Why ATMOSPHERIC OBSCURITY Important in Commercial Pilot training

For a PPL, CPL & ATPL aspirants who wants to become a good pilot, during flying prior to departure or enroute, earth atmosphere plays a vital role for safety of the aircraft.  To ensure this, pilot has to be well versant with earth atmosphere & other topics related to aviation meteorology.  At Gracious Avatar during commercial pilot training classes for PPL, CPL & ATPL aspirants, meteorology will be covered by the expert ground instructors.   Atmospheric Obscurity is one of the important topics which would be covered during CPL & APTL pilot training at Gracious Avatar, Gurgaon (India).




Visibility in pure air should be infinite. However, air is never pure and is laden with dust, smoke, industrial pollutants, aerosols etc. Presence of these suspended obscurities reduces the visibility.

Horizontal Visibility

Horizontal Visibility is the maximum distance along the horizontal up to which prominent objects can be seen with the naked eye and are recognized as such under natural light. Visibility may be different in different directions. The visibility reported by Met Office is the lowest Horizontal Visibility. During day Visibility is estimated by seeing objects at pre-measured distances, within and around the airfield. During night existing lights in and around the airfield at known distances are used. These are called Visibility Land Marks.

Runway Visual Range (RVR)

It is the distance up to which the pilot can see from the cockpit along the runway. RVR is reported when the visibility is less than 1500m. RVR is reported in multiples of 25M when between 50M & 150M, in multiples of 50M when between 150 & 800M, in multiples of 100M when between 800 & 1200M, and in multiples of 200M when more than 1200M.


PoorVisibility Phenomena

1.    Haze: Atmospheric obscurity due to very small particles of smoke, dust, water etc., wherein the visibility reduces to 5000M or less (but more than 2000M) is termed as haze. When the Relative Humidity is 75% or more, this is termed as Moist Haze(or simply Haze) whilst if the RH is less than 75% it is termed as Dust Haze or smoke Haze.It gives a milky appearance to the sky.
2.    Dust Haze: Atmospheric obscurity due to dust particles in suspension with RH less than 75% reducing visibility to 500oM or less is termed as Dust haze. It is caused by the strong winds in the desert or arid areas arising due to a steep pressure gradient kicking up dust in the stable lower layers of the atmosphere.
3.       Smoke Haze: Atmospheric Obscurity due to suspended smoke from industrial or domestic sources reducing visibility to 5000M or less is termed as Smoke haze. Smoke Haze occurs when wind is calm and there is strong ground inversion.
4.    Mist: Atmospheric obscurity due to suspended droplets wherein visibility reduces to 1000 M to less than 2000 M, with RH being 75% or more.
5.    Fog: Atmospheric obscurity due minute water droplets suspended in the air reducing visibility to less than 1000M.In Fog RH is nearly 100%. Fog may be termed as thick, moderate or light depending upon visibility.
6.    Smog: When smoke haze & fog co-exist, it is called Smog. In smoke visibility is very poor.
7.    Dust Storm: The visibility in dust storm is 5000M or less. If the dust storm is followed by rain visibility improves fast.    
8.    Precipitation: The visibility in precipitation depends on the size of the drop and intensity of precipitation. In moderate Rain vis may reduce to 1-3 km, in heavy Rain or showers to less than 1000M, in drizzle to 3 km and in snowfall it may reduce to less than 1000M.

Horizontal, Vertical & Slant Visibility

1.    Visibility reported by Met Office is minimum horizontal vis.
2.    Vertical visibility may be much better during shallow fog as it is the distance up to which one can see objects along the vertical.
3.    Slant visibility is the visibility at an angle and can be defined as the distance an object can be seen along the path that is at an an angle to the horizontal( usually glide path or landing path).In shallow fog this visibility is more than horizontal vis but less than vertical vis.


Instrumentsfor Measuring Visibility

1.    Scopograph or transmissometer are used for measuring vis along the different runways on an aerodrome. RVR equipment are installed along various runways to measure RVR.
2.    Close to take off & landing areas.
3.    The equipment consists of a light source and a photo-electric receiver, which generates electric current according to the obscurities present between the transmitter and receiver. The current so generated gives a measure of RVR. The display units are installed in Met Office and ATC Tower.


