Koppen's Climatic Classification

Koppen Classification of Climate:
 For decades, a climate classification devised by WladimirKöppen (1846–1940) has been the best-known and most used tool for presenting the world pattern of climates.

The Köppen classificationuses easily obtained data: mean monthly and annual values of temperature and precipitation.

Furthermore, the criteria are unambiguous, simple to apply, and divide the world into climate regions in a realistic way.

Köppen believed that the distribution of natural vegetation was the best expression of an overall climate.

Consequently, the boundaries he chose were largely based on the limits of certain plant associations.

For decades, a climate classification devised by WladimirKöppen (1846–1940) has been the best-known and most used tool for presenting the world pattern of climates.

The Köppen classificationuses easily obtained data: mean monthly and annual values of temperature and precipitation.

Furthermore, the criteria are unambiguous, simple to apply, and divide the world into climate regions in a realistic way.

Köppen believed that the distribution of natural vegetation was the best expression of an overall climate.

Consequently, the boundaries he chose were largely based on the limits of certain plant associations.

Köppen’s Classification Scheme:

Köppen recognized five principal climate groups, each designated with a capital letter:

A(humid tropical),

B(dry),

C(humid middle-latitude, mild winters),

D(humid middle-latitude, severe winters),and

E(polar).

Four groups (A, C, D, E) are defined by temperature.

The fifth, the B group, has precipitation as its primary criterion.

Climate Controls:

Order exists in the distribution of climate elements and the pattern of climates is not by chance.

The world's climate pattern reflects a regularand dependable operation of the major climate controls.

 Climate Controls (cont.)

The major controls of climate are::

(1) latitude(variations in the receipt of solar energy and temperature differences are largely a function of latitude),

(2) land/water influence(marine climatesare generally mild, while continental climatesare typically much more extreme),

(3) geographic position and prevailing winds(the moderating effect of water is more pronounced along the windward side of a continent),

(4) mountains and highlands(mountain barriers prevent maritime air masses from reaching far inland, trigger orographic rainfall, and where they are extensive, create their own climatic regions),

(5) ocean currents(poleward-moving currents cause air temperatures to be warmer than would be expected), and

(6) pressure and wind systems(the world distribution of precipitation is closely related to the distribution of Earth's major pressure and wind systems).

Type A Climate:

Situated along the equator, the wet tropics(Af, Am) constant high temperatures and year-round rainfall combine to produce the most luxuriant vegetation in climatic realm—the tropical rain forest.

Temperatures in these regions usually average 25°C (77°F) or more each month and the daily temperature variations characteristically greatly exceed seasonal differences.

Precipitation in Afand Am climates is normally from 175 to 250 centimeters (68 to 98 inches) per year and is more variable thantemperature, both seasonally and from place to place.

Thermally induced convection coupled with convergence along the intertropicalconvergence zone(ITCZ)leads to widespread ascent of the warm, humid, unstable air and ideal conditions for precipitation.

Type B Climate:

Dry regions of the world cover about 30 percent of Earth's land area.

Other than their meager yearly rainfall, the most characteristic feature of dry climates is that precipitation is very unreliable.

Climatologists define a “dry climate”as one in which the yearly precipitation is less than the potential water loss by evaporation.

To define the boundary between dry and humid climates, the Köppen classification uses formulas that involve three variables:

(1) average annual precipitation,

(2) average annual temperature, and

(3) seasonal distribution of precipitation.

Type C Climate:

Humid middle-latitude climateswith mild winters (C climates) occur where the average temperature of the coldest month is less than 18°C (64°F) but above -3°C (27°F).

Several C climate subgroups exist.

Type D Climate:

Humid continental climates with severe winters(D climates) experience severe winters.

The average temperature of the coldest month is -3°C (27°F) or below and the average temperature of the warmest month exceeds 10°C (50°F).

The greatest annual temperature ranges on Earth occur here.

Type E Climate:

Polar climates(ET, EF) are those in which the mean temperature of the warmest month is below 10°C (50°F).

Annual temperature ranges are extreme, with the lowest annual means on the planet.

Although polar climates are classified as humid, precipitation is generally meager, with many nonmarine stations receiving less than 25 centimeters (10 inches) annually.

Polar Climates:

Two types of polar climates are recognized.

Found almost exclusively in North America, the tundra climate(ET), marked by the 10°C (50°F) summer isotherm at its equatorward limit, is a treeless region of grasses, sedges, mosses, and lichens with permanently frozen subsoil, called permafrost.

The ice cap climate(EF) does not have a single monthly mean above 0°C. Consequently, the growth of vegetation is prohibited, and the landscape is one of permanent ice and snow.