Key Points

World Climate and Climate Change

16 Sections
  • Three Approaches to Climate Classification

    Climate is classified using three broad approaches. These are empirical (based on observed data like temperature), genetic (based on causes), and applied (for a specific purpose).

  • Koeppen's Climate Classification Scheme

    The most widely used system is V. Koeppen's empirical classification. It connects climate with vegetation distribution using mean annual and monthly temperature and precipitation data.

  • Koeppen's Five Major Climatic Groups

    Koeppen identified five major climatic groups using capital letters. A, C, D, and E represent humid climates, while B represents dry climates.

  • Group A: Tropical Humid Climates

    Group A climates are defined by an average temperature of 18 C or higher in the coldest month. Sub-types include Af (Tropical wet), Am (Tropical monsoon), and Aw (Tropical wet and dry).

  • Group B: Dry Climates

    In Group B climates, potential evaporation is greater than precipitation. They are subdivided into Steppe or semi-arid (BS) and Desert (BW).

  • Group C: Warm Temperate Climates

    These mid-latitude climates have a coldest month average temperature higher than minus 3 C but below 18 C. They generally have warm summers and mild winters.

  • Group D: Cold Snow Forest Climates

    Found in large continental areas in the Northern Hemisphere, Group D climates have a coldest month average temperature of minus 3 C or below.

  • Group E: Cold Climates

    Group E climates exist poleward of 70 degrees latitude and have an average temperature below 10 C for all months. They include Tundra (ET) and Ice Cap (EF) climates.

  • Koeppen's Sub-classification Letters

    Small letters indicate precipitation patterns: f for no dry season, m for monsoon, w for winter dry, and s for summer dry. Small letters a, b, c, d refer to temperature severity.

  • Climate Change as a Natural Process

    Geological records, tree rings, and historical accounts show that climate change is a natural and continuous process. Earth has witnessed many alterations between glacial and inter-glacial periods.

  • Recent Climate Variability

    The 1990s was the warmest decade of the 20th century. The year 1998 is considered the warmest year of the millennium.

  • Causes of Climate Change

    Causes are grouped into astronomical (sunspots, Milankovitch cycles) and terrestrial (volcanism). The most important human-induced cause is the increasing concentration of greenhouse gases.

  • The Greenhouse Effect Explained

    The greenhouse effect is the process where certain gases in the atmosphere trap long-wave radiation from the Earth's surface, causing the atmosphere to warm.

  • Primary Greenhouse Gases (GHGs)

    The main greenhouse gases are Carbon Dioxide (CO2), Chlorofluorocarbons (CFCs), Methane (CH4), Nitrous Oxide (N2O), and Ozone (O3). CO2 is the most abundant.

  • The Kyoto Protocol

    Proclaimed in 1997, the Kyoto Protocol is an international agreement that binds industrialized nations to reduce their emissions of greenhouse gases.

  • Consequences of Global Warming

    Global warming can lead to rising sea levels from melting glaciers and thermal expansion of seawater. This threatens to inundate large coastal areas and islands.

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