Humidity, Clouds, Precipitation and Cyclones: GK Notes
Exam notes on humidity, condensation, cloud types, the three kinds of rainfall and tropical and temperate cyclones, with the IMD grades and solved questions.
By GK24 Editorial Team· Published · 5 min read

Water vapour is a small part of the atmosphere by volume but it decides the weather. Humidity, condensation, cloud and rainfall together make one chain of cause and effect, and the tropical cyclone is that chain at its most violent. Examiners draw questions from every link: the three ways of measuring humidity, the names of the clouds, the three kinds of rainfall, the conditions a cyclone needs, its structure, the names it carries in different seas and the wind-speed grades the India Meteorological Department uses.
Humidity and the way it is measured
Humidity is the water vapour present in the air, and it is stated in three ways. Absolute humidity is the actual weight of water vapour in a given volume of air, expressed in grams per cubic metre; it falls from the equator towards the poles and from the sea towards the interior. Specific humidity is the weight of water vapour in a unit weight of air, expressed in grams per kilogram, and it does not change when the air expands or contracts, which is why meteorologists prefer it. Relative humidity is the ratio of the water vapour actually present to the maximum the air can hold at that temperature, expressed as a percentage.
The capacity of air to hold vapour rises with temperature, so relative humidity falls when air is heated and rises when it is cooled, even though the quantity of vapour has not changed. Air holding all the vapour it can at a given temperature is saturated, and the temperature at which a given sample becomes saturated is its dew point. Relative humidity is measured with a hygrometer, and the wet and dry bulb thermometers of a psychrometer are the usual working instrument.
| Term | What it states | Unit |
|---|---|---|
| Absolute humidity | Vapour in a given volume of air | Grams per cubic metre |
| Specific humidity | Vapour in a unit weight of air | Grams per kilogram |
| Relative humidity | Vapour present against capacity at that temperature | Percentage |
| Dew point | Temperature at which the air becomes saturated | Degree Celsius |
Condensation, clouds and precipitation
When air is cooled below its dew point the vapour condenses on dust, smoke and salt particles that act as nuclei. The form the condensation takes depends on where it happens and on the temperature. Dew forms on cool surfaces when the dew point is above freezing; frost forms as ice crystals when the dew point is below freezing; fog and mist are condensation around nuclei near the ground, fog being the denser of the two; and clouds are condensation in the free air.
Clouds are classified by height and by form. The high clouds, from about six to twelve kilometres, are cirrus, cirrostratus and cirrocumulus; cirrus is thin, feathery and made of ice crystals. The middle clouds, from about two to six kilometres, are altostratus and altocumulus. The low clouds, up to about two kilometres, are stratus, stratocumulus and nimbostratus, the last being the thick dark sheet that gives steady rain. Cumulus and cumulonimbus grow vertically through these levels; the cumulonimbus, the tallest of them, brings thunder, lightning, heavy showers and hail, and is the cloud of the thunderstorm.
Precipitation is the water that falls back to the surface, as rain when the drops are liquid, as snow when the vapour condenses directly into crystals below freezing, as sleet when raindrops freeze while falling through a cold layer, and as hail when pellets of ice are carried up and down inside a cumulonimbus until they are heavy enough to fall. Rainfall itself is of three types. Convectional rainfall comes from air heated at the surface, rising, cooling and condensing, and gives the equatorial belt its brief, heavy afternoon showers. Orographic or relief rainfall falls where moist air is forced to rise over a mountain barrier, wetting the windward slope and leaving a dry rain-shadow on the leeward side. Cyclonic or frontal rainfall comes where a warm air mass is forced over a cold one along a front, and is typical of the temperate latitudes.
Tropical cyclones
A tropical cyclone is an intense low-pressure system of the warm seas, with winds spiralling inward anticlockwise in the northern hemisphere and clockwise in the southern. It needs a large sea surface with a temperature above about twenty-seven degrees Celsius, abundant moisture, a sufficient Coriolis force, which is why none forms within about five degrees of the equator, small variation of wind with height and divergence of air above the low-pressure centre.
