Investigation of dust storms entering Western Iran using remotely sensed data and synoptic analysis
© Boloorani et al.; licensee BioMed Central Ltd. 2014
Received: 12 February 2013
Accepted: 14 October 2014
Published: 29 October 2014
One of the natural phenomena which have had considerable impacts on various regions of the world, including Iran, is "dust storm". In recent years, this phenomenon has taken on new dimensions in Iran and has changed from a local problem to a national issue. This study is an attempt to investigate the formation of the dust storms crossing the Western Iran.
To find the sources of the dust storms entering Iran, first we examine three determined dust paths in the region and their temporal activities, using MODIS satellite images. Then, four regions were identified as dust sources through soil, land cover and wind data. Finally, atmospheric analyses are implemented to find synoptic patterns inducing dust storms.
Results and discussion
Source 1 has covered the region between the eastern banks of Euphrates and western banks of Tigris. Source 2 is in desert area of western and south-western Iraq. Finally source 3 is bounded in eastern and south-eastern deserts of Saudi Arabia called Rub-Al-Khali desert, or Empty Quarter. Moreover, south-eastern part of Iraq (source 4) was also determined as a secondary source which thickens the dust masses originating from the above mentioned sources. The study of synoptic circulations suggests that the dust storms originating from source 1 are formed due to the intense pressure gradient between the low-pressure system of Zagros and a high-pressure cell formed on Mediterranean Sea. The dust events in sources 2 and 3 are outcomes of the atmospheric circulations dominant in the cold period of the year in mid-latitudes.
KeywordsDust source Dust storm Dust detection Remote sensing Synoptic climatology
The frequent occurrence of this phenomenon in various regions of the world such as Iran has gained attentions from academia and has triggered many research projects on the issue. Remote sensing is one of the most widely-used methods in dust storm studies. Drawing upon a model based on surface conditions and satellite observations, Ozsoy et al. examined one of the greatest dust events in Sahara Desert during the April of 1994 which affected a wide region from Caribbean to Eurasia . El-Askary et al. argued that a synthetic approach is the best way of observing and tracking dust in satellite images . Measuring solar reflectance bands, Qu et al. detected dust masses in satellite images . Alles used air pollution indicatives and MODISa images to determine China’s dust sources; the results have shown that the phenomenon has originated in the cold regions and has caused many problems in Gobi desert while crossing and loading enormous dust particles in this region . Li et al. have analysed the greatest dust in the eastern Australia using MODIS images and (BTDb) index. He detected the high performance of the method in identification of dust masses . Climatological analysis, especially the synoptic approach - the study of relations between global atmospheric circulations and regional and local climates  - has been used in most of the researches performed on the atmospheric conditions during dust events. Investigating the transfer of dust from Sahara to Italy and central Europe, Barkan et al. recognized sub-tropical high pressure system on the south-eastern Mediterranean Sea and a low-pressure centre resulted from Iceland’s trough in the western Africa as the primary factors of dust formation and mobilization . Zolfaghari and Abedzadeh adopted a synoptic approach to investigate the atmospheric systems leading to dust in western Iran in a 5-year period. They have concluded that Azur’s high-pressure system along with westerly-travelling cyclonic and anti-cyclonic systems are the most effective atmospheric factors on the dust events in the region . Dayan et al. have classified dominant synoptic patterns in the region on dusty days and indicated that 60% of the dust events in the south-eastern Mediterranean occur as a result of Cyprus low-pressure system . Gerivani et al. have adopted a different approach and categorized the sources of the dust storms in Iran based on geological maps and the information on wind erosion of the susceptible lands . Although, all the mentioned studies have provided considerable results, the fact that a dust event results from multiple factors requires considering synthetic approaches. Utilizing various perspectives such as remote sensing data, synoptic climatology analysis, and ancillary data including soil texture and land cover of the studied regions, as well as the wind speed and direction maps, the present research tries to study the dust events in western Iran more precisely.
On the other hand, the most climatological studies of the dust storms in Iran are limited to a few numbers of case studies. Moreover, in these works the source-based classification of atmospheric circulations has not been considered to account for environmental conditions leading to dust storm. Therefore, in this work, we have increased the number of investigated events to 40 cases and also atmospheric aspects of dust storms are precisely studied. Significant rise in the number of recent dust storms in Iran and also applying new and up-to-date methods to examine this natural event provide another motivation for the present study.
The rest of this paper is organised as follows. Methods and data are presented in the next section. The research findings are discussed in section 3, and section 4 concludes the paper.
