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A review of marine geomorphometry, the quantitative study of the seafloor

机译:海洋地貌学综述,海底定量研究

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Geomorphometry, the science of quantitative terrain characterization, has traditionally focused on the investigation of terrestrial landscapes. However, the dramatic increase in the availability of digital bathymetric data and the increasing ease by which geomorphometry can be investigated using geographic information systems?(GISs) and spatial analysis software has prompted interest in employing geomorphometric techniques to investigate the marine environment. Over the last decade or so, a multitude of geomorphometric techniques (e.g. terrain attributes, feature extraction, automated classification) have been applied to characterize seabed terrain from the coastal zone to the deep sea. Geomorphometric techniques are, however, not as varied, nor as extensively applied, in marine as they are in terrestrial environments. This is at least partly due to difficulties associated with capturing, classifying, and validating terrain characteristics underwater. There is, nevertheless, much common ground between terrestrial and marine geomorphometry applications and it is important that, in developing marine geomorphometry, we learn from experiences in terrestrial studies. However, not all terrestrial solutions can be adopted by marine geomorphometric studies since the dynamic, four-dimensional (4-D) nature of the marine environment causes its own issues throughout the geomorphometry workflow. For instance, issues with underwater positioning, variations in sound velocity in the water column affecting acoustic-based mapping, and our inability to directly observe and measure depth and morphological features on the seafloor are all issues specific to the application of geomorphometry in the marine environment. Such issues fuel the need for a dedicated scientific effort in marine geomorphometry./br/brThis review aims to highlight the relatively recent growth of marine geomorphometry as a distinct discipline, and offers the first comprehensive overview of marine geomorphometry to date. We address all the five main steps of geomorphometry, from data collection to the application of terrain attributes and features. We focus on how these steps are relevant to marine geomorphometry and also highlight differences and similarities from terrestrial geomorphometry. We conclude with recommendations and reflections on the future of marine geomorphometry. To ensure that geomorphometry is used and developed to its full potential, there is a need to increase awareness of (1)?marine geomorphometry amongst scientists already engaged in terrestrial geomorphometry, and of (2)?geomorphometry as a science amongst marine scientists with a wide range of backgrounds and experiences.
机译:地貌计量学是定量地形特征描述的科学,传统上一直专注于地面景观的研究。但是,数字测深数据的可利用性的急剧增加以及使用地理信息系统(GIS)和空间分析软件进行地貌测量的简便性日益提高,引起了人们对使用地貌测量技术研究海洋环境的兴趣。在过去十年左右的时间里,已经应用了多种地貌技术(例如地形属性,特征提取,自动分类)来表征从沿海地区到深海的海床地形。然而,地貌测量技术在海洋中没有像在陆地环境中那样变化多样,也没有广泛应用。这至少部分是由于与捕获,分类和验证水下地形特征相关的困难。但是,在地面和海洋地貌测量应用之间有很多共同点,重要的是,在发展海洋地貌测量时,我们必须从地面研究中学习。但是,并不是所有的地面解决方案都可以被海洋地形测量研究采用,因为海洋环境的动态四维(4-D)性质会在整个地形测量工作流程中引起其自身的问题。例如,水下定位的问题,水柱中声速的变化会影响基于声波的制图,以及我们无法直接观察和测量海底的深度和形态特征,这些都是地貌学在海洋环境中的应用所特有的问题。 。这些问题激发了对海洋地貌学进行专门科学努力的需要。 这篇综述旨在强调海洋地貌学作为一门独立学科的相对较新的发展,并提供了迄今为止有关海洋地貌学的第一份全面概述。 。我们讨论了地貌测量的所有五个主要步骤,从数据收集到地形属性和特征的应用。我们将重点放在这些步骤与海洋地貌学如何相关的问题上,并着重说明与陆地地貌学的区别和相似之处。最后,我们对海洋地貌学的未来提出了一些建议和思考。为了确保充分利用地貌学并发展其潜力,有必要提高对(1)已经从事陆地地貌学的科学家的海洋地貌学和(2)地貌学作为海洋科学家的认识。广泛的背景和经验。

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