At the centre is the eye, a calm and nearly cloudless column of descending air some tens of kilometres across; around it is the eye wall, a ring of towering cumulonimbus where the strongest winds and the heaviest rain occur, and beyond that the spiral rain bands. The system weakens quickly after landfall because its supply of warm moist air is cut off. The same storm is called a hurricane in the Atlantic and the eastern Pacific, a typhoon in the north-western Pacific and the China Sea, a cyclone in the Indian Ocean, a willy-willy in Australia and a baguio in the Philippines. The India Meteorological Department is the regional body that names the storms of the north Indian Ocean and grades them by sustained wind speed.
| Grade | Sustained wind speed |
|---|---|
| Depression | 31 to 49 kilometres per hour |
| Deep depression | 50 to 61 kilometres per hour |
| Cyclonic storm | 62 to 87 kilometres per hour |
| Severe cyclonic storm | 88 to 117 kilometres per hour |
| Very severe cyclonic storm | 118 to 166 kilometres per hour |
| Extremely severe cyclonic storm | 167 to 221 kilometres per hour |
| Super cyclonic storm | 222 kilometres per hour and above |
Temperate cyclones and other systems
A temperate or extra-tropical cyclone forms along the front where a cold polar air mass meets a warm subtropical one, between about thirty-five and sixty-five degrees latitude. It is larger than a tropical cyclone, has no eye, moves from west to east, lasts longer, brings slow and widespread rain rather than a short violent burst, and is commonest in winter. The western disturbances that bring winter rain to north-west India are systems of this kind. An anticyclone is the opposite case, a high-pressure system with winds blowing outward, clockwise in the northern hemisphere, and it brings clear and settled weather. A tornado is a small, extremely violent funnel of whirling air over land, and the same funnel over water is a waterspout.
Exam Point of View
Three kinds of question come from this topic. The first is definition with unit: which humidity is a percentage, what the dew point is, which instrument measures humidity, where a hydrometer is the planted trap for a hygrometer. The second is classification: clouds by height, the cloud of the thunderstorm, the three types of rainfall, and the local names of the cyclone, which are asked both as a direct question and as a match-the-list. The third is the cyclone itself: the eye and the eye wall, the conditions of formation including the Coriolis rule about five degrees, the wind-speed grades of the India Meteorological Department, and the differences between a tropical and a temperate cyclone. Recent storms and the coast each one struck are also asked, so keep the Arabian Sea and Bay of Bengal names apart.
Important Facts
| Unit of absolute humidity | Grams per cubic metre |
|---|---|
| Unit of specific humidity | Grams per kilogram |
| Instrument for relative humidity | Hygrometer, commonly a wet and dry bulb psychrometer |
| Height of high clouds | About 6 to 12 kilometres |
| Thunderstorm cloud | Cumulonimbus |
| Cloud of steady, continuous rain | Nimbostratus |
| Minimum sea surface temperature for a tropical cyclone | About 27 degrees Celsius |
| Why no cyclone forms at the equator | The Coriolis force is zero there and too weak within about 5 degrees |
| Super cyclonic storm | Sustained wind of 222 kilometres per hour and above |
| Latitudes of temperate cyclones | About 35 to 65 degrees, moving west to east |
Practice MCQs on this topic
The centre of a cyclone is a calm area. It is called the ___________ of the storm.
- A.base
- B.focal point
- C.eye
- D.trigger point
Show answer
Correct answer: C. eye
Explanation
The correct answer is C, the eye. The eye of a tropical cyclone is the roughly circular column of calm, descending air at its centre, usually a few tens of kilometres across, where the pressure is lowest, the winds are light and the sky is often nearly clear. Around it stands the eye wall, a ring of tall cumulonimbus clouds carrying the strongest winds and the heaviest rain, so the passage of a cyclone over a place gives violent weather, then an interval of calm, then violent weather again from the opposite direction. Option A is wrong because base is not a term used for any part of a cyclone. Option B is wrong because focal point belongs to optics and to earthquake studies, not to meteorology. Option D is wrong because trigger point is not a recognised term in the structure of a storm.
Which of the following tropical cyclones had hit the western coast of India in May 2021?
