000			021130000a22003370004500
003			EG-GICUC
005			20250223025457.0
008			061119s2004 ua a 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.2004.Fa.W.
100	0		_aFathy Mohamed Elashmawy
245	1	0	_aWhy 1998 is the warmest summer in the century / _cFathy Mohamed Elashmawy ; supervised Mohamed Magdy Abdelwahab , Hosny Mohamed said Hasanean
246	1	5	_aلماذا عام 1998 اسخن صيف فى القرن العشرين
260			_aCairo : _bFathy Mohamed Elashmawy , _c2004
300			_a94P : _bill , diagrs ; _c30cm
502			_aThesis (M.Sc.) - Cairo University - Faculty Of Science - Department Of Astronomy and Meteorology
520			_aThe study of the coefficient of variability over Egypt in summertime shows that it ranged from 394 to 1084The COV of summer temperature is usually about 5It is indicated that the summertime temperature for Lower Egypt shows stability than the summertime temperature for Upper EgyptThe pattern of increased variability in the Upper Egypt areas contrasted to the decrease of variability in the Lower areas this indicates that there are significant spatial differences in variability across Egyptian regionsThe correlations between COV and mean summertime temperature , latitude , and longitude indicated that cool stations are more variable than warm stations , also stations in the south are more variable than stations in the north and stations in the east are more variable than stations in the westRelationship between COV and latitude is highly significant , while it is non - significant with longitude and mean temperature
530			_aIssued also as CD
653		4	_a1998
653		4	_aCentury
653		4	_aWarmest summer
700	0		_aHosny Mohamed said Hasanean , _esupervisor
700	0		_aMohamed Magdy Abdelwahab , _esupervisor
856			_uhttp://172.23.153.220/th.pdf
905			_aEnas _eCataloger
905			_aMustafa _eRevisor
942			_2ddc _cTH
999			_c13815 _d13815