LEADER 03653nam  2200961z- 450 
001 9910367567203321
005 20231214133021.0
010   $a3-03921-386-5
035   $a(CKB)4100000010106074
035   $a(oapen)https://directory.doabooks.org/handle/20.500.12854/47854
035   $a(EXLCZ)994100000010106074
100   $a20202102d2019      |y         0
101 0 $aeng
135   $aurmn|---annan
181   $ctxt$2rdacontent
182   $cc$2rdamedia
183   $acr$2rdacarrier
200 10$aForest Hydrology and Watershed
210   $cMDPI - Multidisciplinary Digital Publishing Institute$d2019
215   $a1 electronic resource (206 p.)
311   $a3-03921-385-7 
330   $aHydrological 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.
610   $aEast Asia
610   $aclimate variability
610   $ametals
610   $awoody litter
610   $aextreme weather events
610   $afrequency analysis
610   $arelative contribution
610   $astreamflow variability
610   $aprobability distribution
610   $atrace metal
610   $aclimate change
610   $aannual streamflow
610   $ahydroclimatology
610   $aforest disturbances
610   $ariver discharge
610   $aclimate warming
610   $aWeihe River
610   $anon-woody litter
610   $ariparian forest
610   $alow flow
610   $aCentral Asia
610   $acanopy filtering
610   $aflood
610   $aSWAT
610   $aChu River
610   $aannual water yield
610   $aforest hydrology
610   $athroughfall
610   $aflow regimes
610   $aSchrenk spruce (Picea schrenkiana Fisch. et Mey.)
610   $atree rings
610   $aforest floor
610   $areforestation
610   $aland-use change
610   $alow flows
610   $awatershed management
610   $ahigh flow
610   $aforest disturbance
610   $asubalpine forest
610   $agap-edge canopy
610   $ahuman activities
610   $aboreal forest
610   $aTianshan Mountains
610   $aclosed canopy
610   $agroundwater level
610   $afruit tree planting
610   $ahydrological model
610   $ahigh flows
610   $acumulative effects
610   $areconstruction
610   $aheadwater stream
610   $apartial least squares (PLS) regression
610   $astreamflow
700   $aMeng$b Fan-Rui$4auth$01329493
702   $aLi$b Qiang$4auth
702   $aArain$b Altaf$4auth
702   $aPisaric$b Michael$4auth
906   $aBOOK
912   $a9910367567203321
996   $aForest Hydrology and Watershed$93039511
997   $aUNINA