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ارزیابی روند تغییرات کاربری زمین و تغییر اقلیم در سیمای سرزمین تالاب چغاخور با تأکید بر آثار محیطزیستی | ||
| محیط شناسی | ||
| مقاله 7، دوره 40، شماره 3، آذر 1393، صفحه 631-643 اصل مقاله (1.69 M) | ||
| نوع مقاله: مقاله پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22059/jes.2014.52210 | ||
| نویسندگان | ||
| فاطمه جهانی شکیب1؛ بهرام ملک محمدی* 2؛ احمدرضا یاوری3؛ یونس شریفی4؛ فاطمه عادلی5 | ||
| 1دانشجوی دکتری آمایش محیطزیست، دانشکدۀ شیلات و محیطزیست، دانشگاه گرگان | ||
| 2استادیار گروه برنامه‌ریزی و مدیریت محیطزیست، دانشکدۀ محیطزیست، دانشگاه تهران | ||
| 3دانشیار دانشکدۀ محیطزیست، دانشگاه تهران | ||
| 4دانشجوی ارشد RS و GIS، دانشگاه خوارزمی تهران | ||
| 5دانشجوی ارشد برنامه‌ریزی و مدیریت محیطزیست، دانشکدۀ محیطزیست، دانشگاه تهران | ||
| چکیده | ||
| تغییر کاربری زمین و اقلیم از جمله نگرانی‌‌های اصلی محیطزیست جهانی به شمار می‌‌رود. ارزیابی روند تغییرات کاربری اراضی فرایند‌‌ی است که به ایجاد درک صحیحی از نحوۀ تعامل انسان و محیطزیست منجر می‌‌شود. بین تغییر اقلیم و پوشش زمین ارتباط متقابل و پیچیده‌‌ای وجود دارد. تغییرات پوشش و کاربری زمین در اقلیم و بیوسفر جهانی آثار تجمعی و مستقیمی دارند. این مسئله در خصوص مناطق حساس و به خصوص تالاب‌‌ها به علت وابستگی عملکردهای هیدرولوژیکی و بیوژئولوژیکی آن‌ها به جریانات سطحی و زیرزمینی و موقعیت آن‌ها در سیمای سرزمین از اهمیت بیشتری برخوردار است. در این تحقیق تغییرات کاربری اراضی در سیمای سرزمین تالاب چغاخور در خصوص پارامترهای تغییر اقلیم به منظور تحلیل فشارهایی که به محیط وارد می‌‌شوند، بررسی شده است. به منظور شناسایی روند تغییرات در سیمای سرزمین تالاب چغاخور از تصاویر ماهوارۀ لندست در یک دورۀ ده ساله استفاده شد. در طبقه‌‌بندی تصاویر از روش نظارت‌‌شده و الگوریتم حداکثر احتمال استفاده شد. نتایج ضریب کاپا نشاندهندۀ دقت طبقه‌‌بندی در تصاویر سال‌‌های 2003 و 2013 به ترتیب 64 و 68 درصد است. پردازش اطلاعات در این دورۀ زمانی حاکی از افزایش سطح اراضی زراعی و ساخته‌‌‌شده به میزان 18 و 3/26 درصد و کاهش سطح آب، مرتع- جنگل و اراضی بایر به ترتیب به میزان 4/51، 2/4 و 2 درصد در سیمای سرزمین پیرامون تالاب چغاخور است. همچنین، با بررسی شاخص بارش استاندارد، روند تغییر اقلیم در محدودۀ مطالعه بررسی شد. تحلیل همزمان تغییر کاربری و اقلیم با توجه به خشکسالی طولانی‌مدت نشاندهندۀ تحمیل فشارهای زیاد و ایجاد آثار تجمعی در محیطزیست منطقه است. در صورت ادامۀ روند تحولات نامطلوب تغییر کاربری، تالاب چغاخور با خطر جبران‌ناپذیری مواجه می‌‌شود. در انتهای این مقاله راهبردهایی برای کاهش آثار محیطزیستی و خسارات خشکسالی در محدودۀ مورد مطالعه ارائه شده است. | ||
| کلیدواژه‌ها | ||
| تغییر کاربری زمین؛ تغییر اقلیم؛ تالاب چغاخور؛ سنجش از دور؛ فشارهای محیطی | ||
| عنوان مقاله [English] | ||
| Assessment of the Trends of Land Use and Climate Changes in Choghakhor Wetland Landscape Emphasizing on Environmental Impacts | ||
| نویسندگان [English] | ||
| Fatemeh Jahani Shakib1؛ Bahram Malekmohammadi2؛ Ahmad Reza Yavari3؛ Yones Sharifi4؛ Fatemeh Adeli5 | ||
| 1PhD Candiate, Land Use Planning, University of Gorgan, Gorgan, Iran | ||
| 2Assistant Professor, Graduate Faculty of Environment, University of Tehran, Tehran, Iran | ||
| 3Associate Professor, Graduate Faculty of Environment, University of Tehran, Tehran, Iran | ||
| 4MSc Student, GIS and RS, Kharazmi University of Tehran, Iran | ||
| 5MSc Student, Environmental Planning, Management and Education, University of Tehran, Tehran, Iran | ||
| چکیده [English] | ||
| Introduction Land use change and climate change are the major concerns in the global environment. Many environmental parameters affect the behavior of the earth’s climate system and its terrestrial components. Effects of land use and land cover changes have direct influences on climate changes. Now, climate change is known widely as a global health problem that has adverse impacts on natural and man-made environments. Assessment of the trend of land use changes is a process that leads to understanding the interaction between humans and the environment. This problem is more important in the sensitive areas and spatially on wetlands. The hydrological and bio-geological functions of many wetlands depend on ground and surface water ecosystems as well as its place in landscape. Therefore, the development and changes in contiguous ecosystems particularly change in water flow can cause damage and even destroy the wetland. This study aims to identify and analyze the environmental changes and pressures on Choghakhor Wetland landscape. This wetland is located between 50° 52´ to 50° 56´E and 31° 54´ to 31° 56´N in height 2270 meters above mean sea level. Choghakhor Wetland located in Zagros Mountains, with area of 1600 hectares, has freshwater resources. It is located in non-protected area in prohibited hunting zone that 2500 ha proposed for refugee site. Materials and Methods In order to assess the trends of changes in this study, land use changes and Climate change parameters were investigated in a period of ten years. Then, by environmental pressures analysis, some strategies are presented to reduce environmental impacts. In Fig. 1 stages of the research are presented and described in the following. Step 1. Use of the Landsat-7 satellite images (ETM+) with suitable timely coincidence in 2003 and 2013 for land use/cover change assessment. Step 2. Application of the maximum likelihood classification and assessment of classification accuracy with kappa and overall accuracy in ENVI 4.7. Step 3. Evaluation of the trend of climate change factors such as, the average amount of annual precipitation and temperature. Characterizing