2_1 Flashcards
The height of the tropopause:
Will be greater in a warm air mass.
Explanation
The troposphere is the atmosphere”s first layer. Its top can be from 28,000 feet ASL at the poles to 54,000 feet ASL at the equator. In the troposphere, pressure, density and temperature decrease quickly with altitude. Most weather phenomenons occur in the troposphere, and it is the place of most of light aviation.
The troposphere top is called “tropopause.” At the tropopause. the temperature stops decreasing and is constant at about -56°C.
Because of air density, the tropopause will be higher in warm air than in cold air.
Question 02
The lower border of the mesosphere is the _______, and its upper border is the _____
Stratopause; mesopause
Explanation
The acmosphere is divided into 4 different layers. From the Earth surface, chere is Troposphere (its top is called the Tropopause), Stratosphere (its top is called che Stracopause), Mesosphere (its top is called the Mesopause) and finally. Thermosphere.
The air at the centre of a HIGH-pressure system will tend to move _____ and _____ in the direction of the low-pressure systems.
Downward; outward.
Explanation
Wind associated with high pressure is light and relatively constant. It circulates clockwise around the high pressure centre (in the Northern Hemisphere) and heads outward toward the low pressure. There is therefore a divergence in this zone. This move to the outside is compensated by a descending movement. It partially explains why precipitation is not likely in this area.
You are on final approach to an airport that has an elevation of 1,020 feet. The airport altimeter setting is 29.72 inches of mercury but you forget to calibrate your altimeter, which therefore remains at your departure airport altimeter setting of 30.09 inches of mercury. Arriving at an indicated altitude of 1,440 feet, the actual height of your aircraft above the ground is feet
50
Explanation
The altimeter is calibrated for the standard atmosphere, so it has to be set with real pressure conditions to provide pilots with the right altitude above sea level. This pressure (standardized atmospheric pressure) is the altimeter setting given, in North America, in inches of mercury.
With too high an altimeter setting, the altimeter indicates a too high altitude. Each 0.10 inches of mercury added to the altimeter setting increases the altitude on the altimeter by about 100 feet.
To determine your current altitude, remove the altimeter setting from the right altimeter setting and multiply the result by 1,000.
Here: 29.72- 30.09 = -0.37 -0.37 x 1,000 = -370 feet
The current altitude is: 1,440 - 370 = 1,070 feet ASL.
The elevation of the arrival airport is 1.020 feet. Your height over the ground is then: 1,070 - 1,020 = 50 feet.
A temperature of ISA+15 at FL290 corresponds to:
-27
Explanation
In North America, ICAO standard atmosphere is based on average winter and summer at 40° latitude. Here are the conditions:
- air is a dry gas;
- pressure at mean sea level is 29.92 inches of mercury;
- temperature at mean sea level is 15°C;
- temperature decreasing rate with altitude is 1.98°C for every 1,000 feet.
Here : T° = 15 - (29 x 1.98) + 15 = -27°C
You can also use your electronic flight calculator.
What is the definition of “relative humidity”?
What happens when you add water vapour while maintaining a constant pressure and temperature? What happens when we remove water vapour?
The amount of water vapour present in air expressed as a percentage of the amount needed for saturation at the same temperature.
Explanation
Relative humidity is the relation between water vapour in the air and the same quantity this volume of air would contain if it were saturated, keeping the same temperature and the same atmospheric pressure. The air is saturated when it reaches 100% of relative humidity, while dry air has 0% relative humidity.
This relation will change if the temperature or the pressure changes, whereas absolute humidity will not change: when an air mass is warmed up without adding any water vapour, its relative humidity decreases. The opposite happens if we cool it down. If the cooling process lasts, relative humidity reaches 100%, making the air saturated. The less the difference between temperature and dew point is, the higher the relative humidity is.
By adding water vapour while maintaining a constant pressure and temperature, relative humidity increases. The opposite is produced when we remove water vapour.
How does drizzle form?
With the condensation in stratus clouds
Explanation Drizzle (DZ) is a type of precipitation where small water droplets seem to float in the air. Drizzle usually appears in low stratus clouds. It is mostly found in coastal areas and
in high altitude valleys where there are temperature inversions and stratus clouds. As stratus clouds are characterized by stable air, the water droplets cannot develop by collisions: they will principally grow due to condensation.
The moist adiabatic lapse rate is ______ than the dry adiabatic lapse rate because _______
Lower; latent heat from vapourization is released from saturated air during the condensation process.
Explanation
As air rises, it encounters a lower pressure: it expands and cools. This process is called “adiabatic cooling.”
Non-saturated air is cooled by approximately 3°C for each 1,000 feet. This phenomenon is called the “dry adiabatic lapse rate.”
