پژوهش های اقلیم شناسی

پژوهش های اقلیم شناسی

تحلیلی بر نوسانات سطح آب دریاچه خزر و تاثیر آن بر مدیریت سواحل (مطالعه موردی پهنه مرکزی سواحل خزر (بندر امیراباد)

نوع مقاله : مقاله پژوهشی

نویسندگان
1 دانشجوی دوره دکترای رشته آب و هواشناسی دانشگاه آزاد اسلامی علوم وتحقیقات، تهران ، ایران
2 استاد گروه جغرافیای دانشگاه آزاد اسلامی، اسلامشهر، ایران.
3 استادیار گروه جغرافیای دانشگاه آزاد اسلامی علوم وتحقیقات، تهران ، ایران.
10.22034/jcr.2025.485908.1670
چکیده
تحلیلی بر نوسانات سطح آب دریاچه خزر و سناریوهای مدیریت سواحل (مطالعه موردی پهنه مرکزی سواحل خزر (بندر امیرایاد)



چکیده

تغییر سطح آب ها یکی از پدیده هایی است که در آب های آزاد و دریاچه ها اتفاق می افتد. دریای خزر باتوجه به موقعیت استراتژیک و جغرافیایی به عنوان یک منطقه بسیار مهم محسوب می شود. منطقه مورد مطالعه در محدوده بندر امیرآباد در شمال شهرستان نکا می باشد. تغییرپذیری بالا و سریعی در تراز دریای خزر، اثرات عظیم اقتصادی، اجتماعی، سیاسی و زیست‌ محیطی دارد. هدف این مطالعه شناخت تغییرات اقلیمی بر نوسانات سطح دریای خزر می باشد. استفاده از روش کتابخانه ای(توصیفی) – تحلیل روش مطالعه این تحقیق است. نوسانات سطح تراز آب دریای خزر یکی از مهمترین وقایع طبیعی در این حوضه قلمداد می‌گردد. بررسی آمار تراز آب دریای خزر از سال 1900 میلادی تاکنون نمایانگر تغییرات سطح تراز آب دریا به صورت فازهای پسروی و پیشروی می باشد. نوسانات تراز آ ب خزر در دوره تاریخی نشان می دهد که از یک الگوی حادثه ای- تدریجی پیروی می کند. بیشترین فراوانی های تراز به خصوص در 700 سال اخیر بالاتر از (26-)متر بوده است. متغیر بودن بیلان آبی دریای خزر در زمان های مختلف و نوسانات سطح آب، در درجه اول ناشی از تغییر حجم رواناب ورودی به دریا می باشد. دوره افزایشی تراز آب دریای خزر در طول سال به طور معمول از اوایل بهار شروع شده و تا اواسط تابستان ادامه می یابد و این زمان با دوره های سیلابی رودخانه های تأثیر گذار نظیر ولگا کاملا انطباق دارد. سواحل منطقه امیرآباد بدلیل احداث تاسیسات بندری از وضعیت تعادل و
کلیدواژه‌ها

عنوان مقاله English

An analysis of the fluctuations in the water level of the Caspian Sea and its impact on coastal management (case study of the central zone of the Caspian coast (Amirabad Port))

نویسندگان English

abas abkar 1
Azadeh Arbabi Sabzevari 2
Farida Asadian 3
1 Secretary of education and upbringing of Neka city
2 Islamic Azad University of Eslam Shahr., Tehran, Iran
3 , Islamic Azad University of Science and Research Tehran, Iran
چکیده English

An analysis of Caspian lake water level fluctuations and coastal management scenarios (a case study of the central area of the Caspian coast (Amirayad port)

Changing the water level is one of the phenomena that happens in open waters and lakes. The Caspian Sea is considered a very important region due to its strategic and geographical location. The studied area is in the area of Amirabad port in the north of Neka city. The high and rapid variability of the Caspian Sea has economic, social, political and environmental effects. The aim of this study is to understand the climatic changes on the Caspian Sea level fluctuations. Using the library method (descriptive) - analysis is the study method of this research. Fluctuations in the level of the Caspian Sea are considered one of the most important natural events in this basin. Examining the statistics of the water level of the Caspian Sea in 1900 AD shows the changes of the water level of the sea in the form of retrogressive and progressive phases. Fluctuations in the Caspian water level in the historical period show that the cycle follows gradual events. The highest frequency of heights, especially in the last 700 years, was above (-26) meters. The variability of the water balance of the Caspian Sea at different times and water level fluctuations is primarily caused by the change in the volume of runoff entering the sea. The increasing period of the Caspian Sea water level during the year usually starts from early spring and continues until mid-summer, and this time is completely compatible with the flood periods of influential rivers such as the Volga. Due to the construction of port facilities, the coasts of Amirabad region are out of equilibrium and stability, and sedimentation and erosion can be seen in the upstream (western side) and downstream (eastern side) coasts, respectively. Amirabad port ranked 1st in terms of access to rail and air transportation lines and ranked 2nd in terms of identifying categories of environmental pollution and ranked 3rd in terms of habitat destruction and loss of biodiversity according to experts in priority to improve performance. took In order to improve the sustainable performance of Mir Abad port, it is suggested to the managers of this port to pay more attention to the index of access to air transport lines





