Runoff Modelling under Climate Change

A special issue of Hydrology (ISSN 2306-5338). This special issue belongs to the section "Hydrology–Climate Interactions".

Deadline for manuscript submissions: 31 July 2024 | Viewed by 2805

Special Issue Editors


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Guest Editor
Department of Environmental Engineering, University of Calabria, 87036 Rende, Italy
Interests: runoff modeling; shallow water equations; urban flood hazard; border irrigation; overland flow
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Guest Editor
Department of Agriculture and Environmental Sciences, University of Milan, Via Celoria 2, 20133 Milan, Italy
Interests: agriculture water management; shallow water equations; hydraulic analysis; smart irrigation system; water conservation

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Guest Editor
Faculty of Science and Technology, Free University of Bozen-Bolzano, Piazza Università 5, 39100 Bolzano, Italy
Interests: water resources; hydroinformatics
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Special Issue Information

Dear Colleagues,

Runoff modeling under climate change involves predicting changes in the amount and timing of water flows in watersheds due to the impacts of climate change. It plays a crucial role in water resource management, flood forecasting, agricultural management, and the assessment of potential impacts on ecosystems and human populations. The goal of this Special Issue is to collect papers (original research articles and review papers) which provide insights on this topic. This Special Issue will welcome manuscripts that link the following themes:

  • Data collection: Gathering historical climate and hydrological data, including precipitation, temperature, evapotranspiration, and streamflow records. This information is necessary for model calibration and validation;
  • Climate change scenarios: Selecting climate change scenarios based on projections from global climate models (GCMs) or regional climate models (RCMs). These scenarios provide information on future changes in temperature and precipitation patterns;
  • Hydrological model selection: Choosing an appropriate hydrological model that represents watershed physical processes, including rainfall–runoff relationships, infiltration, evapotranspiration, and flow routing. In this context, applications of artificial intelligence (AI) or machine learning (ML) models are more and more frequent;
  • Model calibration: Calibrating hydrological models using historical data to ensure that it accurately represents observed streamflow patterns. This step involves adjusting model parameters to minimize the differences between simulated and observed streamflows;
  • Climate change impact assessment: Applying the selected climate change scenarios to the calibrated hydrological model to simulate future runoff. This involves incorporating the projected changes in temperature and precipitation into the model inputs;
  • Uncertainty analysis: Assessing the uncertainty associated with climate change projections and hydrological model outputs. Uncertainties arise from various sources, including the choice in climate models, emission scenarios, and inherent uncertainties in hydrological modeling;
  • Model validation: Validating hydrological models by comparing simulated runoff under climate change scenarios with observed streamflow data for a specific period. This step helps evaluate the model performance and reliability in representing future runoff conditions;
  • Impact assessment: Analyzing the modeled runoff data to understand the potential impacts of climate change on water resources. This information can guide adaptation strategies and water management decisions in various fields, such as civil protection and agriculture water management;
  • Communicating results: Effective communication of the findings can help raise awareness and facilitate informed decisionmaking regarding water resource management under climate change.

We look forward to receiving your original research articles and reviews.

Dr. Carmelina Costanzo
Dr. Fabiola Gangi
Dr. Majid Niazkar
Guest Editors

Manuscript Submission Information

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Keywords

  • climate change
  • runoff modeling
  • urban flood hazard
  • agriculture water management
  • hydrological modeling
  • machine learning

Published Papers (2 papers)

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Research

22 pages, 6265 KiB  
Article
Hydrologic Sensitivity of a Critical Turkish Watershed to Inform Water Resource Management in an Altered Climate
by Furkan Yunus Emre Cevahir, Jennifer C. Adam, Mingliang Liu and Justin Sheffield
Hydrology 2024, 11(5), 64; https://doi.org/10.3390/hydrology11050064 - 30 Apr 2024
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Abstract
This study introduces a novel sensitivity analysis approach to assess the resilience and susceptibility of hydrologic systems to the stresses of climate change, moving away from conventional top-down methodologies. By exploring the hydrological sensitivity of the upper Kızılırmak River basin using the Variable [...] Read more.
This study introduces a novel sensitivity analysis approach to assess the resilience and susceptibility of hydrologic systems to the stresses of climate change, moving away from conventional top-down methodologies. By exploring the hydrological sensitivity of the upper Kızılırmak River basin using the Variable Infiltration Capacity (VIC) hydrologic model, we employed a sensitivity-based approach as an alternative to the traditional Global Climate Model (GCM)-based methods, providing more insightful information for water managers. Considering the consistent projections of increasing temperature over this region in GCMs, the hydrologic system was perturbed to examine gradients of a more challenging climate characterized by warming and drying conditions. The sensitivity of streamflow, snow water equivalent, and evapotranspiration to temperature (T) and precipitation (P) variations under each perturbation or “reference” climate was quantified. Results indicate that streamflow responds to T negatively under all warming scenarios. As the reference climates become drier, streamflow sensitivity to P increases, indicating that meteorological drought impacts on water availability could be exacerbated. These results suggest that there will be heightened difficulty in managing water resources in the region if it undergoes both warming and drying due to the following setbacks: (1) water availability will shift away from the summer season of peak water demand due to the warming effects on the snowpack, (2) annual water availability will likely decrease due to a combination of warming and lower precipitation, and (3) streamflow sensitivity to hydroclimatic variability will increase, meaning that there will be more extreme impacts to water availability. Water managers will need to plan for a larger set of extreme conditions. Full article
(This article belongs to the Special Issue Runoff Modelling under Climate Change)
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17 pages, 8109 KiB  
Article
Predictive Assessment of Climate Change Impact on Water Yield in the Meta River Basin, Colombia: An InVEST Model Application
by Jhon B. Valencia, Vladimir V. Guryanov, Jeison Mesa-Diez, Nilton Diaz, Daniel Escobar-Carbonari and Artyom V. Gusarov
Hydrology 2024, 11(2), 25; https://doi.org/10.3390/hydrology11020025 - 08 Feb 2024
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Abstract
This paper presents a hydrological assessment of the 113,981 km2 Meta River basin in Colombia using 13 global climate models to predict water yield for 2050 under two CMIP6 scenarios, SSP 4.5 and SSP 8.5. Despite mixed performance across subbasins, the model [...] Read more.
This paper presents a hydrological assessment of the 113,981 km2 Meta River basin in Colombia using 13 global climate models to predict water yield for 2050 under two CMIP6 scenarios, SSP 4.5 and SSP 8.5. Despite mixed performance across subbasins, the model was notably effective in the upper Meta River subbasin. This study predicts an overall increase in the basin’s annual water yield due to increased precipitation, especially in flatter regions. Under the SSP 4.5, the Meta River basin’s water flow is expected to rise from 5141.6 m3/s to 6397.5 m3/s, and to 6101.5 m3/s under the SSP 8.5 scenario, marking 24% and 19% increases in water yield, respectively. Conversely, the upper Meta River subbasin may experience a slight decrease in water yield, while the upper Casanare River subbasin is predicted to see significant increases. The South Cravo River subbasin, however, is expected to face a considerable decline in water yield, indicating potential water scarcity. This study represents a pioneering large-scale application of the InVEST–AWY model in Colombia using CMIP6 global climate models with an integrated approach to produce predictions of future water yields. Full article
(This article belongs to the Special Issue Runoff Modelling under Climate Change)
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