2000
DOI: 10.1007/s007040050005
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Simply Obtained Global Radiation, Soil Temperature and SoilMoisture in an Alley Cropping System in Semi-Arid Kenya

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Cited by 13 publications
(8 citation statements)
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“…The ceptometer was also inverted 1.0 m above the canopy to measure reflected PAR from the canopy-soil scene. Precautions taken and difficulties met with such equipment were as listed by Mungai et al [20].…”
Section: Plant Sampling and Analysismentioning
confidence: 99%
“…The ceptometer was also inverted 1.0 m above the canopy to measure reflected PAR from the canopy-soil scene. Precautions taken and difficulties met with such equipment were as listed by Mungai et al [20].…”
Section: Plant Sampling and Analysismentioning
confidence: 99%
“…However, as opposed to works devoted to an analysis of the impact of the intensity of solar radiation, air temperature and wind speed on soil temperature (Bednarek 1966, Mungai et al 1998, Keryn et al 2004, the results obtained for the impact of the radiation balance at the horizontal surface on the temperature over the area of the sand dune were rather unsatisfactory. The regression models obtained helped explain the said relation in no more than 30%.…”
Section: Conclusion and A Discussion Of Resultsmentioning
confidence: 82%
“…In addition, the shaping of local thermal relations is significantly impacted by the type of active surface and the frequency of sunny and cloudy days (Paszyński 1999, Olecki 2000, Obrębska-Starklowa 2001. One may single out a number of works that have been devoted to the issue of the influence of solar radiation on soil temperature and attempted to achieve a model presentation of the dependences between soil thermal conditions and the intensity of solar radiation, air temperature and wind speed for areas with varied vegetation growth (Bednarek 1966, Keryn et al 2004, Mungai et al, 1998.…”
Section: Thermal and Humidity Conditions Over A Salient Land Form As mentioning
confidence: 99%
“…During the radiation weather days, the temperature changes are more dynamic and the daily amplitudes at each depth are much higher than on the wet weather days. The higher wind speed during the non-radiation days may be considered as an additional factor reducing the heat transfer to the soil (Mungai et al, 1998). In the pine forest, the differences between the soil temperature during the radiation weather and wet weather are not so signifi cant, however, on the wet weather days, hardly any temperature changes under the surface are observed.…”
Section: Discussionmentioning
confidence: 99%