abstract

An analysis of Caspian lake water level fluctuations and coastal management scenarios (a case study of the central area of the Caspian coast (Amirayad port)

Changing the water level is one of the phenomena that happens in open waters and lakes. The Caspian Sea is considered a very important region due to its strategic and geographical location. The studied area is in the area of Amirabad port in the north of Neka city. The high and rapid variability of the Caspian Sea has economic, social, political and environmental effects. The aim of this study is to understand the climatic changes on the Caspian Sea level fluctuations. Using the library method (descriptive) - analysis is the study method of this research. Fluctuations in the level of the Caspian Sea are considered one of the most important natural events in this basin. Examining the statistics of the water level of the Caspian Sea in 1900 AD shows the changes of the water level of the sea in the form of retrogressive and progressive phases. Fluctuations in the Caspian water level in the historical period show that the cycle follows gradual events. The highest frequency of heights, especially in the last 700 years, was above (-26) meters. The variability of the water balance of the Caspian Sea at different times and water level fluctuations is primarily caused by the change in the volume of runoff entering the sea. The increasing period of the Caspian Sea water level during the year usually starts from early spring and continues until mid-summer, and this time is completely compatible with the flood periods of influential rivers such as the Volga. Due to the construction of port facilities, the coasts of Amirabad region are out of equilibrium and stability, and sedimentation and erosion can be seen in the upstream (western side) and downstream (eastern side) coasts, respectively. Amirabad port ranked 1st in terms of access to rail and air transportation lines and ranked 2nd in terms of identifying categories of environmental pollution and ranked 3rd in terms of habitat destruction and loss of biodiversity according to experts in priority to improve performance. took In order to improve the sustainable performance of Mir Abad port, it is suggested to the managers of this port to pay more attention to the index of access to air transport lines.

