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ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS

Year 2020, Volume: 8 Issue: 1, 61 - 72, 28.02.2020
https://doi.org/10.20290/estubtdb.543355

Abstract

Dust transports cause significant
increases in atmospheric concentration and surface PM10 particulate matter. In
recent years, Asian countries have experienced dust transport frequently. Dust
transport has a significant negative impact on human health, the economy and
the environment. This study includes the analysis of source regions and dust
transport dated in 27-29 May 2018 over Turkmenistan. In the study, a general
dust situation of Turkmenistan region has been studied by using MODIS AOD data.
Then, the meteorological conditions and the pathway of this dust transport
event on were examined. The preliminary analysis using synoptic analyzes and
satellite data showed that the dust transport is coming through Uzbekistan and
Kazakhstan. The transport took place on the south direction and affected most
of Turkmenistan on 27 May 2018. Observed AOD data in the region increased
significantly and took its maximum on 27 May 2018. The effect of this movement
in Turkmenistan lasted until 30 May 2018. The global CAMS dust model has
generally estimated dust transport event even some overestimations. MSG/RGB
satellite products were examined detailly in order to analyze the source
regions of this dust transport. The analyzes showed the main source region of
this dust transport as Aral lake.

References

  • [1] Banacos PC and Ekster ML. The association of the elevated mixed layer with significant severe weather events in the Northeast United States. Wea. Forecasting 2010; 25: 1082-1102.
  • [2] Dündar C, Oğuz K and Güllü G. Evaluation of Sand and Dust Storms (SDS) over Eastern Mediterranean Basin. 10. National Conference on Environmental Engineering; 12-14 September 2013; Hacettepe University, Ankara, Turkey.
  • [3] Goudie AS and Middleton NJ. Saharan dust storms: nature and consequences. Earth-Science Reviews 2001; 56; 179–204.
  • [4] Indoitu R, Orlovsky L and Orlovsky N. Dust storms in Central Asia: spatial and temporal variations. J Arid Environ 2012; 85; 62–70.
  • [5] IPCC 2007 Summary for policymakers in Climate Change 2007: the Physical Science Basis; Cambridge University Press, New York, NY, USA.
  • [6] Jickells TD, An ZS, Andersen KK, Baker AR, Bergametti G, Brooks N, Cao JJ, Boyd PW, Duce RA, Hunter KA, Kawahata H, Kubilay N, laRoche J, Liss PS, Mahowald N, Prospero JM, Ridgwell AJ, Tegen I and Torres R. Global iron connections between desert dust, ocean biogeochemistry, and climate. Science 2005; 308; 5718 67– 71.
  • [7] Kalnay et al. The NCEP/NCAR 40-year reanalysis Project. Bull. Amer. Meteor. Soc. 1996; 77; 437-470.
  • [8] Lensky IM and Rosenfeld D. Clouds-Aerosols-Precipitation Satellite Analysis Tool (CAPSAT). Atmos. Chem. Phys. 2008; 8; 6739–6753.
  • [8] Lohmann U and Feichter J Global indirect aerosol effects: a review. Atmospheric Chemistry and Physics 2005; 5 3; 715–737.
  • [9] Moore BJ, Neiman PJ, Ralph FM and Barthold F. Physical processes associated with heavy flooding rainfall in Nashville, Tennessee, and vicinity during 1–2 May 2010: The role of an atmospheric river andmesoscale convective systems. Mon. Weather Rev. 2012; 140; 358–378.
  • [10] Naruse T, Sakai H and Inoue K. Aeolian dust origin of fine quartz in selected soils. Japan Quat Res (Tokyo) 1986; 24; 295–300.
  • [11] Notaro M, Alkolibi F, Fadda E, and Bakhrjy F. Trajectory analysis of Saudi Arabian dust storms. J. Geophys. Res. Atmos. 2013; 118; 6028–6043.
  • [12] Orlovsky L, Orlovsky N and Durdyev A. Dust storms in Turkmenistan. Journal of Arid Environments 2005; 60; 83–97.
  • [13] Prospero JM, Ginoux P, Torres O, Nicholson S, Gill TE. Environmental characterization of global sources of atmospheric soil dust derived from the NIMBUS&TOMS absorbing aerosol product. Rev. Geophys. 2002; 40; 1 2-1-2-31.
  • [14] Rolph GD 2012 Real-time Environmental Applications and DisplaysYstem (READY) website (http://ready.arl.noaa.gov); NOAA AirResources Laboratory, Silver Spring, MD.
  • [15] Solomos S, Ansmann A, Mamouri RE, Binietoglou I, Patlakas P, Marinou E and Amiridis V. Remote sensing and modelling analysis of the extreme dust storm hitting the Middle East and eastern Mediterranean in September 2015. Atmos. Chem. Phys. 2017; 17; 4063-4079.
  • [16] Shen H, Abuduwaili J, Ma L and Samat A. Remote sensing-based land surface change identification and prediction in the Aral Sea bed, Central Asia. International Journal of Environmental Science and Technology 2018; 1-16.
  • [17] https://www.arl.noaa.gov/hysplit/hysplit/
  • [18] https://modis.gsfc.nasa.gov/about/

ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS

Year 2020, Volume: 8 Issue: 1, 61 - 72, 28.02.2020
https://doi.org/10.20290/estubtdb.543355

Abstract

Dust transports cause significant
increases in atmospheric concentration and surface PM10 particulate matter. In
recent years, Asian countries have experienced dust transport frequently. Dust
transport has a significant negative impact on human health, the economy and
the environment. This study includes the analysis of source regions and dust
transport dated in 27-29 May 2018 over Turkmenistan. In the study, a general
dust situation of Turkmenistan region has been studied by using MODIS AOD data.
Then, the meteorological conditions and the pathway of this dust transport
event on were examined. The preliminary analysis using synoptic analyzes and
satellite data showed that the dust transport is coming through Uzbekistan and
Kazakhstan. The transport took place on the south direction and affected most
of Turkmenistan on 27 May 2018. Observed AOD data in the region increased
significantly and took its maximum on 27 May 2018. The effect of this movement
in Turkmenistan lasted until 30 May 2018. The global CAMS dust model has
generally estimated dust transport event even some overestimations. MSG/RGB
satellite products were examined detailly in order to analyze the source
regions of this dust transport. The analyzes showed the main source region of
this dust transport as Aral lake.

References

  • [1] Banacos PC and Ekster ML. The association of the elevated mixed layer with significant severe weather events in the Northeast United States. Wea. Forecasting 2010; 25: 1082-1102.
  • [2] Dündar C, Oğuz K and Güllü G. Evaluation of Sand and Dust Storms (SDS) over Eastern Mediterranean Basin. 10. National Conference on Environmental Engineering; 12-14 September 2013; Hacettepe University, Ankara, Turkey.
  • [3] Goudie AS and Middleton NJ. Saharan dust storms: nature and consequences. Earth-Science Reviews 2001; 56; 179–204.
  • [4] Indoitu R, Orlovsky L and Orlovsky N. Dust storms in Central Asia: spatial and temporal variations. J Arid Environ 2012; 85; 62–70.
  • [5] IPCC 2007 Summary for policymakers in Climate Change 2007: the Physical Science Basis; Cambridge University Press, New York, NY, USA.
  • [6] Jickells TD, An ZS, Andersen KK, Baker AR, Bergametti G, Brooks N, Cao JJ, Boyd PW, Duce RA, Hunter KA, Kawahata H, Kubilay N, laRoche J, Liss PS, Mahowald N, Prospero JM, Ridgwell AJ, Tegen I and Torres R. Global iron connections between desert dust, ocean biogeochemistry, and climate. Science 2005; 308; 5718 67– 71.
  • [7] Kalnay et al. The NCEP/NCAR 40-year reanalysis Project. Bull. Amer. Meteor. Soc. 1996; 77; 437-470.
  • [8] Lensky IM and Rosenfeld D. Clouds-Aerosols-Precipitation Satellite Analysis Tool (CAPSAT). Atmos. Chem. Phys. 2008; 8; 6739–6753.
  • [8] Lohmann U and Feichter J Global indirect aerosol effects: a review. Atmospheric Chemistry and Physics 2005; 5 3; 715–737.
  • [9] Moore BJ, Neiman PJ, Ralph FM and Barthold F. Physical processes associated with heavy flooding rainfall in Nashville, Tennessee, and vicinity during 1–2 May 2010: The role of an atmospheric river andmesoscale convective systems. Mon. Weather Rev. 2012; 140; 358–378.
  • [10] Naruse T, Sakai H and Inoue K. Aeolian dust origin of fine quartz in selected soils. Japan Quat Res (Tokyo) 1986; 24; 295–300.
  • [11] Notaro M, Alkolibi F, Fadda E, and Bakhrjy F. Trajectory analysis of Saudi Arabian dust storms. J. Geophys. Res. Atmos. 2013; 118; 6028–6043.
  • [12] Orlovsky L, Orlovsky N and Durdyev A. Dust storms in Turkmenistan. Journal of Arid Environments 2005; 60; 83–97.
  • [13] Prospero JM, Ginoux P, Torres O, Nicholson S, Gill TE. Environmental characterization of global sources of atmospheric soil dust derived from the NIMBUS&TOMS absorbing aerosol product. Rev. Geophys. 2002; 40; 1 2-1-2-31.
  • [14] Rolph GD 2012 Real-time Environmental Applications and DisplaysYstem (READY) website (http://ready.arl.noaa.gov); NOAA AirResources Laboratory, Silver Spring, MD.
  • [15] Solomos S, Ansmann A, Mamouri RE, Binietoglou I, Patlakas P, Marinou E and Amiridis V. Remote sensing and modelling analysis of the extreme dust storm hitting the Middle East and eastern Mediterranean in September 2015. Atmos. Chem. Phys. 2017; 17; 4063-4079.
  • [16] Shen H, Abuduwaili J, Ma L and Samat A. Remote sensing-based land surface change identification and prediction in the Aral Sea bed, Central Asia. International Journal of Environmental Science and Technology 2018; 1-16.
  • [17] https://www.arl.noaa.gov/hysplit/hysplit/
  • [18] https://modis.gsfc.nasa.gov/about/
There are 19 citations in total.