the drought degrees with the Standardized Precipitation Index (SPI) by data of effective stations in the study area. Step 4. Analysis of the environmental changes and pressures by considering the results of climatic trend and land use changes. Step 5. Presenting management strategies to reduce environmental impacts of land use change and climate change on wetland landscape and its surrounding environment. Results and Discussion The aforementioned steps were performed for landscape of Choghakhor Wetland. Detecting the land use and land cover changes in 2003 and 2013 indicate five distinct classes, including: pasture and forest (cultivated and non-cultivated), bare land, man-made (settlements and roads) and water (snow and water) results (Fig. 2 and 3). Fig. 1. Process of land use/cover and climate changes assessment in this study The results of image classification and remote sensing process in 2003 and 2013 are presented in Table 1. Data processing in this period represent that increase in area of cultivated and man-made lands are 18 and 26.3 percent and decrease in water body, pasture and forest and bare lands are 51.4, 4.2, and 2 percent. The results of the classification accuracy measurement were estimated on 89% and 64% in 2003 and 93% and 68% in 2013 for overall accuracy and Kappa coefficient, respectively. The most effective meteorology data (Overgan Station records) in wetland area in 2012 illustrated that the amount of standard precipitation index is -0.89, which confirmed occurrence of a drought. The probability of drought occurrence is predicted by 41.7% which is in accordance with previous year records. The investigation on climatic change elements showed an increasing trend in average annual temperature with a sharp and irregular fluctuation of rainfall in the recent years. Conclusions Investigation on the trend of thirty-year records of climatic elements and the obtained results by satellite monitoring of landscape illustrated 50% decline in water resources amount. Declining rainfalls, rise of a few degrees in the annual average temperatures in the region, and the recent drought, as confirmed by the remote sensing processing result, show water shortage is in expended trend. Despite, land use changes played an important role in the situation during water shortage period. The agriculture development has imposed an enormous environmental pressure by excessive consumption of water, fertilizers and pesticides. Then, drying of springs, reduction of groundwater level, increase in organic and inorganic contaminants, and finally enrichment and declining of dissolved oxygen in wetlands is a description of the occurred situation due to cascading effects of land use change simultaneously with the climate change which could be effective on ecosystem functions of wetland, such as water purification and regulation. Fig. 2. Classified image of study area in 2003 Fig. 3. Classified image of study area in 2013 Table 1. Results of image classification Relative changes (growth rate) 2013 2003 Land cover classes Area (km2) Area (%) Area (km2) Area (%) Area (km2) Area (%) -16.22 -4.2 372.53 19.7 388.98 20.6 Pasture and forest 77.51 18 508.68 26.9 430.77 22.8 Agriculture -69.6 -2 829.01 43.84 898.98 47.5 Barren land 32.94 26.3 157.90 8.35 125.00 6.6 Man-made land -24.33 -51.24 22.88 1.21 47.28 2.5 Water - - 1891 100 1891 100 Total Increase in man-made areas in terms of urban settlements and tourist areas indicated that some pressures have led to decline in permeable surfaces and groundwater recharge, habitat loss, and reduction in control ability of hazardous pollution and detoxification could raise some disorders in exposition of this wetland ecosystem functions. While increasing pressure is occurred, climate change set regional water resources in critical condition and land use change add an irrational severity by such effects. According to adverse changes of Choghakhor wetland landscape, if the current situation trend continues, the wetland will be faced with some irreparable threats. In such a situation, it seems necessary to ponder to proper programs for logically exit from current crisis and preventing the environmental diminish. Leaning the performed analysis, the strategies to reduce environmental impacts and mitigation of drought in the study area are provided as follows: · Developing the conservation plan and combining them with the integrated wetland management plan in National Development Plans in order to preserve wetland ecosystem functions, · Modifying the cultivation methods, reducing the consumption of chemical fertilizers and pesticides and awareness about the proper way in their use, using the efficient irrigation systems, licensing the drilling and operation wells with accurate specialized measurements, and awareness about their environmental effects, · Identifying the natural drainage paths and leaving open the permeable parts in residential areas, in order to reduce the probability of flooding in cities and preservation of hydrologic balance in the drainage basin, · Dealing with drought losses and declining its effects by applying strategies such as optimum selection and land use change, modifying the culture alternation system, and groundwater levels control. | ||
| کلیدواژه‌ها [English] | ||
| Choghakhor Wetland, climate change, environmental pressures, land use change, remote sensing | ||
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