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CSS Geography Climatology Syllabus
The Climatology syllabus for CSS Geography in full: 4 chapters and 17 topics, every one listed below, plus 53 Climatology flashcards with answers.
Climatology syllabus: all 4 chapters
Expand any chapter to see its topics and sub-topics.
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Atmosphere and Insolation
4 topics- Structure and composition of atmosphere
- Insolation and heat budget of the earth
- Temperature distribution
- Elements and factors of climate
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Pressure and Atmospheric Circulation
5 topics- Pressure belts of the world
- Planetary winds
- Monsoon winds
- Local winds
- Air masses and fronts
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Moisture and Precipitation
4 topics- Hydrological cycle
- Types of condensation
- Types of precipitation
- Factors of global distribution of precipitation
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Weather Systems and Climate Classification
4 topics- Temperate and tropical cyclones
- Jet streams
- Koppen's classification of climate
- Thornthwaite's and Trewartha's classifications
CSS Geography Climatology flashcards — 53 questions with answers
What are the four main gaseous components of dry air by volume, with approximate percentages?
Nitrogen (~78%), Oxygen (~21%), Argon (~0.93%), and Carbon dioxide (~0.03-0.04%).
Name the five vertical layers of the atmosphere from the surface upward.
Troposphere, Stratosphere, Mesosphere, Thermosphere (Ionosphere), and Exosphere.
In which atmospheric layer do nearly all weather phenomena occur, and what is its average thickness?
The troposphere; it averages about 13 km thick (about 8 km at the poles and 16-18 km at the equator).
What is the normal/environmental lapse rate of temperature in the troposphere?
Temperature falls about 6.5°C per 1000 m (6.4°C/km) of altitude gain.
In which atmospheric layer is the ozone layer located, and why is it important?
The stratosphere (roughly 15-35 km); ozone absorbs harmful ultraviolet radiation, protecting life on Earth.
Why does temperature increase with height in the stratosphere?
Because ozone in the stratosphere absorbs ultraviolet solar radiation, warming the upper portion of the layer.
Which atmospheric layer records the lowest temperatures, and what causes meteors to burn there?
The mesosphere, where temperatures fall to about -90°C; friction with its gases burns up incoming meteors.
What is the ionosphere noted for, and which layer contains it?
It contains ionized particles that reflect radio waves back to Earth (enabling long-distance radio communication); it lies in the thermosphere.
Define insolation.
Insolation (incoming solar radiation) is the amount of solar energy received by a unit area of the Earth's surface, usually measured per unit time.
What is the solar constant?
The average amount of solar energy received at the top of the atmosphere on a surface perpendicular to the Sun's rays, about 1.94 cal/cm²/min (≈1361-1367 W/m²).
List the four main factors that control the amount of insolation received at a place.
The angle of the Sun's rays (latitude), duration of daylight, transparency of the atmosphere, and the solar constant/distance from the Sun.
Why do tropical latitudes receive more insolation than polar latitudes?
The Sun's rays strike the tropics more vertically (high angle), concentrating energy over a smaller area and passing through less atmosphere, whereas polar rays are slanted and spread over a larger area.
In Earth's heat budget, what percentage of incoming solar radiation is reflected back to space (planetary albedo)?
About 35% (roughly 27% by clouds, 2% by ice/snow, and 6% by atmospheric scattering).
What is meant by the term 'heat budget' (heat balance) of the Earth?
The balance between incoming solar (shortwave) radiation absorbed by the Earth-atmosphere system and outgoing terrestrial (longwave) radiation, which keeps the planet's average temperature stable.
Of the 100 units of incoming insolation, roughly how much is absorbed by the Earth's surface and how much by the atmosphere?
About 51% is absorbed by the Earth's surface and about 14% is absorbed by the atmosphere; the remaining ~35% is reflected back to space.
Explain the greenhouse effect in relation to the heat budget.
Atmospheric gases (CO2, water vapour, methane) absorb outgoing longwave terrestrial radiation and re-radiate it back, trapping heat and keeping Earth's surface warmer than it would otherwise be.
