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   اثر گسترش شهر بر شرایط آب و هوایی ایستگاه سینوپتیک مهرآباد  
   
نویسنده رنجبر فیروز ,مقبل معصومه
منبع پژوهش هاي جغرافياي طبيعي - 1398 - دوره : 51 - شماره : 2 - صفحه:245 -262
چکیده    تحقیق حاضر با هدف بررسی اثر گسترش شهرنشینی و تغییر کاربری شهر تهران بر شرایط اقلیمی ایستگاه سینوپتیک مهرآباد انجام شده است. برای اجرای این کار، داده‏های روزانه بارش، بیشینه دما، و کمینه دما طی دوره 1966-2016 از سازمان هواشناسی کشور اخذ شد. پس از کنترل کیفی داده‏ها، برای بررسی شرایط اقلیمی، نخست از آزمون من‏– کندال استفاده شد و در مرحله بعد با استفاده از نرم‏افزار rclimdex تغییرات و روند 23 شاخص حدی اقلیمی، متشکل از شاخص‏های دوره‏ای، مطلق، مبتنی بر صدک، و آستانه‏ای متغیرهای دما و بارش روزانه استخراج شد. نتایج نشان داد همگام با افزایش جمعیت و رشد فیزیکی شهر تهران و قرارگیری ایستگاه سینوپتیک مهرآباد در محدوده شهری، هر دو پارامتر دمای کمینه و بیشینه در طی دوره آماری 1966-2016 از روند افزایشی برخوردار است؛ به‏طوری‏که دمای کمینه ایستگاه مهرآباد در دوره 1966-1975 حدود 10.9 درجه سانتی‏گراد بوده و در دوره 2005-2015 به حدود 13.7 درجه سانتی‏گراد افزایش یافته است. از نظر ‏شاخص‏های حدی، افزایشی قابل ملاحظه در ‏شاخص‏های حدی سرد و افزایش در ‏شاخص‏های حدی گرم وجود دارد. شاخص روزهای سرد، شب‏‏های سرد، روزهای همراهِ یخبندان، روزهای یخی با کاهش مواجه‏اند.
کلیدواژه بارش، دما، ‏تهران، شاخص‏های حدی، گسترش شهر
آدرس دانشگاه صنعتی مالک اشتر, ایران, دانشگاه تهران, دانشکده جغرافیا, ایران
پست الکترونیکی moghbel@ut.ac.ir
 
   The Effect of Urban Expansion on Climate Conditions of Mehrabad Synoptic Station  
   
Authors Ranjbar Firuz ,Moghbel Masoumeh
Abstract    IntroductionThe UN Population Demographics in 2014 has indicated that there is a reversal of the demographic trend of urban and rural areas, with the world’s largest population (54%) living in urban areas. This trend is increasing, while by the year 1990, a small population lived in the cities. This undocumented development leads to major changes in the environment including a reduction in natural surfaces and the replacement of them by artificial and human land covers. Urban areas are often identified with impenetrable and constructional surfaces that often have a negative impact on ecosystems. Urbanization changed the natural landscape into built areas of completely different physical characteristics. The transformation in surface land covers has an important effect on energy balance and local climate. As a result, urban climate is formed from the climatic factors of the city that are changing with the impact of urban factors over time.Materials and methodsIn order to study the effects of urban expansion on climatic condition of Tehran, we extracted daily precipitation, minimum and maximum temperature data from Mehrabad synoptic station during a period of 50 statistical periods (19662016). Different methods and tests have been used to analyze trends and changes in climatic conditions. The trend in the cluster data series was studied using the MannKendall test. The MannKendall test is a baserating nonparametric test for trend analysis which was first used by Mann for public applications in 1945 and revised by Kendall in 1948 and presented in a different way. Then, RClimDex software was used to extract the process of extreme weather indicators. This software has been developed by Zheng and Yang (2004 & 2005) at the Canadian Weather Service’s Climate Research Branch. In the present study, 23 indicators of ETCCDI indicators were used using RClimDex. The indicators are divided into five groups based on percentiles, periodic indicators, absolute indices, threshold indicators and other indices such as temperature change overnight.Results and discussion Based on nongraphical MannKendall Test, both temperature parameters (minimum and maximum temperatures) have an increasing trend during the 19662016 period, which is more evident at the minimum temperature; while precipitation in the same period of time has been a slight downward trend. Based on the MannKendall graphical test, when there is a significant trend in data, the lines ui and u’i interrupt each other. The results of the ManKendall test show that the increase in minimum temperature is higher than the maximum temperature. Moreover, during 19761986, Tehran experienced rapid physical growth and this period is coincided with an increase in temperature, which continued until the end of the period. Based on the analysis of the temperature extremes index, the cold day indices (TX10p) are facing a downward slope. On the other hand, the Hot Days Index (TX90p) faces an upward slope in the period of 19662016. In fact, it can be concluded that during the study period, the percentage of hot days in the Mehrabad station has an increasing trend and that of cold days has a decreasing trend. These results are consistent with the studies of Rahimzadeh et al. (2011), Niw et al. (2006) and Brown et al., 2010, on the trend of the temperature range of the night temperature.ConclusionIn recent years, the spread of cities and their growth has had a great impact on the environmental conditions in different parts of the world. In the meantime, some cities have been experiencing rapid and significant growth. Urban change has today had widespread effects on urban climatic conditions. One of these effects is the change in the temperature of the cities (formation of the UHI) and the increase in night temperatures. The present research was carried out to investigate the effects of the expansion of Tehran on the climatic conditions of the Mehrabad synoptic station. The study of the climate conditions of the Mehrabad station shows that during the study period, the air temperature of the Mehrabad station has undergone a change. Thus, the minimum and maximum temperature is facing an increasing trend, which is, of course, more severe at the minimum temperature. The average minimum temperature of the Mehrabad station during the 199675 period was about 10.9 ° C, reaching about 13.7 ° C in the period 20052015. On the other hand, the average maximum temperature during the 19751996 periods was about 5.5 ° C 22 ° C. In the period 20152005, it reached about 23.6 ° C. In addition to temperature averages, temperature indices have also changed significantly at Mehrabad station so that cold and warm extreme events have decreasing and increasing trends, respectively.
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