Data and methods
Data and methods for the identification of dust sources
In this research, only the dust events satisfying the following criteria were studied: (I) recorded at least in 3 synoptic stations, (II) rising from non-local origins, and (III) leading to a maximum horizontal visibility of 1000 meters.
In cases, the stations in the region under study indicated consecutive days with dust, only those days were specified as independent event when dust particles were injected to atmospheric currents from dust-prone areas. Whereas, maybe because of air stillness, dust continued for days over a region without any new dust injection, those dusty days were considered as on dust event.
Mobility of dust plumes from the originating sources to the surrounding regions do not necessarily follow density reduction regime, i.e., there may exist some other dust sources throughout the dust paths which inject new dust particles into the primary mass. Therefore, in the present study, the region where dust originates is not considered as the only source of the event. In fact, all the regions located in the dust path are determined using remote sensing imagery and then, supplementary data and information are taken into account to locate the dust sources more precisely. In order to identify dust paths and to estimate primary and secondary dust sources, approximately 100 MODIS images of Middle East were processed within a five-day period before recording time of each event.
In this research, image processing for dust detection is based on Ackerman’s method , arguing that brightness temperature difference of dust particles in bands 31 and 32 (11 and 12 micrometre wavelengths) is below zero in Kelvin scale. However, it is empirically considered -0.5 in the present work. To distinguish dust particles suspended in the air from land covers, two types of test were used; R-test and BTD-test . After identifying possible dust sources and the relocation paths, more precise identification processes are performed by examining the soil data and land covers of the studied regions, and wind maps.
Visibility data from Iranian Meteorology Organization database,
MODIS images from NASA website,c
Soil information from the Harmonized World Soil Database , and
Land-cover data from ESA websited.
Data and methods to identify atmospheric circulations associated with dust storms
The analysis of synoptic circulations associated with dust storms is carried out according to geopotential height at 850 hPa and 500 hPa levels, temperature, and wind data at height of 10 meters above the ground during the beginning days of studied dust storms. All atmospheric data, except for dust records, were provided by National Centre of Environmental Predicting (NCEP) database .
Result and discussion
Identification of western Iran’s dust sources
The dates of the dust events which have formed and moved through the Northwest-Southeast path
Starting date of dust storm
Observation date of dust storm in study area
The dates of the dust events which have formed and moved through the West–east path
Starting date of dust storm
Observation date of dust storm in study area
The dates of the dust events which have formed and displaced through the southern-northern path
Starting date of dust storm
Observation date of dust storm
As indicated in Table 3, dust masses moving in the third path do not play a significant role in dust events occurring in Iran and thus, it cannot be considered as an influential region of forming the dust storms occurred in the last decade in the study area. Saudi Arabia dust events occurred in the late cold period of the year that is examined in atmospheric analysis section.
Soil characteristics of dust sources
Dominant soil group
Topsoil USDA texture classification
Topsoil sand fraction (%)
The east of Syria and North west of Iraq
GY - Gypsisols
South east of Iraq
The west and south west of Iraq
The east and south east of Saudi Arabia
Soil maps of the northwest–southeast dust path in Syria and Iraq indicated a region of gypsum sediments in the north-western Iraq and the eastern Syria. This area has mainly formed in arid regions with poor vegetation called gypsisole (Figure 4). Despite the fact that southernmost region of the path, i.e. the south-eastern Iraq, consists of solonchaks soil, which is also found in arid and semi-arid regions, one of its distinguishing features is that the water table is close to the surface. Since, the soil is almost wet- a condition sometimes leading to water stillness on the soil surface . Although in the recent years, this region has experienced an increase in depth of groundwater because of drought, and some ponds have changed into limited erodible zones , the south eastern Iraq cannot be considered as a main and wide dust source influencing the western Iran. However, in some cases, dust masses originating from other region have been intensified locally in this region and then entered Iran (not shown here). The quantitative characteristics of soil along northwest–southeast path (80% of the soil has a fine texture including clay and silt) verify that the north-western parts of Iraq and the eastern parts of Syria potentially lead to massive dust storms. Furthermore, these conditions are intensified by the regions with low soil moisture (15–50 mm per 1 m soil depth) and spare land covers. It should be noted that despite the fine texture of the soil in south eastern Iraq, higher moisture (150 mm per 1 m soil depth) and more dense land cover lead to a lower chance of dust event in this region (Table 4, Figures 4 and 5). According to the discussion above, the upper zone of Mesopotamia (Iraq-Syria border) is the most likely region to provide airborne particles for the dust storms in western Iran along the northwest-southeast path.
