2_4 Flashcards
What is the density altitude under the following conditions:
- Airport elevation: 7,000 feet
- OAT: 27°C
- Altimeter setting: 28.46”Hg
- Sea level pressure: 963.72 hPa
11566 feet
Without any correction, your altimeter shows a lower altitude than the actual altitude if the air temperature is _____ than the standard temperature or if the air pressure is ______ than the standard pressure.
Higher; Higher
Explanation
With too high an altimeter setting, the altimeter indicates a too high altitude. Each 0.10 inch of mercury added to the altimeter setting increases the indicated altitude on the altimeter by about 100 feet. From a region of high pressure to a region of low pressure, the altitude indicated by the altimeter (not corrected) is higher than the actual altitude. The same thing occurs when the altimeter passes from a warm air mass to a cold air mass. The opposite occurs from a low pressure to a high pressure from a region of cold air to a region of warm air.
Temperature diurnal variations will be the smallest in the area of:
A temperate ocean.
Explanation
The earth is warmed up when it absorbs solar radiation (short wave type). It then warms up the troposphere by terrestrial radiation and conduction. After sunset, the earth continues to irradiate, which decrease its temperature and air temperature at the surface.
The land is a better conductor than water, so land surfaces cool down a lot at night whereas water surfaces cool down just a little. This is why radiation fog occurs over land.
Since earth is curved, most direct sun rays are on the equator. It is the place where atmosphere is most warmed up. At poles, it is the opposite: Sun rays hit earth with a very inclined angle, so they do not warm much earth surface. The atmosphere does not receive much heat. There is a huge gap of temperature between equator and poles.
Which of the following statements is true regarding the heating of the atmosphere low levels?
The low levels of the atmosphere are heated by the earth, which releases energy after receiving solar radiation.
Solar radiation is absorbed by the earth and not by the atmosphere.
Heat is transferred from the sun to the earth by the method of solar radiation.
Explanation
The earch is warmed up when it absorbs solar radiation (short wave type). It then warms up the troposphere’s low levels through earth radiation (long waves type) and conduction (to a lesser degree). The heat is then distributed to the troposphere’s higher layers by convection, advection, mechanical turbulence and compression (responsible for the subsidence).
In standard atmosphere, temperature at FL310 would be:
-46ºC or -52ºF
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 - (31 x 1.98) = -46°C
You can also use your electronic flight calculator.
To convert Celsius into Fahrenheit and vice versa, use the following formula:
- °F = 9/5 °C + 32
- °C = 5/9 (°F-32)
You are ready to take off from an airport when you notice that smoke from a factory is rising vertically and then spreading at an approximate altitude of 1,000 feet AGL. What does this indicate?
The presence of a temperature inversion and possibly wind shears.
Explanation
An inversion can occur during a calm clear night, when the cold ground cools down the air with which it is in contact. Under the inversion, the air is pretty stable. However, near the top. some important wind shears can be found, especially if it is paired with a low-level jet stream. The more the inversion progresses, the greater the wind shears.
It is at its maximum after midnight and disappears in the morning when the sun is rising and it starts to get warm.
What is the instrument that measures relative humidity? How is it measured?
Explanation
The psychrometer is an instrument used to measure relative humidity. It is made up of two thermometers: the wet-bulb thermometer and the dry-bulb thermometer.
The wet-bulb temperature is the temperature that a parcel of air would attain if it was cooled to saturation (100% relative humidity) if there was water evaporating at constant pressure. Wet-bulb temperature is determined by the actual air temperature (dry-bulb temperature) and the air humidity. When relative humidity is 100%, the wet-bulb temperature and the dry-bulb temperature are equal.
The dry-bulb temperature is the temperature of the air measured by a thermometer freely exposed to the air but protected from solar radiation and moisture. Unlike the
wet-bulb temperature, the dry-bulb temperature does not indicate air humidity.
The process by which water vapour changes directly into ice is called:
deposition
Explanation
Condensation is the physical phenomenon of the change in state from a gas to a liquid. The opposite process is called evaporation. Deposition is when matter goes from a gas to a solid state. It is the opposite of sublimation.
For meteorology, which of the following is the most important in the atmosphere?
Water vapor.
Explanation
Water vapour appears only at lower levels of the atmosphere. In meteorology, it is the most important component of air. Water vapour is the cause of important
meteorological phenomenons, because it can change into droplets or ice crystals in normal temperature and pressure conditions. It is responsible for clouds and fog
creation, which are major phenomena in meteorology.