1.    Fog is composed of tiny water drops or ice crystals. It is nothing but a stratus cloud sitting smack on the ground. Fog occurs due to condensation of water vapour present in the layers of air close to the ground. Condensation can occur either by cooling of the air close to the ground or by feeding moisture in to the air to saturate it. Fog can be various types:
2.    Radiation Fog: Radiation Fog forms due to nocturnal cooling of the ground and the adjacent layers. The conditions favorable for formation of Radiation Fog are: a.    Clear skies b.    High relative Humidity e.g. after Rain c.    Light  freshening wind  of 3 to 8 kt 3.       Radiation fog is most frequent at about sunrise and dissipates within 2-3 hours after sunrise due to heating. If the Fog is thick it may take longer to lift. Generally fog lifts in to low stratus clouds before dissipating. Radiation Fog in India occurs mostly during winters after the passage of active western disturbances. It is almost a daily feature in winter season in the Valley of Brahmaputra River where adequate moisture is present and katabatic flow provides the required degree of turbulence and extra cooling. The most susceptible areas for radiation fog are NW India, UP, Bihar, Bengal and Assam (particularly south of Brahmaputra River).
4.    Vertically radiation Fog extends to only a few hundred feet whilst sometimes it can extend up to about 1500ft.
5.    Advection Fog: Advection Fog forms when warm moist air from elsewhere is transported over the cold surface (ground or water) where the surface temperature is less than the dew point of the advected air. Advection Fog forms both over land & sea. Coastal fogs over Bengal and Orissa during winters are due to a combined effect of advection from sea and radiation cooling. The Brahmaputra valley, the coastal areas and hills of Indian Peninsula experience advection Fog.
6.    Frontal Fog: Frontal Fog forms near the front due to saturation of air in the area of continuous rain ahead of the front. It also forms due to lowering of the cloud to the surface with the passage of a front.
7.    Steaming Fog: This type of Fog is common in higher latitudes when cold air mass flows over a warm sea surface. The water vapour from warm sea when comes in contact with the cold air aloft condenses to form steaming fog. It is common over frozen land, ice covered Polar Regions and over Icelandic and Norwegian regions. Over sea it is often referred to as sea smoke. It looks like steam coming out of the surface.

Fog Dispersal:

1.    Thermal Dispersion: When air is heated to temperatures above dew point, fog or cloud will dissipate.
2.    Dispersal using Hygroscopic Nuclei: When hygroscopic particles are injected into fog water drops form. This lowers the relative humidity of the air and fog dissipates.
For More Info :- https://www.graciousavatar.in/Pilot-Training/CPL.php

How Do I Become a Pilot

For a PPL, CPL & ATPL aspirants who wants to become a good pilot, during flying prior to departure or enroute, earth atmosphere plays a vital role for safety of the aircraft.  To ensure this, pilot has to be well versant with earth atmosphere & other topics related to aviation meteorology.  At Gracious Avatar during commercial pilot training classes for PPL, CPL & ATPL aspirants, meteorology will be covered by the expert ground instructors.   Humidity is one of the important topics which would be covered during CPL pilot training.


  1. Water vapor is always present in the air to a greater or lesser extent, in the troposphere.
  • Water evaporates into the air from oceans, lakes, vegetation etc. It ascends and forms clouds which cause precipitation.
  • Water exists in three phases: the gas (water vapor), liquid (rain, drizzle, shower) and solid(snow, hail).
  • The capacity of air to hold water vapor depends largely on temperature and to some extent on pressure. Higher the temperature, higher is the capacity of air to hold water vapor.
  • Dry Air: Air that contains no water vapor. Exists in upper troposphere or stratosphere.
  • Moist Air: The normal air that we breathe. It is also called unsaturated air.
  • Saturated Air: When air holds maximum water vapor, it is called saturated air.
  • Vapor Pressure: The partial pressure exerted by water vapor in the air. If p is the total pressure of air and e is the vapor pressure, then p-e is the pressure of dry air.
  • Saturated Vapor Pressure: It is the pressure exerted by water vapor when air is saturated.
  1. Absolute Humidity: It is the actual amount of water vapor contained in a given volume of air at a given temperature. It is expressed as g/m3.
  1. Humidity Mixing Ratio: It is defined as the mass of water vapor contained in a given mass of air. It is expressed as g/kg.
  1. Humidity Mixing Ratio for Saturated Air: It is defined as the maximum mass of water vapor that can be contained in a given mass of air at a particular temp and pressure. It is expressed as g/kg.
  1. Relative Humidity: It is defined as the ratio, in percentage, of the actual water vapor present in the air to the maximum it can hold at the same temperature and pressure.
  1. RH= HMRx100/HMR for saturated air.
  1. RH=Vapor pressure of Airx100/Saturation vapour pressure of Air.
  1. Wet Bulb Temperature (Tw Tw): It is the lowest temperature which air would attain by evaporating water into it to saturate it. Desert Coolers work on this principle.
  1. Dew Point Temperature (Td Td): It is the lowest temperature to which air should be cooled at constant pressure to saturate it with respect to water. Cooling below dew point causes condensation.
  1. Frost Point: It is the temperature to which air must be cooled to reach saturation with respect to ice. Cooling below the frost point causes formation of hoar frost.

Important Points

  1. As the temperature of the air increases, the amount of water vapour required to saturate it also increases.
  • At subzero temperatures water molecules have more energy and greater degree of freedom than ice, consequently the saturation vapour pressure over water drops is more than that over ice particles.
  • If water drops and ice particles co-exist, water drops will evaporate and condense on the ice particles. This explains rainfall from clouds which extend above 0oC and have both super cooled water drops and ice crystals co-existing.
  • Small water drops can exist in super cooled state up to -40o C.
  • For saturated Air( in Fog, Rain ) Air Temp(TT)=TwTw=TdTd
  • For unsaturated air: Dry Bulb Temp>Wet Bulb Temp>Dew Point

For more info :- https://www.graciousavatar.in/Pilot-Training/

How to TEMPERATURE Effect in Commercial Pilot Training

For a PPL, CPL & ATPL aspirants who wants to become a good pilot, during flying prior to departure or enroute, earth atmosphere plays a vital role for safety of the aircraft. To ensure this, pilot has to be well versant with earth atmosphere & other topics related to aviation meteorology. At Gracious Avatar during commercial pilot training classes for PPL, CPL & ATPL aspirants, meteorology will be covered by the expert ground instructors. Temperature is one of the important topics which would be covered during CPL pilot training.


