واکاوی نوسانات دمای جنوب غرب ایران بر اساس مدل‌های گردش عمومی جو و شبکه عصبی (مطالعه موردی: ایستگاههای جلگه ای و کوهپایه ای)

نوع مقاله : مقاله پژوهشی

نویسندگان

1 کارشناس ارشد / مرکز ملی خشکسالی و مدیریت بحران هواشناسی.

2 دکتری / آب و هواشناسی، دانشگاه زنجان، ایران.

چکیده

هدف از این مطالعه بررسی و تحلیل چرخه‌های و جهش‌های میانگین دمای جنوب غرب ایران بر اساس شبکه‌های عصبی و مدل‌های گردش عمومی جو تحت سناریوهای تغییر اقلیم می‌باشد. داده‌های مورداستفاده در این پژوهش شامل میانگین دمای روزانه ایستگاه‌های سینوپتیک اهواز، آبادان، دزفول، شهرکرد، لرستان و همدان داده‌های باز تحلیل NCEP و خروجی‌های مدل HadCM3 داده‌های نسل سوم مدل جهانی اقلیم تحت سناریو‌ی A2 و B2 برای دوره پایه (1991-1961 میلادی) می‌باشد. در این مطالعه به جز مراحل پیش‌بینی سایر مراحل از جمله واسنجی داده‌ها، ارزیابی و صحت سنجی مدل در نرم‌افزار متلب و برای ترسیم نقشه‌ها از سورفر بهره گرفته شده است. میزان برآورد دما بر اساس خروجی مدل‌های گردش عمومی Hadcm3 در سناریوی A2a و B2a در اکثر نواحی تا سال 2099 از روند افزایشی تا 5/1 درجه سانتی‌گراد برخوردار بوده است. نتایج حاصل از تحلیل چرخه‌های نشان داد که دما بر اساس خروجی شبکه‌های عصبی و مدل‌های گردش عمومی جو در سناریوی A2a و B2a دارای چرخه‌های کوتاه‌مدت 2 تا 4 ساله حاکم است. نتایج حاصل از آماره الکساندر سون بیانگر این است که میانگین دمای جنوب غرب ایران از سال 2050 به بعد دارای جهش معنی‌دارای می‌باشد.

کلیدواژه‌ها

موضوعات


عنوان مقاله [English]

Analysis of Temperature Fluctuations in the South West of Iran Based on General Circulation Model and Neural Network (Case Study: Plain and Mountainous Stations)

نویسندگان [English]

  • Hengameh Shiravand 1
  • Mehdi Dostkamiyan 2
1 Expert of the National Center for Drought and Meteorological Crisis Management, Iran Meteorological Organization, Tehran, Iran.
2 Ph.D. in Climatology, Zanjan University.
چکیده [English]

The purpose of this study was to analyze the cycle-by and mutations South West's average temperature based on neural networks and models of general circulation of the atmosphere under climate change scenarios is. The data used in this study consisted of an average daily temperature stations in Ahwaz, Abadan, Branch, Branch, Lorestan, Sanandaj, turpentine, Arak and Hamadan NCEP analyzes the data and outputs data model HadCM3 global climate model is the third generation under the A2 and B2 scenarios for the base period (1991-1961 AD) is. In this study, except for the prediction of other Mrajl including calibration data, assessment and validation of the model in MATLAB and have been used to map the Svrfr. The temperature is estimated based on the output of general circulation models scenario A2a and B2a Hadcm3 in most areas by the year 2099 has increased by 5.1 ° C has enjoyed. The results of the analysis showed that the temperature cycles based on the output of neural networks and models of general circulation in the scenario A2a and B2a with short cycles 2 to 4 years of ruling. The results of the test show that the average temperature on the South West Alexander Lumber Iran from 2050 onwards mutation means of extrusion.