Details

Primary Language English
Subjects Engineering
Journal Section Articles
Authors

Kahraman Oğuz 0000-0001-5305-6145

Publication Date February 28, 2020
Published in Issue Year 2020 Volume: 8 Issue: 1

Cite

APA Oğuz, K. (2020). ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS. Eskişehir Teknik Üniversitesi Bilim Ve Teknoloji Dergisi B - Teorik Bilimler, 8(1), 61-72. https://doi.org/10.20290/estubtdb.543355
AMA Oğuz K. ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS. Eskişehir Teknik Üniversitesi Bilim ve Teknoloji Dergisi B - Teorik Bilimler. February 2020;8(1):61-72. doi:10.20290/estubtdb.543355
Chicago Oğuz, Kahraman. “ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS”. Eskişehir Teknik Üniversitesi Bilim Ve Teknoloji Dergisi B - Teorik Bilimler 8, no. 1 (February 2020): 61-72. https://doi.org/10.20290/estubtdb.543355.
EndNote Oğuz K (February 1, 2020) ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS. Eskişehir Teknik Üniversitesi Bilim ve Teknoloji Dergisi B - Teorik Bilimler 8 1 61–72.
IEEE K. Oğuz, “ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS”, Eskişehir Teknik Üniversitesi Bilim ve Teknoloji Dergisi B - Teorik Bilimler, vol. 8, no. 1, pp. 61–72, 2020, doi: 10.20290/estubtdb.543355.
ISNAD Oğuz, Kahraman. “ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS”. Eskişehir Teknik Üniversitesi Bilim ve Teknoloji Dergisi B - Teorik Bilimler 8/1 (February 2020), 61-72. https://doi.org/10.20290/estubtdb.543355.
JAMA Oğuz K. ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS. Eskişehir Teknik Üniversitesi Bilim ve Teknoloji Dergisi B - Teorik Bilimler. 2020;8:61–72.
MLA Oğuz, Kahraman. “ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS”. Eskişehir Teknik Üniversitesi Bilim Ve Teknoloji Dergisi B - Teorik Bilimler, vol. 8, no. 1, 2020, pp. 61-72, doi:10.20290/estubtdb.543355.
Vancouver Oğuz K. ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS. Eskişehir Teknik Üniversitesi Bilim ve Teknoloji Dergisi B - Teorik Bilimler. 2020;8(1):61-72.