The Koppen Climate Classification and its Purpose

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What is climatology? How does it differ from weather? Describe the Koppen

Climate Classification and its purpose.

Climatology is one of the several branches of physical geography, but

it differs from weather in several ways. The term climate implies an average,

or long term record of weather conditions at a certain region. It conveys a

generalization of all the recorded weather observations in a given area.

Weather conditions are recorded in specifics for any given moment in time:

the temperature, percentage of rainfall, and percentage of humidity. Climate

on the other hand, is described in more general terms. Humid Equatorial

climates, Dry climates, and Cold Polar climates are marked by certain

prevailing characteristics that can be mapped such as continuous snow or deserts.

One of the most popular classification systems is the Koppen Climate

Classification system, which gives different climates three letters that

describe that climate. The Koppen Climate Classification system is

comparatively simple and is based on a triad of letter symbols. The first

(capital) letter is the critical one; the A climates are humid and tropical;

the B climates are very dry; the C climates are humid and mild; the D

climates reflect increasing cold; and the E climates mark the polar areas.

The first letter is followed by two more letters that further define the climate

of that region. The second letter represents and explains the dry season:

whether there is or isn't a dry season, whether it is a short or long dry

season, and what season it comes in either a dry winter or a dry summer. The

third letter defines the temperature of different seasons either a hot or cool

summer or a cold or warm winter.

The purpose of the Koppen Climate Classification system is to assist in

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