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Climate Classification Systems Questions and Answers

Answer: A

Correct answer: temperature and rainfall thresholds

Koppen defined his classes by numerical limits on monthly and annual temperature and precipitation - the coldest month above or below a stated value, the driest month against a rainfall threshold, and so on. Those two variables were chosen because they were widely measured and because they governed the vegetation he was really classifying.

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2.

Assertion (A): The Koppen system is described as an empirical classification.
Reason (R): Its boundaries were chosen to match observed vegetation limits rather than derived from circulation.

Answer: B

Correct answer: Both A and R are true, and R is the correct explanation of A

Both are true and the reason gives the sense in which the system is empirical. Koppen was a botanist, and he set his thresholds where the observed vegetation changed - the 10 degree isotherm of the warmest month at the tree line, the 18 degree coldest-month limit for tropical vegetation. The boundaries therefore describe what is there rather than following from any theory of why, which is exactly what distinguishes an empirical classification from a genetic one.

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3.

Match each Koppen letter with the climate group it denotes.
List I
A. A
B. B
C. C
D. D
List II
1. temperate, with a mild winter
2. tropical, with every month above eighteen degrees
3. continental, with a cold winter
4. dry, where evaporation exceeds precipitation

Answer: C

The fifth group, E, covers polar climates where no month is warm. The first letter fixes the broad type and the following letters refine the seasonality of precipitation and the summer temperature. Five groups cover the world.

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Answer: D

Correct answer: aridity, on a variable threshold

Group B is the dry group, and its threshold is not a fixed rainfall figure: it depends on the mean annual temperature, because warmer air evaporates more, and on the seasonality of the rain, because summer rain is less effective than winter rain. A place can therefore be arid at 500 mm and humid at 300 mm depending on where and when the rain falls.

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5.

Assertion (A): The dry group in Koppen's scheme is defined against a temperature dependent threshold.
Reason (R): Evaporation rises with temperature, so more rain is needed to avoid aridity in a warm climate.

Answer: A

Both are true and the reason gives the logic, and it is why a place with four hundred millimetres may be arid in the tropics and humid in a cold climate. Demand as well as supply enters the test. Warm climates need more rain to stay humid.

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6.

Consider the following statements about the Koppen system.
1. The first letter denotes the broad climate group.
2. Subsequent letters describe precipitation seasonality and temperature.
3. The system is derived from the general circulation.

Answer: B

Correct answer: 1 and 2 only

Statements 1 and 2 describe the coding correctly - the first letter gives the broad group, the second the precipitation pattern and the third the temperature detail. Statement 3 is wrong, and it is the standing contrast in this topic: Koppen is empirical, built on observed thresholds, while a genetic classification derives its types from the general circulation that causes them.

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Answer: C

Correct answer: temperate, with no dry season

Reading the three letters in turn: C is the temperate group, f means no dry season - precipitation in every month - and b means a warm rather than hot summer, the warmest month below 22 degrees. It is the climate of north-western Europe, New Zealand and the Pacific north-west of North America.

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8.

Match each Koppen code with a place that exemplifies it.
List I
A. Af
B. BWh
C. Cs
D. ET
List II
1. coastal California or southern Italy
2. the Amazon or Congo basin
3. the Arctic tundra
4. the central Sahara

Answer: D

Learning a representative place for each code fixes the system far better than memorising the thresholds. The s in the third denotes a dry summer, which is the Mediterranean signature. A place fixes a code better than a threshold.

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Answer: A

Correct answer: potential evapotranspiration

Thornthwaite computes how much water the atmosphere could evaporate given the temperature and day length, compares it with the precipitation, and classifies on the resulting moisture surplus or deficit. That makes it a water balance approach, better suited to agriculture and hydrology than Koppen’s thresholds, at the cost of needing a calculation rather than a look-up.

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10.

Assertion (A): Thornthwaite's scheme is more useful than Koppen's for agricultural planning.
Reason (R): It works from a monthly water balance of supply against demand.

Answer: B

Both are true and the reason gives the advantage, since the surplus and deficit it computes are directly what an irrigation or drainage decision requires. Surplus and deficit are computed monthly. Data demands are heavier than for Koppen.

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