تعداد نشریات | 31 |
تعداد شمارهها | 748 |
تعداد مقالات | 7,112 |
تعداد مشاهده مقاله | 10,246,167 |
تعداد دریافت فایل اصل مقاله | 6,899,874 |
Effects of the Caspian Sea water level change on Boujagh National Park, southwest the Caspian Sea | ||
Caspian Journal of Environmental Sciences | ||
دوره 19، شماره 1، فروردین 2021، صفحه 127-138 اصل مقاله (959.22 K) | ||
نوع مقاله: Research Paper | ||
شناسه دیجیتال (DOI): 10.22124/cjes.2021.4503 | ||
نویسندگان | ||
Homayoun Khoshravan* 1؛ Alireza Naqinezhad2؛ Tahereh Alinejad-Tabrizi3؛ Tamara Yanina4 | ||
1Caspian Sea National Research Center, Water Research Institute, Ministry of Energy, Tehran, Iran | ||
2Department of Biology, Faculty of Basic Sciences, University of Mazandaran, Babolsar, Mazandaran, Iran | ||
3Environment Research Management Group (EMRIRAN), Ministry of Science, Research and Technology, Unit 5, Kaj Building, Shahid Amini Alley, Babol, Iran | ||
4Faculty of Geography, Lomonosov Moscow State University, Moscow, Russia | ||
چکیده | ||
Nowadays, climate change and sea level rise are serious threats to the social, economical and environmental vulnerability of the ocean coasts all around the world, and the Caspian Sea rapid fluctuations during the third millennium have set different conditions on the environmental structure of coastal areas. The main target of this study is to evaluate the coastline morphology behavior and the deformation of habitats and ecological condition of Boujagh National Park (BNP) due to Caspian Sea level changing during the progression and regression phases between 1978-2019. Initially, based on the available scientific documents, familiarity with the study area was carried out and the axes of measurements were defined. In field operations, sedimentation and erosion units of coastal zones and also different habitats were identified and geographically determined. In the next step, the rate of deformation of coastal habitats was calculated and classified using satellite images and GIS, and ultimately, validity of the results was verified with field evidence. The comparison of regression amount in BNP indicated that maximum negative shoreline displacement (892 m) has occurred in the east part of Sefid-rud River mouth during 1978-1995. So that, the shoreline negative changing has reached to 850 m in the north- western of central part of study area, while 738 m in north- eastern of central part in the period of 1995- 2019. The inundation zone extent has declined 104 ha between 1995 and 2019. Also the sea regression amount of area was 111 ha in the period of 1978- 1995, while changed to 380 ha during 1995-2019. During the last 24 years, there have been widespread environmental alterations in the studied area and a large part of the coastal wetlands has been dried up. The most important habitats affected by the Caspian Sea fluctuations include coastal lagoons, dry and wet sandy beach, fluvial meadow and river estuary. | ||
کلیدواژهها | ||
Caspian Sea؛ Environment؛ Sefidroud؛ Boujagh؛ habitats؛ morphology | ||
مراجع | ||
Alemi Safaval, P, Kheirkhah Zarkesh, M, Neshaei, SA & Ejlali, F 2018, Morphological changes in the southern coasts of the Caspian Sea using remote sensing and GIS. Caspian Journal of Environmental Sciences, 16: 271-85.
Alesheikh, AA, Ghorbanali, A & Nouri, N 2007, Coastline change detection using remote sensing, International Journal of Environmental Science & Technology, 4: 61-6.
Davidson, NC, Fluet-Chouinard, E & Finlayson, CM 2018, Global extent and distribution of wetlands: trends and issues, Marine and Freshwater Research,69: 620-7.
Devis, PH 1965-1988, Flora of Turkey and the East Aegean Island, 1-10, Edinburgh University Press. Edinburgh.
DOEI (Department of Environment of Islamic Republic of Iran) 1998, Caspian Sea environment. National Report of I.R. Iran. Caspian Environment Programme, Baku, p. 58.
Ghahreman, A, Naqinezahd, AR & Atar, F 2004, Habitats and flora of the Chamkhaleh-Jirbagh coastline and Amirkelayeh Wetland. Journal of Environmental Studies, 33: 46-67 (In Persian with English abstract).
Haghani, S & Leroy, S 2016, Differential impact of longshore currents on coastal geomorphology development in the context of rapid sea level changing: The case of the old Sefidrud River (the Caspian Sea), Quaternary International Journal, 408: 78-92.
