LEADER 04994nam 2201369z- 450 001 9910404090503321 005 20231214132856.0 010 $a3-03928-631-5 035 $a(CKB)4100000011302233 035 $a(oapen)https://directory.doabooks.org/handle/20.500.12854/40686 035 $a(EXLCZ)994100000011302233 100 $a20202102d2020 |y 0 101 0 $aeng 135 $aurmn|---annan 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aAlpine and Polar Treelines in a Changing Environment 210 $cMDPI - Multidisciplinary Digital Publishing Institute$d2020 215 $a1 electronic resource (268 p.) 311 $a3-03928-630-7 330 $aConcerns have been raised with respect to the state of high-altitude and high-latitude treelines, as they are anticipated to undergo considerable modifications due to global changes, and especially due to climate warming. As high-elevation treelines are temperature-limited vegetation boundaries, they are considered to be sensitive to climate warming. As a consequence, in this future, warmer environment, an upward migration of treelines is expected because low air and root-zone temperatures constrain their regeneration and growth. Despite the ubiquity of climate warming, treeline advancement is not a worldwide phenomenon: some treelines have been advancing rapidly, others have responded sluggishly or have remained stable. This variation in responses is attributed to the potential interaction of a continuum of site-related factors that may lead to the occurrence of locally conditioned temperature patterns. Competition amongst species and below-ground resources have been suggested as additional factors explaining the variability in the movement of treelines. This Special Issue (book) is dedicated to the discussion of treeline responses to changing environmental conditions in different areas around the globe. 610 $atree seedling recruitment 610 $ashrubline 610 $alight quality 610 $ahigher altitude 610 $aprecipitation 610 $aexperimental rain exclusion 610 $aPinus cembra 610 $aChangbai Mountain 610 $atreeline dynamics 610 $afungal ecology 610 $athermal continentality 610 $atree regeneration 610 $aelevational transect 610 $amonitoring 610 $aconifer shrub 610 $aplant water availability 610 $apermafrost 610 $afoehn winds 610 $atreeline 610 $aHolocene 610 $anitrogen cycling 610 $acarotenoids 610 $atimberline 610 $a15N natural abundance 610 $aspectrometer 610 $abasal area increment 610 $apalynology 610 $axylem embolism 610 $adiversity 610 $aelevational treeline 610 $aEuropean Alps 610 $atemperature 610 $atree line 610 $awinter stress 610 $aphotosynthetic pigments 610 $aPinus sibirica 610 $awesterly winds 610 $arelative air humidity 610 $aecosystem manipulation 610 $aLarix decidua 610 $amicrosite 610 $apolar treeline 610 $aCentral Austrian Alps 610 $aSwitzerland 610 $amulti-stemmed growth form 610 $aconifers 610 $aforest edge 610 $ahistory of treeline research 610 $asoil drought 610 $adendroclimatology 610 $aknowledge engineering 610 $aRocky Mountains 610 $aapical control 610 $acloud 610 $apostglacial 610 $aalpine timberline 610 $aspace-for-time substitution 610 $aclimate change 610 $aexpert elicitation 610 $ashoot elongation 610 $apit aspiration 610 $aclimate warming 610 $aclimate zone 610 $aalpine treeline 610 $arefilling 610 $aAbies sibirica 610 $agrowth trend 610 $awestern Montana 610 $alight quantity 610 $aPicea abies 610 $aMediterranean climate 610 $aforest climatology 610 $aaltitude 610 $aenvironmental stress 610 $asub-Antarctic 610 $aErman's birch 610 $aphotoinhibition 610 $atocopherol 610 $aelevational gradients 610 $aNDVI 610 $along-term trends 610 $asap flow 610 $apeat 610 $atree seedlings 610 $aSouthern Ocean 610 $achlorophyll 610 $anon-structural carbohydrates (NSCs) 610 $adrought 610 $aupward advance 610 $aremote sensing data 700 $aWieser$b Gerhard$4auth$01328859 906 $aBOOK 912 $a9910404090503321 996 $aAlpine and Polar Treelines in a Changing Environment$93039038 997 $aUNINA