PDF-GLOBAL WIND STATISTICS

02201 GLOBAL INSTALLED WIND POWER CAPACITY 57375MW57374 57373 REGIONAL DISTRIBUTION End 2012 New 2013 Total End of 2013 AFRICA MIDDLE EAST Ethiopia 81 90 171 Egypt 550 550 Morocco 291 291 Tunisia 104 104 Iran 91 91. Konstantin Vinnikov & Eric . Hohman. (Office of State Climatologist for Maryland). Russell Dickerson (Atmospheric and Oceanic Science, University of Maryland). Joel . Dreessen. (Maryland Department of the Environment. Action Plan for Africa 2011-2015 . . Training Component . United Nations Economic Commission for Africa/. UNECA. Addis Ababa, Ethiopia. 27-29 August 2012. Ibrahim Mamma Hussein. Regional Adviser. UNECA/AGROST. Airborne Wind Turbine. What is it?. An airborne wind turbine is a wind power generator for harvesting power in a high altitude (sky). It has no tower and work similar like a kite. This give the benefit to easy adapt to flowing (rough vs. smooth).. Why Air Moves. Wind is created by differences in air pressure. Bigger difference = faster wind. Caused by unequal heating of earth. Air. The air by the equator is warm and rises. Low pressure. The air by the poles is cold and dense. Why Air Moves. Wind is created by differences in air pressure. Bigger difference = faster wind. Caused by unequal heating of earth. Air. The air by the equator is warm and rises. Low pressure. The air by the poles is cold and dense. 19.1 Understanding Air Pressure. Don’t notice change in your day to day activities. Mostly cause-and-effect relationship. Air pressure causes wind. Wind brings change in temperature/humidity/precipitation. Workshop on the Operation of Civil Registration, Vital Statistics and Identity Management Systems and the Production of Vital Statistics Reports for the Eastern Mediterranean Region Countries 19 – 23 March 2018, Casablanca, Morocco A look back at extreme wind events from the last 100 years uncovers six Japan typhoons – hereafter, the “Big-6” - that would cause severe industry losses given current exposure. Our ana air.  or other gases relative to a earth’s surface. . Global winds resulting from the difference in absorption of solar energy between the climatic zones on earth. . Winds . occur on a range of scales, from thunder storms where flows lasting tens of minutes, to local breezes generated by heating of . Torkil. . Veyhe. , Hans Georg Beyer, . Barður. . Niclasen. University of the Faroe Islands, . Tórshavn. , Faroe Islands. Für. On the Faroe Islands it is intended to increase the share of wind energy to the electricity supply. To improve an enhance the mapping of the wind potential, data given by a set of meteorological stations with wind measurements at . Intercomparison. of state-of-the-art . models. Bjarke Tobias Olsen (. btol@dtu.dk. ). Andrea . N. Hahmann. Anna Maria . Sempreviva. Jake Badger. Hans E. Jørgensen. Introduction. Objective. Question. Reanalyses. and CMIP6 Model Simulations. Kaiqiang. . Deng. 1. , Cesar Azorin-Molina. 1. ,2. , . Lorenzo Minola. 1. , . Gangfeng. Zhang. 3. , & . Deliang. . Chen. 1. 1. Regional Climate Group, Department of Earth Sciences, University of . SOURCES. J.H. . . Allton. 1. . K.K. . Allums. 2. , C. P. Gonzalez. 3. 1. NASA . Johnson Space Center, Houston, TX 77058. 2. HX5,LLC-Jacobs . JETS Contract, NASA Johnson Space Center, Houston, TX . 77058, . Action Plan for Africa 2011-2015 . . Training Component . United Nations Economic Commission for Africa/. UNECA. Addis Ababa, Ethiopia. 27-29 August 2012. Ibrahim Mamma Hussein. Regional Adviser. UNECA/AGROST.