Key Points
- 1Three 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).
- 2Koeppen'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.
- 3Koeppen'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.
- 4Group 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).
- 5Group 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).
- 6Group 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.
- 7Group 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.
- 8Group 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.
- 9Koeppen'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.
- 10Climate 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.
- 11Recent Climate Variability
The 1990s was the warmest decade of the 20th century. The year 1998 is considered the warmest year of the millennium.
- 12Causes 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.
- 13The 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.
- 14Primary 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.
- 15The Kyoto Protocol
Proclaimed in 1997, the Kyoto Protocol is an international agreement that binds industrialized nations to reduce their emissions of greenhouse gases.
- 16Consequences 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.
- • Review these points before exams
- • Make flashcards for better retention
- • Connect points to real-world examples
- • Practice explaining each point in your own words