Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Sharika U. S. Senarath"'
Publikováno v:
International Journal of Climatology. 40:4622-4637
Publikováno v:
International Journal of Climatology. 37:180-196
Precipitation measurements in the Mekong River Basin (MRB) are full of variability due to this domain's varied weather systems, climate conditions, elevation, and specific land–atmosphere interactions. This study provides an in-depth evaluation of
Autor:
Ramesh S. V. Teegavarapu, Abhishek Singh, Christopher Olson, A. M. Wasantha Lal, Ceyda Polatel, Sharika U. S. Senarath, Chandra S. Pathak, Vahid Zahraeifard
Publikováno v:
Journal of Hydrologic Engineering. 20
Publikováno v:
Watershed Management 2015.
Autor:
Sharika U. S. Senarath
Publikováno v:
World Environmental and Water Resources Congress 2015.
Publikováno v:
World Environmental and Water Resources Congress 2015.
The Mekong, the longest river in Southeast Asia, has received great attention due to its various water-related issues, including the catastrophic seasonal flooding at the lower part of the basin, extending to the Mekong Delta. A reliable assessment o
Publikováno v:
Vulnerability, Uncertainty, and Risk.
© 2014 American Society of Civil Engineers. The development of detailed flood inundation maps is typically done through the use of hydraulic models. However, the development of a hydraulic model for a large hydrological basin requires the availabili
Autor:
Sharika U. S. Senarath, Chia-Jeng Chen
Publikováno v:
World Environmental and Water Resources Congress 2014.
Publikováno v:
Journal of Climate. 13:4050-4063
At a local scale, the interception capacity of the canopy depends on a variety of climatic and canopy factors. Of particular importance is the intensity of rainfall—interception capacity varies inversely with rainfall intensity. At a field or regio
Publikováno v:
Water Resources Research. 36:1495-1510
Physically based, two-dimensional, distributed parameter Hortonian hydrologic models are sensitive to a number of spatially varied parameters and inputs and are particularly sensitive to the initial soil moisture field. However, soil moisture data ar