Showing posts with label climate. Show all posts
Showing posts with label climate. Show all posts

Monday, 26 November 2012

Middle East and Africa


Climates of the Middle East & Africa.





Population of the Middle East & Africa.




Middle East & Africa: Religion.




Middle East & Africa: Language




Climate


Climate
Climate is defined as the avarage weather conditions at a specific place over a long period. The standard averaging period is 30 years. 
Weather is what the forecasters on the television news predict each day. Weather is elements which we see daily, such as temperature, rain and wind. These can change hour by hour, day by day. Climate on the other hand looks at how the weather changes over a long period of time, typically over 30 years. It can be thought of as the average weather over a long period.




The difference between weather and climate
The difference between weather and climate is a measure of time. Weather is what conditions of the atmosphere are over a short period of time, and climate is the average weather in a place over many years. While the weather can change in just a few hours, climate takes hundreds, thousands, even millions of years to change.




Climate classification system
Scientists (e.g. Wladimir Köppen) have been able to define climate zones around the world. Here in the Netherlands, we have a ‘temperate’ climate that is neither especially hot nor cold, wet nor dry, when compared to other climates. It is a very different climate to that in the Sahara for example, which is known as arid because throughout the year the weather is dry and hot.



Wladimir Köppen (1846-1940), was a Russian-born German climatologist who developed a systematic method of classifying the climates of the world based on long-term patterns of the distribution of temperature and precipitation around 1900. His classification remains the most used climate classification system up to the present day.

Climate and vegetation
The distribution of vegetation is strongly correlated with climate patterns.







Thursday, 24 November 2011

Köppen - climate classification system




Wladimir Köppen (1846-1940), was a Russian-born German climatologist who developed a systematic method of classifying the climates of the world based on long-term patterns of the distribution of temperature and precipitation around 1900. His classification remains the most used climate classification system up to the present day.



Köppen – climate classification system
examples
Tropical climates

Af
Tropical rainforest climate

Belém, Brazil
Aw
Tropical wet and dry / savanna climate
Lagos, Nigeria
Dry (arid and semi-arid) climates
BS
Steppe climate
Denver, Colorado, United States
BW
Desert climate
Dubai, United Arab Emirates
Temperate climates
Cs
Mediterranean climate, dry season in the summer
Barcelona, Spain
Cw
Temperate maritime climate, dry season in the winter
Zhengzhou, China
Cf
Temperate maritime climate, no dry season
Roermond, The Netherlands
Continental climates
Df
Continental climate, no dry season
Chicago, Illinois, United States
Dw
Continental climate, dry in the winter
Vladivostok, Russia
Polar climates
ET

Tundra climate
Vardø, Norway
EF

Ice Cap climate
Antarctica
EH

Highland climate
The Himalayas




Köppen – climate classification system - world map



Thursday, 20 October 2011

Basics of Geography: Climate

http://www.youtube.com/watch?v=95TtXYjOEv4&feature=results_video&playnext=1&list=PL08EA6BBD906C7474


Climate is commonly defined as the weather averaged over a long period. The standard averaging period is 30 years.

Climate includes temperature, humidity, atmospheric pressure, wind and rainfall.
Climate can be contrasted to weather, which is the present condition of these elements and their variations over shorter periods.
The climate of a location is affected by its latitude, terrain, and altitude, as well as nearby water bodies and their currents.


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