نتایج جستجو برای: acquirers unit hydrograph

تعداد نتایج: 396156  

Journal: :مرتع و آبخیزداری 0
حمید رضا مرادی دانشیار دانشکدة منابع طبیعی دانشگاه تربیت مدرس هانیه اسدی کارشناس ارشد دانشکدة منابع طبیعی دانشگاه تربیت مدرس سید حمید رضا صادقی استاد دانشکدة منابع طبیعی دانشگاه تربیت مدرس عبدالرسول تلوری دانشیار پژوهشی مرکز تحقیقات حفاظت خاک و آبخیزداری e

the hydrograph at watershed outlet can be expressed as hydrological response of watershed to geomorphological behavior. in present study with the aid of the gis and the concept of instantaneous unit hydrograph, the watershed response was simulated. in present physical method, the iuh is derived from three parameters of time of concentration, storage coefficient and time-area curve of the basin....

Journal: :ecopersia 0
masome sarhadi former master student, department of rangeland and watershed management, university of zabol, zabol, iran mohammad nohtani assistant professor, department of rangeland and watershed management, faculty of water and soil, university of zabol, zabol, iran mohammad reiki former master student, department of rangeland and watershed management, university of zabol, capacity building for the international project of menarid in sistan and baluchistan province, iran

the effect of drought indices on hydrostatic variations and qualitative parameters of the zahedan plain's aquifer was investigated. for this purpose, 12-year statistics from observational and piezometry wells in the plain, the drought index of percentage normal )pn), standardized precipitation index )spi(, and 30-year precipitation statistics of zahedan station were used. results revealed ...

2002
David M. Mooney

In erosion and sedimentation problems, estimating the range of significant stream flows to include when computing sediment transport can prove challenging in ungauged or under-gauged basins. This paper describes an event-based model incorporating a geomorphologic instantaneous unit hydrograph and stochastic descriptions of peak flows and frequency of storm events from nearby reference watershed...

2017

ions: Forms of precipitation, data analysis, rain gauge networks; Infiltration process, infiltration indices and Horton's equation; Evaporation and Evapo-transpiration Pan evaporation, empirical equations for estimating evaporation and evapo-transpiration; Transpiration, Runoff and Hydrographs: Rainfall runoff relations, time area concept, flow duration curve, mass curve, flow hydrograph, Unit ...

2017
József Szilágyi

A mathematically correct form of the linear storage element’s routing equation is specified requiring only a slight modification of the existing HEC-HMS routine. The new formulation, unlike the current version in use, is unconditionally stable as long as the time step and the storage coefficient values are trivially specified as positive numbers.

2007
Toshisuke Maruyama

To estimate the amount of evapotranspiration in a river basin, the "short period water balance method" was formulated. Then, by introducing the "complementary relationship method," the amount of evapotranspiration was estimated seasonally, and with reasonable accuracy, for both small and large areas. Moreover, to accurately estimate river discharge in the low water season, the "weighted statist...

2013
Yu Chen

Objective of the study The purpose of this thesis is to study acquirers performance persistence issue in merger and acquisition (M&A) market based on empirical evidence from EU 15 countries. This study provides an overview of different factors affecting serial acquirers’ performance in M&A market as measured by excess stock returns. Focus of this thesis is to test the existence of acquirers per...

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Considering the most of country have no gage station, in recent year one method can be proposed with the involvement of other information, which will affect hydrology condition. It can estimate flood water level. In this study, considering relationship between geomorphology and hydrology, using little information, flood hydrograph were simulated. This method is named geomorphological instantane...

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