The study of the ancillary data on path two shows that the calcisols covers most parts of the west and south western Iraq (Figure 4). Calcisols is mainly formed in arid and semi-arid regions especially in foothills, and is known as an alluvial type of soil with fine texture, which makes land cover potentially erodible . Table 4 gives data for an equal mixture of sand, clay, and silt in the west and south western Iraq. In this region, the amount of soil (dominant soil) moisture is about 50 mm per 1 m soil depth (even as low as 15 mm in some regions), which results in sparse vegetation (Figure 5).
The path three just start from southeast of Arabian Peninsula (the desert region of Rub-Al-Khali or Empty Quarter) to southern coasts of Persian Gulf. This part of Arabia is Regosol soil which mainly is composed of gravel and sand coverings (i.e. 84%) (Figure 4 and Table 4). Since the soil has a coarse texture, the number of dust storms reaching Iran throgh this pathway is much less than that from other dust sources (i.e. 3 out of 40 cases). However, the intense dryness (amount of soil moisture in some regions is around zero) and lack of vegetation (Figure 5) result in a large number of limited daily local sand storms in eastern Arabian Peninsula.
According to Figure 6, in the first day of all the studied dust events, wind speed and direction maps are in accordance with the estimated dust sources. During dusty days of the path one the speedy winds (6 to 12 m/s) skirted on Iraq and south-eastern Syria have the potential to make dust plumes in erosion-prone regions (Figure 6A). The composite map of wind speed and direction shows speedy air streams during the beginning days of dust storms in path two. As a result, the western and eastern parts of Iraq are prone to dust if other conditions are available. Along with the formation of dust in path three, two convergent wind currents come together in eastern Saudi Arabia. Surface westerly winds, most likely intensified by temperature differences between the western mountainous regions and the eastern desert area, converge with easterly currents. This circulation transports large amounts of dust masses from the eastern Arabia to upper atmospheric levels and higher latitudes. In fact, because of the coarse soil texture of Saudi Arabia deserts, only such special atmospheric circumstances can make massive dust storms enter regional circulations and subsequently the western Iran (Figure 6C).
Dust source 1: The region between eastern banks of Euphrates to western banks of Tigris
The region located in the north western Iraq and the eastern Syria was recognised as the main source of the dust storms entering western Iran. As discussed above, this region was the origin of 23 dust storms out of the 40. Most of dust events originating in this source have formed in Iraq and a few in Syria.
Dust source 2: The western and south western Iraq
14 cases out of 40 have formed in this region. It also includes parts of Jordan and Syrian Desert.
Dust source 3: The eastern and south-eastern Arabian Peninsula called Rub-Al Khali desert
Some parts of Rub-Al-Khali desert were the source of 3 cases out of the total 40.
Dust source 4: The south-eastern Iraq
This source is not considered as a major dust origin, but it intensifies the dust masses originating from other sources, especially from one and two dust formation areas. Therefore, the number of dust events formed in this region is not given separately.
Tracking dust storms and examination of various data and factors gave us most likely dust sources which send dust particles into Iran. However, the study of atmospheric conditions and identification of synoptic patterns during dust events is crucial to clarify predominant environmental conditions leading to dust storms.
Atmospheric conditions and synoptic patterns
Before discussing the atmospheric conditions governing the occurrence of dust storms in the western Iran, it is necessary to note that the activity of each dust source follows certain temporal distribution. All the dust events originating in the source one, have occurred in the warm periods of the year (April to September), while other dust cases formed in the western and south western Iraq, and eastern and south eastern Saudi Arabia have been recorded in cold and late cold periods. The activity of the source four has happened in both, the warm and cold seasons. Such a clear distinction in the temporal distribution of the dust activities in the sources can be due to the formation of different atmospheric patterns in specific periods of the year. Synoptic circulations associated with the dust sources are discussed in the following subsections –except for atmospheric conditions affecting the fourth source, because it acts as the secondary origin coincidental to the primary sources.