Kazancı N, Gulbabazadeh T, Leroy SA & Ileri Ö 2004, Sedimentary and environmental characteristics of the Guilan-Mazandaran plain, Northern Iran, influence of long and short term Caspian water level fluctuations on geomorphology, Journal of Marine System, 46: 145- 148.
Kazancı, N & Gulbabazadeh, T 2013, Sefidrud Delta and Quaternary evolution of the southern Caspian lowland, Iran. Marine and Petroleum Geology, 44: 120-39.
Khoshraftar, R 2005, Geomorphological evolution of Kiashahr lagoon using aerial photographs and satellite images and GPS. Proceedings of the 9th International Conference on Environmental Science and Technology, 1-3 September 2005, Rhodes Island, Greece, Extended abstract: 381-387.
Khoshravan, H 2007, Beach sediments, morphodynamics and risk assessment of the Caspian Sea coast, Iran, Quaternary International Journal, 167-168: 35-39.
Khoshravan, H & Vafai, B 2016, Caspian Sea level fluctuations (past, recent and future), the 18th International Marine Industries Conference, Kish Island, Persian Gulf, Iran [In Persian].
Khoshravan, H & Naqinejad, AL 2018, Understanding the problems of inland waters: Case study for the Caspian basin (UPCB). International Conference on Environmental Consequence of Caspian Rapid Sea Level Changing in Gorgan Bay, 12-14 May, Baku, Azerbaijan, 314-317.
Komarev, VL 1934-1954, Flora of USSR, 1-21, Izdatel’stvo Akademi Nauk SSSR Leningrad (English translation from Russian, Israel program for scientific translation, Jerusalem, 1968-1977).
Kosarev, AN & Kostianoy, AG 2005, The Caspian Sea Environment, Springer Science & Business Media, DOI: https://doi.org/10.1007/b138238.
Kousari, S 1986, Evolution of Sefidroud Delta, Development in Geological Education, 1: 51-62.
Kroonenberg, SB, Badyukova, EN, Storms, JEA, Ignatov, EI & Kasimov, NS 2000, A full sea level cycle in 65 years: barrier dynamics along Caspian shores, Sedimentary Geology, 134: 257-274.
Naderi Beni, A, Lahijani, H, Mousavi Harami, R, Arpe, K, Leroy, S, Marriner, N, Berberian, M, Andrieu-Ponel, V, Djamali, M, Mahboubi, A & Reimer, PJ 2013, Caspian Sea-level changes during the last millennium: Historical and geological evidence from the South Caspian Sea, Climate of the Past, 9: 1645-1665.
Ramsar Convention Secretariat, 2018, Global wetland outlook state of the world wetlands and their services to people, Gland, Switzerland: Ramsar Convention Secretariat.
Ranjan, SP, Kazama, S and Sawamoto, M 2006, Effects of climate and land use changes on groundwater resources in coastal aquifers. Journal of Environmental Management, 80: 25-35.
Rechinger, KH 1963-1998, Flora Iranica. Vol. 1-173, Akademische Druck-U. Verlagsanstalt. Graz.
Rojas, C, Pino, J, Basnou, C & Vivanco, M, 2013, Assessing land-use and cover changes in relation to geographic factors and urban planning in the metropolitan area of Concepción (Chile). Implications for biodiversity conservation, Applied Geography, 39: 93-103.
Saunders, M, Leon, J, Phinn, S, Callaghan, D, O’Brien, K.R, Roelfsema, Ch, Lovelock, C, Lyons M & Mumby, P 2013, Coastal retreat and improved water quality mitigate losses of seagrass from sea level rise, Global Change Biology, 19: 2569-2583, DOI 10.1111/gcb.12218.
Slangen ABA, Katsman CA, Van deWal R, Vermeersen L & Riva R 2012, Towards regional projections of twenty-first century sea-level change based on IPCC SRES scenarios. Climate Dynamics, 38: 1191-1209, DOI 10.1007/s00382-011-1057-6.
Tutin, TG, Heywood, VH, Burges, NA, Moore, DM, Valentine, DH, Walters, SM and Webb, DA 1964-1980, Flora Europaea, Vol. 1-5. 1st Edition, Cambridge University. | ||
آمار تعداد مشاهده مقاله: 955 تعداد دریافت فایل اصل مقاله: 983 |