论文标题

Pynaple:月球表面冲击火山口检测

PyNAPLE: Lunar Surface Impact Crater Detection

论文作者

Sheward, Daniel, Avdellidou, Chrysa, Cook, Anthony, Sefton-Nash, Elliot, Delbo, Marco, Cantarella, Bruno, Zanatta, Luigi

论文摘要

在过去的20年中,在月球表面已记录了600多个撞击闪光。这些丰富的数据为研究地球环境的流星通量以及近年来影响器的物理特性提供了一个独特的机会。但是,除了通过偶然性事件外,还没有系统的搜索和发现与这些事件相关的陨石坑。这样的流星界链接将使我们能够通过对碰撞的这些实时观察来深入了解火山口的形成。在这里,我们介绍了Pynaple(Python NAC自动化对Lunar评估器)软件管道,用于使用观察到的撞击闪光灯的位置和时期定位新形成的陨石坑。我们提出了Pynaple的第一个结果,该结果已在2017-09-27 Impact Flash上​​实施。 A rudimentary analysis on the impact flash and linked impact crater is also performed, finding that the crater's ejecta pattern indicates an impact angle between 10-30 degree, and although the rim-to-rim diameter of the crater is not resolvable in current LRO NAC images, using crater scaling laws we predict this diameter to be 24.1-55.3 m, and using ejecta scaling predict a diameter of 27.3-37.7 m.我们讨论了Pynaple如何实现对次级尺度围墙率和缩放定律的完善和发光效率的大规模分析。

In the last 20 years, over 600 impact flashes have been documented on the lunar surface. This wealth of data presents a unique opportunity to study the meteoroid flux of the Earth-Moon environment, and in recent years the physical properties of the impactors. However, other than through serendipitous events, there has not been yet a systematic search and discovery of the craters associated to these events. Such a meteoroid-crater link would allow us to get insight into the crater formation via these live observations of collisions. Here we present the PyNAPLE (Python NAC Automated Pair Lunar Evaluator) software pipeline for locating newly formed craters using the location and epoch of an observed impact flash. We present the first results from PyNAPLE, having been implemented on the 2017-09-27 impact flash. A rudimentary analysis on the impact flash and linked impact crater is also performed, finding that the crater's ejecta pattern indicates an impact angle between 10-30 degree, and although the rim-to-rim diameter of the crater is not resolvable in current LRO NAC images, using crater scaling laws we predict this diameter to be 24.1-55.3 m, and using ejecta scaling predict a diameter of 27.3-37.7 m. We discuss how PyNAPLE will enable large scale analyses of sub-kilometer scale cratering rates and refinement of both scaling laws, and the luminous efficiency.

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