WEATHER THEORY Flashcards
THIN VAIL OF ATMOSPHERE EXTENDING FROM THE SURFACE TO 7 MILES OUT
TROPOSPHERE
TROPOSPHERE
WEATHER OCCURS HERE
AIR PRESSURE DECREASES
WITH ALTITUDE
AIR PRESSURE DECREASES
WITH ALTITUDE
LESS DENSE AIR EQUALS
DECREASED PERFORMANCE
DEWPOINT
THE TEMP TO WHICH AIR MUST BE COOL TO BECOME SATURATED
WHICH STAGE OF THUNDERSTORM IS CHARACTERIZED BY DOWNDRAFT?
DISSIPATING
WHAT MAY CREATE DOWNDRAFTS THAT AFFECT UAS PERFORMANCE?
WATER AND VEGITATION, BECAUSE THEY ABSORB WARM AIR AND CREATE COOL AREAS
THUNDERSTORMS REACH THEIR GREATEST INTENSITY DURING THE
MATURE STAGE
WHAT CLOUDS INDICATE CONVECTIVE TURBULANCE
TOWERING CUMULUS CLOUDS, THEY ARE UNSTABLE RISING AIR. UPWARD MOTION (CONVECTION) IS ACCOMPANIED BY SIGNIFICANT TURBULANCE
WHAT CLOUDS INDICATE CONVECTIVE TURBULANCE
TOWERING CUMULUS CLOUDS, THEY ARE UNSTABLE RISING AIR. UPWARD MOTION (CONVECTION) IS ACCOMPANIED BY SIGNIFICANT TURBULANCE
SQUALL LINE
NONFRONTAL NARROW BAND OF ACTIVE THUNDERSTOMRS THAT OFTEN DEVELOP AHEAD OF A COLD FRONT
SQUALL LINE
NONFRONTAL NARROW BAND OF ACTIVE THUNDERSTOMRS THAT OFTEN DEVELOP AHEAD OF A COLD FRONT
ONE WEATHER PHENOMENON WHICH WILL ALWAYS OCCUR WHEN A FRONT PASSES IS A CHANGE IN THE
WIND DIRECTION
ONE OF THE MOST EASILY RECOGNIZED DISCONTINUITIES ACROSS A FRONT IS
CHANGE OF TEMP
CONVECTIVE CIRCULATION PATTERNS ASSOCIATED WITH SEA BREAZES ARE CAUSED BY
COOL DENSE AIR MOVING INLAND FROM OVER THE WATER
CONVECTIVE CIRCULATION PATTERNS ASSOCIATED WITH SEA BREAZES ARE CAUSED BY
COOL DENSE AIR MOVING INLAND FROM OVER THE WATER
WHAT FEATURE IS NORMALLY ASSCOCIATED WITH THE CUMULUS STAGE OF A THUNDERSTORM
CONTINOUS UPDRAFT