000			02687cam a2200313 a 4500
003			EG-GiCUC
008			191201s2019 ua do f m 000 0 eng d
040			_aEG-GiCUC _beng _cEG-GiCUC
041	0		_aeng
049			_aDeposite
097			_aM.Sc
099			_aCai01.12.01.M.Sc.2019.Mo.I
100	0		_aMoetasm Hashem Eltaweel
245	1	0	_aImprovement of precipitation performance in wrf model over Egypt / _cMoetasm Hashem Eltaweel ; Supervised Mohamed Magdy Abdelwahab , Elsayed Mohamed Robaa
246	1	5	_aعلى مصر (WRF) تحسين توقع كمية الأمطار فى نموذج التنبؤ العددى
260			_aCairo : _bMoetasm Hashem Eltaweel , _c2019
300			_a73 P. : _bcharts , photographs ; _c25cm
502			_aThesis (M.Sc.) - Cairo University - Faculty of Science - Department of Astronomy and Meteorology
520			_aThis work aimed to investigate the precipitation prediction problem over Egyptian domain using (NWP) model on mesoscale grid called weather research and forecasting model (WRF) with ARW dynamical core and to improve the sensitivity of resulted precipitation amounts the cloud resolving model (CRM) configuration is been utilized in this study on both (12) Cumulus Convective (CU) and (19) microphysical Parameterization schemes with a coarse domain of 27 Km and fine domain on Egypt area with resolution of 3 Km. By the aid of error estimate variables and observational data comparisons the improved (CU) options appeared to be highly affected by convective amount presence and the improvement only when convective precipitation is the lowest one which was Betts-Miller-Janjic scheme and the the (MP) best performance options was the single moment schemes such as (Lin and WSM5) which perform better with high resolution and CRM configuration in high convective simulations than the double moment schemes such as (Morrison and NSSL) which perform better in the non-convective simulations. Hence, the WRF model shows an obvious overestimation results over the Egyptian domain in extreme rainy events with high convective precipitation. In addition this study showed a more detailed investigation in Microphysical species such as (QCLOUD, QRAIN, SNOW, CAPE, QFX and Surface Evaporation) and those species remarkably affected by configuration and provided more enhancement in precipitation prediction amounts
530			_aIssued also as CD
653		4	_aCumulus convection
653		4	_aMicrophysics
653		4	_aWRF
700	0		_aElsayed Mohamed Abdelhamed Robaa , _eSupervisor
700	0		_aMohamed Magdy Abdelwahab , _eSupervisor
905			_aNazla _eRevisor
905			_aSamia _eCataloger
942			_2ddc _cTH
999			_c75596 _d75596