Snow pellets, hail and ice pellet showers are usually found inside:
Cumulonimbus.
Explanation
Hail implies the presence of strong lifting currents and unstable air. Therefore, it can be found in cumulus clouds at an advanced stage. The cumulonimbus (Cb) is a giant mass of cumulus rising much higher than the freezing point, where hail is formed. When the hail becomes too heavy to be lifted by the lifting currents of the cell, it turns into showers.
Hail can be encountered between 10,000 feet and 30,000 feet in a Cb. It can be encountered in clear air in front of thunderstorms as well, when it has been raised high in the cloud and is thrown outside of it.
The saturated adiabatic lapse rate is lower than the dry adiabatic lapse rate because the air is _____ by the heat _____ during the _____
Heated; released; condensation of the water vapour.
Explanation
The saturated adiabatic lapse rate is 1.5°C for every 1,000 feet.
The dry adiabatic lapse rate is 3°C for every 1,000 feet.
This difference is due to the fact that, when an air parcel rises and cools until it reaches its dew point, it becomes saturated, starting the condensation process. This process implies a heat exchange (vapourization of latent heat), which cools the air at a slower rate than non-saturated air.
What is the main problem caused by haze?
Poor visibility in stable air.
Explanation
Explanation
The process of haze creation results from microscopic natural (dust, salt or volcanic) or artificial (chimney ashes or car pollution) particles lifted into the air. These particles remain dry if the amount of water vapour in the air is low. They can absorb this vapour when the relative humidity is close to by not exceeding the saturation point, in the same manner as the development of cloud droplets and fog.
This process allows the molecules of water vapour to partially dissolve and increase their volume, but does not lead to droplet formation. However, these “pre-droplets” will cause an obstruction of visibility if they have a high enough air density. This natural phenomenon occurs when the air is relatively stable, mostly in an inversion situation when condensation nuclei are added.
Consider a saturated parcel of air that is heated by subsidence. This heating will be made at the ______ adiabatic lapse rate.
Dry
Explanation
The subsidence causes an increase of the ground level atmospheric pressure and, by adiabatic compression, warms up and dries out the air going down, stabilizing the atmosphere by creating a temperature inversion. The result is a dissipation of clouds from the top and a clear sky.
To determine the name given to a frontal system, the main factor is:
ExplanationThe direction of the colder air mass
Middle clouds (altostratus, altocumulus…) are located from _____ foot/feet to ___ feet
6500; 23000
Explanation
Medium level clouds can be found between 6,500 and 23,000 feec.They are made of water droplets (sometimes supercooled) or ice crystals, depending on the freezing point temperature. Those clouds are the altocumulus (Ac), the altocumulus castellanus (Acc) and the altostratus (As).
What is the orographic lift?
An air mass moving up a sloping mountain.
Orographic lift is a lifting agent operating when the air ascends the slope. If the air is unstable, it will continue to rise.
While in low-level flight during a hot summer day, an aircraft will encounter less turbulence when flying over:
A water body.
Explanation
Thermal turbulence (or convection) appears during hot summer days, when the sun heats the ground. Some surfaces heat faster than others. Those temperature
differences result in isolated convective currents which create turbulence. The more a surface is heated by the sun, the more severe the turbulence.
Land warm up faster than the water.
On 250 hPa charts, ______ knot isotachs spaced closer than ____NM indicate sufficient horizontal shear for CAT.
30; 90.
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.
c. On charts for standard isobaric surfaces such as the 250 mbs charts, 30 kt isotachs spaced closer than 90 NM indicate sufficient horizontal shear for CAT. This area is normally on the north (low-pressure) side of the jet stream axis, but in unusual cases may occur on the south side.
Wind-shift areas associated with _____ are frequently the cause of clear air turbulence.
Troughs.
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-shift areas associated with troughs are frequently turbulent.
The sharpness of the wind-shift is the important factor. Also, ridge lines may also have rough air.
When jet stream turbulence is encountered in a CROSSWIND situation, pilots who want to cross the CAT area more quickly should _______ if the outside TEMPERATURE DECREASES.
Descend
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 jet stream turbulence is encountered with direct tailwinds or headwinds, a change of flight level or course should be initiated since these turbulent areas are elongated with the wind but are shallow and narrow. A turn to the south in the Northern Hemisphere will place the aircraft in a more favourable area. If a turn is not feasible because of airway restrictions, a climb or descent to the next flight level will usually result in smoother air.
