Profile Integral, a robust and unified metric for measuring profile concavity

Abstract— To measure the shape of topographic profiles in two dimensions (height v. distance), we propose a new metric (and develop its related toolbox) based on integrating the area under the profile. It is applicable to any cross-valley profile, slope profile, long profile or arbitrary profile. By analogy with the Hypsometric Integral, we term the metric the Profile Integral. It is a normalized value between 0 and 1 with the value of 0.5 representing either a straight-line long profile or a V-shaped cross-profile and values of > 0.5 for convex profiles and <0.5 for concave profiles. Correlations with the V-index, the VWDR, the K-curve, the power curve and the quadratic polynomial are analyzed. The advantages of the Profile Integral are (1) its flexibility in providing a metric with similar interpretations for long profiles, slope profiles and valley cross-profiles and (2) its applicability to asymmetric cross-profiles in full, including those close to the confluence of tributary valleys (asymmetric cross-profiles, reaching different heights on each side, are common yet are excluded from most analyses of valleys and troughs). Our toolbox generates smoothed streamlines (thalwegs) to provide starting points for a series of cross-profiles. Applications to glaciated valleys in the Tian Shan (Daxi) and northern Iceland (Eyjafjarđardalur) are illustrated.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-03-29
DOI
https://doi.org/10.5281/zenodo.15106524
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
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article

Profile Integral, a robust and unified metric for measuring profile concavity

Zenodo (CERN European Organization for Nuclear Research)
Cryospheric studies and observations
article

Profile Integral, a robust and unified metric for measuring profile concavity

article en

Abstract

Abstract— To measure the shape of topographic profiles in two dimensions (height v. distance), we propose a new metric (and develop its related toolbox) based on integrating the area under the profile. It is applicable to any cross-valley profile, slope profile, long profile or arbitrary profile. By analogy with the Hypsometric Integral, we term the metric the Profile Integral. It is a normalized value between 0 and 1 with the value of 0.5 representing either a straight-line long profile or a V-shaped cross-profile and values of > 0.5 for convex profiles and <0.5 for concave profiles. Correlations with the V-index, the VWDR, the K-curve, the power curve and the quadratic polynomial are analyzed. The advantages of the Profile Integral are (1) its flexibility in providing a metric with similar interpretations for long profiles, slope profiles and valley cross-profiles and (2) its applicability to asymmetric cross-profiles in full, including those close to the confluence of tributary valleys (asymmetric cross-profiles, reaching different heights on each side, are common yet are excluded from most analyses of valleys and troughs). Our toolbox generates smoothed streamlines (thalwegs) to provide starting points for a series of cross-profiles. Applications to glaciated valleys in the Tian Shan (Daxi) and northern Iceland (Eyjafjarđardalur) are illustrated.

Zenodo (CERN European Organization for Nuclear Research)
Durham University (GB), Purdue University West Lafayette (US), University of Tennessee at Knoxville (US)
Sustainable cities and communities
Openalex Percentile: Top 54%
Cryospheric studies and observations
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