Numerical modeling of the 2013 meteorite entry in Lake Chebarkul, Russia

The results of the numerical simulation of possible hydrodynamic perturbations in Lake Chebarkul (Russia) as a consequence of the meteorite fall of 2013 (15 February) are presented. The numerical modeling is based on the Navier–Stokes equations for a two-phase fluid. The results of the sim...

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Main Authors: A. Kozelkov, A. Kurkin, E. Pelinovsky, V. Kurulin, E. Tyatyushkina
Format: Article
Language:English
Published: Copernicus Publications 2017-05-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/17/671/2017/nhess-17-671-2017.pdf
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spelling doaj-969866879b4940f197c027ec615c3c622020-11-24T23:14:25ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812017-05-0117567168310.5194/nhess-17-671-2017Numerical modeling of the 2013 meteorite entry in Lake Chebarkul, RussiaA. Kozelkov0A. Kurkin1E. Pelinovsky2V. Kurulin3E. Tyatyushkina4Russian Federal Nuclear Center, All-Russian Research Institute of Experimental Physics, Sarov, 607189, RussiaNizhny Novgorod State Technical University n. a. R. E. Alekseev, Nizhny Novgorod, 603950, RussiaNizhny Novgorod State Technical University n. a. R. E. Alekseev, Nizhny Novgorod, 603950, RussiaRussian Federal Nuclear Center, All-Russian Research Institute of Experimental Physics, Sarov, 607189, RussiaRussian Federal Nuclear Center, All-Russian Research Institute of Experimental Physics, Sarov, 607189, RussiaThe results of the numerical simulation of possible hydrodynamic perturbations in Lake Chebarkul (Russia) as a consequence of the meteorite fall of 2013 (15 February) are presented. The numerical modeling is based on the Navier–Stokes equations for a two-phase fluid. The results of the simulation of a meteorite entering the water at an angle of 20° are given. Numerical experiments are carried out both when the lake is covered with ice and when it is not. The estimation of size of the destructed ice cover is made. It is shown that the size of the observed ice hole at the place of the meteorite fall is in good agreement with the theoretical predictions, as well as with other estimates. The heights of tsunami waves generated by a small meteorite entering the lake are small enough (a few centimeters) according to the estimations. However, the danger of a tsunami of meteorite or asteroid origin should not be underestimated.http://www.nat-hazards-earth-syst-sci.net/17/671/2017/nhess-17-671-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Kozelkov
A. Kurkin
E. Pelinovsky
V. Kurulin
E. Tyatyushkina
spellingShingle A. Kozelkov
A. Kurkin
E. Pelinovsky
V. Kurulin
E. Tyatyushkina
Numerical modeling of the 2013 meteorite entry in Lake Chebarkul, Russia
Natural Hazards and Earth System Sciences
author_facet A. Kozelkov
A. Kurkin
E. Pelinovsky
V. Kurulin
E. Tyatyushkina
author_sort A. Kozelkov
title Numerical modeling of the 2013 meteorite entry in Lake Chebarkul, Russia
title_short Numerical modeling of the 2013 meteorite entry in Lake Chebarkul, Russia
title_full Numerical modeling of the 2013 meteorite entry in Lake Chebarkul, Russia
title_fullStr Numerical modeling of the 2013 meteorite entry in Lake Chebarkul, Russia
title_full_unstemmed Numerical modeling of the 2013 meteorite entry in Lake Chebarkul, Russia
title_sort numerical modeling of the 2013 meteorite entry in lake chebarkul, russia
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2017-05-01
description The results of the numerical simulation of possible hydrodynamic perturbations in Lake Chebarkul (Russia) as a consequence of the meteorite fall of 2013 (15 February) are presented. The numerical modeling is based on the Navier–Stokes equations for a two-phase fluid. The results of the simulation of a meteorite entering the water at an angle of 20° are given. Numerical experiments are carried out both when the lake is covered with ice and when it is not. The estimation of size of the destructed ice cover is made. It is shown that the size of the observed ice hole at the place of the meteorite fall is in good agreement with the theoretical predictions, as well as with other estimates. The heights of tsunami waves generated by a small meteorite entering the lake are small enough (a few centimeters) according to the estimations. However, the danger of a tsunami of meteorite or asteroid origin should not be underestimated.
url http://www.nat-hazards-earth-syst-sci.net/17/671/2017/nhess-17-671-2017.pdf
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