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What is Climate and It’s factors

What is climate?

 

Climate is the average weather conditions in a specific region over a long period of time, typically 30 years or more. It describes the expected patterns of weather, while weather refers to the short-term atmospheric conditions you experience on any given day (e.g., sunny, rainy, windy).

What is climate?
What is climate?

How is climate different from weather?

The primary difference between weather and climate is a matter of time and scope.

  • Weather is the short-term state of the atmosphere at a specific location, changing minute-to-minute, hour-to-hour, day-to-day, and season-to-season.

  • Climate is the long-term average of weather patterns in a particular region, typically calculated over a period of 30 years or more. It represents what conditions are expected.

  • Feature Weather (Short-Term) Climate (Long-Term)
    Definition The current condition of the atmosphere in a specific place. The average weather conditions and patterns over a long period in a region.
    Time Scale Short-term: minutes, hours, days, or weeks. Long-term: decades (usually 30 years) to centuries.
    Scope Specific and localized (e.g., your city today). Regional or global (e.g., a desert climate, the global climate).
    Focus Actual atmospheric events, such as a storm or sunshine. Statistical data, trends, and variability, such as average rainfall or temperature range.
    Forecasting Studied by Meteorologists. Forecasts are short-term (e.g., tomorrow’s temperature). Studied by Climatologists. Predictions are long-term (e.g., warmer summers in 50 years).

Key Elements of Climate:-

 

When describing a region’s climate, scientists look at the statistical averages and variability of meteorological variables, including:

  • Temperature: Average high and low temperatures across different seasons.

  • Precipitation: Total rainfall, snowfall, or other forms of moisture, and their timing.

  • Wind: Average speed and direction of prevailing winds.

  • Sunshine: Average amount of daily or seasonal sunshine.

  • Extremes: The frequency and intensity of extreme weather events like heat waves, droughts, or storms.

Factors That Influence Climate:-

 

The climate of any particular place is determined by a combination of interacting physical and geographical factors:

  • Latitude (Distance from the Equator): This is the most significant factor. Areas near the equator (low latitude) receive more direct sunlight and are warmer, while areas near the poles (high latitude) receive less direct, spread-out sunlight and are colder.

  • Altitude (Elevation): As elevation increases, the air becomes thinner and less able to absorb and retain heat, causing temperatures to decrease. This is why mountains are often snow-capped even in warm regions.

  • Proximity to Water Bodies: Large bodies of water (like oceans and large lakes) have a moderating effect on temperatures because water heats up and cools down slower than land. Coastal areas tend to have milder winters and cooler summers (maritime climate) compared to inland areas (continental climate) at the same latitude.

  • Ocean Currents: Currents circulate warm or cold water around the globe, influencing the temperature of nearby landmasses. For example, warm currents can keep some coastal areas much milder in winter than expected for their latitude.

  • Topography (Shape of the Land): Mountain ranges can create a rain shadow effect. The windward side (facing the wind) receives high rainfall as moist air is forced up and cools, while the leeward side (sheltered side) experiences dry conditions.

  • Prevailing Winds and Air Masses: The direction from which dominant winds blow determines whether an area receives warm/cold or moist/dry air masses.

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    Since climates vary dramatically across the globe, scientists use classification systems to group regions with similar weather patterns.1 The most widely used system is the Köppen Climate Classification, which categorizes climates based on average annual and monthly temperature and precipitation.

    The Köppen system divides the world into five main climate groups, represented by capital letters:3

    Group Letter Name Key Characteristics Examples
    A Tropical Hot and humid; average temperature is 18 C  (64.4 F) or higher in all months. High rainfall. Amazon Rainforest, Congo Basin
    B Dry (Arid/Semi-Arid) Defined by lack of precipitation, where evaporation exceeds rainfall. Wide daily temperature range. Sahara Desert (Hot), Gobi Desert (Cold)
    C Temperate (Mild) Warm, humid summers and mild winters. Coldest month average is between -3C and 18C. Mediterranean coast, Southeastern United States
    D Continental Warm to cool summers and very cold winters. At least one month averages below -3C and at least one month averages above 10C. Inland regions of Canada, Siberia
    E Polar Extremely cold with limited plant life. All months have an average temperature below 10C . Antarctica, Greenland

Climate in India

The climate of India is broadly classified as a tropical monsoon climate, characterized by a significant seasonal variation in temperature and rainfall across its vast and diverse geographical landscape.

Why India has a monsoon type of climate?

 

India experiences a monsoon type of climate primarily due to the differential heating and cooling of the landmass and the surrounding oceans, which leads to a seasonal reversal of wind direction.

Seasons in India

 

The India Meteorological Department (IMD) officially recognizes four seasons:

1. The Hot Weather Season (Summer)

 

        (March to May/June)

  • Characteristics: This is the season of rising temperatures and a sharp drop in atmospheric pressure over the northern plains.

  • Temperature: Temperatures soar, often exceeding $40^\circ\text{C}$ in North and Central India, with the hottest months typically being April and May. Coastal areas are relatively milder due to the influence of the sea.

  • Weather: Characterized by hot, dry local winds like the ‘Loo’ in the North-West, and occasional dust storms.

  • summer


 2. The South-West Monsoon Season (Rainy Season)

 

        (June to September)

  • Characteristics: This season is marked by the onset and advance of the South-West Monsoon winds, which bring the majority of India’s annual rainfall.

  • Wind & Pressure: High pressure over the Indian Ocean forces moisture-laden winds to blow toward the low-pressure area over the heated landmass.

  • Rainfall: The winds split into the Arabian Sea branch and the Bay of Bengal branch, causing heavy rainfall over the west coast (Western Ghats) and North-Eastern India. Rainfall is crucial for Indian agriculture (Kharif crops).

  • winter


3. The Retreating Monsoon Season (Post-Monsoon/Autumn)

 

        (October to November)

  • Characteristics: This is a transition period as the monsoon trough weakens and retreats from the northern plains.

  • Weather: Clear skies and a rise in temperature and humidity characterize the first half of this period, often referred to as ‘October Heat’.

  • Wind Reversal: The low-pressure area shifts to the south, leading to the establishment of the North-East Monsoon circulation over the Bay of Bengal. This retreating monsoon is the main source of rainfall for the Tamil Nadu coast.

monsoon

4. The Cold Weather Season (Winter)

 

         (December to February)

  • Characteristics: This is the season of low temperatures and clear skies, established as a high-pressure system dominates the northern landmass.

  • Temperature: Temperatures are cool to cold in North India, with parts of the Himalayas receiving snowfall. Temperatures rise gradually from north to south.

  • Weather: Cold waves and dense fog are common in the northern plains. Rainfall is generally minimal across the country, except for the winter cyclonic disturbances (Western Disturbances) which bring light rain to the North-West plains, benefiting Rabi crops.

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