Thermal Radiation Anomalies Associated with Major Earthquakes

Dimitar Ouzounov, S. Pulinets, M. Kafatos, P. Taylor
{"title":"Thermal Radiation Anomalies Associated with Major Earthquakes","authors":"Dimitar Ouzounov, S. Pulinets, M. Kafatos, P. Taylor","doi":"10.1002/9781119156949.CH15","DOIUrl":null,"url":null,"abstract":"29 Recent developments of remote sensing methods for Earth satellite data analysis 30 contribute to our understanding of earthquake related thermal anomalies. It was realized 31 that the thermal heat fluxes over areas of earthquake preparation is a result of air 32 ionization by radon (and other gases) and consequent water vapor condensation on newly 33 formed ions. Latent heat (LH) is released as a result of this process and leads to the 34 formation of local thermal radiation anomalies (TRA) known as OLR (outgoing 35 Longwave radiation, Ouzounov et al, 2007). We compare the LH energy, obtained by 36 integrating surface latent heat flux (SLHF) over the area and time with released energies 37 associated with these events. Extended studies of the TRA using the data from the most 38 recent major earthquakes allowed establishing the main morphological features. It was 39 also established that the TRA are the part of more complex chain of the short-term pre40 earthquake generation, which is explained within the framework of a lithosphere41 atmosphere coupling processes. 42 43 List of Acronyms: 44 AVHHRAdvanced Very High Resolution Radiometer( NOAA) 45 ACPAtmospheric chemical potential 46 EMSCEuropean-Mediterranean Seismological Centre 47 EOS Earth Observation System (NASA) 48 AIRS –Atmospheric Infrared Sounder (NASA) 49 EQ-earthquake 50 GMSD –IGS GPS station in Japan 51 GOES Geostationary Operational Environmental Satellite (NOAA) 52 ISTFIntegrated satellite and terrestrial framework 53 LAICLithosphere-Atmosphere-Ionosphere Coupling 54 LH – Latent heat 55 LWR – Long wave radiation 56 LAIMC Lithosphere-Atmosphere-Ionosphere-Magnetosphere Coupling 57 POES Polar Operational Environmental Satellites (NOAA) 58 OLR –Outgoing Longwave Radiation 59 RSTRobust Satellite technique 60 STIRSatellite thermal infrared radiation 61 SW –short wave radiation 62 TIR-Thermal Infrared radiation 63 TOA – Top of the Atmosphere 64 USGS-US Geological Survey 65 66 67 68","PeriodicalId":120736,"journal":{"name":"Pre-Earthquake Processes","volume":"142 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2017-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"17","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Pre-Earthquake Processes","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1002/9781119156949.CH15","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 17

Abstract

29 Recent developments of remote sensing methods for Earth satellite data analysis 30 contribute to our understanding of earthquake related thermal anomalies. It was realized 31 that the thermal heat fluxes over areas of earthquake preparation is a result of air 32 ionization by radon (and other gases) and consequent water vapor condensation on newly 33 formed ions. Latent heat (LH) is released as a result of this process and leads to the 34 formation of local thermal radiation anomalies (TRA) known as OLR (outgoing 35 Longwave radiation, Ouzounov et al, 2007). We compare the LH energy, obtained by 36 integrating surface latent heat flux (SLHF) over the area and time with released energies 37 associated with these events. Extended studies of the TRA using the data from the most 38 recent major earthquakes allowed establishing the main morphological features. It was 39 also established that the TRA are the part of more complex chain of the short-term pre40 earthquake generation, which is explained within the framework of a lithosphere41 atmosphere coupling processes. 42 43 List of Acronyms: 44 AVHHRAdvanced Very High Resolution Radiometer( NOAA) 45 ACPAtmospheric chemical potential 46 EMSCEuropean-Mediterranean Seismological Centre 47 EOS Earth Observation System (NASA) 48 AIRS –Atmospheric Infrared Sounder (NASA) 49 EQ-earthquake 50 GMSD –IGS GPS station in Japan 51 GOES Geostationary Operational Environmental Satellite (NOAA) 52 ISTFIntegrated satellite and terrestrial framework 53 LAICLithosphere-Atmosphere-Ionosphere Coupling 54 LH – Latent heat 55 LWR – Long wave radiation 56 LAIMC Lithosphere-Atmosphere-Ionosphere-Magnetosphere Coupling 57 POES Polar Operational Environmental Satellites (NOAA) 58 OLR –Outgoing Longwave Radiation 59 RSTRobust Satellite technique 60 STIRSatellite thermal infrared radiation 61 SW –short wave radiation 62 TIR-Thermal Infrared radiation 63 TOA – Top of the Atmosphere 64 USGS-US Geological Survey 65 66 67 68
与大地震有关的热辐射异常
29用于地球卫星数据分析的遥感方法的最新发展30有助于我们了解与地震有关的热异常。人们认识到,地震准备地区的热通量是氡(和其他气体)使空气电离的结果,随之而来的是新形成的离子上的水蒸气凝结。潜热(LH)的释放是这一过程的结果,并导致局部热辐射异常(TRA)的形成,称为OLR(外向长波辐射,Ouzounov等,2007)。我们将地表潜热通量(SLHF)在面积和时间上的积分得到的LH能量与与这些事件相关的释放能量进行了比较。利用最近38次大地震的数据对TRA进行了深入研究,确立了主要的形态特征。本文还确定了TRA是40年前短期地震发生的更复杂链的一部分,这可以在岩石圈-大气耦合过程的框架内解释。缩略语列表:高级甚高分辨率辐射计(NOAA)大气化学势欧洲-地中海地震中心EOS地球观测系统(NASA)大气-大气红外探测仪(NASA) EQ-earthquake日本GMSD - igs GPS站GOES地球静止运行环境卫星(NOAA) ist1综合卫星与地面框架岩石圈-大气-电离层耦合LH -潜热LWR -长波辐射极地业务环境卫星(NOAA) OLR -发射长波辐射稳健卫星技术stir卫星热红外辐射SW -短波辐射tir -热红外辐射TOA -大气顶部
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信