Assessment of Modern Landscape Dynamics of the Zapolyarnoe Gas Field Using Satellite Data

Tyumen State University Herald. Natural Resource Use and Ecology


Release:

2018, Vol. 4. №2

Title: 
Assessment of Modern Landscape Dynamics of the Zapolyarnoe Gas Field Using Satellite Data


For citation: Moskovchenko D. V., Moskovchenko M. D. 2018. “Assessment of Modern Landscape Dynamics of the Zapolyarnoe Gas Field Using Satellite Data”. Tyumen State University Herald. Natural Resource Use and Ecology, vol. 4, no 2, pp. 6-16. DOI: 10.21684/2411-7927-2018-4-2-6-16

About the authors:

Dmitrii V. Moskovchenko, Dr. Sci. (Geogr.), Head of the Geoecology Sector, Tyumen Scientific Center of the Siberian Branch of the Russian Academy of Sciences; Lead Research Associate, Institute of Environmental and Agricultural Biology (X-BIO), University of Tyumen; moskovchenko1965@gmail.com

Mikhail D. Moskovchenko, Undergraduate Student, Institute of Earth Sciences, University of Tyumen; moskovchenkomd@yandex.ru

Abstract:

The article analyzes the dynamics of landscapes of the polar deposit located in the forest-tundra zone of Western Siberia. On the basis of data obtained by decoding Landsat satellite images, changes in various indicators (lake area, areas of man-caused disturbances, and areas of post-fire successions) were recorded. Using MODIS satellite data, the NDVI values in 2000-2016 were calculated. Using correlation analysis, the authors have evaluated the factors influencing the processes of landscape dynamics. They have recorded the increase in the area of lakes, which can be explained due to the increase in precipitation and filling of mineral soil quarries with water. There is no trend towards an increase in NDVI values, although there is a gradual increase in the positive temperatures. The lack of changes is due to periodic fires and technogenic disturbances, causing a decrease in NDVI, as in well as in the growth of thermokarst lakes. There is a shift of the vegetation period to later calendar dates: in May, there is a tendency to decrease, in September — to increase the NDVI values. On the territory of the field, the violations, which occurred during the exploration and preparation for the operation, prevail. In 1990-1998, 2.5% of the territory was violated in the subsequent period, after the start of industrial gas production — another 2%. Peat fires are an important factor in landscape dynamics. Post-fire recovery of lichen tundra vegetation continues at least 45 years. In the burned areas instead of the tundra and woodland with a predominance of lichens, new dwarf birch tundra and woodlands emerge with a predominance of mosses and dwarf shrubs.

References:

  1. Moskalenko N. G. (ed.). 2006. Antropogennyye izmeneniya ekosistem Zapadno-Sibirskoy gazonosnoy provintsii [Anthropogenic Changes in the Ecosystems of the West Siberian Gas Province]. Moscow: Institut kriosfery Zemli.
  2. Bryksina N. A., Kirpotin S. N. 2012. “Landshaftno-kosmicheskiy analiz izmeneniya ploshchadi i kolichestva termokarstovykh ozer v zone mnogoletney merzloty Zapadnoy Sibiri” [Landscape-Space Analysis of Changes in the Area and Quantity of Thermokarst Lakes in the Zone of Permafrost in Western Siberia]. Vestnik Tomskogo gosudarstvennogo universiteta. Biologiya, no 4 (20), pp. 185-194 
  3. Bulygina O. N., Razuvayev V. N., Korshunova N. N., Shchvets N. V. “Opisaniye massiva dannykh mesyachnykh summ osadkov na stantsiyakh Rossii” [Description of an Array of Monthly Rainfall Data at Russian Stations]. Rossiyskiy gidrometeorologicheskiy portal: VNIIGMI-MTSD. Accessed on 25 June 2018. http://meteo.ru/data/158-total-pgecipitation# 
  4. Yershov E. D. (ed.). 1989. Geokriologiya SSSR. Zapadnaya Sibir’ [Geocryology of the USSR. Western Siberia]. Moscow: Nedra.
  5. Dneprovskaya V. P. 2009. “Izucheniye izmeneniy termokarsta v zone preryvistogo rasprostraneniya vechnoy merzloty Zapadnoy Sibiri na osnove kosmicheskikh snimkov” [Study of Changes in Thermokarst in the Zone of Intermittent Propagation of the Permafrost of Western Siberia on the Basis of Space Images]. Issledovaniye Zemli iz kosmosa, no 4, pp. 88-96
  6. Zhiltsova Ye. L., Anisimov O. A. 2015. “Dinamika rastitel’nosti severnoy Yevrazii: analiz sovremennykh nablyudeniy i prognoz na 21 vek” [Dynamics of Vegetation in Northern Eurasia: Analysis of Modern Observations and the Forecast for the 21st century] ARKTIKA. XXI vek. Yestestvennyye nauki, no 2 (3), pp. 48-59
  7. Zapolyarnoye mestorozhdeniye. [The Zapolyarnoye Field]. Accessed on 25 June 2018. http://www.gazprom.ru/about/production/projects/deposits/zm/ 
  8. Gudilin I. S. (ed.). 1980. “Landshaftnaya karta SSSR” [Landscape Map of the USSR]. In: Proizvodstvenno-geologicheskoye ob»yedineniye po provedeniyu spetsial’nykh gidrogeologicheskikh i inzhenerno-geologicheskikh rabot (Gidrospetsgeologiya). Moscow.
  9. Pavlov A. V., Malkova G. V. 2010. “Dinamika kriolitozony Rossii v usloviyakh sovremennykh izmeneniy klimata XX-XXI vekov” [Dynamics of the Permafrost Zone of Russia in Conditions of Modern Climate Changes of the 20th-21st Centuries]. Izvestiya RAN. Seriya Geograficheskaya, no 5, pp. 44-51.
  10. Vorobyev V. V., Belov A. V. (eds.). 1985. Rastitel’nyy pokrov Zapadno-Sibirskoy ravniny [Vegetation Cover of the West Siberian Plain]. Novosibirsk: Nauka.
  11. Smith L. C., Sheng Y., MacDonald G. M. et al. 2005. “Disappearing Arctic Lakes”. Science, vol. 308, no 5727, p. 1429. DOI: 10.1126/science.1108142
  12. Walker D. A., Epstein H. E., Raynolds M. K. et al. 2012. “Environment, Vegetation and Greenness (NDVI) along the North America and Eurasia Arctic Transects”. Environmental Research Letters, no 7. DOI: 10.1088/1748-9326/7/1/015504