کلیدواژه‌ها English

: sea level fluctuations
Caspian
Amirabad
sustainable management
 
1- Emam, R., Rasouli, M. 2008. Caspian Sea Environment; Challenges and Solutions, Port and Sea, Year 23, Issue 150, pp. 80-85.. Baradaran Sherka, H., Maleka Lasadati, S. 2008. Good Governance: The Key to the Development of Southwest Asia, Strategy Quarterly, Year 17, Issue 49.
2- Onagh, M., 1990. Study of Geomorphological Evolution of the Qara Su Watershed, PhD Thesis in Physical Geography, Geomorphological Orientation, Faculty of Literature and Humanities, Islamic Azad University, Science and Research Branch, Tehran, 238 pp.
3- Torabi, Omid, Karimi, Nematollah, Shesh-Anghosht, Sara, Rashtbari, Maryam, Kolorajan, Abdullah, 2019, Study of changes in the water area of ​​Miankaleh and Anzali wetlands in relation to changes in the Caspian Sea level and precipitation using remote sensing techniques, 8th National Conference on Water Resources Management of Iran, Mashhad.
4- servati, Mohammad Reza, Mansouri, Reza, Ghahrudi Tali, Manijeh and Ali Naimi. 2017. Study of changes in the coastline of the southeastern shores of the Caspian Sea during the period 1987-2015. Quantitative Geomorphology Research, Year 6, Issue 2, pp. 15-28.
5- Jahandar Lashkari, Bahareh. 2018. Study and evaluation of sustainable management performance in northern Iranian ports (Bandar Noshahr, Bandar Anzali, Bandar Amirabad, Bandar Fereydounkenar). Master's thesis. 117 pages.
6- Chegini, F., Taebi, S., 2008, Determination of wind-induced wave climate in waters off the coast of Bandar Amirabad, Report from the National Oceanographic Center, 150 pages.
7- Daryabari, Seyed Jamal-eddin, 2009. Study of the causes of fluctuations in the Caspian Sea water with emphasis on environmental hazards. Encyclopedia. Scientific Quarterly Journal of Human Geography Research - Year 2, Issue 1.
8- Ramezani Mozairji, F., Yaghoubi, M., Qanqermeh, A., 2011. Forecasting the Caspian Sea Water Level Based on Fuzzy Approximation System. Water and Wastewater Journal. Issue 3, 90-98.
9- Seyouf Jahromi, Maryam and Hamedsam Daliri. 2011. Wind-induced waves in the southern Caspian Sea, Quarterly Journal of Marine Science and Technology, Volume: 25, Issue: 1.
10- Alizadeh, Lahiji. 2004. Geomorphology of the Caspian Sea Coasts, Geomorphology Workshop on Coasts of the North Sea Basins.
11- Qanqermeh, Abdol azim and Beirodian, Nader (2012). Climatic Changes and Fluctuations in the Discharge of Large Rivers on the Southern Coasts of the Caspian Sea. Journal of Geographical Spatial Planning. Year 2/ Serial Number 4/ Summer
12- Kolai, A., Goodarzi, M., 2013. Sea Caspian, Challenges and Prospects, Tehran, . Mizan
13- Kolai, Elaheh, Shayesteh, Mehdi, 2014. Good Governance and Integrated Management of the Caspian Sea Coastal Areas, Environmental Science, Volume 40, Issue 3, Fall 2014, Pages 692-679.
14- Malek, Javad. Bani Hashem, Seyedeh Masoumeh and Kolthoom Gholamnejad. 2012. Study of Changes in the Caspian Sea Coastline in the Area of ​​Amirabad Port. 10th International Conference on Coasts, Ports and Marine Structures, November 19, 2012. Tehran.
15- Yousefi Roshan, Mohammad Reza and Parviz Kardvani, 2013. Water level fluctuations and the efficiency of the Caspian Sea (coastal line of Babolsar city area) Earth Science Research, Year 4, Issue 14, Summer 2013, pages 1-16.
16-Brezgunov, V.S., Nechaev, V.V. and Yakimova, T.V., 1987. Studying Water Exchange in the Northern Caspian Sea Based on the Distribution of the Oxygen Isotopic Composition of Water, Vodn. Resur., v. 1, p. 155-161.
17-Buchberger, S. G. 1995. Conditional Frequency Analysis of Auto correlated Lake Levels, Journal of Water Resources Planning and Management, ASCE, 121 (2): 158-170
18-Hatami Bavarsad, N., Mansoury, D., Khalilabadi, M. R., & Malekilonbar, M. (2021) The impact of the inlet cyclones to the Caspian Sea on the sea level fluctuations. International Journal of coastal and offshore engineering, 5(1), 15-29.
19-Jamshidi, S., Abu Bakar, Md., Noordin, M., (2017), Temperature, Salinity and Density Measurements in the Coastal Waters of the Rudsar, South Caspian Sea, Journal of the Persian Gulf, (Marine Science), PP.27-35.
20-Kakroodi, A., A., Kroonenberg, S., B., Goorabi, A., Yamani, M., 2014a; Shoreline response to rapid 20th century sea-level change along the Iranian Caspian coast, Journal of Coastal Research 30 (6), 1243–1250.
21-Khoshakhlagh, F., Shakouri Katigari, A., Hadinejad Saboori, SH., (2016), Trend of the Caspian Sea surface temperature changes, Natural Environment Change, pp. 57- 66.
22-Kosarev, A.N. and Tuzhilkin V.S., 1997. Climatic annual cycle of the Caspian Sea thermohaline structure variability. Water Resources, v. 2, p. 104-112
23-Kroonrnberg, S.B., Rusakov, G.V., and Svitoch, A.A.,1997. The wandering of the Volga Delta: a response to rapid Caspian Sea- level change. Sedimentary Geology, v.107, p.189,209.
24-Leroy, S.A.G., Kakroodi, A.A., Kroonenberg, S.B., Lahijani, H.A.K., Alimohammadian, H., & Nigarov, A., 0202, Holocene vegetation history and sea level changes in the SE corner of the Caspian Sea: relevance to SW Asia climate Quat. Sci. Rev. 72.
25-Panin G.N., (2007), Caspian Sea Level Fluctuations as a consequence of regional Climatic Change, Humburg, p.216-219.
26-Rodionov. S. 1994. Global and Regional Climate Interaction: The Caspian Sea Experience. NCAR, p150.
27-Rychagov, G.I., Leont'ev, O.K., Nikiforov, L.G., Lukashov, A.A., Ignatov, E.I. and Bolysov, S.I., 1984. Special Geomorphological Training Practical in Dagestan. Moscow University Ed., 132 p.
28-Xu, H., Taylor, R.G., and Xu, Y. 2011. Quantifying Uncertainty in the Impacts of Climate Discharge in Sub-Catchments of the Yangtze and Yellow Basins, China, Hydrol. Earth Syst. Sci. 15: 333-344.doi:10.5194/hess-15-333-2011.