Abstract:The present work describes the development of two collaborative Autonomous Underwater Vehicles (AUV) for Antarctic exploration to use them in the Ecuadorian Expeditions to the Scientific Base Pedro Vicente Maldonado in Antarctica. One vehicle is an AUV, called TAUV, with classical torpedo architecture, can work as a platform to transport scientific payload in a determined path in open waters. The TAUV length is 2m and diameter of 0.16m and has got three degree of freedom: pitch, yaw and surge. The vehicle achi… Show more
“…Although AUV platforms have been used to map under the sea ice in limited studies [1,6] this research demonstrated the ability to conduct concise transects covering 12.42 hectares at very high spatial resolution (5 cm) and high degrees of precision (0.01 m drift) of this cryptic marine environment. Aside from mapping sea ice thickness we have uniquely resolved smooth ice from platelet ice at 5 cm resolution.…”
Section: Discussionmentioning
confidence: 99%
“…Autonomous underwater vehicles (AUVs) have been used in the Arctic since the 1970s, and increasingly in the Antarctic in recent years, to acoustically survey the geometric properties of the underside surface of sea ice [1][2][3][4][5]. There are various motivations that have initiated this research, including mapping sea ice thickness [6]; describing the roughness characteristics of the ice to determine wind and water drag coefficients for dynamical modeling [7]; and monitoring the transition of multiyear sea ice to first year sea ice [8].…”
Antarctic sea ice is known to provide unique ecosystem habitat at the ice-ocean interface. Mapping sea ice characteristics-such as thickness and roughness-at high resolution from beneath the ice is difficult due to access. A Geoswath Plus phase-measuring bathymetric sonar mounted on an autonomous underwater vehicle (AUV) was employed in this study to collect data underneath the sea ice at Cape Evans in Antarctica in November 2014. This study demonstrates how acoustic data can be collected and processed to resolutions of 1 m for acoustic bathymetry and 5 cm for acoustic backscatter in this challenging environment. Different ice textures such as platelet ice, smooth ice, and sea ice morphologies, ranging in size from 1 to 50 m were characterized. The acoustic techniques developed in this work could provide a key to understanding the distribution of sea ice communities, as they are nondisruptive to the fragile ice environments and provide geolocated data over large spatial extents. These results improve our understanding of sea ice properties and the complex, highly variable ecosystem that exists at this boundary.
“…Although AUV platforms have been used to map under the sea ice in limited studies [1,6] this research demonstrated the ability to conduct concise transects covering 12.42 hectares at very high spatial resolution (5 cm) and high degrees of precision (0.01 m drift) of this cryptic marine environment. Aside from mapping sea ice thickness we have uniquely resolved smooth ice from platelet ice at 5 cm resolution.…”
Section: Discussionmentioning
confidence: 99%
“…Autonomous underwater vehicles (AUVs) have been used in the Arctic since the 1970s, and increasingly in the Antarctic in recent years, to acoustically survey the geometric properties of the underside surface of sea ice [1][2][3][4][5]. There are various motivations that have initiated this research, including mapping sea ice thickness [6]; describing the roughness characteristics of the ice to determine wind and water drag coefficients for dynamical modeling [7]; and monitoring the transition of multiyear sea ice to first year sea ice [8].…”
Antarctic sea ice is known to provide unique ecosystem habitat at the ice-ocean interface. Mapping sea ice characteristics-such as thickness and roughness-at high resolution from beneath the ice is difficult due to access. A Geoswath Plus phase-measuring bathymetric sonar mounted on an autonomous underwater vehicle (AUV) was employed in this study to collect data underneath the sea ice at Cape Evans in Antarctica in November 2014. This study demonstrates how acoustic data can be collected and processed to resolutions of 1 m for acoustic bathymetry and 5 cm for acoustic backscatter in this challenging environment. Different ice textures such as platelet ice, smooth ice, and sea ice morphologies, ranging in size from 1 to 50 m were characterized. The acoustic techniques developed in this work could provide a key to understanding the distribution of sea ice communities, as they are nondisruptive to the fragile ice environments and provide geolocated data over large spatial extents. These results improve our understanding of sea ice properties and the complex, highly variable ecosystem that exists at this boundary.
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