAS FOUND AT 30 DEGREES LATITUDE
  4. I-HORSE LATITUDES
  5. G-SEA BREEZE
  6. G-THE SUN
  7. N-DOLDRUMS
  8. B-dew point
  9. G-DIFFERENCES IN AIR PRESSURE
  10. O-cumulonimbus clouds
  11. O-greenhouse effect
  12. I-barometer
  13. N-sling psychrometer
  14. O-precipitation
  15. B-Coriolis Effect
  16. B-CONVECTION CELL
  17. O-POLAR EASTERLIES
  18. N-conduction
  19. I-ultraviolet rays
  20. B-LAND BREEZE
  21. G-cirrus clouds
  22. O-water vapor and dust
  23. I-JET STREAM
  24. B-LOW PRESSURE AREAS AROUND THE EQUATOR
  25. G-GLOBAL WINDS
  26. G-relative humidity
  27. I-prevailing westerlies
  28. N-anemometer
  29. O-FROM AREAS OF HIGH PRESSURE TO LOW PRESSURE