Long-term trends and projections of hydrological fluxes under RCP climate change scenarios for a mountainous river catchment of northeast India

The estimate of changes in hydrological fluxes from a climate change perspective is inevitable for assessing the sustainability of watersheds and conserving water resources. Here, we quantify and assess the changes in different hydrological flux components for the Manu-Deo River Basin (MDRB) of nort...

Full description

Bibliographic Details
Main Authors: S. Murasingh, J. Kuttippurath, S. Sandeep Dash, S. Raj, R. Remesan, Madan K. Jha, P. Kumar
Format: Article
Language:English
Published: IWA Publishing 2022-04-01
Series:Journal of Water and Climate Change
Subjects:
Online Access:http://jwcc.iwaponline.com/content/13/4/1776
_version_ 1828366580753367040
author S. Murasingh
J. Kuttippurath
S. Sandeep Dash
S. Raj
R. Remesan
Madan K. Jha
P. Kumar
author_facet S. Murasingh
J. Kuttippurath
S. Sandeep Dash
S. Raj
R. Remesan
Madan K. Jha
P. Kumar
author_sort S. Murasingh
collection DOAJ
description The estimate of changes in hydrological fluxes from a climate change perspective is inevitable for assessing the sustainability of watersheds and conserving water resources. Here, we quantify and assess the changes in different hydrological flux components for the Manu-Deo River Basin (MDRB) of northeast India using Soil and Water Assessment Tool (SWAT) simulations and multi-temporal data at various resolutions. Sequential Uncertainty Fitting (SUFI-2) optimization is used to calibrate and validate the simulations for the periods 1984–2006 and 2007–2016 and for the four future representative concentration pathway (RCP) scenarios. The model performed reasonably well for the calibration and validation of daily data, in accordance with the Nash–Sutcliffe efficiency and coefficient of determination (0.54/0.55 and 0.52/0.72, respectively). The analysis for the period 1985–2013 reveals a decreasing trend in streamflow, which indicates increasing trends of drought there. Furthermore, it shows an increasing trend in evapotranspiration (ET) and decreasing trend for baseflow (BF), suggesting an adverse impact on agricultural production during lean periods. In addition, the RCP 2.6 and 6.0 scenarios for the monsoon season in future time scales are expected to cause a reduction in different flow components, although RCP 8.5 shows increased water availability there. The sub-basin-scale quantification and multi-temporal analysis of water availability under the present and future climate scenarios, as presented here, can assist water managers in formulating a suitable operational policy to implement a better decision-making framework for river and waterbody management. This is particularly important for mountainous regions, where input data are sparse and modelling of hydrological fluxes is challenging. HIGHLIGHTS A model for a mountain river basin is customized to analyse hydrological fluxes.; The model performs better at a monthly time scale than at a daily time scale.; Streamflow has been decreasing in the basin but increases in all RCP scenarios.; Increase in evapotranspiration in monsoon seasons in both past and future periods.; A multi-model approach provides more reliable estimates of water balance components.;
first_indexed 2024-04-14T05:47:01Z
format Article
id doaj.art-ba68f0eeb6f7465c8906c4d3b7d7e121
institution Directory Open Access Journal
issn 2040-2244
2408-9354
language English
last_indexed 2024-04-14T05:47:01Z
publishDate 2022-04-01
publisher IWA Publishing
record_format Article
series Journal of Water and Climate Change
spelling doaj.art-ba68f0eeb6f7465c8906c4d3b7d7e1212022-12-22T02:09:15ZengIWA PublishingJournal of Water and Climate Change2040-22442408-93542022-04-011341776178910.2166/wcc.2022.424424Long-term trends and projections of hydrological fluxes under RCP climate change scenarios for a mountainous river catchment of northeast IndiaS. Murasingh0J. Kuttippurath1S. Sandeep Dash2S. Raj3R. Remesan4Madan K. Jha5P. Kumar6 CORAL, Indian Institute of Technology Kharagpur, 721 302 Kharagpur, India CORAL, Indian Institute of Technology Kharagpur, 721 302 Kharagpur, India School of Water Resources, Indian Institute of Technology Kharagpur, Kharagpur, India CORAL, Indian Institute of Technology Kharagpur, 721 302 Kharagpur, India School of Water Resources, Indian Institute of Technology Kharagpur, Kharagpur, India AgFE Department, Indian Institute of Technology Kharagpur, Kharagpur, India CORAL, Indian Institute of Technology Kharagpur, 721 302 Kharagpur, India The estimate of changes in hydrological fluxes from a climate change perspective is inevitable for