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Automated iceberg tracking with a machine learning approach applied to SAR imagery: A Weddell sea case study

机译:自动化冰山跟踪采用机器学习方法应用于SAR Imagerery:Weddell Sea案例研究

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Drifting icebergs represent a significant hazard for polar navigation and are able to impact the ocean environment around them. Freshwater flux and the associated cooling from melting icebergs can locally decrease salinity and temperature and thus affect ocean circulation, biological activity, sea ice, and -on larger spatial scales- the whole climate system. However, despite their potential impact, the large-scale operational monitoring of drifting icebergs in sea ice-covered regions is as of today typically restricted to giant icebergs, larger than 18.5 km in length. This is due to difficulties in accurately identifying and following the motion of much smaller features in the polar ocean from space. So far, tracking of smaller icebergs from satellite imagery thus has been limited to open-ocean regions not covered by sea ice. In this study, a novel automated iceberg tracking method, based on a machine learning-approach for automatic iceberg detection, is presented. To demonstrate the applicability of the method, a case study was performed for the Weddell Sea region, Antarctica, using 1213 Advanced Synthetic Aperture Radar (ASAR) satellite images acquired between 2002 and 2011. Overall, a subset of 414 icebergs (3134 re-detections in total) with surface areas between 3.4 km(2) and 3612 km(2) were investigated with respect to their prevalent drift patterns, size variability, and average disintegration. The majority of the tracked icebergs drifted between 1.3 km and 2679.2 km westward around the Antarctic continent, following the Antarctic Coastal Current (ACoC) and the Weddell Gyre, at an average drift speed of 3.6 +/- 7.4 km day(-1). The method also allowed us to estimate an average daily disintegration (i.e. iceberg area decrease) rate of similar to 0.13% (similar to 37% year(-1)) for all icebergs. Using the sum of all detected individual surface area reductions, we estimate a total iceberg mass decrease of similar to 683 Gt year(-1) which can be freshwater input and/or new 'child' icebergs calved from larger icebergs. The extension to an automated long-term tracking method for icebergs is challenging as the iceberg shape can vary significantly due to abrupt disintegration or calving of bergy bits. However, our machine learning approach extended by automatic shape-based tracking capabilities proved to be a reliable alternative for automatic detection and tracking of icebergs, even under the ambiguous SAR background signatures often found in the Southern Ocean. In particular, the method works in the challenging near-coastal environment where the presence of sea ice and coastal ocean dynamics such as surface waves usually pose major obstacles for other approaches.
机译:漂流冰山代表极性导航的重大危害,能够影响它们周围的海洋环境。淡水通量和熔化冰山的相关冷却可以局部降低盐度和温度,从而影响海洋循环,生物活性,海冰,以及更大的空间尺度 - 整个气候系统。然而,尽管存在潜在的影响,但海洋覆盖地区漂流冰山的大规模操作监测截至今天通常仅限于巨型冰山,长度大于18.5公里。这是由于难以准确地识别和遵循极地海洋中的小得多的运动。到目前为止,从卫星图像跟踪较小的冰山,因此仅限于海冰未被海冰覆盖的开放海洋区域。在本研究中,提出了一种基于机器学习方法的新型自动化冰山跟踪方法,用于自动冰山检测。为了证明该方法的适用性,使用2002和2011年之间获得的1213高级合成孔径雷达(ASAR)卫星图像对南极洲,南极地区进行案例研究。总之,414冰山的子集(3134重新检测总共有3.4 km(2)和3612km(2)之间的表面积,相对于其普遍的漂移模式,尺寸可变性和平均崩解。在南极沿海电流(ACOC)和Weddell Gyre之后,南极大陆周围的大多数追踪冰山沿着1.3公里和2679.2 km。平均漂移速度为3.6 +/- 7.4公里(-1)。该方法还允许我们估计所有冰山的平均每日崩解(即冰山区域降低)率类似于0.13%(类似于37%(-1))。使用所有检测到的单独面积减少的总和,我们估计了与683 GT年(-1)相似的总冰山大量减少,这可以是从较大的冰山中计算的淡水输入和/或新的“儿童”冰山。对于冰山的自动化长期跟踪方法的扩展是具有挑战性,因为冰山形状由于突然分解或溃疡位的突然分解而变化。然而,我们的机器学习方法通​​过基于自动形状的跟踪能力而被证明是一种可靠的替代品,用于自动检测和跟踪冰山,即使在南洋常常发现的模糊的SAR背景签名。特别是,该方法在挑战的近沿海环境中工作,其中海冰和沿海海洋动力学等地表波的存在通常为其他方法构成主要障碍。

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