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<bibitem type="J">   <ARLID>0616712</ARLID> <utime>20250320140429.9</utime><mtime>20250211235959.9</mtime>   <SCOPUS>85217008719</SCOPUS>  <WOS>001424557500001</WOS>  <DOI>10.1016/j.jhazmat.2025.137510</DOI>           <title language="eng" primary="1">Spatial-temporal source term estimation using deep neural network prior and its application to Chernobyl wildfires</title>  <specification> <page_count>12 s.</page_count> <media_type>P</media_type> </specification>   <serial><ARLID>cav_un_epca*0257168</ARLID><ISSN>0304-3894</ISSN><title>Journal of Hazardous Materials</title><part_num/><part_title/><volume_id>448</volume_id><volume/><publisher><place/><name>Elsevier</name><year/></publisher></serial>    <keyword>Atmospheric inversion</keyword>   <keyword>Spatial-temporal source</keyword>   <keyword>Deep image prior</keyword>   <keyword>Deep neural networks</keyword>   <keyword>Chernobyl wildfires</keyword>    <author primary="1"> <ARLID>cav_un_auth*0464277</ARLID> <name1>Brožová</name1> <name2>Antonie</name2> <institution>UTIA-B</institution> <full_dept language="cz">Adaptivní systémy</full_dept> <full_dept language="eng">Department of Adaptive Systems</full_dept> <department language="cz">AS</department> <department language="eng">AS</department> <country>CZ</country> <fullinstit>Ústav teorie informace a automatizace AV ČR, v. v. i.</fullinstit> </author> <author primary="0"> <ARLID>cav_un_auth*0101207</ARLID> <name1>Šmídl</name1> <name2>Václav</name2> <institution>UTIA-B</institution> <full_dept language="cz">Adaptivní systémy</full_dept> <full_dept>Department of Adaptive Systems</full_dept> <department language="cz">AS</department> <department>AS</department> <full_dept>Department of Adaptive Systems</full_dept> <fullinstit>Ústav teorie informace a automatizace AV ČR, v. v. i.</fullinstit> </author> <author primary="0"> <ARLID>cav_un_auth*0267768</ARLID> <name1>Tichý</name1> <name2>Ondřej</name2> <institution>UTIA-B</institution> <full_dept language="cz">Adaptivní systémy</full_dept> <full_dept>Department of Adaptive Systems</full_dept> <department language="cz">AS</department> <department>AS</department> <fullinstit>Ústav teorie informace a automatizace AV ČR, v. v. i.</fullinstit> </author> <author primary="0"> <ARLID>cav_un_auth*0363740</ARLID> <name1>Evangeliou</name1> <name2>N.</name2> <country>NO</country> </author>   <source> <url>https://library.utia.cas.cz/separaty/2025/AS/brozova-0616712.pdf</url> </source> <source> <url>https://www.sciencedirect.com/science/article/pii/S0304389425004224?via%3Dihub</url>  </source>        <cas_special> <project> <project_id>GA24-10400S</project_id> <agency>GA ČR</agency> <country>CZ</country> <ARLID>cav_un_auth*0464279</ARLID> </project> <project> <project_id>SGS24/141/OHK4/3T/14</project_id> <agency>GA MŠk</agency> <country>CZ</country> <ARLID>cav_un_auth*0483231</ARLID> </project> <project> <project_id>101008004</project_id> <agency>EC</agency> <country>XE</country>   <ARLID>cav_un_auth*0437505</ARLID> </project>  <abstract language="eng" primary="1">The source term of atmospheric emissions of hazardous materials is a crucial aspect of the analysis of unintended release. Motivated by wildfires of regions contaminated by radioactivity, the focus is placed on the case of airborne transmission of material from 5 dimensions: spatial location described by longitude and latitude in a given area with potentially many sources, time profiles, height above ground level, and the size of particles carrying the material. Since the atmospheric inverse problem is typically ill-posed and the number of measurements is usually too low to estimate the whole 5D tensor, some prior information is necessary. For the first time in this domain, a method based on deep image prior utilizing the structure of a deep neural network to regularize the inversion is proposed. The network is initialized randomly without the need to train it on any dataset first. In tandem with variational optimization, this approach not only introduces smoothness in the spatial estimate of the emissions but also reduces the number of unknowns by enforcing a prior covariance structure in the source term. The strengths of this method are demonstrated on the case of 137Cs emissions during the Chernobyl wildfires in 2020.</abstract>       <reportyear>2026</reportyear>  <RIV>BB</RIV>    <result_subspec>WOS</result_subspec> <FORD0>10000</FORD0> <FORD1>10100</FORD1> <FORD2>10103</FORD2>   <num_of_auth>4</num_of_auth>  <inst_support> RVO:67985556 </inst_support>  <permalink>https://hdl.handle.net/11104/0363797</permalink>  <cooperation> <ARLID>cav_un_auth*0420880</ARLID> <name>NILU Norsk Inst Luftforskning, Kjeller, Norway</name> </cooperation>  <confidential>S</confidential>   <article_num> 137510 </article_num> <unknown tag="mrcbC91"> C </unknown>         <unknown tag="mrcbT16-e">ENVIRONMENTALSCIENCES|ENGINEERING.ENVIRONMENTAL</unknown> <unknown tag="mrcbT16-f">12.4</unknown> <unknown tag="mrcbT16-g">1.9</unknown> <unknown tag="mrcbT16-h">3.9</unknown> <unknown tag="mrcbT16-i">0.18877</unknown> <unknown tag="mrcbT16-j">1.88</unknown> <unknown tag="mrcbT16-k">239998</unknown> <unknown tag="mrcbT16-q">375</unknown> <unknown tag="mrcbT16-s">3.078</unknown> <unknown tag="mrcbT16-y">66.57</unknown> <unknown tag="mrcbT16-x">13.99</unknown> <unknown tag="mrcbT16-3">125960</unknown> <unknown tag="mrcbT16-4">Q1</unknown> <unknown tag="mrcbT16-5">10.100</unknown> <unknown tag="mrcbT16-6">3589</unknown> <unknown tag="mrcbT16-7">Q1</unknown> <unknown tag="mrcbT16-C">94.9</unknown> <unknown tag="mrcbT16-M">1.75</unknown> <unknown tag="mrcbT16-N">Q1</unknown> <unknown tag="mrcbT16-P">95.1</unknown> <arlyear>2025</arlyear>       <unknown tag="mrcbU14"> 85217008719 SCOPUS </unknown> <unknown tag="mrcbU24"> 39922073 PUBMED </unknown> <unknown tag="mrcbU34"> 001424557500001 WOS </unknown> <unknown tag="mrcbU63"> cav_un_epca*0257168 Journal of Hazardous Materials 448 1 2025 0304-3894 1873-3336 Elsevier </unknown> </cas_special> </bibitem>