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Click to edit Master title style• Click to edit Master text styles• Second level• Third level• Fourth level• Fifth level The Positive NAO index phaseshows a stronger than usualsubtropical high pressure centerand a deeper than normal Icelandiclow. The increased pressuredifference results in more andstronger winter storms crossing theAtlantic Ocean on a more northerlytrack. This results in warm and wetwinters in Europe and in cold anddry winters in northern Canada andGreenlandWMODrought and Desertification Workshop, Alanya, 14-16 November 200622TSMS
Click to edit Master title stylepathway.• Click to edit Master text styles• Second level• Third level• Fourth level• Fifth level The negative NAO index phase: aweak subtropical high and a weakIcelandic low. The reduced pressure gradientresults in fewer and weaker winterstorms crossing on a more west-east They bring moist air into theMediterranean and cold air tonorthern Europe The US east coast experiencesmore cold air outbreaks and hencesnowy weather.WMODrought and Desertification Workshop, Alanya, 14-16 November 200623TSMS
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Page 3 and 4: Predicting Drought at regional base
Page 6 and 7: c. Time scalesClick to edit Master
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Page 14 and 15: What about the Future?Click to edit
Page 18 and 19: mPMAJOR AIR MASSES THAT AFFECT CLIM
Page 20 and 21: TOPOGRAPHY OF TURKEYClick to edit M
Page 24: RELATIONSHIP BETWEEN ANNUAL PRECIPI

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