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داده‌کاوی گردشهای جوّی برای بررسی نقش الگوهای بندالی در ایجاد بارشهای شمالشرق ایران | ||
| پژوهش های جغرافیای طبیعی | ||
| مقاله 7، دوره 44، شماره 3، آذر 1391، صفحه 109-126 اصل مقاله (1.23 M) | ||
| شناسه دیجیتال (DOI): 10.22059/jphgr.2012.29217 | ||
| نویسندگان | ||
| قاسم عزیزی1؛ سید امید نبوی2؛ مرتضی میری3 | ||
| 1دانشیار دانشکدهی جغرافیا، دانشگاه تهران | ||
| 2کارشناس ارشد اقلیمشناسی، دانشکدهی جغرافیا، دانشگاه تهران | ||
| 3دانشجوی کارشناسی ارشد اقلیمشناسی، دانشکدهی جغرافیا، دانشگاه تهران | ||
| چکیده | ||
| بررسی نقش الگوی بندالی در وقوع بارشهای شمالشرق ایران، هدف اصلی مطالعهی پیش رو است. برای این کار از میان داده‌های روزانه‌ی بارش 20 ایستگاه همدیدی، اقلیمی و باران‌سنجی منطقهی مورد مطالعه، رخدادهای بارشی با شدّت متوسّط و زیاد بر اساس معیار تعیین شده، بین دوره‌ی زمانی 11 ساله (1995- 2005) شناسایی و ویژگی‌های آنها در مقیاس‌های زمانی متفاوت بررسی شد. در ادامه با استفاده از داده‌های ارتفاع ژئوپتانسیل سطح 500 هکتوپاسکال، گردشهای جوّی در دو مقیاس همدید و نیمکره‌ای، بهترتیب با دو روش چشمی و کمّی شناسایی و ویژگی‌های آماری آنها با استفاده از روش‌های آماری استخراج و تجزیه و تحلیل شدند. واکاوی آماری گردشهای جوّی در مقیاس همدید، بازگو کنندهی این واقعیّت است که (مطابق انتظار)، تنها الگوی همدیدی همزمان با بارشهای شمالشرق کشور ـ خواه شدید و خواه متوسّط ـ الگوی ناوه بادهای غربی است. نتایج حاصل از تفکیک الگوی بندالی از گردشهای جوّی دیگر بر اساس روش کمّی مربوطه و مطالعهی ویژگی‌های آماری آنها نیز، بر نقش انکارنکردنی الگوهای بندالی در ایجاد بیش از نیمی از (کمابیش 65 درصد) رخدادهای بارشی منطقه (شامل بارش متوسّط و شدید) از طریق تأثیر در ایجاد و مکانگزینی الگوی همدیدی یادشده تأکید دارد. از نظر توزیع مکانی، الگوی بندالی اطلس و غرب اروپا دارای بیشترین فراوانی در همزمانی با بارشهای شدید و متوسّط است. از نظر توزیع زمانی نیز، عمده فعّالیّت الگوهای بندالی، به بارش شدید در اواخر دوره‌ی سرد سال و فصل بهار منجر شده، در حالیکه الگوهای بندالی همزمان با بارش متوسّط بهطور عمده در دوره‌ی سرد سال رخ می‌دهند. | ||
| کلیدواژه‌ها | ||
| الگوی ناوه؛ بارشهای شدید و متوسّط؛ داده‌کاوی؛ شاخص بندالی؛ گردشهای جوّی | ||
| عنوان مقاله [English] | ||
| Investigation of Blocking Pattern Role on Precipitation in North East of Iran Using Data Mining Analysis | ||
| نویسندگان [English] | ||
| Ghasem Azizi1؛ S.O Nabavy2؛ M Miri3 | ||
| چکیده [English] | ||
| Extended Abstract Introduction The importance of atmospheric precipitation in human life turns it into one of the most common subject of various studies. Minimal changes in the amount and intensity of precipitation would face the communities’ social and economic infrastructures to serious problems. Even though these studies have yielded very precious results but in most cases atmospheric precipitation patterns were analyzed not only at a limited regional scales but also only for heavy precipitation (high intensity precipitation). However, synoptic weather patterns, creating precipitation or other atmospheric phenomena, are formed within hemisphere-scale pattern. Among them, blocking pattern is one of the most important large scale circulations. As sometimes blockings embrace a wide range of western Atlantic coast to the Far East. Undoubtedly the identification of these patterns naturally requires a study area much wider than synoptic scope. In addition, understanding of the extreme natural phenomenon like heavy precipitation requires the knowledge of their normal modes. Therefore, this study aims at examination of hemispheric and synoptic circulations along with both heavy (high) and normal (moderate) precipitation (intensities) in Khorasan Razavi and Khorasan Shomali provinces. Investigation of relationship between precipitation amount in Khorasan Razavi and Khorasan Shomali provinces and blocking pattern is the main purpose of this study. Methodology To achieve considered goals, statistical data of daily precipitation were obtained from 20 stations located in the mentioned regions. Given the amount of precipitation is different in each area, the intensity of the precipitation cannot be determined based on a fixed number and it should be calculated according to its average quantity in given place. Hence, precipitation rate between ±0.2 and above 7 were considered respectively as normal and heavy precipitation in a normalized scores scale. Besides taking into account aforementioned intensities in at least one station, precipitation rates greater than 1 and 0.1 mm in at least 50% of the stations are also required for choosing heavy and normal cases. As a result of precipitation data processes, 46 and 92 days were identified with normal intensity respectively. Results and Discussion Having determined precipitation cases, atmospheric circulations were analyzed for two synoptic and hemispheric scales. Geopotential height at 500 level extracted from US atmospheric database called National Centers for Environmental prediction ( NCEP ) was used to identify synoptic and hemispheric patterns . Similarly the study has two kinds of methodologies . Synoptic patterns were analyzed by manual ( subjective ) method whereas hemispheric circulations were investigated through quantitative blocking index to determine whether block has happened within large scale circulations. Manual analysis indicates that the only synoptic circulation, creating precipitationwhether heavy and normal quantities, is trough pattern. This result is completely expectable for places like north east of Iran. Because in such regions far from massive water bodies, synoptic-scale dynamic processes play a big role in formation of rainfall. Through this pattern, the study area is located under trough front or upper convergence and surface divergence section. After determination of predominant precipitation synoptic pattern, the main part of study is put forward. In this step, the role of hemispheric blocking pattern on creation and location of trough pattern was investigated based on blocking index. Conclusion According to results, 67% of high intensities and 64% of normal cases are formed (affected) by blocking patterns. This condition not only shows very important role of these circulation in formation of precipitation in north east of Iran but also it would explicate that most precipitation cases in the mentioned areas are prepared by an unusual atmospheric pattern called blocking. The characteristics of block pattern, being unusual and infrequent, justify high annual fluctuations in Khorasan Razavi and KhorasanShomali’s precipitation. Spatial distribution blocking patterns indicates that Atlantic and Western is the main host for most blocking cases during both heavy and normal intensities. In addition to spatial distribution of the blocking pattern, its model is also significant; Omega block has the relative frequency of 74/2 and 72.9 simultaneous with high and normal intensities respectively. Based on block pattern temporal regime, late cold period of year and spring has the highest frequency of blocking pattern along with heavy precipitation, whereas blocking pattern creating normal precipitation takes place mostly during wintertime. Keywords: Heavy And Normal Precipitation, Synoptic Analysis, Trough Pattern, Blocking Index. | ||
| کلیدواژه‌ها [English] | ||
| Blocking Index, Heavy And Normal Precipitation, synoptic analysis, Trough Pattern | ||
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