Climate change scenarios and its impact on water resources of Langtang Khola Basin, Nepal

General Circulation Models (GCMs) successfully simulate future climate variability and climate change on a global scale; however, poor spatial resolution constrains their application for impact studies at a regional or a local level. The dynamically downscaled precipitation and temperature data were...

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Main Authors: T. Raj Adhikari, L. Prasad Devkota, A. Bhakta Shrestha
Format: Article
Language:English
Published: Copernicus Publications 2014-09-01
Series:Proceedings of the International Association of Hydrological Sciences
Online Access:https://www.proc-iahs.net/364/9/2014/piahs-364-9-2014.pdf
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spelling doaj-79e381831d77425a87465da171da80362020-11-24T20:51:31ZengCopernicus PublicationsProceedings of the International Association of Hydrological Sciences2199-89812199-899X2014-09-0136491310.5194/piahs-364-9-2014Climate change scenarios and its impact on water resources of Langtang Khola Basin, NepalT. Raj Adhikari0L. Prasad Devkota1A. Bhakta Shrestha2Central Department of Hydrology and Meteorology, Tribhuvan University, Kathmandu, NepalCentral Department of Hydrology and Meteorology, Tribhuvan University, Kathmandu, NepalInternational Centre for Integrated Mountain Development, Kathmandu, NepalGeneral Circulation Models (GCMs) successfully simulate future climate variability and climate change on a global scale; however, poor spatial resolution constrains their application for impact studies at a regional or a local level. The dynamically downscaled precipitation and temperature data were used for the future climate scenarios prediction for the period 2000–2050s, under the Special Report on Emissions Scenarios (SRES) A2 and A1B scenarios. In addition, rating equation was developed from measured discharge and gauge (stage) height data. The generated precipitation and temperature data from downscale and rating equation was used to run the HBV-<i>Light 3.0</i> conceptual rainfall–runoff model for the calibration and validation of the model, gauge height was taken in the reference period (1988–2009). In the HBV-<i>Light 3.0</i>, a GAP optimization approach was used to calibrate the observed streamflow. From the precipitation scenarios with SRES A2 and A1B emissions at Kyanging, an increase of precipitation during summer and spring and a decrease during winter and autumn seasons was shown. The model projected annual precipitation for the 2050s of both the A2 and A1B scenarios are 716.4 mm and 703.6 mm, respectively. Such precipitation projections indicate the future increase of precipitation in all seasons except the summer. By the end of the 2050s simulation projects an increase maximum (minimum) discharge of 37.8 m<sup>3</sup>/s (13.9 m<sup>3</sup>/s) for A1B scenario and 36.2 m<sup>3</sup>/s (14.3 m<sup>3</sup>/s) for A2 scenario. A maximum projected discharge will increase for all seasons except for spring, whereas the minimum will decrease in summer.https://www.proc-iahs.net/364/9/2014/piahs-364-9-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. Raj Adhikari
L. Prasad Devkota
A. Bhakta Shrestha
spellingShingle T. Raj Adhikari
L. Prasad Devkota
A. Bhakta Shrestha
Climate change scenarios and its impact on water resources of Langtang Khola Basin, Nepal
Proceedings of the International Association of Hydrological Sciences
author_facet T. Raj Adhikari
L. Prasad Devkota
A. Bhakta Shrestha
author_sort T. Raj Adhikari
title Climate change scenarios and its impact on water resources of Langtang Khola Basin, Nepal
title_short Climate change scenarios and its impact on water resources of Langtang Khola Basin, Nepal
title_full Climate change scenarios and its impact on water resources of Langtang Khola Basin, Nepal
title_fullStr Climate change scenarios and its impact on water resources of Langtang Khola Basin, Nepal
title_full_unstemmed Climate change scenarios and its impact on water resources of Langtang Khola Basin, Nepal
title_sort climate change scenarios and its impact on water resources of langtang khola basin, nepal
publisher Copernicus Publications
series Proceedings of the International Association of Hydrological Sciences
issn 2199-8981
2199-899X
publishDate 2014-09-01
description General Circulation Models (GCMs) successfully simulate future climate variability and climate change on a global scale; however, poor spatial resolution constrains their application for impact studies at a regional or a local level. The dynamically downscaled precipitation and temperature data were used for the future climate scenarios prediction for the period 2000–2050s, under the Special Report on Emissions Scenarios (SRES) A2 and A1B scenarios. In addition, rating equation was developed from measured discharge and gauge (stage) height data. The generated precipitation and temperature data from downscale and rating equation was used to run the HBV-<i>Light 3.0</i> conceptual rainfall–runoff model for the calibration and validation of the model, gauge height was taken in the reference period (1988–2009). In the HBV-<i>Light 3.0</i>, a GAP optimization approach was used to calibrate the observed streamflow. From the precipitation scenarios with SRES A2 and A1B emissions at Kyanging, an increase of precipitation during summer and spring and a decrease during winter and autumn seasons was shown. The model projected annual precipitation for the 2050s of both the A2 and A1B scenarios are 716.4 mm and 703.6 mm, respectively. Such precipitation projections indicate the future increase of precipitation in all seasons except the summer. By the end of the 2050s simulation projects an increase maximum (minimum) discharge of 37.8 m<sup>3</sup>/s (13.9 m<sup>3</sup>/s) for A1B scenario and 36.2 m<sup>3</sup>/s (14.3 m<sup>3</sup>/s) for A2 scenario. A maximum projected discharge will increase for all seasons except for spring, whereas the minimum will decrease in summer.
url https://www.proc-iahs.net/364/9/2014/piahs-364-9-2014.pdf
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