دست‌یابی به چشمه توفان‌های گردو غبار به کمک مدل‌های عددی‌: معرفی رویکردی برای پیش‌بینی توفان‌های گردوغبار

Ashrafi, Kh.,M.Shafiepour-Motlagh, A.Aslemand, and S. Ghader. (2014).Dust storm simulation over Iran using HYSPLIT. Journal of Environmental Health Science and Engineering, 12: 1-9.

Azizi. Gh., M. Miri., A. Nabavi., (2012). Tracing of Dust storms in west of Iran, Arid regions Geographic Studies, Issue 2, No. 7:  63-81.

Chen, F.,J.Dudhia.(2001). Coupling an advanced land-surface/hydrology model with the Penn State/NCAR MM5 modeling system. Part I: model description and implementation. Monthly Weather Review, 129:569-585.

Chou, M.D., M.J. Suarez.(1994). An efficient thermal infrared radiation parameterization for use in general circulation models. NASA Technology Memory, 104606, 85p.

Draxler, R.R.(1995). Source Location through Radiological Monitoring (System Design and Concept of Operations). Radionuclide Monitoring Workshop, 15-17 November, 1995.

Draxler, R.R., G.D.Hess. (1997). Description of the HYSPLIT_4 Modeling System. NOAA Technical Memorandum.ERL ARL. 224: 1-25.

Gillette, D.A.(1999). A qualitative geophysical explanation for ‘‘hot spot’’ dust emitting source regions. Contributions to Atmospheric Physics 72: 67-77.

Goudie. A.S., N.J.Middleton.(2001). Saharan dust storms: nature and consequences, Earth-Science Reviews,56: 179-204.

Henley, P., (1990). Unpublished soil sample report, Remote Sensing Division, Research Institute, U.S Army Engineer Topographic Laboratories, Ft Belvoir, VA, 21 Nov 90.

Kain J.S., J.M. Fritsch.(1993). In: Emanuel KA, Raymond DJ (eds) Convective parameterization for mesoscale models: the Kain–Fritsch scheme. The representation of cumulus convection in numerical models. American Meteorology Society, 246p.

Lee, J.A., T.E. Gill, K.R. Mulligan, M.Domı´nguez Acosta,and A.E.Perez.(2008). Land use/land cover and point sources of the 15 December 2003 dust storm in southwestern North America. Geomorphology. http://dx.doi.org/10.1016/j.geomorph. 2007.12.016.

Lin, Y.L., R.D. Farley, and H.D.Orville. (1983). Bulk parameterization of the snow field in a cloud model, Journal of Applied Meteorology, 22: 1065-1092.

Membery, D.A. (1983). Low-level wind profiles during the Gulf Shamal. Weather 38: 18-24.

Mlawer, E.J., SJ. Taubman,P.D. Brown,M.J. Iacono,and S.A. Clough.(1997). Radiative transfer for inhomogeneous atmosphere: RRTM, a validated correlated-k model for the longwave. Journal of Geophysical Research, 102:16663-16682.

Mofidi. A., S. Jafari. (2011). The Role of Regional Atmospheric Circulation over the Middle East on the Occurrence of Summer Dust-storms in Southwest Iran. Arid Regions Geographic Studies. 2 (5) :17-45

Petzold, A., K. Rasp, B.Weinzierl, M. Esselborn, T. Hamburger, and A. Dornbrack.(2009). Saharan dust absorption and refractive index from aircraft-based observation during SAMUM 2006. Tellus;618:118–30. doi:10.1111/j.1600-0889.2008.00383.x.

Rezazadeh, M., P. Irannejad, Y. Shao. (2013). Dust emission simulation with the WRF-Chem model using new surface data in the Middle East region. Journal of the Earth and Space Physics, Issue 33, No. 1: 119-212.

Rousseau, D.D., D.Duzer, J.L. Etienne, G.Cambon, D. Jolly, J.Ferrier, andP.Schevin.(2004). Pollen record of rapidly changing air trajectories to the North Pole. Journal of Geophysical Research, 109, D06116, doi: 10.1029/2003JD003985.

Salazar, C., C. Alvarez, H.A. Silva, and C.Dorantes.(1994). Radioactivity in air around nuclear facilities in Mexico. Environ Int;20:747-56.

Skamarock, W.C., J.Klemp, J. Dudhia, D.O. Gill, D.M. Barker, W. Wang, and J.G. Powers. (2008). A description of the advanced research WRF version 2. NCAR technical note, NCAR/TN-468+STR. Meso-scale and Microscale Meteorology Division, National Center for Atmospheric Research, Boulder, CO, USA.

Stohl, A., (1998). Computation, accuracy and applications of trajectories - a review and bibliography. Atmospheric Environment, 32(6): 947-966.

Wang, Y., G.Zhuang, A. Tang, W. Zhan, Y.Sun, Z. Wang, and Z. An,(2007). The evolution of chemical components of aerosols at five monitoring site of China during dust storms. Atmospheric Environment 41: 1091-1105.