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040 _aEG-GiCUC
_beng
_cEG-GiCUC
041 0 _aeng
049 _aDeposite
097 _aPh.D
099 _aCai01.12.01.Ph.D.2014.Ah.C
100 0 _aAhmed Habib Ibrahim Mohamed
245 1 0 _aContribution of land use to local circulation in the Arabian Gulf /
_cAhmed Habib Ibrahim Mohamed ; Supervised M. M. Abdelwahab
246 1 5 _aمشاركة طبيعة السطح فى محلية الدوران على منطقة الخليج العربى
260 _aCairo :
_bAhmed Habib Ibrahim Mohamed ,
_c2014
300 _a223 P. :
_bcharts , facsimiles , maps ;
_c25cm
502 _aThesis (Ph.D.) - Cairo University - Faculty of Science - Department of Astronomy and Meteorology
520 _aHe weather in many parts of the Middle East is effect by the topography, geographic location especially the subtropical regions, which located between 10{u00B0} to 21{u00B0} south and north. These areas are rarely affected by the synoptic situations approaching from the middle latitude while the local effects are the main feature that affects the weather directly and indirectly. The major finding of this work can be summarized in the following: 1. The desert climate should make use of the given conditions available for weather modification. 2. In the summer, a high percentage of the experimental seeding cases were actually suitable for seeding. Convective clouds with sufficiently warm bases, narrow droplet distributions, and cold cloud tops occur regularly during this season. The summaries and case studies support these generalizations. In order to conduct an evaluation of cloud seeding using a randomized experimental design, a large number of samples are needed. Radar statistics suggest that summer convection occurs frequently enough to produce enough candidate storms for statistical analysis in a 2-3 year program of randomized seeding. This assumes that such a program would include neighboring oman. Clearly, the summer season presents the best and most opportunities for seeding
530 _aIssued also as CD
653 4 _aArabian Gulf
653 4 _aLand
653 4 _aLocal circulation
700 0 _aMohamed Magdy Abdelwahab ,
_eSupervisor
856 _uhttp://172.23.153.220/th.pdf
905 _aNazla
_eRevisor
905 _aSoheir
_eCataloger
942 _2ddc
_cTH
999 _c50987
_d50987