Effects of strong earthquakes in variations of electrical and meteorological parameters of the near-surface atmosphere in Kamchatka region
The diurnal variations in electrical (quasistatic electric field and electrical conductivity) and meteorological (temperature, pressure, relative humidity of the atmosphere, and wind speed) parameters, measured simultaneously before strong earthquakes in Kamchatka region (November 15, 2006, М = 8.3;...
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| Veröffentlicht in: | Geomagnetism and Aeronomy 2017-09, Vol.57 (5), p.610-617 |
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| creator | Smirnov, S. E. Mikhailova, G. A. Mikhailov, Yu. M. Kapustina, O. V. |
| description | The diurnal variations in electrical (quasistatic electric field and electrical conductivity) and meteorological (temperature, pressure, relative humidity of the atmosphere, and wind speed) parameters, measured simultaneously before strong earthquakes in Kamchatka region (November 15, 2006,
М
= 8.3; January 13, 2007,
М
= 8.1; January 30, 2016,
М
= 7.2), are studied for the first time in detail. It is found that a successively anomalous increase in temperature, despite the negative regular trend in these winter months, was observed in the period of six–seven days before the occurrences of earthquakes. An anomalous temperature increase led to the formation of “winter thunderstorm” conditions in the near-surface atmosphere of Kamchatka region, which was manifested in the appearance of an anomalous, type 2 electrical signal, the amplification of and intensive variations in electrical conductivity, heavy precipitation (snow showers), high relative humidity of air, storm winds, and pressure changes. With the weak flow of natural heat radiation in this season, the observed dynamics of electric and meteorological processes can likely be explained by the appearance of an additional heat source of seismic nature. |
| doi_str_mv | 10.1134/S0016793217050164 |
| format | Article |
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М
= 8.3; January 13, 2007,
М
= 8.1; January 30, 2016,
М
= 7.2), are studied for the first time in detail. It is found that a successively anomalous increase in temperature, despite the negative regular trend in these winter months, was observed in the period of six–seven days before the occurrences of earthquakes. An anomalous temperature increase led to the formation of “winter thunderstorm” conditions in the near-surface atmosphere of Kamchatka region, which was manifested in the appearance of an anomalous, type 2 electrical signal, the amplification of and intensive variations in electrical conductivity, heavy precipitation (snow showers), high relative humidity of air, storm winds, and pressure changes. With the weak flow of natural heat radiation in this season, the observed dynamics of electric and meteorological processes can likely be explained by the appearance of an additional heat source of seismic nature.</description><identifier>ISSN: 0016-7932</identifier><identifier>EISSN: 1555-645X</identifier><identifier>EISSN: 0016-7940</identifier><identifier>DOI: 10.1134/S0016793217050164</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Atmosphere ; Diurnal variations ; Earth and Environmental Science ; Earth Sciences ; Earthquakes ; Electric currents ; Electric fields ; Electrical conductivity ; Electrical resistivity ; Geophysics/Geodesy ; Heavy precipitation ; High humidity ; Humidity ; Meteorological parameters ; Meteorology ; Parameter estimation ; Precipitation ; Pressure changes ; Radiation ; Relative humidity ; Seismic activity ; Snowstorms ; Storm winds ; Surface chemistry ; Temperature rise ; Thermal radiation ; Wind ; Wind speed ; Winter</subject><ispartof>Geomagnetism and Aeronomy, 2017-09, Vol.57 (5), p.610-617</ispartof><rights>Pleiades Publishing, Ltd. 2017</rights><rights>Geomagnetism and Aeronomy is a copyright of Springer, 2017.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c382t-57fda6b9508801cf5ad82f36598996ebdda162a0ffc13e9e1c0bce1059898963</citedby><cites>FETCH-LOGICAL-c382t-57fda6b9508801cf5ad82f36598996ebdda162a0ffc13e9e1c0bce1059898963</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S0016793217050164$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0016793217050164$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Smirnov, S. E.</creatorcontrib><creatorcontrib>Mikhailova, G. A.</creatorcontrib><creatorcontrib>Mikhailov, Yu. M.</creatorcontrib><creatorcontrib>Kapustina, O. V.</creatorcontrib><title>Effects of strong earthquakes in variations of electrical and meteorological parameters of the near-surface atmosphere in Kamchatka region</title><title>Geomagnetism and Aeronomy</title><addtitle>Geomagn. Aeron</addtitle><description>The diurnal variations in electrical (quasistatic electric field and electrical conductivity) and meteorological (temperature, pressure, relative humidity of the atmosphere, and wind speed) parameters, measured simultaneously before strong earthquakes in Kamchatka region (November 15, 2006,
М
= 8.3; January 13, 2007,
М
= 8.1; January 30, 2016,
М