- A.Vardah
- B.Tauktae
- C.Titli
- D.Hudhud
Show answer
Correct answer: B. Tauktae
Explanation
The correct answer is B, Tauktae. Tauktae formed in the Arabian Sea in May 2021, intensified into an extremely severe cyclonic storm, moved north along the Konkan coast and made landfall in Gujarat, which is why it is remembered as an Arabian Sea system of the western coast. Option A is wrong because Vardah struck the Tamil Nadu coast near Chennai in December 2016 and came from the Bay of Bengal. Option C is wrong because Titli hit Odisha and Andhra Pradesh in October 2018, again a Bay of Bengal storm of the eastern coast. Option D is wrong because Hudhud crossed the coast at Visakhapatnam in October 2014. Note the useful contrast: the Bay of Bengal produces far more cyclones than the Arabian Sea, so an Arabian Sea landfall such as Tauktae is the one examiners pick out.
Match List - I with List - II and select the correct answer using the codes given below the lists: List - I (Tropical cyclones) List - II (Country) A. Baguio 1. Australia B. Hurricanes 2. China C. Typhoons 3. Philippines D. Willy-Willies 4. United States of America
- A.A) 3, B) 4, C) 1, D) 2
- B.A) 3, B) 4, C) 2, D) 1
- C.A) 2, B) 3, C) 4, D) 1
- D.A) 2, B) 1, C) 3, D) 4
Show answer
Correct answer: B. A) 3, B) 4, C) 2, D) 1
Explanation
The correct answer is B. The local names of the tropical cyclone are a standing favourite: baguio belongs to the Philippines, hurricane to the United States and the wider Atlantic and Caribbean region, typhoon to China and the north-western Pacific, and willy-willy to Australia. That gives A with 3, B with 4, C with 2 and D with 1, which is option B. Option A is wrong because it pairs typhoons with Australia and willy-willies with China, reversing the last two. Option C is wrong because it begins by sending baguio to China. Option D is wrong because it pairs hurricanes with Australia and willy-willies with the United States. Add two more names to the list while revising: the storm is simply called a cyclone in the Indian Ocean and taifu in Japan.
Which of the following cyclones did NOT hit India during the years 2021-2022?
- A.Yaas
- B.Julia
- C.Tauktae
- D.Gulab
Show answer
Correct answer: B. Julia
Explanation
The correct answer is B, Julia. Julia was a storm of the Atlantic basin and never approached India, so it cannot belong to a list of Indian landfalls. Option A is wrong because Yaas crossed the Odisha coast near Balasore in May 2021, only days after Tauktae struck the opposite coast. Option C is wrong because Tauktae formed in the Arabian Sea in May 2021 and made landfall in Gujarat. Option D is wrong because Gulab crossed the north Andhra Pradesh coast in September 2021 and its remnant later re-formed in the Arabian Sea as Shaheen. The point of the question is that the names of the north Indian Ocean storms come from a panel of countries of the region, so a name from the Atlantic list, where the storms are named separately, is the odd one out.
Relative humidity of the air is measured by which of the following instruments?
- A.Barometer
- B.Anemometer
- C.Hygrometer
- D.Hydrometer
Show answer
Correct answer: C. Hygrometer
Explanation
The correct answer is C, a hygrometer. A hygrometer measures the humidity of the air, and the common working form is the psychrometer, a pair of wet and dry bulb thermometers whose difference in reading is converted into relative humidity with a table. Option A is wrong because a barometer measures atmospheric pressure, the mercury barometer and the aneroid barometer being its two forms. Option B is wrong because an anemometer measures wind speed. Option D is wrong because a hydrometer, whose name differs by a single letter, measures the relative density of a liquid and has nothing to do with the atmosphere; this near-identical pair is the trap in the question. Remember the related definitions as well: air that holds all the vapour it can at a given temperature is saturated, and the temperature at which it becomes saturated is the dew point.
Which of the following is expressed as a percentage?
