Electric field and infrared radiation in the troposphere before earthquakes
Some years ago, a model of the generation of local electric fields in the atmosphere a few days before earthquakes and up to a few days after the seismic shock was proposed. In the model, the generation of the electric fields occurs because of an increased ionisation intensity of the atmosphere in t...
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00026486 2023-05-15T16:59:22+02:00 Electric field and infrared radiation in the troposphere before earthquakes Liperovsky, V. A. Meister, C.-V. Mikhailin, V. V. Bogdanov, V. V. Umarkhodgaev, P. M. Liperovskaya, E. V. 2011-12 electronic https://doi.org/10.5194/nhess-11-3125-2011 https://noa.gwlb.de/receive/cop_mods_00026486 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00026441/nhess-11-3125-2011.pdf https://nhess.copernicus.org/articles/11/3125/2011/nhess-11-3125-2011.pdf eng eng Copernicus Publications Natural Hazards and Earth System Sciences -- http://www.bibliothek.uni-regensburg.de/ezeit/?2064587 -- http://www.nat-hazards-earth-syst-sci.net/ -- 1684-9981 https://doi.org/10.5194/nhess-11-3125-2011 https://noa.gwlb.de/receive/cop_mods_00026486 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00026441/nhess-11-3125-2011.pdf https://nhess.copernicus.org/articles/11/3125/2011/nhess-11-3125-2011.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2011 ftnonlinearchiv https://doi.org/10.5194/nhess-11-3125-2011 2022-02-08T22:49:13Z Some years ago, a model of the generation of local electric fields in the atmosphere a few days before earthquakes and up to a few days after the seismic shock was proposed. In the model, the generation of the electric fields occurs because of an increased ionisation intensity of the atmosphere in the presence of aerosols. The generation of the electric field is the result of the fact that the larger aerosols, which are mainly negatively charged, have a larger velocity of gravitational precipitation than the smaller, which are mainly positively charged aerosols. The ionisation in such atmospheric regions is caused by radon, the concentration of which increases in earthquake preparation regions. The formation of mosaic-likely distributed areas of electric fields with intensities of 3 × 102 – 105 Vm−1 and, on the other hand, large areas with increased electrical conductivity cause a series of physical effects, e.g. the occurrence of infrared emissions with a specific spectrum, which may be studied using earth-based, atmospheric and satellite observations. In the present paper, the model of the generation of local electric fields is further developed, improving the description of the force balance on the aerosols in the atmosphere. A recently proposed laboratory experiment is briefly discussed, which is carried out to prove the theoretically predicted intensification of infrared emissions some hours-days before earthquakes. Besides the experiment described, it will be operated on Kamchatka in the near future to scan mosaic-likely distributed regions of electric fields in the atmosphere during earthquake preparation times. Article in Journal/Newspaper Kamchatka Niedersächsisches Online-Archiv NOA Natural Hazards and Earth System Sciences 11 12 3125 3133 |
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article Verlagsveröffentlichung Liperovsky, V. A. Meister, C.-V. Mikhailin, V. V. Bogdanov, V. V. Umarkhodgaev, P. M. Liperovskaya, E. V. Electric field and infrared radiation in the troposphere before earthquakes |
topic_facet |
article Verlagsveröffentlichung |
description |
Some years ago, a model of the generation of local electric fields in the atmosphere a few days before earthquakes and up to a few days after the seismic shock was proposed. In the model, the generation of the electric fields occurs because of an increased ionisation intensity of the atmosphere in the presence of aerosols. The generation of the electric field is the result of the fact that the larger aerosols, which are mainly negatively charged, have a larger velocity of gravitational precipitation than the smaller, which are mainly positively charged aerosols. The ionisation in such atmospheric regions is caused by radon, the concentration of which increases in earthquake preparation regions. The formation of mosaic-likely distributed areas of electric fields with intensities of 3 × 102 – 105 Vm−1 and, on the other hand, large areas with increased electrical conductivity cause a series of physical effects, e.g. the occurrence of infrared emissions with a specific spectrum, which may be studied using earth-based, atmospheric and satellite observations. In the present paper, the model of the generation of local electric fields is further developed, improving the description of the force balance on the aerosols in the atmosphere. A recently proposed laboratory experiment is briefly discussed, which is carried out to prove the theoretically predicted intensification of infrared emissions some hours-days before earthquakes. Besides the experiment described, it will be operated on Kamchatka in the near future to scan mosaic-likely distributed regions of electric fields in the atmosphere during earthquake preparation times. |
format |
Article in Journal/Newspaper |
author |
Liperovsky, V. A. Meister, C.-V. Mikhailin, V. V. Bogdanov, V. V. Umarkhodgaev, P. M. Liperovskaya, E. V. |
author_facet |
Liperovsky, V. A. Meister, C.-V. Mikhailin, V. V. Bogdanov, V. V. Umarkhodgaev, P. M. Liperovskaya, E. V. |
author_sort |
Liperovsky, V. A. |
title |
Electric field and infrared radiation in the troposphere before earthquakes |
title_short |
Electric field and infrared radiation in the troposphere before earthquakes |
title_full |
Electric field and infrared radiation in the troposphere before earthquakes |
title_fullStr |
Electric field and infrared radiation in the troposphere before earthquakes |
title_full_unstemmed |
Electric field and infrared radiation in the troposphere before earthquakes |
title_sort |
electric field and infrared radiation in the troposphere before earthquakes |
publisher |
Copernicus Publications |
publishDate |
2011 |
url |
https://doi.org/10.5194/nhess-11-3125-2011 https://noa.gwlb.de/receive/cop_mods_00026486 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00026441/nhess-11-3125-2011.pdf https://nhess.copernicus.org/articles/11/3125/2011/nhess-11-3125-2011.pdf |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_relation |
Natural Hazards and Earth System Sciences -- http://www.bibliothek.uni-regensburg.de/ezeit/?2064587 -- http://www.nat-hazards-earth-syst-sci.net/ -- 1684-9981 https://doi.org/10.5194/nhess-11-3125-2011 https://noa.gwlb.de/receive/cop_mods_00026486 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00026441/nhess-11-3125-2011.pdf https://nhess.copernicus.org/articles/11/3125/2011/nhess-11-3125-2011.pdf |
op_rights |
uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/nhess-11-3125-2011 |
container_title |
Natural Hazards and Earth System Sciences |
container_volume |
11 |
container_issue |
12 |
container_start_page |
3125 |
op_container_end_page |
3133 |
_version_ |
1766051616639680512 |