Concept

In Köppen’s climate classification, ET means tundra climate. The average temperature of the warmest month is at least 0°C but below 10°C. Such low temperatures prevent the normal growth of tall trees, although mosses and small plants may survive. Am denotes tropical monsoon climate, BWh hot desert climate, and Cs Mediterranean climate, so none of those symbols fits ET.

In Köppen’s classification, EF denotes ice-cap climate. Even the average temperature of the warmest month remains below 0°C, so permanent snow and ice cover the surface and vegetation is extremely limited. BS represents steppe climate, Aw represents tropical savanna, and Am represents tropical monsoon climate. Therefore, ice-cap climate is the only correct interpretation of EF.

Köppen Group A represents tropical climates, which are generally hot because their monthly temperatures remain high throughout the year. Many Group A climates are also humid, although their rainfall pattern may differ: Af has no distinct dry season, Am is monsoonal, and Aw has a dry winter. Group E is polar, Group B is dry, and altitude alone does not define a group.

Group B in Köppen’s system is the dry-climate group. Its defining feature is that precipitation is insufficient compared with the moisture lost through potential evaporation, producing a water deficit. BW climates are deserts and BS climates are steppes or semi-arid regions. Dense rainforest belongs mainly to Group A, while permanent ice and tundra belong to Group E.

Köppen Group C represents warm temperate or mild mid-latitude climates. These regions have a relatively mild winter compared with Group D and are not as cold as polar Group E. They may have dry summers, dry winters, or rainfall in all seasons; Cs is Mediterranean, for example. Group B is dry and Group E includes tundra and ice-cap climates.

Group D is commonly called the snow or continental climate group and is characterized by cold winters. It generally occurs in higher-latitude interiors where seasonal temperature contrasts are strong. This group is not defined by dryness alone, and it can receive substantial snow or rain. Group C has milder winters, Group B is dry, and Group E is polar.

Group E represents polar climates in Köppen’s classification. The average temperature of the warmest month remains below 10°C. ET is tundra climate, where the warmest month is at least 0°C but below 10°C, while EF is ice-cap climate, where it remains below 0°C. Equatorial and monsoon climates belong to Group A, and hot deserts belong to Group B.

Am is the Köppen symbol for tropical monsoon climate. The capital A places it in the tropical group, while m identifies the monsoonal rainfall pattern, usually with a short or less pronounced dry period. Af is tropical rainforest climate with no distinct dry season, BS is steppe climate, and ET is tundra. Thus Am is the only suitable symbol.

Aw denotes tropical savanna climate. A identifies the tropical group, and w indicates a dry winter; consequently, rainfall is concentrated mainly in the warmer part of the year. Af is tropical rainforest climate with rainfall in every month, EF is ice-cap climate, and Cf is a warm temperate climate with rainfall throughout the year. Therefore Aw is correct.

Af is the symbol for tropical rainforest climate. A indicates a tropical climate, and f means that there is no distinct dry season; every month receives sufficient rainfall under the classification criterion. BW is desert climate, Cs is Mediterranean climate with dry summers, and ET is tundra. The combination Af therefore identifies a hot, wet rainforest environment.

Cs is the usual Köppen symbol for Mediterranean climate. C places it in the warm temperate group, while s indicates a dry summer. Mediterranean regions typically have warm, dry summers and milder, wetter winters. Am is tropical monsoon, BW is desert, and EF is ice-cap climate, so those symbols do not match the characteristic seasonal rainfall of the Mediterranean type.

In the dry-climate group B, lowercase h indicates a hot thermal condition, conventionally a mean annual temperature of 18°C or more. Thus BWh means a hot desert climate: BW identifies desert conditions and h identifies the hot thermal subtype. Lowercase k indicates a cold dry climate, while winter rainfall and ice-cap conditions are represented by different symbols.

Within Köppen Group B, lowercase k marks the cold thermal subtype of a dry climate, conventionally associated with a mean annual temperature below 18°C. BWk therefore means cold desert, while BSk means cold semi-arid steppe. The letter h marks the hot subtype; rainfall throughout the year and summer dryness belong to other parts of the Köppen system.

In Köppen temperature suffixes, lowercase a means a hot summer. The average temperature of the warmest month is at least 22°C. For example, Cfa has a hot summer, although it may also have rainfall throughout the year. Lowercase b indicates a warm or mild summer, while w describes a dry winter; neither severe winter nor dry winter is the meaning of a.

Lowercase b is a temperature suffix indicating a warm or mild summer. The warmest month has a mean temperature below 22°C, but at least four months have means above 10°C. Cfb is a familiar example. Lowercase a means a hotter summer, w indicates dry winter, and continuous snow is related to polar conditions rather than the b suffix.

Köppen symbols provide a concise and systematic way to classify climates using measurable temperature and precipitation characteristics. The first capital letter identifies the major group, while later letters describe rainfall seasonality or thermal conditions. For example, Csa indicates a warm temperate climate with dry summers. River length, population, and mineral output are unrelated to this classification.

Af is the tropical rainforest climate in Köppen’s system. Its defining rainfall feature is the absence of a distinct dry season: every month receives sufficient precipitation according to the classification rule. A long dry season would suggest a different climate, such as savanna or a seasonal tropical type. Aw has a dry winter, while Mediterranean Cs has a dry summer, so neither describes Af.

Am is tropical monsoon climate, so seasonal monsoon circulation is commonly the main source of its rainfall. Moist air, often arriving from nearby seas or oceans, is forced to rise and produces heavy seasonal rain. Glacier melting is not a rainfall mechanism, desert winds are generally dry, and polar night is a seasonal absence of sunlight rather than a source of precipitation.

In Aw, the capital A identifies a tropical climate and the lowercase w indicates a dry winter. Rainfall is therefore concentrated mainly in the summer or warmer season, while winter is comparatively dry. This differs from As, where summer is dry, and from Af, where no distinct dry season occurs. The term ‘rainy season’ cannot itself be the dry season, so it is not a suitable answer.

BW is the desert subtype of Köppen’s dry Group B and is drier than BS. In BW climates, precipitation is extremely limited compared with potential evaporation. BS represents steppe or semi-arid climate, which receives somewhat more precipitation and can support more grassland. Af is a wet tropical rainforest climate, so it is not a dry-climate alternative at all.