- A.Absolute humidity
- B.Relative humidity
- C.Specific humidity
- D.Dew point
Show answer
Correct answer: B. Relative humidity
Explanation
The correct answer is B, relative humidity. Relative humidity compares the water vapour actually present in the air with the maximum amount the air could hold at that temperature, so it is a ratio and is stated as a percentage; air at a hundred per cent relative humidity is saturated. Option A is wrong because absolute humidity is the actual weight of vapour in a given volume of air and is stated in grams per cubic metre. Option C is wrong because specific humidity is the weight of vapour in a unit weight of air, stated in grams per kilogram, and it is preferred in weather work because it does not change as the air expands or contracts. Option D is wrong because the dew point is a temperature, stated in degrees. Note also that heating air lowers its relative humidity even when no vapour has been added or removed.
Which cloud is known for bringing thunder, lightning and hail, and is called the thunderstorm cloud?
- A.Cirrus
- B.Altostratus
- C.Stratus
- D.Cumulonimbus
Show answer
Correct answer: D. Cumulonimbus
Explanation
The correct answer is D, cumulonimbus. The cumulonimbus is a cloud of great vertical extent that can rise from near the ground almost to the top of the troposphere, and the strong updraughts inside it produce thunder, lightning, heavy showers and hail; it is the cloud of the thunderstorm and the eye wall of a cyclone is built of such clouds. Option A is wrong because cirrus is a high, thin, feathery cloud of ice crystals that gives no rain. Option B is wrong because altostratus is a middle cloud forming a grey sheet through which the sun shows faintly. Option C is wrong because stratus is a low, uniform, layered cloud associated with drizzle and dull weather. Remember the height classes: high clouds about six to twelve kilometres, middle clouds two to six, low clouds up to two.
The brief, heavy afternoon showers of the equatorial belt are an example of which type of rainfall?
- A.Convectional rainfall
- B.Orographic rainfall
- C.Frontal rainfall
- D.Cyclonic rainfall
Show answer
Correct answer: A. Convectional rainfall
Explanation
The correct answer is A, convectional rainfall. In the equatorial belt the ground is strongly heated through the morning, the warm moist air rises in powerful convection currents, cools as it rises, condenses into towering cumulonimbus and falls as a short, very heavy shower in the afternoon, which is why it is nicknamed four o'clock rain. Option B is wrong because orographic rainfall needs a mountain barrier to force the moist air upward, and it leaves a rain shadow on the leeward slope. Options C and D are wrong because frontal or cyclonic rainfall is produced where a warm air mass rides over a cold one along a front; it is slow, widespread and typical of temperate latitudes, as in the western disturbances that water north-west India in winter. The three types to keep apart are therefore convectional, orographic and cyclonic.
Tropical cyclones do not form within about five degrees of the equator because
- A.the sea surface temperature there is too low
- B.there is not enough moisture in the air
- C.the Coriolis force is too weak to set the air spinning
- D.the air there is always descending
Show answer
Correct answer: C. the Coriolis force is too weak to set the air spinning
Explanation
The correct answer is C. The Coriolis force, which arises from the rotation of the earth, is zero at the equator and very weak for a few degrees on either side, so converging air cannot be deflected into the spiral that makes a cyclone; the belt within about five degrees of the equator is therefore free of tropical cyclones even though it is warm. Option A is wrong because the equatorial seas are the warmest in the world, well above the twenty-seven degrees Celsius a cyclone needs. Option B is wrong because the equatorial air is the most humid on earth. Option D is wrong because the equatorial belt is a zone of rising air and low pressure, not of descending air; descending air belongs to the subtropical high-pressure belts near thirty degrees. The other conditions are a wide warm sea, weak change of wind with height and divergence aloft.
According to the classification used by the India Meteorological Department, a storm is called a super cyclonic storm when the sustained wind speed is
- A.62 to 87 kilometres per hour
- B.88 to 117 kilometres per hour
- C.118 to 166 kilometres per hour
- D.222 kilometres per hour and above
Show answer
Correct answer: D. 222 kilometres per hour and above
Explanation
The correct answer is D. The India Meteorological Department grades a system of the north Indian Ocean by its sustained wind speed, and the highest grade, the super cyclonic storm, begins at two hundred and twenty-two kilometres per hour. Option A is wrong because sixty-two to eighty-seven kilometres per hour is the band of an ordinary cyclonic storm, the stage at which the system is given a name. Option B is wrong because eighty-eight to one hundred and seventeen kilometres per hour is a severe cyclonic storm. Option C is wrong because one hundred and eighteen to one hundred and sixty-six kilometres per hour is a very severe cyclonic storm, and the band above it, up to two hundred and twenty-one, is the extremely severe cyclonic storm. Below the storm stages lie the depression at thirty-one to forty-nine and the deep depression at fifty to sixty-one kilometres per hour.
