WEATHER THEORY Flashcards

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1
Q

THIN VAIL OF ATMOSPHERE EXTENDING FROM THE SURFACE TO 7 MILES OUT

A

TROPOSPHERE

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2
Q

TROPOSPHERE

A

WEATHER OCCURS HERE

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3
Q

AIR PRESSURE DECREASES

A

WITH ALTITUDE

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4
Q

AIR PRESSURE DECREASES

A

WITH ALTITUDE

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5
Q

LESS DENSE AIR EQUALS

A

DECREASED PERFORMANCE

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6
Q

DEWPOINT

A

THE TEMP TO WHICH AIR MUST BE COOL TO BECOME SATURATED

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7
Q

WHICH STAGE OF THUNDERSTORM IS CHARACTERIZED BY DOWNDRAFT?

A

DISSIPATING

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8
Q

WHAT MAY CREATE DOWNDRAFTS THAT AFFECT UAS PERFORMANCE?

A

WATER AND VEGITATION, BECAUSE THEY ABSORB WARM AIR AND CREATE COOL AREAS

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9
Q

THUNDERSTORMS REACH THEIR GREATEST INTENSITY DURING THE

A

MATURE STAGE

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10
Q

WHAT CLOUDS INDICATE CONVECTIVE TURBULANCE

A

TOWERING CUMULUS CLOUDS, THEY ARE UNSTABLE RISING AIR. UPWARD MOTION (CONVECTION) IS ACCOMPANIED BY SIGNIFICANT TURBULANCE

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10
Q

WHAT CLOUDS INDICATE CONVECTIVE TURBULANCE

A

TOWERING CUMULUS CLOUDS, THEY ARE UNSTABLE RISING AIR. UPWARD MOTION (CONVECTION) IS ACCOMPANIED BY SIGNIFICANT TURBULANCE

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11
Q

SQUALL LINE

A

NONFRONTAL NARROW BAND OF ACTIVE THUNDERSTOMRS THAT OFTEN DEVELOP AHEAD OF A COLD FRONT

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12
Q

SQUALL LINE

A

NONFRONTAL NARROW BAND OF ACTIVE THUNDERSTOMRS THAT OFTEN DEVELOP AHEAD OF A COLD FRONT

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13
Q

ONE WEATHER PHENOMENON WHICH WILL ALWAYS OCCUR WHEN A FRONT PASSES IS A CHANGE IN THE

A

WIND DIRECTION

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14
Q

ONE OF THE MOST EASILY RECOGNIZED DISCONTINUITIES ACROSS A FRONT IS

A

CHANGE OF TEMP

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15
Q

CONVECTIVE CIRCULATION PATTERNS ASSOCIATED WITH SEA BREAZES ARE CAUSED BY

A

COOL DENSE AIR MOVING INLAND FROM OVER THE WATER

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15
Q

CONVECTIVE CIRCULATION PATTERNS ASSOCIATED WITH SEA BREAZES ARE CAUSED BY

A

COOL DENSE AIR MOVING INLAND FROM OVER THE WATER

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16
Q

WHAT FEATURE IS NORMALLY ASSCOCIATED WITH THE CUMULUS STAGE OF A THUNDERSTORM

A

CONTINOUS UPDRAFT

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17
Q

WHAT FEATURE IS NORMALLY ASSCOCIATED WITH THE CUMULUS STAGE OF A THUNDERSTORM

A

CONTINOUS UPDRAFT

18
Q

DEVELOPMENT OF THERMALS DEPENDS UPON

A

SOLAR HEATING

19
Q

DEW, FOG, CLOUDS FORM WHEN

A

WATER VAPOR CONDENSES, AKA WHEN TEMP AND DEW POINT CONVERGE

19
Q

DEW, FOG, CLOUDS FORM WHEN

A

WATER VAPOR CONDENSES, AKA WHEN TEMP AND DEW POINT CONVERGE

20
Q

WHAT ARE THE PROCESSES BY WHICH MOISTURE IS ADDED TO UNSATURATED AIR

A

EVAPORATION AND SUBLIMATION

21
Q

CUMULONIMBUS FORMATION

A

LIFTING ACTION, AND UNSTABLE MOIST AIR

21
Q

CUMULONIMBUS FORMATION

A

LIFTING ACTION, AND UNSTABLE MOIST AIR

22
Q

EVERY PHYSICAL PROCSS OF WEATHER IS ACCOMPANIED BY

A

HEAT EXCHANGE

23
Q

BOUNDARY BETWEEN 2 DIF AIR MASSES IS REFFERED TO A

A

FRONT

23
Q

BOUNDARY BETWEEN 2 DIF AIR MASSES IS REFFERED TO A

A

FRONT

24
Q

FROST OCCURS WHEN THE SURFACE IS AT OR BELOW THE DEWPOINT OF THE ADJACENT AIR

A

AND THE DEWPOINT IS BELOW FREEZING

25
Q

LENTICULAR CLOUDS CAUSE

A

HIGH WINDS AND TURBULANCE

26
Q

INFLIGHT ICING REQUIRES

A

VISIBLE MOISTURE

27
Q

INFLIGHT ICING REQUIRES

A

VISIBLE MOISTURE

28
Q

THE AMOUNT OF WATER VAPOR WHICH AIR CAN HOLD IS DEPENDENT ON

A

AIR TEMP

29
Q

NIMBUS

A

RAIN CLOUD

30
Q

DENSITY ALTITUDE

A

MEASURE OF ATMOSPHERIC DENSITY IN TERMS OF ALTITUDE UNDER STANDARD CONDITIONS

30
Q

DENSITY ALTITUDE

A

MEASURE OF ATMOSPHERIC DENSITY IN TERMS OF ALTITUDE UNDER STANDARD CONDITIONS

31
Q

STANDARD ATMOSPHERIC CONDITIONS AT SEA LEVEL

A

59 F AND 29.92”Hg mercury (pressure)

32
Q

true altitude

A

is msl

33
Q

absolute altitude is

A

agl

34
Q

standard datum plane

A

where the standard pressure line is

35
Q

pressure altitude

A

height above the standard datum plane

36
Q

when conditions are standard

A

pressure altitude and density altitude are equal

37
Q

density altitude

A

pressure altitude corrected for nonstandard temp

38
Q

barometric pressure descreases by approx 1’Hg per 1000 ft

A
39
Q

high density altitude describes low density air

A
39
Q

high density altitude describes low density air

A
40
Q

high density altitude describes

A

low density air, which you should expect reduced performance and shorter battery life