= 7.2), are studied for the first time in detail. It is found that a successively anomalous increase in temperature, despite the negative regular trend in these winter months, was observed in the period of six–seven days before the occurrences of earthquakes. An anomalous temperature increase led to the formation of “winter thunderstorm” conditions in the near-surface atmosphere of Kamchatka region, which was manifested in the appearance of an anomalous, type 2 electrical signal, the amplification of and intensive variations in electrical conductivity, heavy precipitation (snow showers), high relative humidity of air, storm winds, and pressure changes. With the weak flow of natural heat radiation in this season, the observed dynamics of electric and meteorological processes can likely be explained by the appearance of an additional heat source of seismic nature.</description><subject>Atmosphere</subject><subject>Diurnal variations</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Electric currents</subject><subject>Electric fields</subject><subject>Electrical conductivity</subject><subject>Electrical resistivity</subject><subject>Geophysics/Geodesy</subject><subject>Heavy precipitation</subject><subject>High humidity</subject><subject>Humidity</subject><subject>Meteorological parameters</subject><subject>Meteorology</subject><subject>Parameter estimation</subject><subject>Precipitation</subject><subject>Pressure changes</subject><subject>Radiation</subject><subject>Relative humidity</subject><subject>Seismic activity</subject><subject>Snowstorms</subject><subject>Storm winds</subject><subject>Surface chemistry</subject><subject>Temperature rise</subject><subject>Thermal radiation</subject><subject>Wind</subject><subject>Wind speed</subject><subject>Winter</subject><issn>0016-7932</issn><issn>1555-645X</issn><issn>0016-7940</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kMtOwzAQRS0EEqXwAewssQ7YSZ0mS1SVh6jEgi7YRVNnnKRN4nTsIPELfDVJywIJsbI199wz0jB2LcWtlNHs7k0IGc_TKJRzoYbv7IRNpFIqiGfq_ZRNxjgY83N24dxWiEgoJSfsa2kMau-4Ndx5sm3BEciX-x526HjV8g-gCnxl2wOD9UBTpaHm0Oa8QY-WbG2Lw6gDgnFEB9aXyNvBFrieDGjk4BvruhIJR_ELNLoEvwNOWAz-S3ZmoHZ49fNO2fphuV48BavXx-fF_SrQURL6QM1NDvEmVSJJhNRGQZ6EJopVmqRpjJs8BxmHIIzRMsIUpRYbjVKMeZLG0ZTdHLUd2X2Pzmdb21M7bMzkIFWpkuFIySOlyTpHaLKOqgboM5MiGy-e_bn40AmPHTewbYH0y_xv6RtIZ4Vf</recordid><startdate>20170901</startdate><enddate>20170901</enddate><creator>Smirnov, S. 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V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c382t-57fda6b9508801cf5ad82f36598996ebdda162a0ffc13e9e1c0bce1059898963</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Atmosphere</topic><topic>Diurnal variations</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earthquakes</topic><topic>Electric currents</topic><topic>Electric fields</topic><topic>Electrical conductivity</topic><topic>Electrical resistivity</topic><topic>Geophysics/Geodesy</topic><topic>Heavy precipitation</topic><topic>High humidity</topic><topic>Humidity</topic><topic>Meteorological parameters</topic><topic>Meteorology</topic><topic>Parameter estimation</topic><topic>Precipitation</topic><topic>Pressure changes</topic><topic>Radiation</topic><topic>Relative humidity</topic><topic>Seismic activity</topic><topic>Snowstorms</topic><topic>Storm winds</topic><topic>Surface chemistry</topic><topic>Temperature rise</topic><topic>Thermal radiation</topic><topic>Wind</topic><topic>Wind speed</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Smirnov, S. E.</creatorcontrib><creatorcontrib>Mikhailova, G. A.</creatorcontrib><creatorcontrib>Mikhailov, Yu. M.</creatorcontrib><creatorcontrib>Kapustina, O. V.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>Aerospace Database</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Science Database</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><jtitle>Geomagnetism and Aeronomy</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Smirnov, S. E.</au><au>Mikhailova, G. A.</au><au>Mikhailov, Yu. M.</au><au>Kapustina, O. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Effects of strong earthquakes in variations of electrical and meteorological parameters of the near-surface atmosphere in Kamchatka region</atitle><jtitle>Geomagnetism and Aeronomy</jtitle><stitle>Geomagn. Aeron</stitle><date>2017-09-01</date><risdate>2017</risdate><volume>57</volume><issue>5</issue><spage>610</spage><epage>617</epage><pages>610-617</pages><issn>0016-7932</issn><eissn>1555-645X</eissn><eissn>0016-7940</eissn><abstract>The diurnal variations in electrical (quasistatic electric field and electrical conductivity) and meteorological (temperature, pressure, relative humidity of the atmosphere, and wind speed) parameters, measured simultaneously before strong earthquakes in Kamchatka region (November 15, 2006,
М
= 8.3; January 13, 2007,
М
= 8.1; January 30, 2016,
М
= 7.2), are studied for the first time in detail. It is found that a successively anomalous increase in temperature, despite the negative regular trend in these winter months, was observed in the period of six–seven days before the occurrences of earthquakes. An anomalous temperature increase led to the formation of “winter thunderstorm” conditions in the near-surface atmosphere of Kamchatka region, which was manifested in the appearance of an anomalous, type 2 electrical signal, the amplification of and intensive variations in electrical conductivity, heavy precipitation (snow showers), high relative humidity of air, storm winds, and pressure changes. With the weak flow of natural heat radiation in this season, the observed dynamics of electric and meteorological processes can likely be explained by the appearance of an additional heat source of seismic nature.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0016793217050164</doi><tpages>8</tpages></addata></record> |
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| subjects | Atmosphere Diurnal variations Earth and Environmental Science Earth Sciences Earthquakes Electric currents Electric fields Electrical conductivity Electrical resistivity Geophysics/Geodesy Heavy precipitation High humidity Humidity Meteorological parameters Meteorology Parameter estimation Precipitation Pressure changes Radiation Relative humidity Seismic activity Snowstorms Storm winds Surface chemistry Temperature rise Thermal radiation Wind Wind speed Winter |
| title | Effects of strong earthquakes in variations of electrical and meteorological parameters of the near-surface atmosphere in Kamchatka region |
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