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Titlebook: Alpine Plant Life; Functional Plant Eco Christian Körner Textbook 19991st edition Springer-Verlag Berlin Heidelberg 1999 Flora.Relief.cell

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https://doi.org/10.1007/978-3-642-57338-5 meteorological station with all its weather masts confirms: +4°C air temperature, 5 ms. wind speed, 40% relative humidity. While our mountaineer experiences the harsh life in the mountains, the world looks different for those who stay close to ground. Micrometeorological research in alpine vegetati
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G. W. Bassett Jr.,M. -Y. S. Tam,K. Knightration of anywhere between 330 and a few days (in the tropics) per year. In some cases, at higher latitudes, alpine plants may even have to (and do) survive one or two years of permanent snowpack, as can happen due to yearly variable snow distribution by wind (Moser et al. 1977). Snow cover strongly
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https://doi.org/10.1007/978-3-642-57338-5distances one can find a large variety of alpine soil types, ranging from alpine sand drifts to peat bogs, from shallow A/C (e.g. rendzina) soils to the deeply weathered profiles of some alpine grassland soils. Vegetation mosaics closely follow these below-ground patterns as was documented in a firs
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Lift-zonoid and Multivariate Depths, beyond which massive single stems and tall crowns either can not be developed, become unaffordable or are disadvantageous (Fig. 7.1). Why do trees disappear above a certain elevation, what causes the alpine zone to be treeless, i.e. “alpine”? The answer to this question would also indicate which fu
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Developments in Rubber Technology—2hortage does occur, and contributes to the overall impact of the physical environment on mountain plants (Fig. 9.1). In this chapter I will first discuss the overall hydrological situation, the land area based water balance and soil moisture at alpine altitudes — aspects which have strong links with
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Quality Requirements and Rubber Mixing,. by a plant depends on the specific activity of its leaves and the total amount (mass or area) of leaves present per total plant mass. Leaf photosynthesis depends on three processes: (1) the diffusion of CO. from the free atmosphere to the site of carboxylation in chloroplasts, (2) the biochemical
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