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پهنهبندی روزهای شرجی در نیمه جنوبی ایران
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نویسنده
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محمودی پیمان ,طاوسی تقی ,دانشمند حجت اله ,شباب مقدم عبدالمجید
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منبع
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تحليل فضايي مخاطرات محيطي - 1393 - دوره : 1 - شماره : 2 - صفحه:47 -63
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چکیده
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در حاشیه دریاهای گرم، بر اثر افزایش دما و رطوبت نسبی پدیده ی اقلیمی شرجی رخ می دهد که سبب سلب آسایش و بروز مشکلاتی در زندگی روزمره ی انسان می شود. در این مطالعه، طبقه بندی روزهای شرجی در نیمه ی جنوبی ایران بررسی شد و پهنه بندی ویژگی های آماری روزهای شرجی با استفاده از سامانه ی اطلاعات جغرافیایی صورت گرفت. برای دستیابی به این اهداف، داده های ساعتی و روزانه فشار جزئی بخار آب برای یک دوره ی 15 ساله (2009- 1995) مربوط به 13 ایستگاه منتخب از سازمان هواشناسی کشور اخذ گردید. سپس، روزهای شرجی براساس آستانه ی فشار جزئی بخار آب 8/18 هکتوپاسکال استخراج و در قالب هشت طبقه ی جداگانه تقسیم شد و پهنه بندی ویژگی های آماری روزهای شرجی با روش میانیابی کریجینگ صورت گرفت. نتایج این مطالعه نشان داد که بیشترین روزهای شرجی در مقیاس ماهانه در دو ماه ژوئن و ژولای و کمترین آن در ماه ژانویه اتفاق می افتد. در مقیاس فصلی، نیز بیشترین تعداد روزهای شرجی متعلق به فصل تابستان و کمترین آن مربوط به فصل زمستان است. از لحاظ مکانی نیز جنوب شرق ایران در مقایسه با جنوب غرب بیشترین تعداد روزهای شرجی را دارد. طبقه بندی روزهای شرجی نیز نشان داد که ایستگاه چابهار با بیشترین تعداد روزهای شرجی طبقه ی هشت (کل 24 ساعت شبانه روز دارای شرایط شرجی) حادترین ایستگاه در بین ایستگاه های مورد مطالعه بوده و ایستگاه هایی همچون کرمان، زاهدان و شیراز با داشتن کمترین روز شرجی طبقه ی هشت بهترین شرایط را دارا بوده اند.
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کلیدواژه
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شرجی، فشار بخار آب، کریجینگ، جنوب ایران، gis
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آدرس
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دانشگاه سیستان و بلوچستان, ایران, دانشگاه سیستان و بلوچستان, ایران, دانشگاه سیستان و بلوچستان, ایران, دانشگاه سیستان و بلوچستان, ایران
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Spatial Classification of the Sultry Days in the Southern Half of Iran
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Authors
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Mahmoudi Peyman ,Tavosi Taghi ,Hojjat Daneshmand ,Shabab Moghadam Abdolmajid
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Abstract
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Hot, humid weather causes to the sultry feel. Sultry condition is usually accompanied with loss of physical ability and human respiratory and it has an adverse effect on peoples who have circulatory or other heart problems and this feeling is more than others. Sultry feel is a feeling like any other sensitive reflections of mental state. And this state apparently can rsquo;t be measured by special instruments. With this description, there are a lot of efforts has been done to identify this phenomenon by meteorologists and climatologists. And a series of psychological climate tests show that we can examine the creation and incidence of this sense based on empirical studies as a scientific and objective attitude. Therefore, this study aims to classify the sultry days in the southern half of Iran based on sultry continuous hours. And the obtained results are presented as a form of zoning maps. The studied zone in this research is selected stations in the southern half of the country located in the province of Sistan Baluchestan, Kerman, Hormozgan, Fars, Bushehr and Khuzestan. This area is located between two latitude 25 and 35 north and length of 47 to 63 east degrees. To achieve this goal, hourly partial pressure of water vapor of 13 selected stations were obtained for a period of 15 years (19952009) from Meteorological agency. After obtaining data and creating the database, to separate sultry conditions from nonsultry conditions, threshold of partial pressure of water vapor of Scharlou which was equivalent to 8.18 Hpa were used. Based on these data, the hours and days that the partial pressure of water vapor was equal or greater than 8.18 hpa will have sultry conditions and otherwise, they have nonsultry conditions. Then, based on this threshold, sultry days were divided into eight categories. The basis of this classification is that if in a particular day among eight branches of observation, one station, only in one observation record a pressure equal to or greater than 8.18 hpa was observed, it will be placed in first class and if only two observed records a value equal or greater than defined value, it will be placed in second catagory and finally, if all eight observations amounts equal to or greater than 8.18 had been recorded, it will be placed in eight class. After placing the sultry days in one of eight branches of classes, longterm averages of monthly, quarterly, quarterly and annual were calculated and mapped. Based on defined thresholds, sultry days were separated from nonsultry days, then sultry days were extracted and it was placed in first to eighth classes. The results of this classification showed that on monthly scale, January has the fewest sultry days in twelve months of the year. In this month, only two stations of Chabahar and Bandar Abbas had the sultry days of eighth classes. It means that 24 hours, they were in sultry conditions. Other stations that have a sultry day in this month, often their sultry days are from first to fourth classes and it means that they had maximum 3 to 12 hours of sultry conditions during the day. Most sultry days can be seen in two June and July months. So, in these two months, all studied stations have at least one sultry day,Specially in three stations of Chabahar, Bandar Abbas and Bushehr. And all 61 days, they have sultry conditions. In terms of classification of sultry days, all 61 days of Chabarhar station are part of sultry days of eighth class. In two stations of Bandar Abbas and Bushehr, except few days that are from sixth and seventh classes, other days are from eightth class, other stations experienced one of the eightth classes of sultry days with different ratios. , and at the seasonal scale, winter has the lowest days of sultry and summer has the most days of sultry days. In term of classification of sultry days in seasonal scale, there are conditions as monthly scale. The interesting point in summer season is that sultry days on two stations of Zabul (35 days) and Iranshahr (51 days) are considered due to their Geographical locations. In Zabul station, the reason of these sultry days can be due to the neighborhood of this station with Hamoon Lake. But it should be mentioned about Iranshahr stationthat the reason of its sultry condition is entrance of monsoon low pressure and moisture transfer by the system on the southeast of Iran an especially Iranshahr. On an annual basis, it was also observed that always in south east of Iran (Especially Chabahar station), the number of sultry days is much more than south west of Iran, also occurring sultry days with eighth, seventh and sixth classes in this zone is so different from southwest of Iran. The reason of these differences in number of sultry days and sultry classes related to the latitude of south east of Iran which is lower that south west and in other words, we can say that climate of south East of Iran is more similar to tropical climate than subtropical climate.
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Keywords
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Sultry ,Vapour Pressure ,Kriging ,GIS ,the southern half of Iran. ,GIS
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