Which of the following is true of a temperate cyclone but not of a tropical cyclone?
- A.It forms along a front where two air masses of different temperature meet
- B.It has a calm central eye surrounded by a wall of cumulonimbus
- C.It weakens rapidly as soon as it crosses the coast
- D.It cannot form within five degrees of the equator
Show answer
Correct answer: A. It forms along a front where two air masses of different temperature meet
Explanation
The correct answer is A. A temperate or extra-tropical cyclone is a frontal system: it forms between about thirty-five and sixty-five degrees latitude where a cold polar air mass meets a warm subtropical one, and the warm air is forced to rise along the front, giving slow and widespread rain over a large area. Option B is wrong because the eye and the eye wall belong only to the tropical cyclone; a temperate cyclone has no eye. Option C is wrong because it is the tropical cyclone that dies quickly over land, having lost its supply of warm moist air, while a temperate cyclone travels across continents from west to east. Option D is wrong because the five-degree rule describes where tropical cyclones cannot form; temperate cyclones form far from the equator in any case, so the statement does not distinguish them.
Condensation that takes place on a cold surface when the dew point is below the freezing point gives
- A.dew
- B.frost
- C.fog
- D.mist
Show answer
Correct answer: B. frost
Explanation
The correct answer is B, frost. When the surface on which condensation occurs is below the freezing point and the dew point is also below it, the vapour changes directly into tiny ice crystals instead of water droplets, and that white deposit is frost; it is common on clear, calm winter nights when the ground loses heat rapidly by radiation. Option A is wrong because dew forms in the same way but when the dew point is above freezing, so the moisture settles as drops of water. Option C is wrong because fog is condensation on dust and smoke nuclei in the air near the ground, which reduces visibility sharply. Option D is wrong because mist is the thinner, less dense form of the same phenomenon, with better visibility than fog. The essential conditions for dew and frost are a clear sky, still air, high relative humidity and a cold long night.
Frequently Asked Questions
What is the difference between absolute, specific and relative humidity?
Absolute humidity is the weight of water vapour in a given volume of air, in grams per cubic metre. Specific humidity is the weight of vapour in a unit weight of air, in grams per kilogram, and it stays the same when the air expands or contracts, which is why meteorologists use it. Relative humidity is the ratio of the vapour present to the maximum the air can hold at that temperature, stated as a percentage; it falls when the air is heated.
Why does a tropical cyclone weaken after it crosses the coast?
Its energy comes from the latent heat released when water vapour from a warm sea condenses in the rising air at its centre. Over land the supply of warm moist air is cut off and friction with the rough surface slows the inflowing winds, so the pressure gradient weakens and the system decays into a depression within a day or two, although it may still bring very heavy rain inland.
What is the difference between a tropical and a temperate cyclone?
A tropical cyclone forms over warm seas between about five and thirty degrees latitude, has a calm eye and a wall of cumulonimbus, is small but violent, lasts a few days and dies quickly over land. A temperate cyclone forms along a front between two air masses between about thirty-five and sixty-five degrees, has no eye, is much larger, moves from west to east, brings slow widespread rain and is commonest in winter.
What are the three types of rainfall?
Convectional rainfall, where surface heating lifts the air, as in the afternoon showers of the equatorial belt; orographic or relief rainfall, where a mountain barrier forces moist air to rise, wetting the windward slope and leaving a rain shadow to leeward; and cyclonic or frontal rainfall, where warm air is forced over cold air along a front, the slow widespread rain of the temperate latitudes.
What is the eye of a cyclone?
The eye is the roughly circular central region of a tropical cyclone, a few tens of kilometres across, where the air descends, the pressure is lowest, the winds are light and the sky is nearly clear. It is ringed by the eye wall, a band of towering cumulonimbus with the strongest winds and heaviest rain, so a place on the storm's track gets violent weather, a lull, and then violent weather from the opposite direction.





