Hydrological projections over the Upper Indus Basin at 1.5 °C and 2.0 °C temperature increase.

Global Climate Models Hydrological modeling Paris Agreement Upper Indus Basin Water availability

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
20 Sep 2021
Historique:
received: 08 01 2021
revised: 09 05 2021
accepted: 10 05 2021
entrez: 17 6 2021
pubmed: 18 6 2021
medline: 18 6 2021
Statut: ppublish

Résumé

We analyse an ensemble of statistically downscaled Global Climate Models (GCMs) to investigate future water availability in the Upper Indus Basin (UIB) of Pakistan for the time horizons when the global and/or regional warming levels cross Paris Agreement (PA) targets. The GCMs data is obtained from the 5th Phase of Coupled Model Inter-Comparison Project under two Representative Concentration Pathways (RCP4.5 and RCP8.5). Based on the five best performing GCMs, we note that global 1.5 °C and 2.0 °C warming thresholds are projected in 2026 and 2047 under RCP4.5 and 2022 and 3036 under RCP8.5 respectively while these thresholds are reached much earlier over Pakistan i.e. 2016 and 2030 under RCP4.5 and 2012 and 2025 under RCP8.5 respectively. Interestingly, the GCMs with the earliest emergence at the global scale are not necessarily the ones with the earliest emergence over Pakistan, highlighting spatial non-linearity in GCMs response. The emergence of 2.0 °C warming at global scale across 5 GCMs ranges from 2031 (CCSM4) to 2049 (NorESM) under RCP8.5. Precipitation generally exhibits a progressive increasing trend with stronger changes at higher warming or radiative forcing levels. Hydrological simulations representing the historical, 1.5 °C and 2.0 °C global and region warming time horizons indicate a robust but seasonally varying increase in the inflows. The highest inflows in the baseline and future are witnessed in July. However, the highest future increase in inflows is projected in October under RCP4.5 (37.99% and 65.11% at 1.5 °C and 2.0 °C) and in April under RCP8.5 (37% and 62.05% at 1.5 °C and 2.0 °C). These hydrological changes are driven by increases in the snow and glacial melt contribution, which are more pronounced at 2.0 °C warming level. These findings should help for effective water management in Pakistan over the coming decades.

Identifiants

pubmed: 34134357
pii: S0048-9697(21)02830-8
doi: 10.1016/j.scitotenv.2021.147759
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

147759

Informations de copyright

Copyright © 2021 Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Rida Sehar Kiani (RS)

Department of Environmental Sciences, Quaid-i-Azam University, Islamabad, Pakistan; Global Change Impact Studies Centre (GCISC), Ministry of Climate Change, Pakistan.

Shaukat Ali (S)

Global Change Impact Studies Centre (GCISC), Ministry of Climate Change, Pakistan.

Moetasim Ashfaq (M)

Computational Sciences and Engineering Division, Oak Ridge National Laboratory, Oak Ridge, TN, USA.

Firdos Khan (F)

School of Natural Sciences (SNS), National University of Sciences and Technology (NUST), Islamabad, Pakistan.

Sher Muhammad (S)

International Centre for Integrated Mountain Development (ICIMOD), Kathmandu, Nepal; Institute of International Rivers and Eco-security, Yunnan University, Kunming, China.

Michelle S Reboita (MS)

Instituto de Recursos Naturais, Universidade Federal de Itajubá, Brazil.

Abida Farooqi (A)

Department of Environmental Sciences, Quaid-i-Azam University, Islamabad, Pakistan. Electronic address: afarooqi@qau.edu.pk.

Classifications MeSH