CHAPTER 6 JEPPESEN KNOWLEDGE TEST GUIDE Flashcards
WHAT CAUSES VARIATION IN ALTIMETER SETTINGS BETWEEN WEATHER REPORTING PONTS
UNEQUAL HEATING OF THE EARTH’S SURFACE
THE WIND AT 5,000 FEET AGL IS SOUTHWESTERLY, WHILE THE SURFACE WIND IS SOUTHERLY. THIS IS DIFFERENCE IN DIRECTION IS PRIMARILY DUE TO
FRICTION BETWEEN THE WIND AND THE EARTH’S SURFACE
CONVECTIVE CIRCULATION PATTERNS ASSOCIATED WITH SEA BREEZES ARE CAUSED BY
COOL, DENSE AIR MOVING INLAND FROM OVER THE WATER
EVERY PHYSICAL PROCESS OF WEATHER IS ACCOMPANIED BY OR IS THE RESULT OF A
HEAT EXCHANGE
WHEN THERE IS A TEMPERATURE INVERSION, YOU WOULD EXPECT TO EXPERIENCE
AN INCREASE IN TEMPERATURE AS ALTITUDE INCREASES
THE MOST FREQUENT TYPE OF GROUND OR SURFACE-BASED TEMPERATURE INVERSION IS THAT WHICH IS PRODUCED BY
TERRESTRIAL RADIATION ON A CLEAR RELATIVELY STILL NIGHT
WHICH WEATHER CONDITIONS SHOULD BE EXPECTED BENEATH A LOW-LEVEL TEMPERATURE INVERSION LAYER WHEN THE RELATIVE HUMIDITY IS HIGH?
SMOOTH AIR, POOR VISIBILITY, FOG HAZE OR LOW CLOUDS
WHAT IS MEANT BY DEWPOINT
THE TEMPERATURE TO WHICH AIR MUST BE COOLED TO BECOME SATURATED
THE AMOUNT OF WATER VAPOR WHICH AIR CAN HOLD DEPENDS ON THE
AIR TEMPERATURE
CLOUDS, FOG, OR DEW WILL ALWAYS FORM WHEN
WATER VAPOR CONDENSES
WHAT ARE THE PROCESSES BY WHICH MOISTURE IS ADDED TO UNSATURATED AIR
EVAPORATION AND SUBLIMATION
WHICH CONDITIONS RESULT IN THE FORMATION OF FROST
THE TEMPERATURE OF THE COLLECTING SURFACE IS AT OR BELOW THE DEWPOINT OF THE ADJACENT AIR, AND THE DEWPOINT IS BELOW FREEZING
THE PRESENCE OF ICE PELLETS AT THE SURFACE IS EVIDENCE THAT THERE
IS A TEMPERATURE INVERSION WITH FREEZING RAIN AT HIGHER ALTITUDES
WHAT MEASUREMENT CAN BE USED TO DETERMINE THE STABILITY OF THE ATMOSPHERE
ACTUAL LAPSE RATE
WHAT WOULD DECREASE THE STABILITY OF AN AIR MASS
WARMING FROM BELOW
WHAT IS A CHARACTERISTIC OF STABLE AIR
STRATIFORM CLOUDS
WHEN WARM
MOIST AIR FLOWS UPSLOPE, IT
PRODUCES STRATUS TYPE CLOUDS
IF AN UNSTABLE AIR MASS IS FORCED UPWARD, WHAT TYPE CLOUDS CAN BE EXPECTED
CLOUDS WITH CONSIDERABLE VERTICAL DEVELOPMENT AND ASSOCIATED TURBULENCE
WHAT FEATURE IS ASSOCIATED WITH A TEMPERATURE INVERSION
A STABLE LAYER OF AIR
WHAT IS THE APPROXIMATE BASE OF THE CUMULUS CLOUDS IF THE SURFACE AIR TEMPERATURE AI 1,000’ MSL IS 70 DEG F AND THE DEWPOINT IS 48 DEG F
6,000’ MSL
- TEMP AND DEWPOINT CONVERGE @ 4.4DEG F / 1,000 ‘
- ESTIMATE THE CLOUD BASE BY …..
(70 DEG F - 48 DEG F) / 4.4 DEG F X 1000’ = 5,000’
BECAUSE THE SURFACE IS 1,000’ + 5,000 = 6,000’
AT APPROXIMATELY WHAT ALTITUDE ABOVE THE SURFACE WOULD THE PILOT EXPECT THE BASE OF CUMULIFORM CLOUDS IF THE SURFACE AIR TEMPERATURE IS 82 DEG F AND THE DEWPOINT IS 38 DEG F
10,000 MSL
TEMP AND DEWPOINT CONVERGE @ 4.4 DEF F / 1,000’
(82 DEG F - 38 DEG F) / 4.4 DEG F X 1000’ = 10,000’
WHAT ARE THE CHARACTERISTICS OF A MOIST, UNSTABLE AIR MASS?
CUMULIFORM CLOUDS AND SHOWERY PRECIPITATION
WHAT ARE THE CHARACTERISTICS OF UNSTABLE AIR
TURBULENCE AND GOOD SURFACE VISIBILITY
A STABLE AIR MASS IS MOST LIKELY TO HAVE WHICH CHARACTERISTIC
SMOOTH AIR
THE SUFFIX “NIMBUS” USED IN NAMING CLOUDS MEANS
A RAIN CLOUD
CLOUDS ARE DIVIDED INTO FOUR FAMILIES ACCORDING TO THEIR
HEIGHT RANGE