2003
DOI: 10.1016/s0304-3800(02)00387-3
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Testing a climato-topographic index for predicting wetlands distribution along an European climate gradient

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Cited by 97 publications
(74 citation statements)
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“…At such scales the contour interval is 5 m, and riparian areas with less than 5 m difference in elevation between the upland and riparian area cannot be delineated. Indices that combine surface topographical information with local climatic data, soil maps or groundwater table maps are often used to delineate riparian zones and wetlands (Beven and Kirkby, 1979;Merot et al, 2003;Rodhe and Seibert, 1999;Andersson and Nyberg, 2009). While these indices are generally suitable for areas with hilly topography and shallow soils overlying confined layers, they have shortcomings in more gently sloping terrain (Buttle et al, 2004;Buttle et al, 2001).…”
Section: Biogeochemistry In Riparian Zones and Delivery To Streamsmentioning
confidence: 99%
“…At such scales the contour interval is 5 m, and riparian areas with less than 5 m difference in elevation between the upland and riparian area cannot be delineated. Indices that combine surface topographical information with local climatic data, soil maps or groundwater table maps are often used to delineate riparian zones and wetlands (Beven and Kirkby, 1979;Merot et al, 2003;Rodhe and Seibert, 1999;Andersson and Nyberg, 2009). While these indices are generally suitable for areas with hilly topography and shallow soils overlying confined layers, they have shortcomings in more gently sloping terrain (Buttle et al, 2004;Buttle et al, 2001).…”
Section: Biogeochemistry In Riparian Zones and Delivery To Streamsmentioning
confidence: 99%
“…As a matter of fact, the local slope substitution with the downhill element led us to take into account both down-slope and up-slope. Moreover, it has been shown that CTI has the higher potential for determining the position and the general extent of wetlands in a reliable manner, even if it decreases when the soil has a highly heterogeneous permeability (Merot et al, 2003). In addition, maximum TI values extend over larger areas than the CTI, while the minimum values almost coincide.…”
Section: Discussionmentioning
confidence: 99%
“…Therefore, the TI was introduced (Beven et al, 1979;Beven, 1986) where Vr is the volume of effective annual rainfall, which is calculated by multiplying drainage area with the mean annual effective rainfall depth. Merot et al (2003) determinated the mean annual effective rainfall as:…”
Section: Suitable Indices To Predict Wetlands Distributionmentioning
confidence: 99%
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