- When jet stream turbulence is encountered in a crosswind situation, pilots wanting to cross the CAT area more quickly should, either climb or descend based on temperature change. If temperature is rising - climb; if temperature is falling - descend. This will prevent following the sloping tropopause or frontal surface and staying in the turbulent area. If the temperature remains constant, either climb or descend.
Virga is:
An indicator of cooling and evaporation.
Explanation
“Virga” is any type of precipitation that does not reach the ground. Depending on the temperature, it is made of ice crystals sublimating or liquid droplets evaporating under a cloud passing through a thick non-saturated layer of air. We can find virga under any type of clouds giving precipitations, whatever their altitude.
Evaporation of water droplets cools down the air.
Virga is:
An indicator of cooling and evaporation.
Explanation
“Virga” is any type of precipitation that does not reach the ground. Depending on the temperature, it is made of ice crystals sublimating or liquid droplets evaporating under a cloud passing through a thick non-saturated layer of air. We can find virga under any type of clouds giving precipitations, whatever their altitude.
Evaporation of water droplets cools down the air.
The mountain waves causing pressure changes and very cold temperatures can cause the altimeter to over-read by as much as ______ feet.
3,000.
Explanation
Mountain effect error is caused by a wind blowing at altitude above mountain ranges. This wind will create mountain waves which are going to cause the wrong reading of the altimeter. In addition to the mountain waves, if the air temperature is different from the standard temperature (which is often the case), the altimeter may indicate an error of up to 3,000 feet higher than true altitude.
During a descent from a height of thousands of feet, wind direction will _____ and wind speed will _____
Back; decrease.
During a final approach, the headwind suddenly increases and remains high. To maintain the same angle of descent and the same airspeed, the pilot should first _____ the power, then ______ .
Reduce; increase it above the power setting that was used before the wind increased.
Jet streams associated with a frontal surface flows approximately ______ the front
Parallel to
Explanation
Developed surface lows, which are under upper troughs and lows, result in strong, long jet streams. Jet streams associated with a frontal surface flow almost parallel to the front.
At what plane and conditions does an air mass keep the same properties?
Explanation
The troposphere is divided into several large sections. Each of them is a specific air mass since it has the properties, on the horizontal plane, regarding temperature and moisture.
The features of an air mass (humidity and temperature) are determined by the area over which it was formed. However, as the mass moves away from this area, its
features change with the new conditions it meets along its path. In the event of major changes, horizontally and vertically, the air mass name changes. For example, a continental Arctic air mass travelling over a warm water area gains some humidity and becomes maritime polar.
Which of the following will be present during the passage of a warm front if the air of the warm area is stable and moist?
Continuous precipitations of rain from nimbostratus.
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.
Continuous rain comes from stratus clouds. Both these clouds and bad visibility are found in stable air area. There are few possibilities of experiencing turbulence under these clouds.
The nimbostratus cloud is a dark-grey cloud made of low layers. It is usually associated with a warm front and is responsible for continuous rain or snow.
A Continental Arctic air mass is:
Cold and dry.
Explanation
Continental arctic (cA) and continental polar (cP) air masses both consist of dry and cold air. They arise from extremely cold surfaces (covered by ice and snow) of the extreme north.
The name of a front corresponds to:
The name of the coldest air mass.
Fronts are named after the coldest air mass name of the system involved.
On a summer afternoon, you are at an airport where a cold front is passing. The sky, which was earlier covered with a wide range of stratus, becomes completely clear. After the passage of the front, the temperature will probably:
Start to slightly increase then drop.
Explanation
Usually, ground temperature gradually decreases as a cold front passes. The warm ground has already warmed the air right behind the front and above. Therefore, several hours are required before the temperature goes down to the cold air mass real temperature.
Clear ice will form when:
Large supercooled water droplets hit the aeroplane’s surfaces and spread over them.
Explanation
Clear icing is a heavy, glassy, solid ice layer that accumulates as it passes through a dense cloud or a precipitation zone of freezing rain. It extends irregularly on wing surfaces, tail, blades, antennas, etc. The ice only appears when a small portion of the large droplet of supercooled water freezes on impact. The aircraft surface temperature increases to 0°C because of heat released accompanying water state changes, from liquid to solid, during the impact of a part of the droplet. The portion of the droplet that is now liquid spreads over the aircraft and slowly freezes and meets other droplets.
The type of cloud where large supercooled droplets can be found is a cumulus. Cumulus clouds are characteristics of rising currents, necessary to create large enough water droplets.