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2016
DOI: 10.5963/jwrhe0501002
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Climate Change Impacts on Hydrological Niches of Restionaceae Species in Jonkershoek, South Africa

Abstract: Abstract-The Restionaceae species of the Fynbos biome is part of the Cape Floristic Kingdom is threatened by urbanization, agricultural expansion, groundwater extraction, and climate change. Therefore, it is necessary to assess and monitor the Restionaceae species under the impact of climate change. South Africa is a semi-arid environment, and hydrological factors are the main variables in the determination of species niches. This study investigates the microclimate at Jonkershoek, and examines the impact of c… Show more

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Cited by 4 publications
(4 citation statements)
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References 14 publications
(24 reference statements)
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“…The future climate variables of fog and relative humidity have been used in the spatial modelling process [15,18] to project the suitable bioclimatic envelope for both Conophytum and Lithops in the present and in the future. In addition, geology, altitude, morphology and soil type were used as environmental constraints.…”
Section: Projected Future Changes and Discussionmentioning
confidence: 99%
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“…The future climate variables of fog and relative humidity have been used in the spatial modelling process [15,18] to project the suitable bioclimatic envelope for both Conophytum and Lithops in the present and in the future. In addition, geology, altitude, morphology and soil type were used as environmental constraints.…”
Section: Projected Future Changes and Discussionmentioning
confidence: 99%
“…with λi = ( λ1, λ2,..., λm) as the weight vector, λi being the weight parameters, fi(x) representing species i's probability distribution, L being the m-dimensional space, each element x is a pixel of the investigated area, and Zλ(x) being the normalized constant, and the probabilities fi(x) represent the relative suitability of the environmental variable in each pixel [13,[15][16][17].…”
Section: Climate Data and Methodologymentioning
confidence: 99%
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“…Precipitation (P) is the primary source of the soil moisture. As such a future climate signal was mathematically calculated from the current and future P following [38]. This procedure obtained the ratio between the current and future annual average P and multiplying it by the observed mean water table depth (MWTD) to obtain an estimate of the future climate signal (i.e.…”
Section: Environmental Variablesmentioning
confidence: 99%