Forest Hydrology and Watershed

Hydrological processes in forested watersheds are influenced by environmental, physiological, and biometric factors such as precipitation, radiation, temperature, species type, leaf area, and extent and structure of forest ecosystems. Over the past two centuries, forest coverage and forest structure...

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Bibliographic Details
Main Author: Meng, Fan-Rui (auth)
Other Authors: Li, Qiang (auth), Arain, Altaf (auth), Pisaric, Michael (auth)
Format: Book Chapter
Published: MDPI - Multidisciplinary Digital Publishing Institute 2019
Subjects:
Online Access:Get Fullteks
DOAB: description of the publication
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020 |a books978-3-03921-386-3 
020 |a 9783039213856 
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024 7 |a 10.3390/books978-3-03921-386-3  |c doi 
041 0 |a English 
042 |a dc 
100 1 |a Meng, Fan-Rui  |4 auth 
700 1 |a Li, Qiang  |4 auth 
700 1 |a Arain, Altaf  |4 auth 
700 1 |a Pisaric, Michael  |4 auth 
245 1 0 |a Forest Hydrology and Watershed 
260 |b MDPI - Multidisciplinary Digital Publishing Institute  |c 2019 
300 |a 1 electronic resource (206 p.) 
506 0 |a Open Access  |2 star  |f Unrestricted online access 
520 |a Hydrological processes in forested watersheds are influenced by environmental, physiological, and biometric factors such as precipitation, radiation, temperature, species type, leaf area, and extent and structure of forest ecosystems. Over the past two centuries, forest coverage and forest structures have been impacted globally by anthropogenic activities, for example, forest harvesting, and conversion of forested landscapes for plantations and urbanization. In addition, since the industrial revolution, climate change has resulted in profound impacts on forest ecosystems due to higher carbon dioxide (CO2) concentration or CO2 fertilization, warmer temperatures, changes in frequency and intensity of extreme weather events and natural disturbances. As a result, hydrological processes in forested watersheds have been altered by these natural and anthropogenic factors and these changes are expected to accelerate due to future changing climatic conditions. 
540 |a Creative Commons  |f https://creativecommons.org/licenses/by-nc-nd/4.0/  |2 cc  |4 https://creativecommons.org/licenses/by-nc-nd/4.0/ 
546 |a English 
653 |a East Asia 
653 |a climate variability 
653 |a metals 
653 |a woody litter 
653 |a extreme weather events 
653 |a frequency analysis 
653 |a relative contribution 
653 |a streamflow variability 
653 |a probability distribution 
653 |a trace metal 
653 |a climate change 
653 |a annual streamflow 
653 |a hydroclimatology 
653 |a forest disturbances 
653 |a river discharge 
653 |a climate warming 
653 |a Weihe River 
653 |a non-woody litter 
653 |a riparian forest 
653 |a low flow 
653 |a Central Asia 
653 |a canopy filtering 
653 |a flood 
653 |a SWAT 
653 |a Chu River 
653 |a annual water yield 
653 |a forest hydrology 
653 |a throughfall 
653 |a flow regimes 
653 |a Schrenk spruce (Picea schrenkiana Fisch. et Mey.) 
653 |a tree rings 
653 |a forest floor 
653 |a reforestation 
653 |a land-use change 
653 |a low flows 
653 |a watershed management 
653 |a high flow 
653 |a forest disturbance 
653 |a subalpine forest 
653 |a gap-edge canopy 
653 |a human activities 
653 |a boreal forest 
653 |a Tianshan Mountains 
653 |a closed canopy 
653 |a groundwater level 
653 |a fruit tree planting 
653 |a hydrological model 
653 |a high flows 
653 |a cumulative effects 
653 |a reconstruction 
653 |a headwater stream 
653 |a partial least squares (PLS) regression 
653 |a streamflow 
856 4 0 |a www.oapen.org  |u https://mdpi.com/books/pdfview/book/1498  |7 0  |z Get Fullteks 
856 4 0 |a www.oapen.org  |u https://directory.doabooks.org/handle/20.500.12854/47854  |7 0  |z DOAB: description of the publication