Abstract

This study assessed the impact of climate change on flood frequency and flood source area at basin scale considering Coupled Model Intercomparison Project phase 5 General Circulation Models (CMIP5 GCMs) under two Representative Concentration Pathways (RCP) scenarios (2.6 and 8.5). For this purpose, the Soil and Water Assessment Tool (SWAT) hydrological model was calibrated and validated for the Talar River Basin in northern Iran. Four empirical approaches including the Sangal, Fill–Steiner, Fuller, and Slope-based methods were used to estimate the Instantaneous Peak Flow (IPF) on a daily basis. The calibrated SWAT model was run under the two RCP scenarios using a combination of twenty GCMs from CMIP5 for the near future (2020–40). To assess the impact of climate change on flood frequency pattern and to quantify the contribution of each subbasin on the total discharge from the Talar River Basin, Flood Frequency Index (FFI) and Subbasin Flood Source Area Index (SFSAI) were used. Results revealed that the projected climate change will likely lead to an average discharge decrease in January, February, and March for both RCPs and an increase in September and October for RCP 8.5. The maximum and minimum temperature will likely increase for all months in the near future. The annual precipitation could increase by more than 20% in the near future. This is likely to lead to an increase of IPF. The results can help managers and policy makers to better define mitigation and adaptation strategies for basins in similar climates.

Highlights

  • Floods are complex natural hazards that can cause massive social and economic damage [1].According to the Intergovernmental Panel on Climate Change (IPCC), recent climate change has had a significant impact on the magnitude and frequency of extreme hydrological events in many regions of the world [2]

  • We evaluated the potential impact of climate change on flood frequency pattern and flood source area in the Talar River Basin

  • This study addressed the temporal and spatial impact of climate change on flood frequency and source area in subbasins of the Talar River Basin in northern Iran under low and high Representative Concentration Pathways (RCP) scenarios

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Summary

Introduction

Floods are complex natural hazards that can cause massive social and economic damage [1]. Assessing the impact of present and future climate requires estimation of future land use for achieving appropriate adaptation policy [9,10,11] In this regard, hydrological modeling plays an important role in simulating possible future changes and their impact, helping to determine proper watershed management practices [12]. F ut, i and T minGCM.his,i are the long-term average of ith month for minimum temperature in the future and historical (present) period, respectively Various statistical checks such as student’s t-test, F-test, and chi-square test are adopted in the LARS-WG environment to compare calculated and observed weather data for the investigated period [37]. Is surfaceofrunoff, Ea is evapotranspiration, wseep interflow, and Qwas gw is used to

A Digital
A Digital Elevationfield
SWAT Model Set Up
The subbasins drainage area 3453 kmbased were then further divided into 1110
Evaluation of Model Performance
IPF Estimation Methods
Climate Change Models and Downscaling
Variation
SWAT Model Calibration and Validation
Analysis
Statistical comparison
Figure
11 Spatial illustrates spatial distribution of Flood Frequency
Subbasin
Summary and Conclusions
Full Text
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