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Semi-automatic classification of glaciovolcanic landforms: An object-based mapping approach based on geomorphometry

机译:冰川火山地貌的半自动分类:基于地貌的基于对象的映射方法

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摘要

A new object-oriented approach is developed to classify glaciovolcanic landforms (Procedure A) and their landform elements boundaries (Procedure B). It utilizes the principle that glaciovolcanic edifices are geomorphometrically distinct from lava shields and plains (Pedersen and Grosse, 2014), and the approach is tested on data from Reykjanes Peninsula, Iceland. The outlined procedures utilize slope and profile curvature attribute maps (20 m/pixel) and the classified results are evaluated quantitatively through error matrix maps (Procedure A) and visual inspection (Procedure B). In procedure A, the highest obtained accuracy is 94.1%, but even simple mapping procedures provide good results (>90% accuracy). Successful classification of glaciovolcanic landform element boundaries (Procedure B) is also achieved and this technique has the potential to delineate the transition from intraglacial to subaerial volcanic activity in orthographic view.
机译:开发了一种新的面向对象的方法来对冰川火山地貌(程序A)及其地貌元素边界(程序B)进行分类。它利用冰川融化的建筑物在地貌学上与熔岩盾构和平原不同的原理(Pedersen和Grosse,2014年),并对冰岛雷克雅尼斯半岛的数据进行了测试。概述的过程利用坡度和轮廓曲率属性图(20 m /像素),通过误差矩阵图(过程A)和目视检查(过程B)对分类结果进行定量评估。在过程A中,获得的最高准确度为94.1%,但即使是简单的映射过程也可以提供良好的结果(准确度> 90%)。还成功完成了冰川火山地貌要素边界的分类(程序B),该技术具有在正射影像学中描绘从冰川内火山活动到地下火山活动的过渡的潜力。

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