  1. Temperature is a measure of heat.
  • It is measured by means of thermometer in degrees Celsius or Fahrenheit. These scales are arbitrarily fixed with reference to the melting point of ice and the boiling point of pure water at normal pressure. On the Celsius scale these are respectively as 0⁰ C and 100⁰ C and in Fahrenheit scale as 32⁰ F and 212⁰ F. Celsius scale is used internationally, in aviation and science. Use of Fahrenheit scale is confined to English- speaking countries only.
  • Heat is a form of energy. As heat is extracted from a substance, its internal energy is reduced and the random motion of its molecules slows down. The molecules get arranged in a more orderly pattern than before. As more heat is extracted the cooling and orderliness increases. Finally a state is reached when no more heat can be extracted and the molecules reach their maximum orderliness and the molecular motion almost ceases. The lowest temperature is reached. This minimum temperature is the same for all substances, and is accordingly called the absolute zero (K). 1K=-273.16 ⁰ C.

Conversion to C, F & K

  1. F= 9C/5 + 32
  2. C= 5/9 (F-32)
  3. K= C+ 273
  4. Note that -40 ⁰ C = -40 ⁰ F


Instruments for Measurement

  1. Dry Bulb Thermometer, Wet Bulb Thermometer (the bulb is covered with a muslin cloth which is kept moist), Maximum Thermometer (like doctors Thermometer), Minimum Thermometer and Thermograph, are used for measuring temperature.
  • Mercury is used in thermometers except in Minimum Thermometer in which alcohol is used instead of mercury.
  • In Thermographs and in Upper Air temperature measurement, bi- metallic strips are used.
  • A minimum thermometer has dumbbell shaped iron index, which permits alcohol to pass through it when the temperature rises. When temperature falls the alcohol, which has a conclave meniscus, drags the index back to indicate minimum temperature.
  • Surface temperature is recorded at a height of 4 ft(1.25m) from the ground in shade(inside a Stevenson’s Screen).

Dry Air & Moist Air

  1. Air which has no water vapour content is called dry air. Such air may exist at very high levels. For all practical purposes unsaturated air is called dry air.
  • With water vapour <4 % (RH <100%) air is called unsaturated or dry.
  • With water vapour >4 %(RH 100%) air is called saturated air.


Heat & Temperature

  1. Specific Heat: It is defined as the heat required to raise the temperature of unit mass of a substance by 1⁰C. The specific heat of water, regarded as the highest is 1, that of ice 0.5 and of soil 0.2.
  • Latent Heat: It is defined as the amount of heat absorbed or released during change of phase from/to solid/liquid/vapour. It is absorbed during change from solid to liquid and liquid to gas and released during change of phase from vapour to liquid and liquid to solid.
  • When water changes to vapour, a certain quantity of heat is supplied. To change boiling water into vapour, more than five times as much heat is required as is needed to bring the temperature of ice cold water to a boil. Once the boiling begins, the temperature remains constant and the heat released is stored as latent heat. It is released as latent heat when the water vapour condenses to water.

Heat Transfer Processes

  1. Heat is transferred from one place to the other by conduction, convection and radiation.
  • Conduction: In this Process heat is physically transferred by the molecules by contact. Conduction is important process of heat transfer very close to the ground.
  • Convection: In this process heat is bodily transferred to the colder part of the fluid. As more than 70% of the earth is covered with water, hence the importance of convection.  In the atmosphere free Convection is triggered by intense solar heating and the forced Convection by topography.
  • Radiation: Everybody radiates heat at its temperature. In this process of heat transfer the medium is neither affected nor required. The solar radiation directly heats up the earth without affecting the atmosphere.
  • Other Methods: Advection, Latent Heat release, Turbulence, Up and downward motion of air are the other methods of heat transfer.

Diurnal Variation of Surface Temperature

  1. Diurnal variation of temperature is more over land areas than over sea/coastal areas.
  • Sea Surface temperature shows an average variation from day to night of less than 1⁰C, whereas over land the variation may average as much as 20⁰C.
  • Variation is max when wind is calm.
  • Due to nocturnal cooling the surface temperature continues to fall even after sunrise till a balance is reached between the incoming and outgoing radiation. The balance occurs a little after sunrise.
  • Cloud cover can hamper both cooling and heating.
  • Cloudy nights are warmer than clear nights
  • Cloudy days are less warm than clear days.

For more info :- https://www.graciousavatar.in/Pilot-Training/CPL.php

Blog at WordPress.com.

Up ↑

Create your website at WordPress.com
Get started