If air is cooled to the dew point, condensation forms and clouds appear. During condensation, latent heat of vapourization is released in the rising air, which reduces the
speed at which the air temperature decreases as it rises. This is called “saturated adiabatic lapse rate.” The air is cooled by approximately 1.5°C for every 1,000 feet.
What lifting process can cause the formation of towering cumulus clouds in the centre of a low pressure system?
Convergence
Explanation
When several airflows are converging in one area, they rise after they meet. This lift supports thunderstorm development and precipitations like rain, hail or snow. This is
what happens in a low-pressure area: air arrives from several high-pressure areas and blows through the isobars toward the depression centre. Air collects and overflow
rises. The convergence is a lift agent.
Wind shear and its accompanying CAT in jet streams is more intense ______ of mountain ranges.
Above and to the lee
Explanation
AIM, AIR 2.10: These rules of thumb are given to assist pilots in avoiding clear air turbulence (CAT). They apply to westerly jet streams. The Air Command Weather Manual (TP 9352E) available from Transport Canada discusses this subject more thoroughly.
- Wind shear and its accompanying CAT in jet streams is more intense above and to the lee of mountain ranges. For this reason, CAT should be anticipated whenever the flight path crosses a strong jet stream in the vicinity of a mountain range.
If clear air turbulence is encountered with an abrupt wind-shift associated with a sharp pressure trough, you should:
Cross the trough.
Explanation
AIM, AIR 2.10: These rules of thumb are given to assist pilots in avoiding clear air turbulence (CAT). They apply to westerly jet streams. The Air Command Weather Manual (TP 9352E) available from Transport Canada discusses this subject more thoroughly.
- If turbulence is encountered with an abrupt wind-shift associated with a sharp pressure trough, a course should be established to cross the trough rather than to fly parallel to it. A change in flight level is not as likely to reduce turbulence.
Determine the wind speed and its approximate direction over water under the following conditions:
- Pressure gradient: constant
- Surface wind speed over land: 35 knots
- Angle between the surface wind over land and isobars: 35°
45 knots and 25°.
Explanation
As altitude decreases, a force influences air speed and direction circulating from high-pressure areas to low-pressure areas. Friction between air masses and the Earth’s surface causes air movement deceleration, reducing the wind speed. Deceleration reduces the Coriolis force (proportional to wind speed), changing the initially dextrorotatory wind movement (to the right) in the Northern Hemisphere. Air moving away from high-pressure areas, associated with the Coriolis force, is then levorotatory and blows counterclockwise around low pressures.
Above 2,000 feet, wind blows almost parallel to the isobars, whereas at low altitude it tends to cross them.
The stronger the surface friction, the higher the deviation angle of the air compared to the isobars and the stronger its deceleration. This angle is lower over water than
over land, especially if the land is rough. Over land, deviation can go up to 40°, whereas over water it rarely goes over 10°.
A sudden increase in wind speed over a long period of time is called:
Squall
Explanation
A squall is approximately the same as a gust: it is an abrupt wind strength increasing, but lasting longer. It can be the result of a fast cold front passing or a thunderstorm (refer to squall line).
A wind shear
An important difference in wind speed or direction over a relatively short distance in the atmosphere.
It can be vertical or horizontal. It causes strong turbulence at the friction-layer level.
What is associated with the increase of wind shear performances (positive wind shear)?
With an increase of the headwind and a decrease of the tailwind.
Explanation
A positive wind shear is a headwind speed increasing or a tailwind speed decreasing. In such a case, the aircraft inertia leads to a delay of seconds before the aircraft reacts to this change. During this time, the aircraft airspeed increases. If the increase occurs during approach, airspeed will suddenly be greater. Lift will be greater as well, and rate of descent lower. You should therefore decrease power.
How is a low-level nocturnal jet stream created? What does it cause? What happens when the conditions that produce it are no longer active? When does it reach its maximum? what about its minimum?
It is a phenomenon caused by a nocturnal inversion.
This jet stream generally causes winds about fifty knots and dangerous low-level wind shears.
The wind speed near the ground increases when the inversion dissipates.
Maximum shortly after midnight and decreases in intensity in the morning
Explanation
A low-level nocturnal jet stream is a phenomenon caused by a nocturnal inversion. The wind shear, near the inversion’s top, is at its maximum shortly after midnight and decreases in intensity in the morning because of daytime heating, which dissipates the inversion. During dissipation, the wind shear moves closer to the ground, causing wind shifts and increased wind speed close to the ground.
The associated low level is represented by a layer of strong winds. It arises over flat terrains, usually in summer with southwest winds, and is thousands of miles long, hundreds of miles wide and hundreds of feet thick. This jet stream usually causes winds of about fifty knots and dangerous low-level wind shears.