assessing the sustainability of watersheds and conserving water resources. Here, we quantify and assess the changes in different hydrological flux components for the Manu-Deo River Basin (MDRB) of northeast India using Soil and Water Assessment Tool (SWAT) simulations and multi-temporal data at various resolutions. Sequential Uncertainty Fitting (SUFI-2) optimization is used to calibrate and validate the simulations for the periods 1984–2006 and 2007–2016 and for the four future representative concentration pathway (RCP) scenarios. The model performed reasonably well for the calibration and validation of daily data, in accordance with the Nash–Sutcliffe efficiency and coefficient of determination (0.54/0.55 and 0.52/0.72, respectively). The analysis for the period 1985–2013 reveals a decreasing trend in streamflow, which indicates increasing trends of drought there. Furthermore, it shows an increasing trend in evapotranspiration (ET) and decreasing trend for baseflow (BF), suggesting an adverse impact on agricultural production during lean periods. In addition, the RCP 2.6 and 6.0 scenarios for the monsoon season in future time scales are expected to cause a reduction in different flow components, although RCP 8.5 shows increased water availability there. The sub-basin-scale quantification and multi-temporal analysis of water availability under the present and future climate scenarios, as presented here, can assist water managers in formulating a suitable operational policy to implement a better decision-making framework for river and waterbody management. This is particularly important for mountainous regions, where input data are sparse and modelling of hydrological fluxes is challenging. HIGHLIGHTS A model for a mountain river basin is customized to analyse hydrological fluxes.; The model performs better at a monthly time scale than at a daily time scale.; Streamflow has been decreasing in the basin but increases in all RCP scenarios.; Increase in evapotranspiration in monsoon seasons in both past and future periods.; A multi-model approach provides more reliable estimates of water balance components.;http://jwcc.iwaponline.com/content/13/4/1776climate changehydrological fluxeslinear trendsnortheast indiarcp scenariosswat
spellingShingle S. Murasingh
J. Kuttippurath
S. Sandeep Dash
S. Raj
R. Remesan
Madan K. Jha
P. Kumar
Long-term trends and projections of hydrological fluxes under RCP climate change scenarios for a mountainous river catchment of northeast India
Journal of Water and Climate Change
climate change
hydrological fluxes
linear trends
northeast india
rcp scenarios
swat
title Long-term trends and projections of hydrological fluxes under RCP climate change scenarios for a mountainous river catchment of northeast India
title_full Long-term trends and projections of hydrological fluxes under RCP climate change scenarios for a mountainous river catchment of northeast India
title_fullStr Long-term trends and projections of hydrological fluxes under RCP climate change scenarios for a mountainous river catchment of northeast India
title_full_unstemmed Long-term trends and projections of hydrological fluxes under RCP climate change scenarios for a mountainous river catchment of northeast India
title_short Long-term trends and projections of hydrological fluxes under RCP climate change scenarios for a mountainous river catchment of northeast India
title_sort long term trends and projections of hydrological fluxes under rcp climate change scenarios for a mountainous river catchment of northeast india
topic climate change
hydrological fluxes
linear trends
northeast india
rcp scenarios
swat
url http://jwcc.iwaponline.com/content/13/4/1776
work_keys_str_mv AT smurasingh longtermtrendsandprojectionsofhydrologicalfluxesunderrcpclimatechangescenariosforamountainousrivercatchmentofnortheastindia
AT jkuttippurath longtermtrendsandprojectionsofhydrologicalfluxesunderrcpclimatechangescenariosforamountainousrivercatchmentofnortheastindia
AT ssandeepdash longtermtrendsandprojectionsofhydrologicalfluxesunderrcpclimatechangescenariosforamountainousrivercatchmentofnortheastindia
AT sraj longtermtrendsandprojectionsofhydrologicalfluxesunderrcpclimatechangescenariosforamountainousrivercatchmentofnortheastindia
AT rremesan longtermtrendsandprojectionsofhydrologicalfluxesunderrcpclimatechangescenariosforamountainousrivercatchmentofnortheastindia
AT madankjha longtermtrendsandprojectionsofhydrologicalfluxesunderrcpclimatechangescenariosforamountainousrivercatchmentofnortheastindia
AT pkumar longtermtrendsandprojectionsofhydrologicalfluxesunderrcpclimatechangescenariosforamountainousrivercatchmentofnortheastindia