Analyzing uncertainty drivers of climate change impact studies in tropical and arid climates

Uncertainty in climate change impact studies can be identified in general circulation models (GCM), emission scenarios, downscaling techniques, hydrological models and data. Despite being aleatory or epistemic -sourced uncertainties, their effect size on impact model output can be variable in differ...

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Main Authors: Galavi, Hadi, Mirzaei, Majid
Format: Article
Published: Springer Verlag 2020
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Online Access:http://eprints.um.edu.my/36692/
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Institution: Universiti Malaya
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spelling my.um.eprints.366922024-07-15T00:14:29Z http://eprints.um.edu.my/36692/ Analyzing uncertainty drivers of climate change impact studies in tropical and arid climates Galavi, Hadi Mirzaei, Majid TC Hydraulic engineering. Ocean engineering Uncertainty in climate change impact studies can be identified in general circulation models (GCM), emission scenarios, downscaling techniques, hydrological models and data. Despite being aleatory or epistemic -sourced uncertainties, their effect size on impact model output can be variable in different climate zones. To test this hypothesis, the present study explored the uncertainty level of each source in the projected streamflow scenarios of the Sarbaz river basin (SRB) with arid climate properties and the tropical Hulu Langat river basin (HLB). An ensemble of five GCMs bias-corrected using EquiDistant-CDF-matching method, two representative concentration pathways (RCPs), and hydrological model parameters sets sourced the overall uncertainty in each case study. Investigations were performed at mean monthly scale of three 30-year periods of baseline, 2016-2045 (2030s), and 2046-2075 (2060s). In both climates, on average, GCM uncertainty was the largest contributor at monthly scale analysis and its effect size escalated following the monsoon months. In the tropical HLB, GCM uncertainty increased across the periods, but it did not show a similar pattern in the arid region of SRB. The RCP uncertainty showed the least effect size during the baseline period and it peaked in 2030s in the HLB climate. However, the only pattern recognizable in the arid SRB was the intensified effect size of all uncertainty sources along with the tremendous impacts projected in monsoon months; at least twice the size of uncertainty sources effect and impacts projected for the tropical HLB. The uncertainty sources effect size altered dramatically as the climate-of the study area-changed. Thus, this research emboldens the need for seasonal-based analysis of uncertainty sources in climate change impact studies at dry climate zones. Springer Verlag 2020-04 Article PeerReviewed Galavi, Hadi and Mirzaei, Majid (2020) Analyzing uncertainty drivers of climate change impact studies in tropical and arid climates. Water Resources Management, 34 (6). pp. 2097-2109. ISSN 0920-4741, DOI https://doi.org/10.1007/s11269-020-02553-0 <https://doi.org/10.1007/s11269-020-02553-0>. 10.1007/s11269-020-02553-0
institution Universiti Malaya
building UM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Malaya
content_source UM Research Repository
url_provider http://eprints.um.edu.my/
topic TC Hydraulic engineering. Ocean engineering
spellingShingle TC Hydraulic engineering. Ocean engineering
Galavi, Hadi
Mirzaei, Majid
Analyzing uncertainty drivers of climate change impact studies in tropical and arid climates
description Uncertainty in climate change impact studies can be identified in general circulation models (GCM), emission scenarios, downscaling techniques, hydrological models and data. Despite being aleatory or epistemic -sourced uncertainties, their effect size on impact model output can be variable in different climate zones. To test this hypothesis, the present study explored the uncertainty level of each source in the projected streamflow scenarios of the Sarbaz river basin (SRB) with arid climate properties and the tropical Hulu Langat river basin (HLB). An ensemble of five GCMs bias-corrected using EquiDistant-CDF-matching method, two representative concentration pathways (RCPs), and hydrological model parameters sets sourced the overall uncertainty in each case study. Investigations were performed at mean monthly scale of three 30-year periods of baseline, 2016-2045 (2030s), and 2046-2075 (2060s). In both climates, on average, GCM uncertainty was the largest contributor at monthly scale analysis and its effect size escalated following the monsoon months. In the tropical HLB, GCM uncertainty increased across the periods, but it did not show a similar pattern in the arid region of SRB. The RCP uncertainty showed the least effect size during the baseline period and it peaked in 2030s in the HLB climate. However, the only pattern recognizable in the arid SRB was the intensified effect size of all uncertainty sources along with the tremendous impacts projected in monsoon months; at least twice the size of uncertainty sources effect and impacts projected for the tropical HLB. The uncertainty sources effect size altered dramatically as the climate-of the study area-changed. Thus, this research emboldens the need for seasonal-based analysis of uncertainty sources in climate change impact studies at dry climate zones.
format Article
author Galavi, Hadi
Mirzaei, Majid
author_facet Galavi, Hadi
Mirzaei, Majid
author_sort Galavi, Hadi
title Analyzing uncertainty drivers of climate change impact studies in tropical and arid climates
title_short Analyzing uncertainty drivers of climate change impact studies in tropical and arid climates
title_full Analyzing uncertainty drivers of climate change impact studies in tropical and arid climates
title_fullStr Analyzing uncertainty drivers of climate change impact studies in tropical and arid climates
title_full_unstemmed Analyzing uncertainty drivers of climate change impact studies in tropical and arid climates
title_sort analyzing uncertainty drivers of climate change impact studies in tropical and arid climates
publisher Springer Verlag
publishDate 2020
url http://eprints.um.edu.my/36692/
_version_ 1805881099922964480