1964
DOI: 10.1080/00288306.1964.10420166
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Diurnal and seasonal ground temperature variations at Wairakei

Abstract: Weekly readings of ground temperatures to a depth of 6' I) metres were made at Wairakei, New Zealand, between 195R and 1962. These readings were supplemented by multi-point Brown potentiometer recordings to a depth of 3 m for more than a year. Air temperatures were also available for the five-year period. Results show that the mean annual air temperature was 12°c; the range of the diurnal variation (from max. to min.) was less than 1 deg C at depths greater than 30 cm; the range of the seasonal variation was l… Show more

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Cited by 20 publications
(14 citation statements)
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“…In future work it will be important to test how these interact, and the consequence to spatial coordination when plants are under physiological conditions. Of particular interest will be temperature, which is known to differ between the air and the ground (52) and deviate from the photoperiod (53). In fact, it has already been demonstrated that temperature is preferentially sensed by the clock in specific cell types (10,11).…”
Section: Discussionmentioning
confidence: 99%
“…In future work it will be important to test how these interact, and the consequence to spatial coordination when plants are under physiological conditions. Of particular interest will be temperature, which is known to differ between the air and the ground (52) and deviate from the photoperiod (53). In fact, it has already been demonstrated that temperature is preferentially sensed by the clock in specific cell types (10,11).…”
Section: Discussionmentioning
confidence: 99%
“…Plot location was minimally adjusted where necessary to ensure plots occurred in homogeneous areas. Transects were considered complete when the soil temperature measured on a plot was at ambient levels (approximately 16°C in March: Dawson & Fisher 1964) and remained constant or decreased with depth. Soil temperatures on steam-heated soils increase with depth.…”
Section: Areas Of Te Kopia Scenicmentioning
confidence: 99%
“…Where hot ground, with a mean annual temperature increase between the surface and 1 m depth of 25°c or above, was indicated, either by these measurements or visually, more numerous measurements were made at a depth of 15 em. The latter temperature data enabled the hot ground to be classified according to the nine categories of the soil temperature to heat intensity relationship established by Dawson (1964).…”
Section: Ground Measurementsmentioning
confidence: 99%
“…It has been assumed that the soil conditions at and around Taupo are the same as at Wairakei (Dawson and Fisher, 1964), 8 kilometres away. The results obtained are shown in Table 2.…”
Section: Heat Flow Through the Soil Dominantly By Conductionmentioning
confidence: 99%