Intradiurnal and seasonal variability of soil temperature, heat flux, soil moisture content, and thermal properties under forest and pasture in Rondônia.

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dc.contributorR. C. S. ALVALA, Instituto Nacional de Pesquisas Espaciais/SP
dc.contributorR. GIELOW, Instituto Nacional de Pesquisas Espaciais/SP
dc.contributorH. R. DA ROCHA,, USP/SP
dc.contributorH. C. FREITAS, USP/SP
dc.contributorJ. M. LOPES, USP
dc.contributorA. O. MANZI,, Instituto Nacional de Pesquisas Espaciais/SP
dc.contributorC. VON RANDOW, Instituto Nacional de Pesquisas Espaciais
dc.contributorM. A. F. S. DIAS, USP
dc.contributorOSVALDO MACHADO RODRIGUES CABRAL, CNPMA
dc.contributorM. J. WATERLOO, Vrije Universiteit Amsterdam, Amsterdam, Netherlands.
dc.creatorALVALÁ, R. C. S.
dc.creatorGIELOW, R.
dc.creatorROCHA, H. R. da
dc.creatorFREITAS, H. C.
dc.creatorLOPES, J. M.
dc.creatorMANZI, A. O.
dc.creatorRANDOW, C. von
dc.creatorDIAS, M. A. F. S.
dc.creatorCABRAL, O. M. R.
dc.creatorWATERLOO, M. J.
dc.date2017-09-19T00:13:31Z
dc.date2017-09-19T00:13:31Z
dc.date2007-07-04
dc.date2002
dc.date2017-09-19T00:13:31Z
dc.date.accessioned2026-07-07T05:04:47Z
dc.descriptionSoil temperatures depend on the soil heat flux, an important parameter in meteorological and plant growth-energy balance models. Thus, they were measured, together with soil moisture contents, within the LBA program at forest (Reserva Jaru) and pasture (Fazenda Nossa Senhora) sites in Rondônia, Brazilian Amazonia during wet (February) and dry (August) periods of 1999. The wet period showed maxima of the heat flux into the soil around five to six times smaller at the forest than at the pasture, except for some spikes that are related to stronger solar forcing, such as those due to sunspecks in the forest. This pattern remained during the dry period, but with doubled maximum values. Also, the soil heat flux and the soil temperatures responded very significantly to the passage of cold fronts in both periods at both sites. Temperature profiles measured in the 0.10-0.40 m soil layer showed daily averages and ranges smaller at the forest than at the pasture. The daily average of the soil moisture content in the same layer, during the wet season, increased with depth at both sites, with consistently lower values at the forest. However, their ranges were smaller at the pasture, except for the 0.40 m depth. During the dry period, these ranges were much higher at the pasture, but with nearer average values. Finally, the computed daily apparent soil thermal diffusivities, volumetric heat contents, and thermal conductivities are presented, with the first ones crossed with the measured soil moisture content.
dc.identifierJournal of Geophysical Research, Washington, v. 107, n. D20, p. LBA10-1 - LBA 10-20, 2002.
dc.identifierhttp://www.alice.cnptia.embrapa.br/alice/handle/doc/15531
dc.identifier.urihttp://hdl.handle.net/123456789/479614
dc.languageeng
dc.rightsopenAccess
dc.subjectFluxo de calor
dc.subjectVariabilidade
dc.subjectBalanço de Energia
dc.subjectFloresta
dc.subjectPastagem
dc.subjectUmidade do Solo
dc.subjectTemperatura do Solo
dc.subjectAmazonia
dc.titleIntradiurnal and seasonal variability of soil temperature, heat flux, soil moisture content, and thermal properties under forest and pasture in Rondônia.
dc.typeArtigo de periódico

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