تحقیقات کاربردی علوم جغرافیایی

تحقیقات کاربردی علوم جغرافیایی

استخراج و تحلیل الگوهای سینوپتیک و پایش منشاء و مسیر عبور توفان‌های گردوغبار مطالعه موردی: استان اردبیل، ایران

نویسندگان
بهروز سبحانی 1
مهدی عالی جهان 2
1 عضو هیات علمی گروه جغرافیای طبیعی، دانشگاه محقق اردبیلی، اردبیل، ایران
2 دانشگاه محقق اردبیلی، اردبیل، ایران
10.61186/jgs.24.73.137
چکیده


امروزه ریزگردها و توفان­های گردوغبار به یکی از مسائل و مشکلات مهم کشور ایران و سایر مناطق جهان تبدیل شده است. این پژوهش درصدد استخراج الگوهای سینوپتیک توفان­های گردوغبار استان اردبیل و پایش و منشأیابی مکان برخواست آن به انجام رسیده است. بازه زمانی موردمطالعه 34 ساله (2013 – 1979) می­باشد. از داده­های ایستگاه­های سینوپتیک استان اردبیل و داده‌های سطوح فوقانی جو سازمان ناسا جهت انجام پژوهش پیش­رو استفاده به عمل آمد. جهت نیل به اهداف پژوهش از روش­های محیطی به گردشی، خوشه­بندی سلسله مراتبی و مدل HYSPLIT بهره گرفته شد. با توجه به نتایج حاصل شده 3 الگوی ارتفاع ژئوپتانسیل تراز 500 هکتوپاسکال شناسایی گردید. الگوی شماره 1 و 2 تقریباً مشابه به یکدیگر بوده و بیانگر رخ­داد ناوه عمیق است که از اروپای مرکزی شکل‌گرفته و تا نیمه­های دریای سرخ امتداد داشته است. در الگوهای یادشده منطقه مورد مطالعه در شرق ناوه مذکور قرار داشته است. الگوی سوم بیانگر رخ­داد بلوکینگ بریده کم­فشار بر فراز دریای سیاه و مناطق هم‌جوار و قرارگیری استان اردبیل در شرق ناوه متشکل از بلوکینگ می­باشد. منشأ ریزگردها در الگوهای 1 و 2 نواحی شرقی کشور عراق و غرب کشور ایران و در الگوی شماره 3 در ارتفاع 500 هکتوپاسکال نواحی مرکزی کشور عراق و در ارتفاعات 850 و 1000 هکتوپاسکال نواحی مرکزی کشور سوریه می­باشد.

واژگان کلیدی: توفان گردوغبار؛ استخراج الگو؛ تحلیل سینوپتیک؛ مدل HYSPLIT؛ استان اردبیل




کلیدواژه‌ها
توفان گردوغبار
استخراج الگو
تحلیل سینوپتیک
مدل HYSPLIT
استان اردبیل

عنوان مقاله English

The extraction of synoptic patterns, and monitoring the origin and pathway of dust storms; Case study: Ardabil province, Iran

نویسندگان English

Behrouz Sobhani 1
Mehdi Aalijahan 2
1 Department of Natural Geography, University of Mohaghegh Ardabili: Ardabil, Iran
2 University of Mohaghegh Ardabili: Ardabil, Iran
چکیده English



Today, fine dust and dust storms have become one of the important issues and problems of Iran and other regions of the world. This study is conducted to identify synoptic patterns of the dust storms in Ardabil Province (Iran) and monitor the origin and pathway of its places. The studied period is 34 years (1979-2013). The data used in this work are from synoptic stations of Ardabil province and the NASA’s upper atmosphere database. To achieve the goals of the study, the Environment to Circulation, Hierarchical Clustering Methods, and HYSPLIT model were used. According to the results, three patterns of geopotential height at 500 hPa levels were identified. Pattern No. 1 and 2 are almost similar to each other and represent the occurrence of a deep trough that formed from Central Europe and extended to the middle of the Red Sea. Based on these patterns, the study area is located in the East of this trough. The third pattern represents the occurrence of cut-of-low pressure blocking over the Black Sea and adjacent areas and placement of Ardabil province in the East trough of the formed blocking. The origin of dust in patterns 1 and 2 is the Eastern regions of Iraq and West of Iran while in pattern 3 is at 500 hPa level of the central areas of Iraq and at pressure levels of 850 and 1000 hPa of the central regions of Syria.

