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WEATHER

BY BRAYDEN CORLEY
Across
FRONT FORMED DURING THE PROCESS OF CYCLOGENESIS WHEN A COLD FRONT OVERTAKES A WARM FRONT
MASS OF COLD, DRY AIR THAT FORMS OVER LAND
HEATING FROM THE WARMER LAND CAUSES LIFTING AND CONVECTION IN THE AIR MASS
A PAIR OF AIR MASSES, NEITHER OF WHICH IS STRONG ENOUGH TO REPLACE THE OTHER
A BOUNDARY SEPARATING TWO MASSES OF AIR OF DIFFERENT DENSITIES
THE TRANSITION ZONE WHERE A COLD AIR MASS IS REPLACING A COLD AIR MASS
THE DEGREE OF HOTNESS OR COLDNESS MEASURED BY A THERMOMETER
Down
THE TRANSITION ZONE WHERE A COLD AIR MASS IS REPLACING A WARMER AIR MASS
A BALLOON USED TO MEASURE METEOROLOGICAL DATA
WHEN AIR IS FORCIBLY LIFTED UP SLOPE AS IT IS PUSHED AGAINST A MOUNTAIN
MASS OF COLD AIR THAT FORMS OVER HIGHER LATITUDES OF BOTH LAND AND SEA
THE MASS PER UNIT VOLUME OF EARTH'S ATMOSPHERE
MASS OF HOT, DRY AIR THAT FORMS ON LAND
THE UPWARD MOVING AIR IN A THUNDERSTORM
PRESSURE WITHIN THE ATMOSPHERE OF EARTH