Synoptic patterns of source one
To explain how this circulation pattern is formed, the effects of seasonal thermal processes should be examined. In summertime, apart from the low pressure of the Bay of Bengal, another thermal low forms in Pakistan and sometimes in the north-western India known as Paki-India low. According to Bollasina and Nigam, the intensified surface heating of the Iranian plateau, especially Zagros Mountains, is one of the factors involved in deepening Paki-India low and its movement into Iran . As mentioned before, surface heating of Zagros Mountains in normal conditions also leads to a low-pressure centre at 800–850 hPa levels. But along with Iran dust storms, heating process of Zagros Mountains and eastern deserts of Iran increases dramatically (Figure 9B). Based on the classic definition of thermal atmospheric circulations, this condition also results in the formation of high and low pressure systems in upper and lower-troposphere, respectively. Records of temperature in the composite map at 850 hPa show anomaliese over 6 to 9 degrees Celsius in Zagros Mountains. 500 hPa composite map for dusty days occurred in North West Iraq and east Syria origins shows relocation of tropical high air mass, indicated by 5880-gpm contour, to the southern Iran which locates over Saudi Arabia Peninsula in the long term map (Figure 9C). Given that 500 hPa level is not usually affected by low surface thermal conditions, the locating of this high could be due to the significant rise in surface temperature on Zagrus Mountains. It is necessary to note that the deepening of low-pressure system located on Iraq and western Iran is not only affected by surface diabatic heating but also in some cases it is affected by dynamic processes resulted from travelling troughs . Within the beginning days of dust storms formed in source one, trough patterns, located on Iraq and subsequently Iran, might deepen lower-troposphere thermal cyclones.
Synoptic circulations during dust events originating from sources 2 and 3
The dynamic processes of westerly winds in mid-troposphere have a very significant role in the formation of surface mid-latitude cyclones and anticyclones. As seen in Figure 9C and 9D, cyclonic and anti-cyclonic circulations are formed respectively under the front and back of trough. During dusty days of the western and south western Iraq, a trough lies at 500 hPa level which leads to the formation of cyclonic (low pressure) and anti-cyclonic (high pressure) circulations in Iran and eastern shores of the Mediterranean sea. In fact, the dust source is strengthened by being located between low and high-pressure centres and subsequently, being affected through pre-cold front (cold sector), west–east, high-speed winds. While trough gets deeper, cyclonic circulation relocates toward lower latitudes on Saudi Arabia. In these cases, speedy winds causing extensive dust storms will form in warm sector of the cyclone with a roughly south–north direction.
Path 1: the northwest-southeast path, from the north-western Iraq and the south eastern Syria, to western Iran,
Path 2: the second pathway with eastern-western direction, from Iraq-Jordan borders extended to the western Iran,
Path 3: the last path from southern banks of Persian Gulf to western Iran through a south–north directing.
Source 1: the eastern banks of Euphrates and the western banks of Tigris as main western Iran dust sources,
Source 2: the western and south western Iraq, and also small parts of Syria and Jordan,
Source 3: the eastern and south-eastern deserts of Arabia called Rub-Al-Khali Desert,
Source 4: the south-eastern Iraq, as a secondary source.
The examination of the atmospheric conditions governing each dust source indicates that synoptic patterns during dust events originating from source one have been mainly affected by the surface diabatic processes. Whereas, dust storm in sources two and three are caused by cyclonic and anti-cyclonic circulations and are largely outcome of dynamic processes of westerly winds.
aModerate Resolution Imaging Spectroradiometer.
bBrightness Temperature Difference.
eTemperature anomaly = (daily temperature - average daily temperature).
The most parts of this study including: research scheme, data analysis, and manuscript preparation were implemented by first two authors. Third author has helped to find an effective dust detection algorithm and make it convenient by programing in MATLAB software. Other authors have accompanied in editing, cohesion and translating presented paper. All authors read and approved the final manuscript.
This research paper is made possible through the help and financial support from science and technology affairs of Islamic republic of Iran.