Caution: In this question, it is asked to find the “false” answer.
Expected weather at a frontal system is dependent on the stability and moisture content of the _____
In a cold front, if ____ _____ is unstable, you will encounter _____ clouds. The lifting agent will be the ____. Vertical development will depend on the front’s ____ and ____
Warm air mass.
Warm air mass; cumulus; frontal surface; slope; speed
Explanation
Meteorological conditions at frontal systems are predicted according to the warm air mass features.
At a warm front, if warm air is moist and stable, stratus clouds will be what you encounter. If warm air is moist and unstable, you can expect to encounter convective clouds, sometimes hidden in stratus clouds. Therefore, you should expect strong showers in front of the frontal surface.
At a cold front, if warm air is stable, you will encounter stratus clouds. If warm air is unstable, you will encounter cumulus clouds. Here, the lifting agent is the frontal surface, so the vertical development force will depend on the front’s slope and speed.
A mT air mass moving northward over the Great Lakes during spring will probably cause:
The formation of low stratus clouds, fog and drizzle on the north shore of the lakes.
A tropical maritime air mass (mT) is warm and moist.
Stratus clouds usually appear when a layer of moist air is stable and cooled down under the saturation point. They appear in horizontal layers.
Fog is a cloud, usually stratus, on the ground. It appears when air is cooled down to a temperature below its dew point or when the dew point is risen to the outside air temperature by the addition of water steam.
Stratus clouds look like fog, except they do not touch the g
Drizzle (DZ) is a type of precipitation where small water droplets seem to float in the air. Drizzle usually appears in low stratus clouds. It is mostly found in coastal areas and
in high altitude valleys where there are temperature inversions and stratus clouds. As stratus clouds are characterized by stable air, the water droplets cannot develop by collisions: they will principally grow due to condensation.
In winter, over North America, the most common air masses are:
mP
mA
cA
Explanation
In North America, air masses are mostly, from north to south, continental Arctic (cA), continental polar (cP). maritime Arctic (mA), maritime polar (mP) and maritime tropical (mT).
In winter, the most common air masses are the maritime polar, the maritime Arctic and the continental Arctic air masses.
What is frontogenesis?
The formation of a front.
Explanation
Frontogenesis is the creation process of a front or a frontal zone intensification with physics (like radiation) or kinematics (like air movement) influences. The frontolysis is the process of a front or a frontal zone dissipation with physics (like radiation) or kinematics (like air movement) influences.
In flight, an aircraft is heading toward a warm front. From the cold air to the warm air, it will encounter, in this sequence:
High clouds, a lowering cloud cover and continuous rain.
Explanation
It is easy to see a warm active front approaching. The first clue is high cirrus clouds. Immediately afterward, you can see cirrostratus. It keeps growing until it becomes a solid altostratus and altocumulus mass. Low nimbostratus join altostratus to create a bench of compact clouds with their base close to the surface and their top up to 25,000 feet (sometimes more), which covers the whole area. Precipitation, usually abundant, will create precipitation fog (or frontal fog) and will develop because of extra humidity.
Weather conditions that can be expected at a cold front are determined with:
Bonus questions:
What happens if the cold front is moving quickly?
What happens if the air of the warm air mass is unstable and moist?
The moisture and the stability of the warm air mass and with the speed of the advancing cold front.
Explanation
The weather associated with a cold front depends both on the stability and the moisture of the warm air mass lifted by the cold air mass and the cold front speed. If the cold front is moving quickly, surface winds and gusts tend to increase. In addition, if the air of the warm air mass is unstable and moist, convective clouds (towering cumulus, cumulonimbus, etc.) and thunderstorms will appear. They result in strong rain or hail showers.
A pilot is in flight with a heading of 270 through a trowal. The temperature:
Increases then drops.
Explanation:
A trowal (TROugh of Warm air Aloft) is a trough of warm air in altitude. It is found in warm or cold occlusion, or, in other words, when there are three air masses: a cool air mass moving over a cold air mass or a cold air mass moving over a cool air mass, and a third air mass, of warm air, that creates a trough above those two colder air masses.
When there is a formation of clear ice on the aircraft wings, you can deduce that:
In what type of clouds can large supercooled droplets be found?
What has an effect on the rate of catch when there is ice accumulation?
When does clear ice appear?
The catch rate is high, the supercooled water droplets are large and the aircraft temperature is just below the freezing level.
In winter, an aircraft encounters freezing rain while flying through a warm front. What should the pilot do?
