Impact of forest maintenance on water shortages: Hydrologic modeling and effects of climate change
Creators
- 1. School of Environmental Science and Engineering, Chang'an University, Xi'an 710064 (China)
- 2. Key Laboratory of Subsurface Hydrology and Ecological Effects in Arid Region, Ministry of Education, Chang'an University, Xi'an 710064 (China)
- 3. Disaster Prevention Research Institute (DPRI), Kyoto University, Uji, Kyoto 6110011 (Japan)
- 4. School of Engineering, University of California – Merced, 5200 Lake R, Merced, CA 95343 (United States)
- 5. Dept. Civil and Environmental Engineering, UC Davis, Ghausi Hall, One Shields Ave, Davis, CA 95616 (United States)
Description
Highlights: • We present a model to explore impact of forest management on hydrologic processes. • Results indicate that surface flow and soil water increases after forest management. • Climate change has little impact on near-future discharge, dramatic impact by 2100. • Climate change leads to reduced soil moisture in the future period. • Forest hydrology models show potential for informing environmental management. The importance of water quantity for domestic and industrial water supply, agriculture, and the economy more broadly has led to the development of many water quantity assessment methods. In this study, surface flow and soil water in the forested upper reaches of the Yoshino River are compared using a distributed hydrological model with Forest Maintenance Module under two scenarios; before and after forest maintenance. We also examine the impact of forest maintenance on these variables during extreme droughts. Results show that surface flow and soil water increased after forest maintenance. In addition, projections of future water resources were estimated using a hydrological model and the output from a 20 km mesh Global Climate Model (GCM20). River discharge for the near-future (2015–2039) is similar to that of the present (1979–2003). Estimated river discharge for the future (2075–2099) was found to be substantially more extreme than in the current period, with 12 m3/s higher peak discharge in August and 7 m3/s lower in July compared to the discharges of the present period. Soil water for the future is estimated to be lower than for the present and near future in May. The methods discussed in this study can be applied in other regions and the results help elucidate the impact of forests and climate change on water resources.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2017.09.044Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2017.09.044;
- PII
- S0048969717323859;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 615
- Journal Page Range
- p. 1355-1363
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 53039371
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- AGRICULTURE; CLIMATE MODELS; CLIMATIC CHANGE; DROUGHTS; FORESTS; HYDROLOGY; MAINTENANCE; MOISTURE; RIVERS; SHORTAGES; SOILS; WATER RESOURCES; WATER SUPPLY
- Descriptors DEC
- MATHEMATICAL MODELS; RESOURCES; SURFACE WATERS
Optional Information
- Copyright
- Copyright (c) 2017 Elsevier B.V. All rights reserved.