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Present status of urban hydrology - A research report by National Institute of Hydrology
The study reviews the present status of urbanization in the developed and developing countries and assesses the changes in urban hydrological cycle owing to this. Posted on 25 Jun, 2010 07:13 PM

The study reviews the present status of urbanization in the developed and developing countries and assesses the changes in urban hydrological cycle owing to this. The softwares used for studying urbanization and sanitation issues in the urban areas have been reviewed.

Review of hydrological studies in the North-eastern region - A research report by National Institute of Hydrology
The report tries to review the hydrological studies done in the north-eastern region of India by all agencies, governmental or non-governmental. Posted on 25 Jun, 2010 06:03 PM

The report tries to review the hydrological studies done in the northeastern region of India by all agencies, governmental or non-governmental. Sufficient care has been taken to include all the salient features of the studies to make it comprehensive. The various information  included in this report are the purpose and year of study, location and extent of the study area with its brief description, data used, list of specific studies along with its results and recommendations wherever possible.

An attempt has been made to pull together all the studies related to hydrology and its allied field. Besides these planned studies done by various departments, research studies done by academic institutions and research and development organizations has also been included.

Hydrological inventory of river basins in Uttar Pradesh - A research report by National Institute of Hydrology
The hydrological inventory of Ganga basin provides information regarding availability of hydrological data and highlights major hydrological problems of the basins. Posted on 25 Jun, 2010 05:47 PM

The hydrological inventory of Ganga basin provides information regarding availability of hydrological data and highlights major hydrological problems of the basins. The information is a useful input in water resources planning, management and research activities.

Implementation and testing of storm water management model - A research report by National Institute of Hydrology
The study endeavours to test the Storm Water Management Model (SWMM) in an urban area, presenting the technical summary of the model, its structure, input and output requirement. Posted on 25 Jun, 2010 05:25 PM

The study endeavors to test the Storm Water Management Model (SWMM) in an urban area. The report presents the technical summary of the model, its structure, interaction between the various blocks of SWMM, the input requirements and the output. The Windows implementation of the blocks, including descriptions of the screen sequences, corresponding blocks, changes made for ease of use and limitations of the implementation are presented. The minimum hardware requirements and installation information for the Windows SWMM are discussed.

Snow and glacier contribution in the Satluj river at Bhakra dam - A research report by National Institute of Hydrology
The study estimates the average contribution of snow and glacier melt runoff in the annual flow of Satluj river at Bhakra dam. Posted on 25 Jun, 2010 12:07 AM

The study estimates the average contribution of snow and glacier melt runoff in the annual flow of Satluj river at Bhakra dam. This study is restricted to the Indian part of Satluj basin. A water balance approach was used to determine the average snow and glacier contribution to the annual flows.

Study of Lake Nainital: Groundwater interaction using Isotope techniques - A research report by National Institute of Hydrology
The study undertakes hydrological investigations to develop a conceptual model for the water balance of Lake Nainital in Kumaon Himalayas. Posted on 25 Jun, 2010 12:03 AM

The study undertakes hydrological investigations to develop a conceptual model for the water balance of Lake Nainital in Kumaon Himalayas. All the components of lake water balance, except the sub-surface ones, have been measured or estimated using standard methods like isotope mass balance method in conjunction with the conventional water balance method. The sub surface outflow from the lake was assessed by studying the hydraulic interconnection of the lake and downstream springs using environmental tracers.

Simulation of flood hydrograph using an event based rainfall-runoff model - A research report by National Institute of Hydrology
The study deals with flood estimation using a flood hydrograph for the ungauged Narmada catchment upto Jamtara using the physical and geo-morphological characteristics of the catchment. Posted on 25 Jun, 2010 12:00 AM

The study deals with flood estimation through computation of a flood hydrograph for the ungauged Narmada catchment upto Jamtara using the physical and geo-morphological characteristics of the catchment. The catchment area of 17100 sqkm has been sub-divided into five sub-catchments for the purpose of flood estimation.

Soil classification of Dudhnai representative basin (Assam and Meghalaya) - A research report by National Institute of Hydrology
The study attempts to do field and laboratory determination of soil classification properties in the Dudhnai river basin of Assam and Meghalaya. Posted on 24 Jun, 2010 11:55 PM

The study attempts to do field and laboratory determination of soil classification properties in the Dudhnai river basin of Assam and Meghalaya. Point infiltration tests using double ring infiltrometer were conducted at various locations (forty-four sites) in respect of different land use conditions. Soil samples were collected from these infiltration testing sites.

The saturated hydraulic conductivity was determined in the field using Guelph Permeameter for the selected sites. The undisturbed soil samples and disturbed soil samples (50 cm below the ground) were collected and subjected to elaborate laboratory tests. 

Changes in land use and land cover and establishment of SCS runoff Curve Number in Suddagedda basin – A research report by National Institute of Hydrology
The study was taken up as a part of the representative basin studies being done by NIH and involved hydrological land use & land cover mapping for the Suddagedda basin of Andhra Pradesh. Posted on 24 Jun, 2010 11:52 PM

The study was taken up as a part of the representative basin studies being done by NIH and involved hydrological land use & land cover mapping for the Suddagedda basin of Andhra Pradesh. Mapping was carried out through visual interpretation for the years December 1987, April 1989, December 1992 and November 1996 using IRS IB-LISS II, LANDSAT 5-TM and IRS IC-LISS III data.

Land use and land cover are the most important surface characteristics of a basin. They are very dynamic features over space and time and it is difficult to get real time information on them through conventional means. Planners need to update knowledge of natural resources, which can be obtained quickly, economically and accurately through remote sensing techniques. Further, the land use map of a basin or region provides hydrologically significant categories, which are essential for estimation of reliable runoff from ungauged basins.

Geomorphological study of Devak basin - A research report by National Institute of Hydrology
The study attempts to find out the effects of geomorphology on watershed runoff response in the Devak basin and tries to identify the parameters that are more closely related to runoff. Posted on 24 Jun, 2010 11:49 PM

The study attempts to find out the effects of geomorphology on watershed runoff response in the Devak basin and tries to identify the parameters that are more closely related to runoff. A chief objective of the study is to regionalize the hydrologic models describing the rainfall-runoff process. 

The advanced knowledge of geomorphology of the region is of importance in the field of flood control measures and engineering projects, since geomorphological characteristics of river basins in mountainous areas affect runoff processes and formation of floods in the areas.

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