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GS1 - climate and climate regions

CLIMATE AND CLIMATE REGIONS

Introduction

Climate refers to the long-term patterns of temperature, humidity, wind, and precipitation in a particular region over extended periods, typically 30 years or more. It encompasses the average weather conditions and the variations and extremes that occur in a given area

Definition

1.Climate vs. Weather: While climate and weather are related, they are distinct concepts. Weather describes the short-term atmospheric conditions in a specific place at a specific time, including daily fluctuations in temperature, precipitation, humidity, and wind. For example, a rainy day in London or a sunny afternoon in Mumbai are instances of weather.

i.Weather: Weather is highly variable and can change from hour to hour or day to day. It is what people experience on a daily basis and is influenced by immediate atmospheric conditions. For instance, a thunderstorm lasting a few hours or a hot spell lasting a few days are considered weather events.

ii.Climate: Climate, on the other hand, is the statistical representation of weather conditions over a longer period, usually 30 years or more. It includes not only the average conditions but also the range of variability and the frequency of extreme events. For example, the Mediterranean climate is characterized by hot, dry summers and mild, wet winters, while the climate of the Amazon rainforest is hot and humid year-round with significant rainfall.

iii.Analogy: A common analogy is that "climate is what you expect, weather is what you get." If you think of climate as a person's personality, weather is like their mood—subject to change on a daily basis.

2.Elements of Climate: The climate of a region is determined by various elements, including temperature, precipitation, humidity, wind, and atmospheric pressure. These elements interact to create the distinctive climatic conditions of a place.

i.Temperature: Temperature is a fundamental element of climate, influencing the thermal characteristics of a region. It varies with latitude, altitude, and proximity to oceans. For example, tropical regions near the equator experience high temperatures year-round, while polar regions have cold climates with significant seasonal variation.

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