Global wind patterns By : Renu R ajbahak Neha A dhikari
Contents Wind Formation of wind Coriolis effect Types of winds: Global and Local wind Prevailing wind Location of Nepal
Wind relates to air Air is the combination of all the gases – that surrouds the earth atmosphere- -like carbon dioxide, argon, oxygen, nitrogen, hydrogen and many more The movement of Air from place to place, typically from a high-pressure area to a low-pressure area i.e , wind Winds behave differently in many different places and conditions around the earth. A 'wind' is simply the flow of a huge amount of air, usually from a high pressure-area to a low-pressure area. Fig: layers of atmosphere Fig: pressure and wind direction
Formation of wind Begins with sun’s radiation- absorbed differently on the earth’s surface and heated differently – Due to cloud cover, water bodies, vegetation, uneven surface like mountains, valleys Variation of temperature on earth surfaces Air on surfaces with higher temperatures -begin to rise - it is lighter, - creates low atmospheric pressure Air on surfaces with cooler temperatures sink - sinking creates higher atmospheric pressure. Fig: formation of wind
Formation of wind The behaviour when warm gases or liquids moving upward and being replaced by cooler particles is called Convection . The energy moving during convection is called convectional current . Convection occurs in liquids and gases – land breeze and sea breeze Sea breeze occurs at day time where as land breeze at night time Fig: formation of wind Sea breeze Land breeze
Coriolis effect Wind appears to curve due to earth’s rotation Northern hemisphere- wind curves to the right Southern hemisphere- wind curve to the right
Pressure belt
Types of winds Different classified winds like gentle breeze, moderate winds, strong winds gale winds( end up as tornadoes and hurricane) Types are: Local wind and Global wind Local wind- created as a result of scenery such as mountains, vegetation, water bodies and so on- ex:sea breezes and land breezes, and mountain and valley breezes. Slope wind
Types of winds Global wind - large air masses - created mainly as a result of the earth’s rotation, the shape of the earth and the sun’s heating power . Types – Polar easterlies Prevailing westerlies Tropical easterlies/ trade winds Doldrums
Types of winds Polar easterlies- covers from 60 ° latitudes to the north and south poles- wind blows from east to west Prevailing westerlies- covers 30° to 60° latitude to the north and south - wind blows opposite direction from west to east-Horse lati tudes:Where the Westerlies meet the trade winds at about 30 degrees (Jacksonville, Florida) is the Horse latitudes , also Variables of Cancer, Subtropical High, or Subtropical ridge . This is a region of high pressure, dry air, and variable winds, and is associated with deserts over land. Trade wind- covers 0 ° to 30 ° latitude- wind blows from east to west Doldrums - 0° to 5° latitude to the north and south of equatorial area- very low pressure area caused by constant heating of the sun – calm area with very little wind
Prevailing winds Prevailing winds are the directions that wind typically come from a location Distribute large amounts of solar energy across the world Cause variety of precipitation like rain or snow
Location of nepal The main latitude and longitude of Nepal is 28° North and 84° East . small Asian country falls within the Tropic of Cancer and the Arctic Circle. The climatic condition of Nepal is not typically a temperate one as the country is located at the foothills of the Himalayas.
conclusion Hot/moist air rises up and cool/dry air sinks down Low pressure due to hot air High pressure due to cool air Coriolis –curve wind due to earth’s rotation Types local and global wind