Abstract
From 1979 to 2006, the Red Sea trough (RST) in spring was objectively detected and classified into three categories (short, moderate and long) depending on its northward extension. The results indicated that most short RSTs appeared during a cold spring (larger by 7% in March than May), while most long RSTs appeared during a warm spring, where reached 71.7% in April and May. The dust events during the study period were identified using a threshold value of the Total Ozone Monitoring Satellite (TOMS) aerosol index (AI). The identified dust cases were used to classify each RST category into two classes, dust RSTs and non-dust RSTs. The synoptic characteristics of the RSTs associated with dust events that influenced the northern and western Arabian Peninsula (AP) were studied using each dust category (i.e., comparing dust and non-dust cases) and were compared between the different categories (i.e., comparing the dust cases among short, moderate and long categories). The synoptic study shows that the condition favorable for transporting dust westward into the AP occurs when an interaction is produced between the low pressure over the southern AP and Sudan low and forms a wavy zonal pressure gradient. When the RST is relatively strong, i.e., the situation has a pronounced wavy zonal and meridional pressure gradient area, it produces conditions favorable for transporting dust around the Red Sea. Commonly, dust RSTs are atmospherically integrated systems with pronounced circulation (downward motion in the eastern AP and upward motion in the western AP), a vertical westward trough tilt, horizontal tropical–extratropical interactions and north–south orientations of pressure/geopotential isolines.
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References
Ackerman SA (1989) Using the radiative temperature difference at 3.7 and 11 mm to track dust outbreaks. Remote Sens Environ 27:129–133
Alharbi BH, Maghrabi A, Tapper N (2013) The March 2009 dust event in Saudi Arabia: precursor and supportive environment. Bull Am Meteorol Soc 94:515–528
Almazroui M, Awad AM (2016) Synoptic regimes associated with the eastern Mediterranean wet season cyclone tracks. Atmos Res 180: 92–118. https://doi.org/10.1016/j.atmosres.2016.05.015
Almazroui M, Awad AM, Islam NM, Al-Khalaf AK (2015) A climatological study: wet season cyclone tracks in the East Mediterranean region. Theor Appl Climatol 120: 351–365. https://doi.org/10.1007/s00704-014-1178-z
Alpert P, Osetinsky I, Ziv B, Shafir H (2004a) Semi-objective classification for daily synoptic systems: application to the eastern Mediterranean climate change. Int J Climatol 24(8):1001–1011. https://doi.org/10.1002/joc.1036
Alpert P, Osetinsky I, Ziv B, Shafir H (2004b) A new seasons definition based on classified daily synoptic systems: an example for the Eastern Mediterranean. Int J Climatol 24(8):1013–1021. https://doi.org/10.1002/joc.1037
Annesi-Maesano I, Forastiere F, Kunzli N, Brunekref B (2007) Particulate matter, science and EU policy. Eur Respir J 29:428–431. https://doi.org/10.1183/09031936.00129506
Attada R, Dasari HP, Chowdary JS, Yadav RK, Knio O, Hoteit I (2019) Surface air temperature variability over the Arabian Peninsula and its links to circulation patterns. Int J Climatol 39:445–462. https://doi.org/10.1002/joc.5821
Awad AM, Almazroui M (2016) Climatology of the winter Red Sea. Atmos Res 182:20–29. https://doi.org/10.1016/j.atmosres.2016.07.019
Awad AM, Mashat AS (2014a) Synoptic features associated with dust transition processes from North Africa to Asia. Arab J Geosci 7(6):2451–2467. https://doi.org/10.1007/s12517-013-0923-4
Awad A, Mashat A (2014b) The synoptic patterns associated with spring widespread dusty days in Central and Eastern Saudi Arabia. Atmosphere 5(4):889–913
Awad AM, Mashat AS (2015) Synoptic characteristics of spring dust days over northern Saudi Arabia. Air Qual Atmos Health. https://doi.org/10.1007/s11869-015-0320-0
