Multibeam Bathymetry of the Håkon Mosby Mud Volcano
Multibeam Bathymetry of the Håkon Mosby Mud Volcano
复制标题
哈康莫斯比泥火山的多波束测深
DOI：
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发表时间：
2005
期刊：
影响因子：
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通讯作者：
H. Schenke
中科院分区：
文献类型：
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作者：
A. Beyer;Rike Rathlau;H. Schenke
哈孔莫斯比泥火山是一个天然实验室，研究与深水泥火山活动有关的地质、地球化学和生态过程。在北极星号考察船方舟XIX/3号考察期间，利用多波束系统Hydrosweep DS-2记录了Håkon Mosby泥火山的高分辨率水深测量。测量线的密集间距和缓慢的船速（5节）提供了必要的点密度，以生成规则的10米网格。泛化应用于适当地保存和表示形态结构。绘制的等高线显示了Håkon Mosby泥火山中心的详细地形和附近的一般等高线。本文简要介绍了哈康莫斯比泥火山地区，详细描述了数据记录和处理方法，以及该地区的地貌。精度评估是为了评估10米分辨率地形模型的可靠性。多波束侧扫数据与深度测量一起沿着记录，并显示从Håkon Mosby泥火山中心的浅灰色值到周围护城河的深灰色值（反射性较低）的反射率变化。
The Håkon Mosby Mud Volcano is a natural laboratory to study geological, geochemical, and ecological processes related to deep-water mud volcanism. High resolution bathymetry of the Håkon Mosby Mud Volcano was recorded during RV Polarstern expedition ARK XIX/3 utilizing the multibeam system Hydrosweep DS-2. Dense spacing of the survey lines and slow ship speed (5 knots) provided necessary point density to generate a regular 10 m grid. Generalization was applied to preserve and represent morphological structures appropriately. Contour lines were derived showing detailed topography at the centre of the Håkon Mosby Mud Volcano and generalized contours in the vicinity. We provide a brief introduction to the Håkon Mosby Mud Volcano area and describe in detail data recording and processing methods, as well as the morphology of the area. Accuracy assessment was made to evaluate the reliability of a 10 m resolution terrain model. Multibeam sidescan data were recorded along with depth measurements and show reflectivity variations from light grey values at the centre of the Håkon Mosby Mud Volcano to dark grey values (less reflective) at the surrounding moat.