کلیدواژه‌ها [English]

  • Atmospheric General Circulation Models
  • Neural Networks
  • Temperature
  • Fluctuation
  • Alksanderson
Abbasi F, Babaeian I, Melbosi Sh, Imari M, Goli Mokhtari L (2012)  Assessment of Iran's Climate change in the decades (2025-2100) using the exponential microscopy of Joe's general circulation models. Quarterly Journal of Research Geographical 104:17979-18005 (In Persian)
Abbasi F, Imari M (2012) Prediction and evaluation of changes in Iran's temperature and precipitation over the next decades with the MAGICC-SCENGEN model. Water and soil Journal 25(1):83-70 (In Persian)
Alexanderson H A (1986) A homogeneity test applied to precipitation data. Journal of Climate 6:661-675
Asakereh H (2009) Spectral analysis of time series of annual temperature in Tabriz. Geographical Research 93:33-50 (In Persian)
Asakereh H, Doostkamian M, Sadrafshary S (2015) Anomalies and cycles of precipitable water over Iran in recent decades. Arab J Geosci, DOI 10.1007/s12517-015-1888-2
Asakereh H, Doshkamian M, Ghaemi H (2015) Analysis of rainfall water cycle abnormalities baroque Iran. Journal of Natural Geography, University of Tehran 4:444-435 (In Persian)
Biasutti M, Yuter S, Burleyson C, Sobel A (2011) Very high resolution rainfall patterns measured by TRMM precipitation radar: Seasonal and diurnal cycles. Climate Dynamics 39(1-2): 239–258
Blasing T J (1981) Characteristic anomaly patterns of summer sea-level pressure for the Northern Hemisphere. Tellus 33:428-437
Broccli A J, Harnack RP (1981) Predictability of monthly north Pacific Sea level pressure from monthly sea surface temperature for the period 1933-1976. Monthly Weather Review 109:2107-2117
Brooks C E P, Carrthers N (1953) Handbook of statistical methods in meteorology. London, H.M.S.O, 412 p
Chathield C (2002) An introduction to time series analysis. Hassan Ali Nirmand and Abolghasem Big Nia, Ferdowsi Publications of Mashhad (In Persian)
Davis E R (1976) Predictability of sea surface temperature and pressure anomalies over the North Pacific Ocean. Journal of Physical Oceanography 6(3):249-266
Dibike Y B, Coulibaly P (2005) Hydrologic impact of climate change in the Saguenay watershed: comparison of downscaling methods and hydrologic models. Journal of Hydrology 307:145-163
Fildes R, Kourentzes N (2011) Validation and forecasting accuracy in models of climate change. International Journal of Forecasting 27(4):968-995
Garcia J A, Serrano A, Cruz Gallego M (2002) A spectral analysis of Iberian Peninsula monthly rainfall. Theoretical and Applied Climatology 71:77-95
Jones P D, Wigley T, Wright P B (1986) Global temperature variation between 1861 and 1984. Nature 322:430-432
Lana M, Martinez D, Serra C, Burguen A (2005) Periodicities and irregularities of indices describing the daily pluviometric regime of the Fabre Observatory (NE Spain) for the years 1917-1999. Theoretical and Applied Climatology 82:183-198
Lee M, Schubert S, Suarez M, Held I, Lau N, Plushy J, Kumar A, Kim H, Schema J (2007) An analysis of the warm-season diurnal cycle over the continental United States and northern Mexico in general circulation models. Journal of Hydrometeor 8(3):344-366
Mapes B, Waner T, Xu M, Negri A J (2003) Diurnal patterns of rainfall in northwestern South America. Part II: Model simulations. Monthly Weather Review 131(5):813-829
Michael S, PritchardC, Richard C, Somerville J (2009) Empirical orthogonal function analysis of the diurnal cycle of Precipitation in a multi-scale climate model. Geophysical Research Letters 36:1- 5
Mohammadi B (2015) Identification of spatial and temporal abnormalities of sea level pressure in Iran. Geographical Research 1:43-58 (In Persian)
Nesbitt S, Zipser E (2003) The diurnal cycle of rainfall and convective intensity according to three years of TRMM measurements. Journal of Climate 16:1456-1475
Pandzic K, Likso T (2009) Homogeneity of average annual air temperature time series for Croatia. Journal of Climatology 30(8):1215-1225
Rouco J, Jimenez J, Quesada L, Valero V (2000) Quality control and homogeneity of precipitation data in the southwest of Europe. Journal of Climate 14:964-978
Santer B D, Taylor K E, Wigley T M, Johns T C, Jones P D, Karoly D J, Mitchell J F B, OortA H, Penner J E, Ramaswamy V, Schwarzkopf M D, Stouffer R J, Tett S (1996) A search for human influences on the thermal structure of the atmosphere. Nature 382:39-46
Yang G, slinger J (2001) the diurnal cycle in the tropics. Review Monthly weather 129:784-801