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Climate change and water resources in arid regions : uncertainty of the baseline time period

Mohammed, Ruqayah and Scholz, Miklas LU (2019) In Theoretical and Applied Climatology 137(1-2). p.1365-1376
Abstract

Recent climate change studies have given a lot of attention to the uncertainty that stems from general circulation models (GCM), greenhouse gas emission scenarios, hydrological models and downscaling approaches. Yet, the uncertainty that stems from the selection of the baseline period has not been studied. Accordingly, the main research question is as follows: What would be the differences and/or the similarities in the evaluation of climate change impacts between the GCM and the delta perturbation scenarios using different baseline periods? This article addresses this issue through comparison of the results of two different baseline periods, investigating the uncertainties in evaluating climate change impact on the hydrological... (More)

Recent climate change studies have given a lot of attention to the uncertainty that stems from general circulation models (GCM), greenhouse gas emission scenarios, hydrological models and downscaling approaches. Yet, the uncertainty that stems from the selection of the baseline period has not been studied. Accordingly, the main research question is as follows: What would be the differences and/or the similarities in the evaluation of climate change impacts between the GCM and the delta perturbation scenarios using different baseline periods? This article addresses this issue through comparison of the results of two different baseline periods, investigating the uncertainties in evaluating climate change impact on the hydrological characteristics of arid regions. The Lower Zab River Basin (Northern Iraq) has been selected as a representative case study. The research outcomes show that the considered baseline periods suggest increases and decreases in the temperature and precipitation (P), respectively, over the 2020, 2050 and 2080 periods. The two climatic scenarios are likely to lead to similar reductions in the reservoir mean monthly flows, and subsequently, their maximum discharge is approximately identical. The predicted reduction in the inflow for the 2080–2099 time period fluctuates between 31 and 49% based on SRA1B and SRA2 scenarios, respectively. The delta perturbation scenario permits the sensitivity of the climatic models to be clearly determined compared to the GCM. The former allows for a wide variety of likely climate change scenarios at the regional level and are easier to generate and apply so that they could complement the latter.

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author
and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Baseline time period, Climate change uncertainty, Hydro-climatic parameter forecasting, Streamflow prediction
in
Theoretical and Applied Climatology
volume
137
issue
1-2
pages
1365 - 1376
publisher
Springer
external identifiers
  • scopus:85055700261
ISSN
0177-798X
DOI
10.1007/s00704-018-2671-6
language
English
LU publication?
yes
id
c0262b18-f8ca-4edf-97a5-ed2511f9d260
date added to LUP
2018-12-07 11:34:46
date last changed
2022-04-25 19:40:35
@article{c0262b18-f8ca-4edf-97a5-ed2511f9d260,
  abstract     = {{<p>Recent climate change studies have given a lot of attention to the uncertainty that stems from general circulation models (GCM), greenhouse gas emission scenarios, hydrological models and downscaling approaches. Yet, the uncertainty that stems from the selection of the baseline period has not been studied. Accordingly, the main research question is as follows: What would be the differences and/or the similarities in the evaluation of climate change impacts between the GCM and the delta perturbation scenarios using different baseline periods? This article addresses this issue through comparison of the results of two different baseline periods, investigating the uncertainties in evaluating climate change impact on the hydrological characteristics of arid regions. The Lower Zab River Basin (Northern Iraq) has been selected as a representative case study. The research outcomes show that the considered baseline periods suggest increases and decreases in the temperature and precipitation (P), respectively, over the 2020, 2050 and 2080 periods. The two climatic scenarios are likely to lead to similar reductions in the reservoir mean monthly flows, and subsequently, their maximum discharge is approximately identical. The predicted reduction in the inflow for the 2080–2099 time period fluctuates between 31 and 49% based on SRA1B and SRA2 scenarios, respectively. The delta perturbation scenario permits the sensitivity of the climatic models to be clearly determined compared to the GCM. The former allows for a wide variety of likely climate change scenarios at the regional level and are easier to generate and apply so that they could complement the latter.</p>}},
  author       = {{Mohammed, Ruqayah and Scholz, Miklas}},
  issn         = {{0177-798X}},
  keywords     = {{Baseline time period; Climate change uncertainty; Hydro-climatic parameter forecasting; Streamflow prediction}},
  language     = {{eng}},
  number       = {{1-2}},
  pages        = {{1365--1376}},
  publisher    = {{Springer}},
  series       = {{Theoretical and Applied Climatology}},
  title        = {{Climate change and water resources in arid regions : uncertainty of the baseline time period}},
  url          = {{http://dx.doi.org/10.1007/s00704-018-2671-6}},
  doi          = {{10.1007/s00704-018-2671-6}},
  volume       = {{137}},
  year         = {{2019}},
}