Explanation
Here are the precipitations you should expect from HIGH to LOW when crossing a warm front frontal surface in winter:
SNOW, RAIN, FREEZING RAIN, ICE PELLETS
- snow in the higher cloud part of the warm air mass in which the temperature is below freezing point;
- rain in the cloud part of the air mass in which the temperature is above freezing point;
- freezing rain, caused by the rain going through cold air (usually under warm air), becoming supercooled and freezing upon contact of cold objects (like an aircraft flying at this frontal surface level);
- ice pellets in the area preceding freezing rain, which result from rain freezing when passing through cold air.
If you fly at high altitude, you will only encounter snow. However, if you are at a relatively low altitude and pass from cold air frontal surface to warm air, you will first encounter snow, followed by ice pellets and freezing rain.
Ice will first accumulate on:
The antennas.
Explanation
Frost usually first appears on surfaces with slender leading edges: antennae, outside thermometers, propeller blades, horizontal stabilizers, rudders, gears, etc. Wings are the last thing on which frost appears.
Aerodynamic heating eliminates the risks of ice formation on an aircraft flying at a:
Speed above 500 knots.
Explanation
Aerodynamic heating is the heating of a solid body produced by the passage of a fluid around a body. In the case of an aircraft, aerodynamic heating is the heating of the aircraft skin produced by the passage of the air around it. It is caused by friction and compression processes, and is most significant at high speeds (supersonic and hypersonic aircraft), above a TAS of 350 knots. The increase in surface temperature is approximately proportional to the square of speed. If weather conditions are favourable to ice formation, a speed of 500 knots will ensure a good protection to the aircraft. In these conditions aircraft icing is not a problem, as the temperature on the surface is well above the freezing point.
In a thunderstorm, lightning and rumblings appear when it reaches the _____ stage.
Mature
A mature thunderstorm can reach heights of over 60,000 feet. Lifting currents are found in it, reaching up to 6,000 feet per minute. When the water droplets are heavy enough to fall, they take with them a certain amount of air, creating a descending current (up to 2,000 feet per minute), at the centre of the thunderstorm cell. Ascending and descending currents give way to severe turbulence.
Precipitation on the ground is a sign of maturity of the thunderstorm. Generally, it will stay at this stage for approximately 15 minutes.
Other phenomena indicating the maturity of the thunderstorm are lightning, micro gusts, wind shears, hail and tornados.
How can metereologists detect tornados?
How fast and far does a tornado move?
What is the shape of a tornado and what can you say about its pressure?
Meteorologists often use the Doppler radar to detect tornados.
Tornados can move a few miles over the ground at speeds between 25 and 50 knots.
Tornados are very deep and narrow low-pressure areas.
Explanation
Tornados, associated with strong thunderstorms, are very deep and narrow (diameter between 100 and 3,000 feet) low-pressure areas. They are funnel-shaped, arise under cumulonimbus clouds and reach the ground. Tornados can move a few miles over the ground at speeds between 25 and 50 knots. This destructive phenomenon suctions dust and debris from the ground to its centre where winds can reach several hundred knots. Meteorologists often use Doppler radar to detect tornados.
Mammatus clouds:
Where can they be found?
What are kind of winds are they associated with?
What kind of thunderstorms are they associated with?
An be found under altostratus clouds.
Are associated with strong wind-shears.
Are often associated with strong thunderstorms.
Explanation
The mammatus cloud is a cellular pattern of pouches hanging underneath the base of a convective cloud such as altocumulus or cumulonimbus. It appears in very unstable air and is often associated with serious thunderstorms, but can also appear under a nonviolent cloud such as altostratus. They can be found away from precipitations (like the anvil).
The presence of mammatus clouds does not necessarily mean that there will be violent weather. However, as mammatus form in the layer where there is convection, there might be strong wind shears and lightning. It is therefore recommended to avoid areas of mammatus clouds.
The dry microburst:
Is intensified by the virga (characteristic of the dry microburst) that cools the air.
Explanation
A burst is a combination of strong descending currents and destroyer winds on the ground and in its vicinity. The bursts are divided into two categories:
- macrobursts: descending gusts of a diameter of 2 NM or more reaching the ground and lasting 5 to 20 minutes. The strongest could cause damages as severe as tornadoes;
- microbursts: descending gusts of a maximum diameter of 2 NM. Winds are significant for five minutes.
There are two types of microbursts:
- Wet microburst: occurs in the presence of storm clouds with precipitations that reach the ground.
- Dry microburst: comes from moisture-laden towering cumulus clouds. In this case, the descending air column contains virga, which further cools the air. increasing the microburst strength.
_____ fog forms when dew point increases to the same value as the temperature.
Steam.
Explanation
Steam fog occurs when cold air moves over a warm water surface. Water evaporation saturates cold air. Condensation forms and creates this fog which occurs most of the time in fall over lakes and rivers.