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dc.contributor.authorFrenck G
dc.contributor.authorLeitinger G
dc.contributor.authorObojes N
dc.contributor.authorHofmann M
dc.contributor.authorNewesely C
dc.contributor.authorDeutschmann M
dc.contributor.authorTappeiner U
dc.contributor.authorTasser E
dc.date.accessioned2018-10-11T15:59:43Z
dc.date.available2018-10-11T15:59:43Z
dc.date.issued2018
dc.identifier.issn1726-4170
dc.identifier.urihttp://dx.doi.org/10.5194/bg-15-1065-2018
dc.identifier.urihttp://hdl.handle.net/10863/6479
dc.description.abstractFor central Europe in addition to rising temperatures an increasing variability in precipitation is predicted. This will increase the probability of drought periods in the Alps, where water supply has been sufficient in most areas so far. For Alpine grasslands, community-specific imprints on drought responses are poorly analyzed so far due to the sufficient natural water supply. In a replicated mesocosm experiment we compared evapotranspiration (ET) and biomass productivity of two differently drought-adapted Alpine grassland communities during two artificial drought periods divided by extreme precipitation events using high-precision small lysimeters. The drought-adapted vegetation type showed a high potential to utilize even scarce water resources. This is combined with a low potential to translate atmospheric deficits into higher water conductance and a lower biomass production as those measured for the non-drought-adapted type. The non-drought-adapted type, in contrast, showed high water conductance potential and a strong increase in ET rates when environmental conditions became less constraining. With high rates even at dry conditions, this community appears not to be optimized to save water and might experience drought effects earlier and probably more strongly. As a result, the water use efficiency of the drought-adapted plant community is with 2.6 gDW kg−1 of water much higher than that of the non-drought-adapted plant community (0.16 gDW kg−1). In summary, the vegetation's reaction to two covarying gradients of potential evapotranspiration and soil water content revealed a clear difference in vegetation development and between water-saving and water-spending strategies regarding evapotranspiration.en_US
dc.language.isoenen_US
dc.rights
dc.titleCommunity specific hydraulic conductance potential of soil water decomposed for two Alpine grasslands by small-scale lysimetryen_US
dc.typeArticleen_US
dc.date.updated2018-10-11T15:26:49Z
dc.language.isiEN-GB
dc.journal.titleBiogeosciences
dc.description.fulltextopenen_US


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