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  • The amount and intensity of atmospheric precipitation and throughfall were measured in a young fully closed untended spruce stand in the Drahanská vrchovina Upland. The same measurement was also carried out in the stand after the accomplishment of a heavy thinning measure. On average, the studied spruce stand before thinning intercepted 50% precipitation (amplitude 37%). Decrease in stand density resulted in the decrease of average interception by 10% (interception after thinning 40% atmospheric precipitation) at the simultaneous increasing the amplitude of values of interception losses (amplitude 46%) and decrease in the value of interception for particular cases. The amount of stand precipitation temporarily increased.
  • The amount and intensity of atmospheric precipitation and throughfall were measured in a young fully closed untended spruce stand in the Drahanská vrchovina Upland. The same measurement was also carried out in the stand after the accomplishment of a heavy thinning measure. On average, the studied spruce stand before thinning intercepted 50% precipitation (amplitude 37%). Decrease in stand density resulted in the decrease of average interception by 10% (interception after thinning 40% atmospheric precipitation) at the simultaneous increasing the amplitude of values of interception losses (amplitude 46%) and decrease in the value of interception for particular cases. The amount of stand precipitation temporarily increased. (en)
  • Množství a intenzita atmosférických a podkorunových srážek byla měřena v mladém, plně zapojeném, nevychovávaném smrkovém porostu na Drahanské vrchovině. Stejná měření probíhala v tomto porostu také po provedení silného probírkového zásahu. V průměru sledovaný smrkový porost před probírkou zadržoval 50 % srážek (amplituda 37 %). Snížení hustoty porostu vedlo ke snížení průměrné intercepce o 10 % (intercepce po probírce 40 % atmosférických srážek) při současném zvýšení amplitudy hodnot intercepčních ztrát (amplituda 46 %) a poklesu hodnot intercepce pro jednotlivé případy. Množství porostních srážek se dočasně zvýšilo. (cs)
Title
  • Effects of stand tending on the interception of atmospheric precipitation
  • Vliv výchovy porostu na intercepci atmosférických srážek (cs)
  • Effects of stand tending on the interception of atmospheric precipitation (en)
skos:prefLabel
  • Effects of stand tending on the interception of atmospheric precipitation
  • Vliv výchovy porostu na intercepci atmosférických srážek (cs)
  • Effects of stand tending on the interception of atmospheric precipitation (en)
skos:notation
  • RIV/62156489:43410/05:00057305!RIV06-GA0-43410___
http://linked.open.../vavai/riv/strany
  • 1;5
http://linked.open...avai/riv/aktivita
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  • P(GP526/01/D079)
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
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  • 519623
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  • RIV/62156489:43410/05:00057305
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  • atmospheric precipitation; interception; throughfall (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [E60702F1B1CE]
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  • Křtiny
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  • Bioklimatologie současnosti a budoucnosti
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  • Kamlerová, Klára
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number of pages
http://purl.org/ne...btex#hasPublisher
  • ČSBS, MZLU v Brně, SPU v Nitře, TU ve Zvolenu, ČHMÚ
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  • 80-86690-31-8
http://localhost/t...ganizacniJednotka
  • 43410
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