2008
DOI: 10.1016/j.agrformet.2008.01.001
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Above-ground thermal energy storage rates, trunk heat fluxes and surface energy balance in a central Amazonian rainforest

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Cited by 81 publications
(43 citation statements)
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“…Poucos são os estudos que tratam da estimativa de armazenamento de calor na biomassa (Moore & Fisch, 1986;McCaughey & Saxton, 1988;Meesters & Vugts, 1996;Michiles & Gielow, 2008). Isto porque a estimativa da energia estocada na biomassa se torna complexa devido à variação de temperatura no dossel e no caule, o que requer um grande número de sensores (McCaughey & Saxton, 1988;Oliphant et al, 2004;Barr et al, 2006;Roupsard et al, 2006) ou um quadro matemático sofisticado (Moore & Fisch, de 1986;Meesters & Vugts , 1996).…”
Section: Introductionunclassified
“…Poucos são os estudos que tratam da estimativa de armazenamento de calor na biomassa (Moore & Fisch, 1986;McCaughey & Saxton, 1988;Meesters & Vugts, 1996;Michiles & Gielow, 2008). Isto porque a estimativa da energia estocada na biomassa se torna complexa devido à variação de temperatura no dossel e no caule, o que requer um grande número de sensores (McCaughey & Saxton, 1988;Oliphant et al, 2004;Barr et al, 2006;Roupsard et al, 2006) ou um quadro matemático sofisticado (Moore & Fisch, de 1986;Meesters & Vugts , 1996).…”
Section: Introductionunclassified
“…2.1, the maximum canopy heights at YK, AR and GT were 1.8 m, 0.2-0.3 m and 20 m, respectively; therefore, the canopy heat storage at the three sites cannot be neglected. According to the studies of Jacobs et al (2008) and Michiles and Gielow (2008), taking the canopy heat storage into consideration could improve the EBR by 0.5% and 5% in middle latitude grasslands and forests (average tree height 23.5 m), respectively. The energy balance ratio was within a range of 79% to 89% in this study; thus, it seems that there were other reasons for the imbalance.…”
Section: Energy Balance Closure Of Ecmentioning
confidence: 99%
“…The strong correlation of basal area with temperature and its related variables may be because leaf area scales closely with basal area (Enquist 2002); leaf area reduces the transmission of radiation to the forest interior (Asner 1998) whereas tree stems significantly absorb infrared radiation and redistribute heat under the forest canopy (Haverd et al 2007, Michiles & Gielow 2008. Fallow age predicted better than basal area the successional changes in RH, VPD and soil temperature, because it is a variable that integrates various ecosystem processes that affect the understorey environment (e.g.…”
Section: Understorey Environment and Forest Structurementioning
confidence: 99%