航空气象学课后习题.pdf
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1、Thunderstorm hazards:are only encountered in the cloud口 are unlikely under the base of the cloudQ may be encountered some miles from the cloud口 are unlikely near the top of the cloudA microburst associated with a Cb cloud will normally occur from a point m dw ay up in the cloudQ near the base of the
2、 cloud口 only ahead of the surface impact point口 anywhere up to 10 miles ahead of the cloudThe cumulus stage of a TS is characterised by:口 the beginning of preciprtationD updraughts only口 stronger downdraughts than updraughts口 the anvilThe mature stage of a TS is characterised by:the anvil updraughts
3、 onlyQ the beginning of precipitation stronger downdraughts than updraughtsVertical windshear is the change of_(1)wind vector with height,and horizontalwindshear is the change of_(2)wind vector with distanceo 1 vertical 2 horizontalQ 1 horizontal 2 horizontal口 1 horizontal 2 vertical口 1 vertical 2 v
4、erticalWhen the aircraft encounters turbulence it can experience fluctuations in its indicatedairspeed Fluctuations of between 15 and 25 knots would indicate light turbulence bad turbulenceQ moderate turbulence severe turbulenceWhich of the following situations will give the most severe airframe ici
5、ng?口 stratiform clouds in the tropics口 cumuliform clouds in temperate regions口 stratiform clouds in temperate regions口 cumuliform clouds in the tropicsRain ice most commonly occurs behind a cold front below the freezing level口 behind a warm front below the freezing level口 ahead of a cold front above
6、 the freezing levelQ ahead of a warm front above the freezing levelThe ITCZ will normally reach its most northerly point of travel in:The sub-tropical highs are due to an accumulation of air at the_latitudeThe monsoon low of Asia is an important example of:Q a thermal low which forms in summer口 all
7、of the alternatives are correct口 an orographic low which forms in winter口 a tropical depression which forms in summerA cold low:口 deepens at altitude and turns into a high pressure口 weakens at altitude and turns into a high pressureQ deepens at altitude and is more intense than a warm low weakens at
8、 altitude and is less intense that a warm lowA warm occlusion occurs when theQ air ahead of the warm front is colder than the air behind the cold front air behind the cold front is colder than the air ahead of the warm front口 warm front is catching up the cold front口 air ahead of the warm front is w
9、armer than in the warm sectorThe speed of movement for a cold occlusion is:about the same as for the warm frontThe average gradient of the slope of a cold front is:D 1 50口 1 200口 1 150 1:600The average gradient of the slope of a warm front is:a 1 iso 1 200口 1:50 1:600Virga is:口 precipitation from th
10、e anvil of a Cb behind a cold frontD precipitation that doesnt reach the ground the first precipitation to reach the ground ahead of the warm front口 precipitation from St ahead of the warm frontFor an aircraft flying directly towards a warm front from the cold side,the succession ofcloud types to be
11、 expected as the front is approaches is:Ci-Cc-Ac-Ns口 Ac-Cu-Sc-Sta Ci-Cs-As-Ns口 Ci-Cs-As-AcWhat factors associated with the passage of a front would indicate an increased risk ofwindshear?_ Front speed 20 knots or more,small change in wind direction,temperature change+/-口 10俱Front speed 20 knots or m
12、ore,sharp isobar angle temperature difference across thefront+/-10 俱 Front speed 30 knots or more,temperature change+/-10建,shallow isobar angleFront speed 30 knots or more,temperature difference across the front of 5筑 or more,sharp isobar angleIf air transit is heated from below it ends to become mo
13、re口 stable口 none of the alternatives are correcto neutrally stableQ unstableAn air mass is a large volume of air with similar characteristics of:口 pressure and stability口 pressure tendency and dew pointQ temperature and humidity口 relative humidity and pressureLeast reduction in visibility is caused
14、byPrecipitation from Sc is most likely to be口 light showersQ light intermittentRain/hail showers are descnbed as moderate when the amount of precipitation is:D 2 to 10 mm per hour口 4 to 50 mm per hour口 0 5 to 4 mm per hour口 2 to 10 cm per hourPrecipitation falling from Ns is most likely to be口 moder
15、ate drizzle口 heavy hail showersQ moderate continuous rain light snow showersWhich of the following could be the precipitation falling from Cu?Moderate continuous snowQ Snow showers口 Heavy continuous rain Moderate continuous rainFrom which cloud is hail most like to fall?Drizzle is most likely to fal
16、l from:Greatest reduction in visibility is caused by:Frontal fog:is very low frontal stratus口 often forms at cold fronts rather than wam frontsQ forms when frontal rain cools down the air ahead of the front口 is advection fog in the warm sectorSteaming fog occurs in thewinter when very coki air picks
17、 up moisture from,and is heated by relatively warm waterwinter over land when warm and moist air moves in over the cold surfacearctic regions during the summer when warm air from the south moves in over the coldseatropical regions during the day when wet ground is heated by the sunWhen surface visib
18、ility is reduced to 1200 m due to water droplets in suspension,theweather is referred to as:When surface visibility is reduced to 5000 m by dust particles in suspension,the weatheris termed:Fog is defined as visibility reduced to口 1000 m or less due to water vapour in the atmosphereQ below 1000 m du
19、e to water droplets in the atmosphere口 1000 m to 2000 m due to water droplets in the atmosphere口 1000 m or above due to water droplets in the atmosphereCirriform clouds are mainly composed of:water droplets a mixture of water droplets and ice particles口 supercooled water droplets ice particlesThe tw
20、o main families of clouds are cirriform and cumuliform altoform and stratoform口 nimbus and layeredstratiform and cumuliformAltocumulus lenticularis is associated with:instabilrty through a thick layerQ mountain waves口 an area of turbulence immediately behind a mountain range口 a surface inversionThe
21、halo phenomenon is normally caused by a thin layer of stratusQ layer of cirrostratus口 layer of cirrus before a cold front thin layer of cumulusWhich of the following processes within a layer of air may lead to the building ofcumuliform clouds?Q Convection口 Subsidence口 Frontal lifting wrthin stable l
22、ayers口 RadiationA cap cloud will form:口 above a turbulence layer口 around the top of a cumulrform cloudQ because of orographic uplift in a layer with instabilityAdiabatic cooling is said to occur when a parcel of airAn ELR which is absolutely unstable is:4篌 per 1000 ftAn ELR which is absolutely stabl
23、e is口 1 per 1000 ft口 4 俱 per 1000 ft口 2 俱 per 1000 ft口 3 per 1000 ftAn ELR which is conditionally unstable is:4 仪 per 1000 ft 0 5 per 1000 ftH 2 per 1000 ft口 12 per 1000 ftThe SALR in tropical areas is less than that in temperate regions because:a large amount of latent heat is released during conde
24、nsation which reduces the rate ofcoolinga large amount of latent heat is absorbed dunng condensation which reduces the rate ofcooling口 the saturation content in the tropics is lowera small amount of latent heat is released during condensation which increases the rateof coolingWhen a parcel of air as
25、cends it willJ release latent heat when becoming saturated口 be cooled by the value of the environmental lapse rate口 cool faster if it becomes saturated口 expand and become less humki since the surrounding air is cold and dryBoth dry and saturated air will be unstable when:口 ELRDALR ELRSALR口 ELRDALRWh
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