Chinese Physics B, Volume. 29, Issue 8, (2020)

Mesoscale eddies and their dispersive environmental impacts in the Persian Gulf

Amin Raeisi1, Abbasali Bidokhti2、†, Seyed Mohammad Jafar Nazemosadat3, and Kamran Lari4
Author Affiliations
  • 1Faculty of Natural Resources and Environment, Science and Research Branch, Islamic Azad University, Tehran 477893855, Iran
  • 2Geophysics Institute, University of Tehran, Tehran 1417614418, Iran
  • 3Department of Water Engineering, Oceanic and Atmospheric Research Center, Shiraz University, Shiraz 71444165186, Iran
  • 4Department of Physical Oceanography, Faculty of Marine Science and Technology, Tehran North Branch, Islamic Azad University, Tehran 1987973133, Iran
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    Figures & Tables(11)
    (a) Map of the Persian Gulf region based on ETOPO2 data, depth in terms of meters.[4] (b) Water circulation in the Persian Gulf from August to November.[9]
    Height contours in the Persian Gulf for various seasons on (a) 19 August 2014 and (b) 12 February 2014.
    Histogram of the mean number of eddies in different months from 2010 to 2014.
    Percentage of the monthly mean of eddies considering their polarity (2010–2014) (the red and blue histograms are assigned to anti-cyclonic and cyclonic eddies, respectively).
    The dispersion histogram of the percentage of the mean of eddy diffusion coefficient over a tensile interval (the red and blue histograms are assigned to the anti-cyclonic and cyclonic eddies, respectively).
    Maps showing the place of eddies in winter (a) and summer (b) 2014 (the cyclonic and anti-cyclonic eddies with the highest diffusion coefficient are represented by five-pointed blue and red stars, respectively).
    The contour maps showing eddy diffusion coefficients in summer (2014) (the high-risk areas are marked with a number).
    (a) and (b) Maps extracted from simulations provided by Thoppil and Hugan[8] (left) and SSH maps plotted based on AVISO data (right).
    • Table 1. Percentage of the seasonal mean of eddies considering the polarity (2010–2014).

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      Table 1. Percentage of the seasonal mean of eddies considering the polarity (2010–2014).

      SpringSummerAutumnWinterTotal
      Cyclonic62.10%58.60%55.90%60.90%59.10%
      Anti-cyclonic37.90%41.40%44.10%39.10%40.90%
    • Table 2. Eddies with the highest diffusion coefficients kxy (2014).

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      Table 2. Eddies with the highest diffusion coefficients kxy (2014).

      SeasonNumber of eddiesLeff/kmkxy/(m2/s)Lifetime/weekDate of event
      Winter20102.9576.70126 February
      2(AC)105.2754.2125 December
      1865.7953.1535 March
      2173.8852.33126 February
      Spring2148.3487.2533 June
      2185.5982.68327 May
      2452.7969.35110 June
      1349.8662.8516 May
      Summer453.79116.81415 July
      395.69108.6728 July
      1102.42108.09215 July
      960.12107.0162 September
      Autumn577.8079.11321 October
      3463.1472.53123 December
      14(AC)57.5169.9342 December
      32(AC)47.2568.08123 December
    • Table 3. Areas of eddy occurrence along with the mean of diffusion coefficients in summer (2014).

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      Table 3. Areas of eddy occurrence along with the mean of diffusion coefficients in summer (2014).

      Number of areaArea/km2The mean of diffusion coefficient in the target area/(m2/s)Location
      Longitude/degreeLatitude/degree
      fromtofromto
      115220.9978.0525.7827.5751.3853.82
      22443.0976.0225.7426.4253.4253.98
      34573.5570.0825.5126.154.3755.28
      43901.5965.2327.5728.4048.9250.21
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    Amin Raeisi, Abbasali Bidokhti, Seyed Mohammad Jafar Nazemosadat, Kamran Lari. Mesoscale eddies and their dispersive environmental impacts in the Persian Gulf[J]. Chinese Physics B, 2020, 29(8):

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    Paper Information

    Received: Mar. 21, 2020

    Accepted: --

    Published Online: Apr. 29, 2021

    The Author Email: Bidokhti Abbasali (bidokhti@ut.ac.ir)

    DOI:10.1088/1674-1056/ab96a3

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