Hypsometric Analysis of Headwater Rock Basins in the Dolomites (Eastern Alps) Using High‐Resolution Topography. Issue 2 (29th September 2014)

• Record Type: Journal Article
• Authors: Marchi, Lorenzo; Cavalli, Marco; Trevisani, Sebastiano
• Is Part Of: Geografiska annaler. Volume 97:Issue 2(2015)
• Page Start: 317
• Page End: 335
• Publication Date: 2014-09-29
• Subjects: Physical geography -- Periodicals; 551.4
• DOI: 10.1111/geoa.12067
• Languages: English
• ISSNs: 0435-3676

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>Hypsometric curves and integrals are effective tools for rapid quantitative assessments of topography. High‐resolution digital terrain models derived from airborne LiDAR data have been analysed to study the hypsometry of small headwater rock basins (drainage areas up to 0.13 km<sup>2</sup>) in three study areas in the Dolomites (Eastern Alps) that have similar lithologies and climatic conditions. Hypsometric curves in the studied rocky headwaters display a variety of shapes and present remarkable differences between neighbouring basins. Hypsometric integrals show generally high values in the three study areas (>0.42, mean values between 0.51 and 0.65). The extent of the scree slopes located at the foot of rock basins in the three study areas is larger in the area with lower hypsometric integrals and indicates consistency between the development of basin erosion, which is shown by the hypsometric integral, and debris yield, represented by the extent of scree slope. No clear relations were observed between the hypsometric integrals and basin area and shape. When extending the analysis to larger basins, which encompass rocky headwaters and downslope soil‐mantled slopes, a negative correlation is found between the hypsometric integral and catchment area, suggesting that the scale independency of the hypsometric integral occurs essentially in headwater rock basins. Geomorphometric indices (residual relief and surface roughness) have contributed to interpreting the variability of surface morphology, which is related to the geo‐structural complexity of the catchments.</p> </abstract>