Keywords: Dust storm, Pattern extraction, synoptic analyses, HYSPLIT model, Ardabil province



کلیدواژه‌ها English

Dust storm
Pattern extraction
synoptic analyses
HYSPLIT model
Ardabil province
1. Azizi. Gh, Shamsipour A, Miri M, Safar rad T (2012) synoptic – Statistical analysis of dust phenomena in half western of Iran. J of Envir Stud (in Persian) 38(3): 134-123.
2. Ali Abadi K, AsadiZanganeh MA, DadashiRoudbari A (2015) assessment and monitoring dust storms using remote sensing methods. J of relief and rescue (in Persian) 7(1): 20-1.
3. Dagsson PW, Olafur A, Haraldur O (2013) Long-term frequency and characteristics of dust storm events in Northeast Iceland (1949e2011). AtmosphEnvir 77: 117-127.
4. Dodangeh E, Shao Y, Daghestani M (2012) L-Moments and fuzzy cluster analysis of dust storm frequencies in Iran. Aeolian Res 5: 91–99.
5. Draxler R, Rolph G (2011) HYSPLIT (HYbrid Single-Particle Lagrangian Integrated Trajectory). NOAA Air Resources Laboratory, Silver Spring, Maryland. Model access via NOAA ARL READY Website.
6. Draxler RR, Hess GD (1998) an overview of the HYSPLIT_4 modelling system for trajectories. Austrameteo m 47(4): 295-308.
7. Draxler RR, Rolph GD (2003) HYSPLIT (HYbrid Single-Particle Lagrangian Integrated Trajectory) model access via NOAA ARL READY website (http://www. arl. noaa. gov/ready/hysplit4. html). NOAA Air Resources Laboratory Silver Spring.
8. Flaounas E, Kotroni V, Lagouvardos K, Kazadzis S, Gkikas A, Hatzianastassiou N (2015) Cyclone contribution to dust transport over the Mediterranean region. AtmosScie Let 16(4): 473-478.
9. Falahgalhari GA (2014) Fundamentals of Meteorology. Hakim Sabzevari University Press, Mashhad, Iran.
10. Gao T, Han J, Wang Y, Pei H, Lu Sh (2011) Impacts of climate abnormality on remarkable dust storm increase of the Hunshdak Sandy Lands in northern China during 2001–2008. MeteoApplic 19(3): 265-278.
11. Goudie AS, Middleton NJ (2006) Desert Dust in the Global System. Springer.
12. Goudie AS (2009) Dust storms: Recent developments. J of EnvirManag 90: 89–94.
13. Han Y, Dai X, Fang X, Chen Y, Kang F (2008) Dust aerosols: a possible accelerant for an increasingly arid climate in North China. J Arid Envir 72: 1476–1489.
14. Hahnenberger M, Kathleen N (2012) Meteorological characteristics of dust storm events in the eastern Great Basin of Utah, U.S.A. AtmosEnvir 60: 601- 612.
15. Han Z, Ueda H, Matsuda K, Zhang R, Arao K, Kanai Y, Hasome H (2004) Model study on particle size segregation and deposition during Asian dust events in March 2002. J of GeophyResear 109: 1-22.
16. Hervada-Salaa C, Jarauta-Bragulat E (2004) A program to perform Ward’s clustering method on several regionalized variables. Comput&Geosc 30: 881–886.
17. Indoitu RL, Orlovsky N (2012) ust storms in Central Asia: Spatial and temporal variations. J of Arid Envir 85: 62-70.
18. John JQu, Kafatos M (2006) Asian dust storm monitoring combining Terra and Aqua MODIS SRB measurements. Geosci and Remo Sens lette 3(4): 484-486.
19. Kinoshita K, Ning W, Gang Z, Tupper A, Iino N, Hamada S, Tsuchida S (2005) Long-Term Observation of Asian Dust Inchangchun and Kagoshima. Wat Air and Soil PolluFoc 5: 89–100.
