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| This weeks hot offer 
  24: Series 5 
 In association with Amazon.co.uk £26.97
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| Contents
 
 
  Climate versus weather 
  Climate determinants 
  Climate indices 
  Classifications 
 
 
 
  Climate versus weather - Contents 
 In the most succinct words, weather is the combination of events in the atmosphere and climate is the overall accumulated weather in a certain location.The exact boundaries of what is climate and what is weather are not well defined and depend on the application. For example, in some senses an individual  El Niño event could be considered climate; in others, as weather.When the original conception of climate as a long-term average came to be considered, perhaps towards the end of the 19th century, the idea of  climate change was not current, and a 30 year average seemed reasonable (but see  note 1). Given the current availability of long-term trends in the  temperature record, it is harder to give a precise noncontradictory definition of climate: over a 30 year period, averages may shift; over a shorter period, the statistics are less stable.
 
 
 
  Climate determinants - Contents 
 In a given geographical region, the climate generally does not vary over time on the scale of a human life span. However, over  geological time, climate can vary considerably for a given place on the Earth. For example,  Scandinavia has been through a number of ice ages over hundreds of thousands of years (the last one ending about 10,000 years ago).  Paleoclimatology is the study of these past climates, their origin, and by extension, the origin of today's climate.Over historic time spans there are a number of static variables that determine climate including: altitude, proportion of land to water, and proximity to oceans and mountains. Other climate determinants are more dynamic: The  thermohaline circulation of the ocean distributes heat energy between the equatorial and polar regions; other  ocean currents do the same between land and water on a more regional scale. Degree of vegetation coverage affects solar heat absorption, water retention, and rainfall on a regional level. Alterations in the quantity of atmospheric greenhouse gases determines the amount of solar energy retained by the planet, leading to global warming or  global cooling. The variables which determine climate are numerous and the interactions complex but there is general agreement that the broad outlines are understood, at least in so far as the determinates of historical climate change are concerned.
 
 
 
  Climate indices - Contents 
 Scientists use climate indices in their attempt to characterize and understand the various climate mechanisms that culminate in our daily weather. Much in the way the Dow Jones Industrial Average, which is based on the stock prices of 30 companies, is used to represent the fluctuations in the stock market as a whole, climate indices are used to represent the essential elements of climate. Climate indices are generally identified or devised with the twin objectives of simplicity and completeness, and each typically represents the status and timing of the climate factor they represent. By their very nature, indices are simple, and combine many details into an generalized, overall description of the atmosphere or ocean which can be used to characterize the factors which impact the global climate system. Because the climate indices are generally determined from measurements made in a localized area, they can have impacts in other areas around the globe, through processes sometimes called teleconnections.References:
 
       
         Why and how do scientists study climate change in the Arctic? What are the Arctic climate indices?
         Climate index and mode information 
 
 
  Classifications - Contents 
 In the original sense, climate is a concept used to divide the world into regions sharing similar climatic parameters. Climate regions can be classified on the basis of temperature and  precipitation alone. Examples of such climate schemes are the  Köppen climate classification or the  Thornthwaite climate classification schemes.For more details about specific climates, see:
 
       For the climate of a specific place or area, see the article on that place or area.
         Tropical climate
         Subtropical climate
         Arid climate
         Semiarid climate
         Mediterranean climate
         Temperate climate
         Oceanic climate
         Continental climate
         Alpine climate
         Subarctic climate
         Polar climate
         Climate of Antarctica |  
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