1961
DOI: 10.1007/bf02244639
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Die Bodentemperaturverhältnisse an einer zentralalpinen Hanglage beiderseits der Waldgrenze

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Cited by 6 publications
(12 citation statements)
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“…24) found, between 10:00 a.m. and 6:00 p.m., maximum differences in average surface temperatures of 2 °C between microsites receiving different amounts of direct sunlight in small gaps in subalpine P. abies forests. In contrast, direct radiation can strongly influence temperatures at the soil surface in high-elevation environments [3], and instantaneous values at 1 cm depth [27]. These results suggest that, given an intermediate direct energy input, the time of day of exposure to direct light is unlikely to influence the growth of P. abies seedlings by a soil temperature-root growth path.…”
Section: Performance Of Light Treatments and Effects On Soil Temperaturesupporting
confidence: 37%
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“…24) found, between 10:00 a.m. and 6:00 p.m., maximum differences in average surface temperatures of 2 °C between microsites receiving different amounts of direct sunlight in small gaps in subalpine P. abies forests. In contrast, direct radiation can strongly influence temperatures at the soil surface in high-elevation environments [3], and instantaneous values at 1 cm depth [27]. These results suggest that, given an intermediate direct energy input, the time of day of exposure to direct light is unlikely to influence the growth of P. abies seedlings by a soil temperature-root growth path.…”
Section: Performance Of Light Treatments and Effects On Soil Temperaturesupporting
confidence: 37%
“…Soil temperature within this layer limits root growth [4,16], which starts at a temperature of 8 and 12°C [42] and increases up to about 20 °C [41,42]. Site factors affecting near-surface soil temperatures are air temperature, direct sunlight, vegetation cover [3,16,28], snow cover [3], and soil properties such as water content [38].…”
Section: Introductionsupporting
confidence: 38%
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“…Auch im Zuge von glaziologischen Studien wurden Überlegungen zum Kleinklima angestellt (Hoinkes & Rudolph 1961). Die Bedeutung der Bodentemperatur für das Pflanzenwachstum erkannte bereits Aulitzky (1961). Anhand von Bodentemperaturmessungen über und unter der Waldgrenze zeigte er "kleinstandörtliche" Unterschiede und die Abhängigkeit von der Schneebedeckung auf (Aulitzky 1961(Aulitzky , 1962a(Aulitzky , 1962b.…”
Section: Gewässerbeschreibung Und Zonierungunclassified
“…Die Bedeutung der Bodentemperatur für das Pflanzenwachstum erkannte bereits Aulitzky (1961). Anhand von Bodentemperaturmessungen über und unter der Waldgrenze zeigte er "kleinstandörtliche" Unterschiede und die Abhängigkeit von der Schneebedeckung auf (Aulitzky 1961(Aulitzky , 1962a(Aulitzky , 1962b. Im Rahmen des Man and Biosphere-Projekts (MAB; Moser 1975, Patzelt 1987 einer Wiese bei Obergurgl durchgeführt (Rott 1979(Rott , 1987Staudinger 1987 …”
Section: Gewässerbeschreibung Und Zonierungunclassified