]1[. خسروی، محمود؛ پودینه، محمدرضا (1389). تحلیلی بر تأثیرات اقلیمی سیکلون حارهای گونو (خرداد 1386) بر جنوب شرق ایران، پژوهشهای جغرافیای طبیعی، شمارة 72: 72-53.
]2[. قویدل رحیمی، یوسف (1390). نگاشت و تحلیل همگرایی جریان رطوبت جو طی بارش فوق سنگین ناشی از توفان حارهای فت در سواحل چابهار، مدرس علوم انسانی – برنامهریزی و آمایش فضا، دورۀ پانزدهم، شمارة 2: 118-101.
]3[. لشکری، حسن؛ کیخسروی، قاسم (1389). تحلیل سینوپتیکی توفان گونو و اثرات آن بر جنوب شرق ایران، مجلة جغرافیا و برنامهریزی محیطی، سال 21، شمارة پیاپی 39، شمارة 3: 20–1.
]4[. مقیمی، ابراهیم (1393). دانش مخاطرات برای زندگی با کیفیت بهتر و محیط پایدارتر، تهران: انتشارات دانشگاه تهران.
[5]. Bhaskaran, P. K., et al. (2013). "Performance and validation of a coupled parallel ADCIRC–SWAN model for THANE cyclone in the Bay of Bengal." Environmental Fluid Mechanics 13(6): 601-623. DOI:10.1007/s10652-013-9284-5.
[6]. Briegel, L. M. and W. M. Frank (1997). "Large-scale influences on tropical cyclogenesis in the western North Pacific." Monthly weather review 125(7): 1397-1413. DOI:http://dx.doi.org/10.1175/1520-0493.
[7]. Dunkerton, T., et al. (2009). "Tropical cyclogenesis in a tropical wave critical layer: Easterly waves." Atmos. Chem. Phys 9: 5587-5646.Doi:10.5194/acp-9-5587-.
[8]. Emanuel, K. ((2005). "Increasing destructiveness of tropical cyclones over the past 30 years." Nature 436(7051): 686-688. Doi:10.1038/nature03906.
[9].Emanuel, K. A. (1991). "The theory of hurricanes." Annual Review of Fluid Mechanics 23(1): 179-196.DOI: 10.1146/annurev.fl.23.010191.
[10].Gray, W. M. (1998). "The formation of tropical cyclones." Meteorology and atmospheric physics 67(1-4): 37-69. DOI: 10.1007/ BF01277501.
[11].Gulev, S., et al. (2001). "Extratropical cyclone variability in the Northern Hemisphere winter from the NCEP/NCAR reanalysis data." Climate Dynamics 17(10): 795-809. DOI: 10.1007/s003820000145.
[12].Jullien, S., et al.(2012) "Impact of tropical cyclones on the heat budget of the South Pacific Ocean." Journal of Physical Oceanography 42(11): 1882-1906. Doi: http://dx.doi.org/10.1175/JPO-D-11-0133.1.
[13].KING, D., DAVIDSON, J. & ANDERSON-BERRY, L. 2010. Disaster Mitigation and Societal Impacts. Global Perspectives on Tropical Cyclones: From Science to Mitigation, 4, 409. Doi: 10.1142/9789814293488_0013.
[14].Lin, C.H., et al. (2013)."The Effect of Tropical Cyclones (Typhoons) on Emergency Department Visits." The Journal emergency medicine45(3):372-379. DOI: 10.1016/j.jemermed.2013.02.002.
[15].Liou, C.-S. (2007). "Sensitivity of high-resolution tropical cyclone intensity forecasts to surface flux parameterization." Natural Hazards 41(3): 387-399. DOI: 10.1007/s11069-006-9046-5.
[16].Nie, H., et al. (2012). "Simulating a typhoon storm surge using a nested Ecomsed model." Procedia Engineering 31: 775-780. Doi:10.1016/j.proeng.2012.01.1101
[17].Rao, R. (1987). "Further analysis on the thermal response of the upper Bay of Bengal to the forcing of pre-monsoon cyclonic storm and summer monsoonal onset during MONEX-79." Mausam 38(2): 147-156Doi: 10.12691/ajmo-2-2-2.
[18].Roy, C. and R. Kovordányi (2012). "Tropical cyclone track forecasting techniques―A review." Atmospheric research 104: 40-69. Doi: http://dx.doi.org/10.1016/j.atmosres.2011.09.012.
[19].Sadhuram, Y. (2004). "Record decrease of sea surface temperature following the passage of a super cyclone over the Bay of Bengal." Current Science 86(3): 383-384p.Doi: 10.12691/ajmo-2-2-2.
[20]. Schade, L. R. (2000). "Tropical cyclone intensity and sea surface temperature." Journal of the atmospheric sciences 57(18): 3122-3130. Doi:http://dx.doi.org/10.1175/15200469(2000)0572.0.CO;2
[21].Simmonds, I. and K. Keay (2000). "Variability of Southern Hemisphere extratropical cyclone behavior, 1958-97." Journal of Climate13(3):550561.Doi:http://dx.doi.org/10.1175/15200442(2000)0132.0.CO;2.
[22]. Vincent, E. M., et al. (2012). "Processes setting the characteristics of sea surface cooling induced by tropical cyclones." Journal of Geophysical Research: Oceans (1978–2012) 117(C2). DOI: 10.1029/ 2011JC007396.
[23].Webster, P. J., et al. (2005). "Changes in tropical cyclone number, duration, and intensity in a warming environment." Science 309(5742): 1844-1846. DOI: 10.1126/science.1116448.
[24].http://www.havagerash.ir/post/346