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Canopy structure in savannas along a moisture gradient on Kalahari sands

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dc.contributor.author Scholes, RJ en_US
dc.contributor.author Frost, PGH en_US
dc.contributor.author Tian, Y en_US
dc.date.accessioned 2007-03-26T07:14:57Z en_US
dc.date.accessioned 2007-06-07T10:02:11Z
dc.date.available 2007-03-26T07:14:57Z en_US
dc.date.available 2007-06-07T10:02:11Z
dc.date.issued 2004-03 en_US
dc.identifier.citation Scholes, RJ, Frost, PGH and Tian, Y. 2004. Canopy structure in savannas along a moisture gradient on Kalahari sands. Global Change Biology, vol. 10(3), pp 292-302 en_US
dc.identifier.issn 1354-1013 en_US
dc.identifier.uri http://hdl.handle.net/10204/2028 en_US
dc.identifier.uri http://hdl.handle.net/10204/2028
dc.description.abstract Measurements of tree canopy architecture were made at six savanna sites on deep, sandy soils, along a gradient of increasing aridity. There was substantial variation in the leaf area estimated within each site, using the same sample frame, but different measurement techniques. The trends in canopy properties in relation to the aridity gradient were consistent, regardless of the technique used for estimating the properties. The effective plant area index for the tree canopy (the sum of the stem area index and the leaf area index (LAI)) declined from around 2 to around 0.8 m(2) m(-2) over a gradient of mean annual rainfall from 1000 to 350 mm. Stems contributed 2-5% of the tree canopy plant area index. Since the tree canopy cover decreased from 50% to 20% over this aridity range, the leaf area index within the area covered by tree canopies remained fairly constant at 3-4 m(2) m(-2). Tree leaves tended from a horizontal orientation to a more random orientation as the aridity increased. On the same gradient, the leaf minor axis dimension decreased from around 30 mm to around 3 mm, and the mean specific leaf area decreased from 14 to 5 m(2) kg ha(-1). There was good agreement between LAI observed in the field using a line ceptometer and the LAI inferred by the MODIS sensor on the Terra satellite platform, 2 months later in the same season. en_US
dc.format.extent 150906 bytes en_US
dc.format.mimetype application/pdf en_US
dc.language.iso en en_US
dc.publisher Blackwell Publishing Ltd en_US
dc.rights Copyright: 2004 Blackwell Publishing Ltd en_US
dc.subject Canopy architecture en_US
dc.subject Leaf area index en_US
dc.subject Plant canopy en_US
dc.subject MODIS en_US
dc.subject Biodiversity conservation en_US
dc.subject Ecology en_US
dc.subject Environmental sciences en_US
dc.title Canopy structure in savannas along a moisture gradient on Kalahari sands en_US
dc.type Article en_US
dc.identifier.apacitation Scholes, R., Frost, P., & Tian, Y. (2004). Canopy structure in savannas along a moisture gradient on Kalahari sands. http://hdl.handle.net/10204/2028 en_ZA
dc.identifier.chicagocitation Scholes, RJ, PGH Frost, and Y Tian "Canopy structure in savannas along a moisture gradient on Kalahari sands." (2004) http://hdl.handle.net/10204/2028 en_ZA
dc.identifier.vancouvercitation Scholes R, Frost P, Tian Y. Canopy structure in savannas along a moisture gradient on Kalahari sands. 2004; http://hdl.handle.net/10204/2028. en_ZA
dc.identifier.ris TY - Article AU - Scholes, RJ AU - Frost, PGH AU - Tian, Y AB - Measurements of tree canopy architecture were made at six savanna sites on deep, sandy soils, along a gradient of increasing aridity. There was substantial variation in the leaf area estimated within each site, using the same sample frame, but different measurement techniques. The trends in canopy properties in relation to the aridity gradient were consistent, regardless of the technique used for estimating the properties. The effective plant area index for the tree canopy (the sum of the stem area index and the leaf area index (LAI)) declined from around 2 to around 0.8 m(2) m(-2) over a gradient of mean annual rainfall from 1000 to 350 mm. Stems contributed 2-5% of the tree canopy plant area index. Since the tree canopy cover decreased from 50% to 20% over this aridity range, the leaf area index within the area covered by tree canopies remained fairly constant at 3-4 m(2) m(-2). Tree leaves tended from a horizontal orientation to a more random orientation as the aridity increased. On the same gradient, the leaf minor axis dimension decreased from around 30 mm to around 3 mm, and the mean specific leaf area decreased from 14 to 5 m(2) kg ha(-1). There was good agreement between LAI observed in the field using a line ceptometer and the LAI inferred by the MODIS sensor on the Terra satellite platform, 2 months later in the same season. DA - 2004-03 DB - ResearchSpace DP - CSIR KW - Canopy architecture KW - Leaf area index KW - Plant canopy KW - MODIS KW - Biodiversity conservation KW - Ecology KW - Environmental sciences LK - https://researchspace.csir.co.za PY - 2004 SM - 1354-1013 T1 - Canopy structure in savannas along a moisture gradient on Kalahari sands TI - Canopy structure in savannas along a moisture gradient on Kalahari sands UR - http://hdl.handle.net/10204/2028 ER - en_ZA


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