- Goudie AS, Middleton N: Desert dust in the global system. New York: Springer Berlin Heidelberg; 2006.Google Scholar
- Shao Y, Wyrwoll KH, Chappell A, Huang J, Lin Z, McTainsh GH, Mikami M, Tanaka TY, Wangh X, Yoon S: Dust cycle: an emerging core theme in earth system science. Aeolian Res 2011, 2: 181–204. 10.1016/j.aeolia.2011.02.001View ArticleGoogle Scholar
- Ardehjani SS: I.R of Iran national report on regional action plan to combat dust and sand storm. ., [http://icap.atmos.und.edu/AERP/MeetingPDFs/RemoteSensing/Shirkani_Iran_Dust_Report%20(NXPowerLite).pdf]
- Ozsoy E, Nilgun K: A hemispheric dust storm affecting the Atlantic and Mediterranean in April 1994: Analyses, modeling, ground-based measurements and satellite observations. J Geophys Res 2001, 106: 18439–18460. 10.1029/2000JD900796View ArticleGoogle Scholar
- El-Askary HM, Sarkar S, Kafatos M, El-Ghazawi TA: A multisensor approach to dust storm monitoring over the Nile Delta. Geosci Remote Sens 2003, 41: 2386–2391. 10.1109/TGRS.2003.817189View ArticleGoogle Scholar
- Qu JJ, Hao X, Kafatos M, Wang L: Asian dust storm monitoring combining terra and aqua MODIS SRB measurements. Geosci Remote Sens Lett 2006, 3: 484–486. 10.1109/LGRS.2006.877752View ArticleGoogle Scholar
- Alles DL: geomorphology and dust storm in the China. ., [http://fire.biol.wwu.edu/trent/alles/ChinaDust.pdf]
- Li X, Ge L, Dong Y, Chang HC: Estimating the greatest dust storm in eastern Australia with MODIS satellite images. In Proceedings of IGARSS. Honolulu, HI: 2010:1039-1042.Google Scholar
- Barry RG, Perry AH: Synoptic Climatology: Methods and Applications. London: Methuen; 1973.Google Scholar
- Barkan J, Alpert P, Kutiel H, Kishcha P: Synoptics of dust transportation days from Africa toward Italy and central Europe. J J Geophys Res 2005, 110: 1984–2012.Google Scholar
- Zolfaghari H, Abedzadeh H: A synoptic analysis of dust systems at the west part of Iran. Geography Dev Q 2006, 6: 173–188.Google Scholar
- Dayan U, Ziv B, Shoob T, Enzel Y: Suspended dust over south-eastern Mediterranean and its relation to atmospheric circulations. Int J Climatol 2008, 28: 915–924. 10.1002/joc.1587View ArticleGoogle Scholar
- Gerivani H, Lashkaripour GR, Ghafoor IM, Jalili N: The source of dust storm in Iran: a case study based on geological information and rainfall data. Carpathian J Earth Environ Sci 2010, 6: 297–308.Google Scholar
- Ackerman SA: Remote sensing aerosols using satellite infrared observations. J Geophys Res 1997, 102: 17069–17079. 10.1029/96JD03066View ArticleGoogle Scholar
- Zhao TXP, Ackerman S, Guo W: Dust and smoke detection for multi-channel imagers. Remote Sens 2010, 2: 2347–2368. 10.3390/rs2102347View ArticleGoogle Scholar
- Harmonized World Soil Database (version 1.1). ., [http://webarchive.iiasa.ac.at/Research/LUC/External-World-soil-database/HTML/]
- Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woollen J, Zhu Y, Leetmaa A, Reynolds B, Chelliah M, Ebisuzaki W, Higgins W, Janowiak J, Mo KC, Ropelewski C, Wang J, Jenne R, Bull JD: The NCEP/NCAR 40-year reanalysis project. Am Meteorol Soc 1996, 77: 437–472. 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2View ArticleGoogle Scholar
- ENVISAT global land cover map. ., [http://www.esa.int/spaceinimages/Images/2008/12/Envisat_global_land_cover_map]
- IUSS Working Group WRB: World Reference Base for Soil Resources. ., [http://www.fao.org/fileadmin/templates/nr/images/resources/pdf_documents/wrb2007_red.pdf]
- UNEP, Partow H: The Mesopotamian Marshlands: Demise of an Ecosystem Early Warning and Assessment Technical Report. ., [http://eoimages.gsfc.nasa.gov/images/imagerecords/1000/1716/meso2.pdf]
- Aurelius L, Buttgereit V, Cammelli S, Zanina M: The impact of Shamal winds on tall building design in the Gulf Region. ., [https://www.dm.gov.ae]
- Zaitchik BF, Evans JP, Smith RB: Regional impact of an elevated heat source: the Zagros Plateau of Iran. J Clim 2007, 20: 4133–4146. 10.1175/JCLI4248.1View ArticleGoogle Scholar
- Zarrin A, Ghaemi H, Azadi M, Mofidi A, Mirzaei E: The effect of the Zagros Mountains on the formation and maintenance of the Iran Anticyclone using RegCM4. Meteorol Atmos Phys 2011, 112: 91–100. 10.1007/s00703-011-0134-zView ArticleGoogle Scholar
- Bollasina M, Nigam S: The summertime "heat" low over Pakistan/north-western India: evolution and origin. Clim Dynam 2010, 37: 957–970. 10.1007/s00382-010-0879-yView ArticleGoogle Scholar
This article is published under license to BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0) which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated.