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Global estimates of glacier equilibrium-line altitude ratios for enhanced paleoclimate reconstructions
Abstract Glacial landforms record valuable information about past climates, but quantitative reconstructions depend on robust estimates of glacier characteristics, particularly the equilibrium-line altitude. Traditional approaches rely on global mean or median values of equilibrium-line altitude ratios (Accumulation Area Ratio, Toe-to-Headwall Altitude Ratio, and Area-Altitude Balance Ratio) to calculate equilibrium-line altitude.
Glacier mass loss on the southeastern Tibetan Plateau since the Little Ice Age
Supporting Information Filename Description jqs3715-sup-0001-Supplementary_S1.docx505.2 KB Figure S1. Dating results were analyzed using the P-CAAT. Table S1. Recalculated10Be exposure ages for the SETP and its surrounding regions. Table S2. Compilation of glacial ages over the past millennium in the SETP and its surrounding regions. References , , , , , et al. (2015) Clouds, circulation and climate sensitivity. Nature Geoscience, 8, 261–268.
An AI-Based Workflow for Fast Registration of UAV-Produced 3D Point Clouds
5. Discussion The average spacing of the point clouds from our test area is about 1.2 to 1.4 cm, indicating that any detailed horizontal changes less than this average spacing are likely not to be detected. However, it is hard to evaluate the accuracy of the changes in elevation.
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