Awad AM, Mashat AWS (2018) Climatology of the autumn Red Sea trough. Theor Appl Climatol. https://doi.org/10.1007/s00704-018-2453-1
Awad AM, Mashat AS, Alamoudi AO, Assiri ME (2015a) Synoptic study of the seasonal variability of dust cases observed by the TOMS satellite over northern Saudi Arabia. Theor Appl Climatol. https://doi.org/10.1007/s00704-015-1486-y
Awad AM, Mashat AS, Abo Salem FFA (2015b) Diagnostic study of spring dusty days over the southwest region of the Kingdom of Saudi Arabia. Arab J Geosci 8:2265–2282
Babu CA, Jayakrishnan PR, Varikoden H (2016) Characteristics of precipitation pattern in the Arabian Peninsula and its variability associated with ENSO. Arab J Geosci 9:186. https://doi.org/10.1007/s12517-015-2265-x
Baseer NM, Awad AM, Almazroui M (2019) Climatology of the spring Red Sea Trough. Int J Climatol. https://doi.org/10.1002/joc.6069
Beegum SN, Gherboudj I, Chaouch N, Temimi M, Ghedira H (2018) Simulation and analysis of synoptic scale dust storms over the Arabian peninsula. Atmos Res 199:62–81
Bitan A, Saaroni H (1992) The horizontal and vertical extension of the Persian Gulf pressure trough. Int J Climatol 12(7):733–747. https://doi.org/10.1002/joc.3370120706
Blake DW, Krishnamurti TN, Low-Nam SV, Fein JS (1983) Heat low over the Saudi Arabian Desert during May 1979 (Summer MONEX). Mon Weather Rev 111:1759–1775
Crosbie E, Sorooshian A, Monfared NA, Shingler T, Esmaili OA (2014) Multi-year aerosol characterization for the greater Tehran Area using satellite, surface, and modeling data. Atmosphere 5:178–197
Dayan U, Ziv B, Shoop T, Enzel Y (2008) Suspended dust over south-eastern Mediterranean and its relation to atmospheric circulations. Int J Climatol 28(7):915e924. https://doi.org/10.1002/joc.1587
De Vries AJ, Tyrlis E, Edry D, Krichak SO, Steil B, Lelieveld J (2013) Extreme precipitation events in the Middle East: dynamics of the active Red Sea Trough. J Geophys Res Atmos 118:7087–7108. https://doi.org/10.1002/jgrd.50569
El-Fandy MG (1948) The effect of Sudan monsoon low on the development of thundery conditions in Egypt, Palestine and Syria. Quarter J Royal Meteorol Soc 74:31–38
El-Fandy MG (1950) Effects of topography and other factors on the movement of lows in the Middle East and Sudan. Bull American Meteorol Soc 10:375–381
El Kenawy AM, McCabe MF (2016) A multi-decadal assessment of the performance of gauge- and model-based rainfall products over Saudi Arabia: climatology, anomalies and trends. Int J Climatol 36:656. https://doi.org/10.1002/joc.4374-674
El Kenawy AM, McCabe MF, Stenchikov G, Raj J (2014) Multi-decadal classification of synoptic weather types, observed trends and links to rainfall characteristics over Saudi Arabia. Front Environ Sci Eng 2:37
Ganor E, Osetinksy I, Stupp A, Pinhas A (2010) Increasing trend of African dust, over 49 years, in the eastern Mediterranean. J Geophys Res Atmos. https://doi.org/10.1029/2009JD012500
Gates WL (1961) Static stability in the atmosphere. J Meteorol 18:526–533
Gherboudj I, Naseema Beegum S, Ghedira H (2017) Identifying natural dust source regions over the Middle-East and North-Africa: estimation of dust emission potential. Earth Sci Rev 165:342–355. https://doi.org/10.1016/j.earscirev.2016.12.010
Goudie AS, Middleton NJ (2001) Saharan dust storms: nature and consequences. Earth Sci Rev 56:179–204. https://doi.org/10.1016/S0012-8252(01)00067-8
Goudie A, Middleton N (2006) Desert dust in the global system. Springer, Heidelberg
Haggag M, El-Badry H (2013) Mesoscale numerical study of quasi-stationary convective system over Jeddah in November 2009. Atmos Clim Sci 3(1):73–86. https://doi.org/10.4236/acs.2013.31010
Hamidi M, Kavianpour MR, Shao Y (2013) Synoptic analysis of dust storms in the Middle East. Asia Pac J Atmos Sci 49:279–286
Hannachi A, Awad A, Ammar K (2011) Climatology and classification of Spring Saharan cyclone tracks. Clim Dyn 37:473–491. https://doi.org/10.1007/s00382-010-0941-9
