ارزیابی آسیب‌پذیری سواحل نسبت به بالا آمدن تراز آب دریا در شهرستان بابلسر

پژوهش درباره ی سوانح بزرگ طبیعی و سوانح ناشی از فناوری ها به موضوعی مهم در جغرافیا و کاربرد آن تبدیل شده است. امکان تحلیل پیچیدگی مسئله در رویکرد سیستمی و در نگاه جامع گرای به جغرافیای نظری و کاربردی و جامع بودن جغرافیای طبیعی و انسانی محقق است. با توجه به اینکه نوسانات سطح آب دریای خزر از جمله در منطقه ی ساحلی بابلسر حتی در مقیاس دهه ای بسیار سریع اتفاق می افتد، رعایت عنصر ایمنی در سایه ی مدیریت یک پارچه ساحلی با تعیین حریم دریا در این سواحل امکان پذیر خواهد بود که جغرافیا و، به ویژه، ژئومورفولوژی یکی از ارکان اصلی در این نوع از مدیریت سواحل است. تعیین حریم نوسانات تراز آب دریا، که باعث تغییرات مورفولوژیکی در سطح زمین و وارد آمدن خساراتی به تاسیسات انسانی می شود، ضرورت اجرای این پژوهش را در قالب بررسی نقش شاخص های ژئومورفولوژیکی در ساخت و ساز منطقه ساحلی شهرستان بابلسر به خوبی روشن می سازد. در این پژوهش، از شاخص آسیب پذیری سواحل (cvi) به منزله ی شاخص ژئومورفیک تاثیرگذار در ساخت و ساز منطقه ی ساحلی بابلسر استفاده شد. ابتدا با استفاده از داده های توپوگرافی (مدل رقومی ارتفاع ده متری) و با توجه به نوسانات تراز آب دریای خزر، محدوده ی حایل عمودی اولیه و ثانویه در اراضی شهرستان تعیین شد. محدوده ی حایل عمودی اولیه شامل اراضی است که در ارتفاع پایین تر از 24.7 متر قرار دارند و محدوده ی حایل عمودی ثانویه اراضی را با ارتفاع بین 24.7 تا 23.5 متر شامل می شود. در ادامه ی همین بحث و در داخل اراضی محدوده ی حایل عمودی اولیه و ثانویه، شاخص آسیب پذیری ساحل بر مبنای پنج پارامتر ارتفاع، شیب، لندفرم ژئومورفولوژی، کاربری اراضی و فاصله از جاده در دو زیر شاخص با منشا طبیعی و با منشا انسانی اجرا گردید. با توجه به شاخص آسیب پذیری ساحل بر مبنای متغیرهای طبیعی (ncvi)، انسانی (hcvi) و شاخص آسیب پذیری نهایی (tcvi)، بخش های وسیعی از سواحل شهرستان بابلسر (به ویژه در محدوده های شهری بابلسر و فریدونکنار) در طبقات با درجه های آسیب پذیری بالا و بسیار بالا قرار می گیرند.

Assessment of Coastal Vulnerability to Sea-Level Rise in Babolsar ownship

Abstract Coastal areas are dynamic and complex multifunction systems. A wide number of often conflicting human socioeconomic activities occur in these areas. These include urbanization, tourism and recreational activities, industrial production, energy production and delivering, port activities, shipping, and agriculture. Coastal systems are also characterized by important ecological and natural values their high habitat and biological diversity is fundamental to sustain coastal processes and provide ecosystem services which are essential also for human wellbeing. Human activities often conflict with the need to preserve natural coastal systems and their ecological processes. One of the most important applied problems in coastal geology today is determining the physical response of the coastline to sealevel rise. Predicting shoreline retreat and land loss rates is critical to planning future coastal zone management strategies and assessing biological impacts due to habitat changes or destruction. Presently, longterm (>50 years) coastal planning and decisionmaking has been done piecemeal, if at all, for the nation's shoreline. Consequently, facilities are being located and entire communities are being developed without adequate consideration of the potential costs of protecting or relocating them from sealevel riserelated erosion, flooding and storm damage. Research on major natural disasters and related technologies has become an important subject in geography and its application. The complexity analysis of the issue is possible in a system approach to theoretical and applied geography also in the integrity of physical and human geography.Due to the Caspian Sea waterlevel fluctuation in coastal zone of Babolsar which happens very quickly in decade scale, the observance of safety element will be possible in light of the integrated coastal zone management with determine of sea frontage. In this context, geography and especially geomorphology is a main basic in this kind of coastal management. Detection of sea level fluctuations causing morphological changes in the earth surface and damage to facilities, clarifies the necessary of the present research to study the role of geomorphological indices in Babolsar coast zone constructions. The Coastal Vulnerability Index (CVI) is one of the most commonly used and simple methods to assess coastal vulnerability to sea level rise, in particular due to erosion and/or inundation. The CVI provides a simple numerical basis for ranking sections of coastline in terms of their potential for change that can be used by managers to identify regions where risks may be relatively high. The CVI results can be displayed on maps to highlight regions where the factors that contribute to shoreline changes may have the greatest potential to contribute to changes to shoreline retreat.In this study, coastal vulnerability index (CVI) is used as effective geomorphic index on Babolsar coast zone constructions. In first, primary and secondary vertical frontages were detect using topographic data (digital elevation model with cell size 10meter) and Caspian Sea waterlevel fluctuations. The primary vertical frontage includes areas which have the lower height of 24.7 meters and secondary vertical frontage consists of areas which are placed between 24.7 and 23.5 meters. Following this issue, within the primary and secondary vertical frontage, coastal vulnerability index was performed based on five parameters, elevation, slope, landform, land use and distance from main road. According to the coastal vulnerability based on natural (NCVI), human (HCVI) and total vulnerability index (TCVI), large parts of the Babolsar coastal zone (especially in Fereidoonkenar and Babolsar city areas) placed in classes of high and very high vulnerability. With respect to detection of the primary (level 24.7 m) and secondary (from level 24.7 to 23.5 m) frontages in Babolsar township area, 345 and 7177 hectares of the township lands are located in the primary and secondary vertical frontages, respectively. The most area of the township land uses in primary frontage belongs to natural structures that have 153 hectares of area. Survey of lands distribution in the height of 24.7 to 23.5 m (secondary vertical frontage) shows that agriculture land use has the most extent in this area the area of this land use is 5293 hectares that equivalent to 74 percent of all lands which are located in the secondary frontage. Urban and industrial structures have 45 and 522 hectares of area in the primary and secondary frontages of Caspian Sea in Babolsar Township, respectively.