An estimation of nature of temperature anomalies on the space pictures of the black sea
DOI:
https://doi.org/10.36023/ujrs.2016.9.78Keywords:
gashydrates, mud volcanoes, methane gas emissions, gas vultures, gas flares, seasonal thermocline, fractured zones, deep canyonsAbstract
In the article are given the results of comparison of temperature anomalies which are displayed on the satellite images AVHR with geological and tectonic information in limits of a northeast shelf of the Black sea. The satellite images were decoded with the help of software’s ERDAS IMAGINE. Comparison of temperature anomalies with geological and geophysical materials shows, that the temperature anomalies displayed on satellite images AVHR are probably connected to bleeding of gases, mainly, on faults to zones, which arise, at shift motions on deep faults of the northeast and latitudinal strikes.
References
Dando P. R., Hovland M. (1992). Environmental effects of submarine seeping natural gas. Continental Shelf Research, 12 (10), 1197–1207.
Dimitrov L. I. (1989). Characteristics of gas-acoustic anomalies on the South Bulgarian Black sea shelf. Oceanology, 19, 34–41.
Egorov V. N. et al. (2003). Modern ideas about the environment-forming and ecological role of jet methane gas emissions from the bottom of the Black Sea. Marine Ecological Journal, 3, II.
Efremova A. G., Zhichenko V. R. (1974). Detection of crystalline hydrates in sediments of modern water areas. Dokl. Academy of Sciences of the USSR, 214 (5), 1179–1181.
Gevorkyan V. Kh. et al. (1991). Gas-emitting structures on the bottom of the northwestern part of the Black Sea. Doc. Academy of Sciences of the Ukrainian SSR, 4, 80–85.
Ginsburg G. D., Soloviev V. A. (1998). Submarine gashydrates. VNII Okeangeologia, St. Petersburg.
Ivanov M.K. et al. (1989). Mud volcanoes in the deep-sea part of the Black Sea. West. Moscow Univ. Ser. 4. Geology, 3, 48–54.
Polikarpov H.G., Egorov V.M. (1989). Active gas emissions from the bottom of the Black Sea have been detected. Ex. Academy of Sciences of the Ukrainian SSR, 10, 108–111.
Polikarpov G. G. et al. (1989). The phenomenon of active gas release from uplifts on the slope of the depths of the western part of the Black Sea. Dokl. Academy of Sciences of the Ukrainian SSR, Ser. B, 12, 13–15.
Shnyukov E. F. et al. (1999). Gas flares at the bottom of the Black Sea. Kiev, OR NAS of Ukraine.
Shnyukov E. F. et al. (2007). New manifestations of gas and mud volcanism in the Black Sea. Geology and Minerals of the World Ocean, 2, 107–110.
Shnyukov E. F. et al. (2005). The deep nature of gas plumes in the western part of the Black Sea according to the results of geophysical research. Geology and Minerals of the World Ocean, 1, 70–82.
Zankevich B. A., Shafranskaya N. V. (2009). Tectonic position of the zone of gas torches in the northwestern part of the Black Sea. Geology and Minerals of the World Ocean, 3, 35–54.
Downloads
Published
Issue
Section
License
Licensing conditions: the authors retain their copyrights and grant the journal the right of first publication of a work, simultaneously licensed in accordance with the Creative Commons Attribution License International CC-BY, which allows you to share the work with proof of authorship of the work and initial publication in this journal.
The authors, directing the manuscript to the editorial office of the Ukrainian Journal of Remote Sensing of the Earth, agree that the editorial board transfers the rights to protection and use of the manuscript (material submitted to the journal editorial board, including such protected copyright objects as photographs of the author, drawings, charts, tables, etc.), including reproduction in print and on the Internet; for distribution; to translate the manuscript into any languages; export and import of copies of the journal with the article of the authors for the purpose of distribution, informing the public. The above rights are transferred by the authors to the editors, without limitation of their validity, and in the territory of all countries of the world without limitation, including in Ukraine.
The authors guarantee that they have exclusive rights to use the submitted material. The editors are not liable to third parties for breach of data by the authors of the guarantees. The authors retain the right to use the published material, its fragments and parts for personal, including scientific and educational purposes. The rights to the manuscript are considered to be transferred by the authors of the editorial board from the moment of the publication of the issue of the journal in which it is published. Reprinting of materials published in the journal by other individuals and legal entities is possible only with the consent of the publisher, with the obligatory indication of the issue of the journal in which the material was published.