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008 161130s2016 my ab f abm 000 0 eng d
020 _aTHE0000420(Local)
039 9 _a201905151438
_bnazirah
_y201611300954
_zsaini
040 _aUMP
090 _aFKASA .F389 2016 r Bc.
100 0 _aFauzan Hanisah Zulhaimi
245 1 0 _aPrediction of water stream flow in the context of climate change /
_cFauzan Hanisah Zulhaimi
260 _aKuantan, Pahang :
_bUMP,
_c2016
300 _axiii, 78 p. :
_bill. (some col.), maps (some col.) ;
_c30 cm. +
_e1 CD-ROM
500 _aFaculty of Civil Engineering and Earth Resources
502 _aProject Paper (Bachelors of Civil Engineering) -- Universiti Malaysia Pahang – 2016
504 _aBibliography : p. 72-78
520 3 _aThe increase in global surface temperature in response to the changing composition of the atmosphere will significantly impact upon local hydrological process and water sources. This situation will lead to the need for an assessment of regional climate change impacts. The application of Statistical Downscaling Model (SDSM) and Identification of Unit Hydrograph and Component Flows from Rainfall, Evaporation and Streamflow Data (IHACRES) were used as rainfall runoff models to stimulate streamflow event in Sungai Kecau, Kuala Lipis, Pahang catchment based on daily rainfall. The rainfall station is taken at Kampung Bandar at Ulu Kechau. The SDSM model is the derivation of National Centre for Environmental Prediction (NCEP) reanalysis data and observation of locally methodological variables that have been calibrated using large – scale predictors variables. The SDSM model validation has been done by independent period of NCEP reanalysis. The outcome obtained was used to generate the possible future scenarios of meteorological variables and then the input is used to the IHACRES model. Stimulation of corresponding future streamflow changes was stimulated by IHACRES model and the observed station data in the catchment Sungai Kecau, Kampung Dusun.
610 2 0 _aFaculty of Civil Engineering and Earth Resources
_xDissertations
650 0 _aUniversities and Colleges
_xDissertations
650 0 _aTheses
999 _aVIRTUA40
_c6715
_d6721
999 _aVTLSSORT0080*0200*0400*0900*1000*2450*2600*3000*5000*5020*5040*5200*6100*6500*6501*9992