Hasanean HM, Almazroui M (2016) Teleconnections of the tropical sea surface temperatures to the surface air temperature over Saudi Arabia in summer season. Int J Climatol 37:1040–1049. https://doi.org/10.1002/joc.4758
Herman JR, Bhartia PK, Torres O, Hsu C, Seftor C, Celarier E (1997) Global distribution of UV-absorbing aerosols from Nimbus-7/TOMS data. J Geophys Res 102:16911–16922
Hsu NC, Herman JR, Torres O, Holben BN, Tanre D, Eck TF, Smirnov A, Chatenet B, Lavenu F (1999) Comparisons of the TOMS aerosol index with sun-photometer aerosol optical thickness: results and applications. J Geophys Res 104:6269–6279
Huneeus N, Schulz M, Balkanski Y, Griesfeller J, Prospero J, Kinne S, Bauer S, Boucher O, Chin M, Dentener F, Diehl T, Easter R, Fillmore D, Ghan S, Ginoux P, Grini A (2011) Global dust model intercomparison in Aerocom Phase I. Atmos Chem Phys 11:7781–7816
Joseph JH, Manes A, Ashbel D (1973) Desert aerosols transported by Khamsinic depressions and their climatic effects. J Appl 12:792–797
Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iridell M Saha S, White G, Woollen J, Zhu Y, Chelliah M, Ebisuzaki W, Higgins W, Janowiak J, Mo KC, Ropolewski C, Wang J, Leetma A, Reynolds R, Jenne R, Joseph D (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteorol Soc 77:437–471
Kaufman YJ, Koren I, Remer A, Rosenfeld D, Rudich Y (2005) The effect of smoke, dust, and pollution aerosol on shallow cloud development over the Atlantic Ocean. Proc Natl Acad Sci USA 102:11207–11212. https://doi.org/10.1073/pnas.0505191102
Kistler R, Collins W, Saha S, White G, Woollen J, Kalnay E, Chelliah M, Ebisuzaki W, Kanamitsu M, Kouskyvanden Dool VH, Jenne R, Fiorino M (2001) The NCEP/NCAR 50-year reanalyses: monthly CD-ROM and documentation. Bull Am Meteorol Soc 82:247–267
Krichak SO, Alpert P (1998) Role of large scale moist dynamics in November 1–5, 1994 hazardous Mediterranean weather. J Geophys Res 103:19453–19458
Krichak SO, Alpert P, Krishnamurti TN (1997b) Red Sea Trough/cyclone development—numerical investigation. Meteorol Atmos Phys 63:159–169
Krichak SO, Tsidulko M, Alpert P (2000) Monthly synoptic patterns associated with wet/dry conditions in the eastern Mediterranean. Theoret Appl Climatol 65:215–229
Krichak SO, Breitgand JS, Feldstein SB (2012) A Conceptual Model for the Identification of Active Red Sea Trough Synoptic Events over the Southeastern Mediterranean. J. Appl. Meteor. Climatol. 51:962–971. https://doi.org/10.1175/JAMC-D-11-0223.1
Laurent B, Marticorena B, Bergametti G, Le’on JF, Mahowald NM (2008) Modeling mineral dust emissions from the Sahara desert using new surface properties and soil database. J Geophys Res 113:D14218. https://doi.org/10.1029/2007JD009484
Mahowald NM, Luo C, del Corral J, Zender C (2003) Interannual variability in atmospheric mineral aerosols from a 22-year model simulation and observation data. J Geophys Res. https://doi.org/10.1029/2002JD002821
Mashat A, Awad AM (2010) The classification of the dusty areas over the middle-east. Bull Fac Sci Cairo Univ 78:1–19
Mashat AW, Awad A (2016) Synoptic characteristics of the primary widespread winter dust patterns over the northern Arabian Peninsula. Air Qual Atmos Health 9(5):503–516
Mashat AWS, Alamoudi AO, Awad AM, Assiri ME (2018) Seasonal variability and synoptic characteristics of dust cases over southwestern Saudi Arabia. Int J Climatol 38:105–124. https://doi.org/10.1002/joc.5164
Middleton NJ (1986a) Dust storms in the Middle East. J Arid Environ 10:83–96
Middleton NJ (1986b) A geography of dust storms in south-west Asia. J Climatol 6:183–196
Mohalfi S, Bedi HS, Krishnamurti TN, Cocke SD (1998) Impact of shortwave radiative effects of dust aerosols on the summer season heat low over Saudi Arabia. Mon Weather Rev 126:3153–3168
Natsagdory L, Jugder D, Chung YS (2003) Analysis of dust storms observed in Mongolia during 1937–1999. Atmos Environ 37:1401–1411
Notaro M, Alkolibi F, Fadda E, Bakhrjy F (2013) Trajectory analysis of Saudi Arabian dust storms. J Geophys Res Atmos 118:6028–6043
