TY  - GEN
AU  - Meng,Fan-Rui
AU  - Li,Qiang
AU  - Arain,Altaf
AU  - Pisaric,Michael
TI  - Forest Hydrology and Watershed
SN  - books978-3-03921-386-3
PY  - 2019///
PB  - MDPI - Multidisciplinary Digital Publishing Institute
KW  - East Asia
KW  - climate variability
KW  - metals
KW  - woody litter
KW  - extreme weather events
KW  - frequency analysis
KW  - relative contribution
KW  - streamflow variability
KW  - probability distribution
KW  - trace metal
KW  - climate change
KW  - annual streamflow
KW  - hydroclimatology
KW  - forest disturbances
KW  - river discharge
KW  - climate warming
KW  - Weihe River
KW  - non-woody litter
KW  - riparian forest
KW  - low flow
KW  - Central Asia
KW  - canopy filtering
KW  - flood
KW  - SWAT
KW  - Chu River
KW  - annual water yield
KW  - forest hydrology
KW  - throughfall
KW  - flow regimes
KW  - Schrenk spruce (Picea schrenkiana Fisch. et Mey.)
KW  - tree rings
KW  - forest floor
KW  - reforestation
KW  - land-use change
KW  - low flows
KW  - watershed management
KW  - high flow
KW  - forest disturbance
KW  - subalpine forest
KW  - gap-edge canopy
KW  - human activities
KW  - boreal forest
KW  - Tianshan Mountains
KW  - closed canopy
KW  - groundwater level
KW  - fruit tree planting
KW  - hydrological model
KW  - high flows
KW  - cumulative effects
KW  - reconstruction
KW  - headwater stream
KW  - partial least squares (PLS) regression
KW  - streamflow
N1  - Open Access
N2  - 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
UR  - https://mdpi.com/books/pdfview/book/1498
UR  - https://directory.doabooks.org/handle/20.500.12854/47854
ER  -