Abstract
Hydrological modeling and the hydrological response to land-use/land-cover changes induced by human activities have gained enormous research interest over the last few decades. The study presented here analyzes the spatial and qualitative changes in the rainfall–runoff that have resulted from the land-cover changes between 1985–2014 in the Godavari River Basin using the Hydrologic Engineering Centre-Hydrologic Modeling System(HEC-HMS) model and remote sensing—GIS (geographic information system) techniques. The purpose of this paper is to analyze the dynamics of land-use/land-cover (LULC) changes for the years 1985, 1995, 2005, and 2014 for the Godavari Basin. The findings reveal an increase of 0.64% of built-up land, a decrease of 0.92% in shrubland, and an increase of 0.56% in waterbodies between 1985–2014. The LULC change detection results between the years 1985–2014 indicated a drastic change in the cropland, forest, built-up land, and water bodies among all of the other classes. The urbanization and agricultural activities are the major reasons for the increase of cropland, built-up land, and water bodies, at the expense of decreases in shrubland and forest. The study had an overall classification accuracy of 92% and an overall Kappa coefficient of 0.9. The HEC-HMS model is used to simulate the hydrology of the Godavari Basin. The analyses carried out were mainly focussed on the impact of LULC changes on the streamflow pattern. The surface runoff was simulated for the year 2014 to quantify the changes that have taken place due to changes in LULC. The observed and the simulated peak streamflow was found to be the same i.e., 56,780 m3/s on 9 September 2014. In the validation part, the linear regression method was used to correlate the observed and simulated streamflow data at the prominent gauge station of the Badrachalam outlet for the Godavari River Basin and give a correlation coefficient value of 0.83. It was found that the HEC-HMS model is compatible and works better for the rainfall–runoff modeling, as it takes into account the various parameters that are influencing the process. The hydrological modeling that was carried out using the HEC-HMS model has brought out the significant impact of LULCC on rainfall–runoff at the Pranhita sub-basinscale, indicating the model’s ability to successfully accommodate all of the environmental and landscape variables. The study indicates that deforestation at the cost of urbanization and cropland expansions leads to decreases in the overall evapotranspiration (ET) and infiltration, with an increase in runoff. The results of the study show that the integration of remote sensing, GIS, and the hydrological model (HEC-HMS) can solve hydrological problems in a river basin.
Highlights
Water Resources Management is an important and integrated approach that includes all of the hydrological components and their linkages with one another
The water and energy fluxes of the earth system are integrated through the hydrological cycle, and in turn, it affects the fluxes of the system
Over the past several years, remote sensing data have had an active part in mapping the LULC changes in various parts of India [1,2,3,4,5,6,7,8,9,10,11,12]
Summary
Water Resources Management is an important and integrated approach that includes all of the hydrological components and their linkages with one another. It is very important to assess and understand the hydrological components of a river basin and the impact of LULC for its efficient management of water resources. A proper understanding of the rainfall–runoff relation at different scales for the Godavari river basin is important Despite this background, an attempt of hydrological modeling for the Godavari Basin using the HEC-HMS model has not been carried out so far. The main objectives of this study are (i) to assess the past and potential land-cover changes between 1985–2005, and prepare the land-use and land-cover map of the year 2014; (ii) detect the land-use and land-cover changes over the past 30 years; (iii) to assess the water resources in Godavari Basin using the HEC-HMS model and compare the output. Geo-Inf. 2018, 7, 206 ISPRS Int. J. OBbatadirnaecdhablyamtheoumtloedt eolfwthitehbthaseinobfsoerrtvheedygeraoru2n0d14d;aatandsu(cihv)atsodsitsucdhayrtgheeaitmthpeacBtaodfrathcheaLlaUmLCoucthleatnogfe thone bthaesirnafinorfatlhl–eryuenaorff20in14th; aenPdra(invh)itoa wstuatdeyrsthheedi,mGpoadcat voafrtihReiLvUerLBCascihna.nge on the rainfall–runoff in the Pranhita watershed, Godavari River Basin
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