Impacts of Climate Change on Hydrological Processes

A special issue of Climate (ISSN 2225-1154). This special issue belongs to the section "Climate and Environment".

Deadline for manuscript submissions: 31 December 2025 | Viewed by 2026

Special Issue Editors


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Department of hydrology, Geological Survey of Denmark and Greenland, 1350 Copenhagen, Denmark
Interests: large-scale hydrological modeling; data-driven methods; remote sensing
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Guest Editor
School of Engineering, University of Newcastle, Callaghan, NSW 2308, Australia
Interests: data assimilation; satellite remote sensing; land surface modelling; model calibration; hydrographic mapping
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Special Issue Information

Dear Colleagues,

Climate change is one of the most pressing global issues that we currently face. Global warming, changes in precipitation patterns or glacier retreat have a profound impact on the water cycle and hydrological processes across local, regional and global scales. These effects permeate into changes in rainfall intensity, fluctuations in river flows, intensity of evapotranspiration, variations in soil moisture, the rise and fall of groundwater levels, adjustments in lake levels and volumes, reductions in glacier area and volume, the deterioration of water quality and adjustments in irrigation and other water demands.

In this context, a deep understanding of how climate change specifically affects hydrological systems and water resources is not only essential for maintaining ecological balance but also for ensuring the stable functioning of socio-economic systems. This Special Issue aims to collect the latest research results in the intersection of hydrology and climate change, from basic discussions on the dynamics and mechanisms of climate change to how specific climate change affects hydrological processes and their changing trends in global and local areas. Potential topics include, but are not limited to, the following:

  • Dynamics and mechanisms of climate change;
  • Simulation of hydrological processes and changes at different scales in different climate regions;
  • Monitoring and early warning of extreme climate and hydrological events;
  • Hydrological processes in land–atmosphere interactions;
  • Development of coupled climate–hydrological models;
  • Climate adaptation policy design based on hydrological processes;
  • Effects of human activities on climate–hydrological systems.

Dr. Jun Liu
Dr. Mehdi Khaki
Guest Editors

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Keywords

  • climate change
  • hydrological processes
  • water cycle
  • extreme events
  • hydrological model
  • climate model

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Published Papers (1 paper)

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Research

18 pages, 4915 KB  
Article
Snowmelt Streamflow Trends over Colorado (U.S.A.) Mountain Watersheds
by Steven R. Fassnacht and Anna K. D. Pfohl
Climate 2025, 13(9), 177; https://doi.org/10.3390/cli13090177 - 28 Aug 2025
Viewed by 1767
Abstract
Streamflow generated from snowmelt is important, and changing, in snow dominated regions of the world. We used a recently developed technique to estimate the start and end of snowmelt streamflow for 39 gauging stations across Colorado and determined the 40-year trends from 1981 [...] Read more.
Streamflow generated from snowmelt is important, and changing, in snow dominated regions of the world. We used a recently developed technique to estimate the start and end of snowmelt streamflow for 39 gauging stations across Colorado and determined the 40-year trends from 1981 to 2020. Most watersheds showed a trend towards an earlier start (34 watersheds) or end (29 watersheds) of snowmelt streamflow, but the mean of the start and end dates showed mixed trends (earlier in 12 watersheds and later in 20). We determined the correlation between these streamflow snowmelt trends and terrain parameters plus trends in canopy cover, winter precipitation, peak snow water equivalent, and melt-period temperature. There were some significant correlations, primarily for total annual streamflow and the timing and volume of the end of snowmelt streamflow contribution to winter precipitation (decreasing), minimum temperature (warming), and slope (negatively). Higher elevation watersheds tend to be steeper, less snow has been observed at higher elevations, and the snowpack is melting sooner. Snowmelt streamflow trends are partially explained by climate trends and watershed characteristics. Full article
(This article belongs to the Special Issue Impacts of Climate Change on Hydrological Processes)
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