What is the difference between insolation and terrestrial radiation in terms of wavelength?
Insolation is shortwave radiation (the hot Sun emits mostly short waves), while terrestrial radiation is longwave radiation (the cooler Earth emits mostly long waves).
Define isotherm.
An isotherm is a line on a map joining places that have the same temperature (usually reduced to sea level).
State the main factors that control the horizontal distribution of temperature on Earth.
Latitude (angle of insolation), altitude, distance from the sea (continentality), ocean currents, prevailing winds, cloud cover, and the nature of the surface.
What is the annual range of temperature, and where is it greatest?
It is the difference between the mean temperature of the warmest and coldest months; it is greatest in continental interiors of high latitudes (e.g., Siberia) and smallest over oceans and the equator.
Show the other 33 Climatology flashcards
Why do oceans have a smaller temperature range than landmasses?
Water heats and cools more slowly than land (higher specific heat, transparency, mixing, and evaporation), so maritime climates are moderate while continental climates are extreme.
Distinguish between the elements and the factors of climate.
Elements are the measurable conditions describing climate (temperature, pressure, wind, humidity, precipitation). Factors are the controls that influence those elements (latitude, altitude, continentality, ocean currents, winds, relief).
How does altitude affect temperature and pressure?
Both temperature and atmospheric pressure decrease with increasing altitude (temperature about 6.5°C per 1000 m; pressure roughly halves every ~5.5 km).
What instrument measures atmospheric pressure, and what is the standard sea-level pressure?
The barometer (mercury or aneroid); standard sea-level pressure is about 1013.25 millibars (760 mm of mercury).
Name the four major pressure belts of the world.
Equatorial low-pressure belt, Subtropical high-pressure belt (~30°N/S), Sub-polar low-pressure belt (~60°N/S), and Polar high-pressure belt (~90°N/S).
Why is the equatorial low-pressure belt also called the Doldrums?
Intense heating causes air to rise (convection), creating low pressure with calm, light, and variable winds — the belt of calms known as the Doldrums.
What are the 'Horse Latitudes' and where are they located?
The subtropical high-pressure belts around 30°N and 30°S, characterized by calm, descending air and light variable winds.
Distinguish between thermally induced and dynamically induced pressure belts.
Thermally induced belts result from heating/cooling of air (equatorial low, polar high), while dynamically induced belts result from Earth's rotation and air movement/subsidence (subtropical high, sub-polar low).
Name the three major planetary (prevailing) wind systems.
The Trade winds, the Westerlies, and the Polar easterlies.
From which pressure belts do the Trade winds blow, and in what direction in each hemisphere?
They blow from the subtropical highs (~30°) toward the equatorial low; they are northeast trades in the Northern Hemisphere and southeast trades in the Southern Hemisphere.
What is Ferrel's Law / the Coriolis effect's impact on wind direction?
Due to Earth's rotation, moving winds are deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
Where do the Westerlies blow, and why are they called the 'Roaring Forties'?
They blow from the subtropical highs (~30°) toward the sub-polar lows (~60°), from the SW in the N. Hemisphere and NW in the S. Hemisphere; in the Southern Hemisphere their strength over open ocean earns the names Roaring Forties, Furious Fifties, and Shrieking Sixties.
State Buys Ballot's Law.
If you stand with your back to the wind in the Northern Hemisphere, low pressure lies to your left and high pressure to your right (reversed in the Southern Hemisphere).
What is a monsoon, and from which word is the term derived?
A monsoon is a seasonal reversal of wind direction (and associated rainfall) between summer and winter; the word derives from the Arabic 'mausim' meaning season.
Describe the summer (southwest) monsoon over the Indian subcontinent.
In summer the landmass heats, forming low pressure that draws moist Southwest winds from the Indian Ocean toward the land, bringing heavy rainfall (roughly June-September).
Describe the winter (northeast) monsoon over the Indian subcontinent.
In winter the land cools and develops high pressure, so dry Northeast winds blow from the land toward the sea, producing the dry season (and some rain on the southeast coast).
Besides differential heating of land and sea, what modern factor is used to explain the monsoon?
