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HYDROLOGICAL MODELING IN YUVACIK DAM BASIN WITH GIS INTEGRATION. HOW CAN WE MODEL THE HYDROLOGY OF A BASIN

Автор:   Fatih K.
мягкая обложка
148 страниц
2009 год
Издательство:   Книга по Требованию
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2413 руб
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Описание:In order to model the Yuvacik dam basin, semi-distributed hydrological model studies were carried out with the Mike11 model. The resulting CN values were used in the UHM module and the suggested CN approach has been validated with the classical SCS-CN approach with GIS analysis. The largest peaks of inflow were observed when the storm events occur due to both snowmelt and rain. Rainfall-Runoff Model (NAM) module of the model was used for the simulation of daily snowmelt and rain on snow events and Unit Hydrograph Method (UHM) module was used for the simulation of hourly rainfall events. A new methodology is suggested for the determination of Curve Number (CN) of the sub-basins by using the fractional area and topographic index values combined with hourly model simulations. The basin with a drainage area of 257. 8 km2 is located in 12 km South East of Izmit city in Turkey. Therefore, observed flows for the period of 2001-2006 were grouped as daily and hourly storm events according to the event types such as rainfall, snowmelt or mixed events. Hydrological modeling is an important issue for determining the hydrological responses of a basin under several weather conditions.


Orthomol Immun Junior Сила иммунитета на страже Вашего ребенка Orthomol Immun Junior Сила иммунитета на страже Вашего ребенка

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The World in 2050: Four Forces Shaping Civilization's Northern Future

When it comes to climate genies, the West Antarctic Ice Sheet is an ugly-looking lamp. Frankly, we donБЂ™t understand the physics of sliding glaciers and ice sheet collapses well enough yet to model the futures of Greenland and Antarctica with confidence. Many things affect the speed and dynamics of that long slide that are hard to measure or see. They include the interplay between the sliding ice and its bed, the heat and lubrication added by meltwater percolating to the bed from the surface, the importance of buttressing ice shelves (which help dam ice up on the land), the ocean water temperature at the ice edge, and others.507 Computer models and field studiesБЂ”like the one Jason and I were conducting in GreenlandБЂ”are in their infancy. Scientists are still discovering new things and debating what may or may not be important. This is why the likelihood of accelerated sea-level rise was kept out of the last IPCC assessment, and may be kept out of the next one as well. Might the ice sheets start slipping faster, with higher sea levels right behind? PerhapsБЂ”but without well-constrained models, we donБЂ™t yet know how likely that is ...»

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