Osetinsky I, Alpert P (2006) Calendaricities and multimodality in the Eastern Mediterranean cyclonic activity. Nat Hazards Earth Syst Sci 587–596
Pease PP, Tchakerian VP, Tindale NW (1998) Aerosols over the Arabian Sea: geochemistry and source areas for aeolian desert dust. J Arid Environ 39:477–496
Pinto JG, Spangeh T, Ulbrich U, Speth P (2005) Sensitivities of a cyclone detection and tracking algorithm: individual tracks and climatology. Meteorol Z 14:823–838
Prakash PJ, Stenchikov G, Kalenderski S, Osipov S, Bangalath H (2015) The impact of dust storms on the Arabian Peninsula and the Red Sea. Atmos Chem Phys 15:199–222. https://doi.org/10.5194/acp-15-199
Prospero JM, Nees RT, Uematsu M (1987) Deposition rate of particulate and dissolved aluminum derived from Saharan dust in precipitation at Miami, Florida. J Geophys Res 92:14723–14731
Prospero JM, Ginoux P, Torres O, Nicholson SE, Gill TE (2002) Invironmental characterization of global sources of atmospheric soil dust identified with the Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) absorbing aerosol product. Rev Geophys 40:1002. https://doi.org/10.1029/2000RG000095
Rezazadeh M, Irannejad P, Shao Y (2013) Climatology of the Middle East dust events. Aeolian Res 10:103–109
Rosenfeld D, Rudich Y, Lahav R (2001) Desert dust suppressing precipitation: a possible desertification feedback loop. Proc Natl Acad Sci USA 98:5975–5980. https://doi.org/10.1073/pnas.101122798
Saaroni H, Bitan A, Alpert P, Ziv B (1996) Continental polar outbreaks into the Levant and eastern Mediterranean. Int J Climatol 16:1–17
Saaroni H, Ziv B, Bitan A, Alpert P (1998) Easterly wind storms over Israel. Theoret Appl Climatol 59:61–77
Schneider T, Bischoff T, Haug GH (2014) Migrations and dynamics of the intertropical convergence zone. Nature 513:45–53
Torres O, Bhartia PK, Herman JR, Ahmad Z, Gleason K (1998) Derivation of aerosol properties from satellite measurements of backscattered ultraviolet radiation: theoretical basis. J Geophys Res 103:17099–17110
Tsvieli Y, Zangvil A (2005) Synoptic climatological analysis of “wet” and “dry” Red Sea troughs over Israel. Int J Climatol 25:1997–2015. https://doi.org/10.1002/joc.1232
Tsvieli Y, Zangvil A (2007) Synoptic climatological analysis of Red Sea Trough and non-Red Sea Trough rain situations over Israel. Adv Geosci Euro Geosci Union 12:137–143
Tyrlis E, Lelieveld J, Steil B (2013) The summer circulation over the eastern Mediterranean and the Middle East: influence of the South Asian monsoon. Clim Dyn 40(5–6):1103–1123. https://doi.org/10.1007/s00382-012-1528-4
Washington RW, Todd MC, Middleton N, Goudie AS (2003) Dust-storm source areas determined by the total ozone monitoring spectrometer and surface observations. Ann Assoc Am Geogr 93:297–313
Yu Y, Notaro M, Liu Z, Kalashnikova O, Alkolibi F, Fadda E, Bakhrjy F (2013) Assessing temporal and spatial variations in atmospheric dust over Saudi Arabia through satellite, radiometric, and station data. J Geophys Res Atmos 118:13253–13264
Acknowledgements
This work was funded by the Deanship of Scientific Research (DSR), King Abdulaziz University, Jeddah, under Grant no. G: 257-155-1440. The authors, therefore, acknowledge and are grateful to the DSR for technical and financial support. The authors also acknowledge the National Centers for Environmental Prediction (NCEP) and the National Center for Atmospheric Research (NCAR) for providing meteorological data and the National Aeronautics and Space Administration (NASA) for providing the TOMS data online.
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Mashat, AW.S., Awad, A.M., Assiri, M.E. et al. Synoptic pattern of the Red Sea trough associated with spring dust over the northern and western Arabian Peninsula. Meteorol Atmos Phys 133, 655–673 (2021). https://doi.org/10.1007/s00703-020-00771-0
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DOI: https://doi.org/10.1007/s00703-020-00771-0