The seasonal migration of the Inter-Tropical Convergence Zone (ITCZ) and the shifting of the upper-air jet streams (subtropical and tropical easterly jet).
What is a local wind? Give two examples.
A local wind is a wind affecting a small area produced by local differences in temperature and pressure; examples include land/sea breezes, mountain/valley breezes, Chinook, Foehn, Loo, Mistral, and Sirocco.
Explain the difference between a sea breeze and a land breeze.
A sea breeze blows from cooler sea to warmer land during the day; a land breeze blows from cooler land to warmer sea at night.
What are the Foehn and Chinook winds, and what effect do they have?
They are warm, dry winds blowing down the leeward side of mountains (Foehn in the Alps, Chinook in the Rockies); they raise temperatures rapidly and melt snow.
Identify the local winds: Loo, Mistral, and Sirocco.
Loo is a hot, dry summer wind of northern India/Pakistan; Mistral is a cold, dry wind blowing down the Rhône valley to the Mediterranean; Sirocco is a hot, dusty wind from the Sahara toward southern Europe.
Define an air mass.
An air mass is a large body of air with fairly uniform temperature and humidity characteristics throughout, acquired from its source region.
How are air masses classified by source region?
By moisture: maritime (m, from oceans) or continental (c, from land); and by temperature/latitude: Arctic (A), Polar (P), Tropical (T), Equatorial (E) — e.g., mT (maritime tropical), cP (continental polar).
Define a front in meteorology.
A front is the boundary or transition zone separating two air masses of different temperature, humidity, and density.
What is a warm front and how does it produce precipitation?
A warm front is where an advancing warm air mass rises gently over a retreating cold mass; the gradual ascent produces widespread layered (stratiform) clouds and prolonged light rain.
What is a cold front and what weather does it bring?
A cold front is where an advancing cold air mass undercuts and forces warm air to rise steeply; this causes towering cumulonimbus clouds, heavy showers, thunderstorms, and a temperature drop.
What is an occluded front?
An occluded front forms when a faster-moving cold front overtakes a warm front, lifting the warm air completely off the ground; it often marks the dissipating stage of a depression.
List the main stages/processes of the hydrological (water) cycle.
Evaporation (and transpiration), condensation, precipitation, and runoff/infiltration that returns water to oceans — a continuous closed cycle driven by solar energy and gravity.
Define condensation and state the conditions needed for it.
Condensation is the change of water vapour into liquid (or solid) form; it requires the air to be cooled to its dew point (saturation) and the presence of hygroscopic condensation nuclei.
Name the major forms/types of condensation.
Dew, frost, fog, mist, and clouds (with frost being condensation directly into ice when the dew point is below 0°C).
Differentiate between fog and mist.
Both are clouds near the ground formed by condensation; fog reduces visibility to less than 1 km, while mist is thinner and allows visibility greater than 1 km.
Define precipitation and name its common forms.
Precipitation is the fall of moisture from the atmosphere to the Earth's surface in liquid or solid form; forms include rain, snow, sleet, hail, and drizzle.
Describe the three main types of rainfall by mechanism of uplift.
Convectional (heated air rises, common in equatorial regions/afternoons), Orographic/relief (air forced to rise over mountains, with a wet windward side and dry leeward rain shadow), and Cyclonic/frontal (warm and cold air masses meet along a front).
CSS Geography Climatology FAQ
What is in the CSS Geography Climatology syllabus?
CSS Geography Climatology is split into 4 chapters: Atmosphere and Insolation, Pressure and Atmospheric Circulation, Moisture and Precipitation and Weather Systems and Climate Classification. Together they contain 17 topics.
How many chapters are in CSS Geography Climatology?
4 chapters, containing 17 topics. The largest chapter is Pressure and Atmospheric Circulation, with 5 topics.
Are there flashcards for CSS Geography Climatology?
Yes — a 53-card Climatology deck, printed in full in the flashcards section of this page and available in the Examius app with spaced repetition. The free plan covers one exam of your choice, including its flashcards; Examius Pro, a one-time purchase, unlocks every other exam and deck.