20. Khosravi M, Kavoosi T, reeispoor K (2010) synoptic analysis of dust systems in Khuzestan province. J of Geogra and Develo (in Persian) 20: 97-118.
21. Li J, Zhiwei H, Renjian Z (2011) Model study of atmospheric particulates during dust storm period in March 2010 over East Asia. AtmosEnvir 45: 3954 -3964.
22. Liu CM, Zheng-An Q, Ming-Chin W (2004) A Composite Study of the synoptic Differences between Major and Minor Dust Storm Springs over the China-Mongolia Areas. TAO 15(5) 999-1018.
23. Lashkari H, Keykhosravi G (2008) synoptic – Statistical analysis of Khorasan Razavi dust storms in (1993 – 2005) period of time. J of PhysiGeograp rese 65: 17 33.
24. McGowan H, Clark A (2008) Identification of dust transport pathways from Lake Eyre, Australia using Hysplit. AtmosEnvir 42(29): 6915-6925.
25. McTainsh GH. Pitblado JR (1987) Dust storm and related phenomena measured from meteorological record in Australia. Ear Sur Pro Land 12: 415-424.
26. Mohammadi F, kamali S, Eskandari M (2015) Tracing Dust Sources in Different Atmosphere Levels of Tehran Using Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) Model. Geograp and envirhaz (in Persian) 4(16): 39-54.
27. Masoudian SA (1388) Iran’s Coastal Areas, Geog and Devel 13, 91-79.
28. Masoudian SA, Atayi H (2005) Identification of Iran’s Casual Seasons by Cluster Analysis. Resea J of Isfahan Univ 1, 12-1.
29. Natsagdorj L, Jugder D, Chung YS (2003) Analysis of dust storms observed in Mongolia during 1937–1999. AtmosEnvir 37: 1401–1411.
30. Nickovic S, Dobricic S (1996) a model for long-range transport of desert dust. Mon. Wea. Rev 124: 2537–2544.
31. Rashedi E, Mirzaei A. Rahmati M (2015) an information theoretic approach to hierarchical clustering combination. Neuro 148: 487–497.
32. Rasouli A, Sari Sarraf B, Mohammadi GH (2010) Trend Analysis of dust Climatic phenomena occurrence In the West of the Iran country in 55 years. J of PhysiGeograp (in Persian) 9: 15-28.
33. Stunder BJB (1997) NCEP Model Output–FNL ARCHIVE DATA, TD-6141. Prepared for National Climatic Data Center (NCDC). This document and archive grid domain maps are also available at http://www. arl. noaa. gov/ss/transport/archives. html.
34. Tavoosi T, Khosravi M, Reispour K (2010) synoptic analysis of Khuzestan province dusts. Geog and Develo 20: 97-118.
35. Wang F, Chen DS, Cheng SY, Li JB, Li MJ, Ren ZH (2010) Identification of regional atmospheric PM 10 transport pathways using HYSPLIT, MM5-CMAQ and synoptic pressure pattern analysis. Envir Mode & Soft 25(8): 927-934.
36. Xu J (2006) Sand-dust storms in and around the Ordos Plateau of China as influenced by land use change and desertification. Catena 65: 279-284.
37. Zeinali B, Asghari S (2016) Mapping and monitoring of dust storms in Iran by fuzzy clustering and remote sensing techniques. Arab J of Geos 9(9): 1-10.
38. Zeinali B (2013) identification and monitoring of dust storms index using MODIS and AVHRR sensors. Physical Geography - Climatology PhD thesis, Tabriz UniDepar of PhysiGeograp Tabriz Iran.