About: Evaporation of a young spruce and beech stand after the canopy closure disturbance by snow disaster in the growing season 2006     Goto   Sponge   NotDistinct   Permalink

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Description
  • Tato studie navazuje na analýzu výparu z povrchu půdy a přízemní vegetace v mladém smrkovém a bukovém porostě a na volné ploše prováděné na stacionáru Deštné v Orlických horách v roce 2005. Tyto porosty byly v zimě 2005/2006 zasaženy neobvykle velkým přívalem sněhu, kdy celková vodní hodnota sněhové pokrývky dosahovala ve smrkovém porostě 819,0 mm a v buku 832,7 mm, při celkové výšce 157,2 cm a 164,1 cm. Při přívalech mokrého sněhu v první dekádě února (158 mm) a v období od 6.3. do 13.3. dokonce (182 mm), bylo poškozeno 98 % smrků. Jednalo se především o vrcholové zlomy, ale u 50 % stromů zůstaly na kmenech živé pouze 2 až 3 přesleny větví. Bukový porost nebyl prakticky poškozen vůbec, poškozeno bylo pouze 10 % podúrovňových stromů s nepříznivým štíhlostním kvocientem. To v konečném důsledku znamenalo, že v roce 2005, kdy byly hodnoty na hranici statistické průkaznosti vyšší v bukovém porostě, a to maximálně o 3 až 5 mm za měsíc, došlo po kalamitní situaci v průměru k dvojnásobnému navýšení evapora (cs)
  • The study is a follow-up of the analysis of evaporation from the soil surface and ground vegetation in a young spruce and beech stand and in the open area carried out in the permanent field experiment station Deštné in the Orlické hory in 2005. These stands were affected by an unusually large amount of snow when the total snow-water content reached 819.0 mm in the spruce stand and 832.7 mm in the beech stand at the total height of snow 157.2 and 164.1 cm, respectively. After the %22flood%22 of wet snow in the first decade of February (158 mm) and in the period from 6/3 to 13/3 (even 182 mm), some 98% spruce was damaged. It referred particularly to top breaks but in 50%, only 2 to 3 whorls of branches remained living. The beech stand was not virtually damaged at all. Only 10% subdominant trees with unfavourable slenderness ratio were damaged. This finally meant that in 2005, on average the double increase of evaporation occurred in the spruce stand after the disaster situation.
  • The study is a follow-up of the analysis of evaporation from the soil surface and ground vegetation in a young spruce and beech stand and in the open area carried out in the permanent field experiment station Deštné in the Orlické hory in 2005. These stands were affected by an unusually large amount of snow when the total snow-water content reached 819.0 mm in the spruce stand and 832.7 mm in the beech stand at the total height of snow 157.2 and 164.1 cm, respectively. After the %22flood%22 of wet snow in the first decade of February (158 mm) and in the period from 6/3 to 13/3 (even 182 mm), some 98% spruce was damaged. It referred particularly to top breaks but in 50%, only 2 to 3 whorls of branches remained living. The beech stand was not virtually damaged at all. Only 10% subdominant trees with unfavourable slenderness ratio were damaged. This finally meant that in 2005, on average the double increase of evaporation occurred in the spruce stand after the disaster situation. (en)
Title
  • Evaporation of a young spruce and beech stand after the canopy closure disturbance by snow disaster in the growing season 2006
  • Evaporation of a young spruce and beech stand after the canopy closure disturbance by snow disaster in the growing season 2006 (en)
  • Evaporace mladého smrkového a bukového porostu po narušení zápoje sněhovou kalmitou ve vegetačním období 2006 (cs)
skos:prefLabel
  • Evaporation of a young spruce and beech stand after the canopy closure disturbance by snow disaster in the growing season 2006
  • Evaporation of a young spruce and beech stand after the canopy closure disturbance by snow disaster in the growing season 2006 (en)
  • Evaporace mladého smrkového a bukového porostu po narušení zápoje sněhovou kalmitou ve vegetačním období 2006 (cs)
skos:notation
  • RIV/62156489:43410/07:00114537!RIV08-MZE-43410___
http://linked.open.../vavai/riv/strany
  • 25;30
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(1G57016), Z(MSM6215648902)
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 420821
http://linked.open...ai/riv/idVysledku
  • RIV/62156489:43410/07:00114537
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • evaporation; evapotranspiration; spruce; beech; clear felling (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [20FDB275C580]
http://linked.open...v/mistoKonaniAkce
  • Zvolen
http://linked.open...i/riv/mistoVydani
  • Zvolen
http://linked.open...i/riv/nazevZdroje
  • Management of forests in changing environmental conditions
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Karl, Zdeněk
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
http://linked.open...n/vavai/riv/zamer
number of pages
http://purl.org/ne...btex#hasPublisher
  • Technická univerzita vo Zvolene
https://schema.org/isbn
  • 978-80-228-1779-0
http://localhost/t...ganizacniJednotka
  • 43410
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