2017
DOI: 10.3390/cli5040082
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Investigation of the Spatio-Temporal Variations in Atmosphere Thickness Pattern of Iran and the Middle East with Special Focus on Precipitation in Iran

Abstract: Abstract:In this study, Geopotential Height (between 500 and 1000 hPa) and precipitation data were obtained from the NCEP/NCAR and IRIMO (Iran Meteorological Organization) for 60 years , respectively. Descriptive features of Atmospheric Thickness (hereafter AT) were calculated and analyzed by using the Mann-Kendall method. The results showed that the maximum AT was recorded in summer because of the dominance of the dynamic, hot subtropical high pressure. Furthermore, upper latitudes experienced more variations… Show more

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Cited by 26 publications
(11 citation statements)
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“…In contrast, dust storm frequency decreased over time in Hail, Qaisumah, Hafar Al-Batin, Al-Qassim, and Bisha. Also, our results showed a shift in dust storms from the northeast, possibly caused by the wind between the high pressure over the Mediterranean Sea and the low pressure in Saudi Arabia [80] to the southeast. The prevailing wind direction during dust-free and dust storm days varied across different parts of the country.…”
Section: Discussionmentioning
confidence: 58%
“…In contrast, dust storm frequency decreased over time in Hail, Qaisumah, Hafar Al-Batin, Al-Qassim, and Bisha. Also, our results showed a shift in dust storms from the northeast, possibly caused by the wind between the high pressure over the Mediterranean Sea and the low pressure in Saudi Arabia [80] to the southeast. The prevailing wind direction during dust-free and dust storm days varied across different parts of the country.…”
Section: Discussionmentioning
confidence: 58%
“…Land surface temperature (LST) is a principal characteristic for the evaluation of energy exchange between the land and the atmosphere [1][2][3]. This parameter is applicable to numerous sciences such as climatology, hydrology, agriculture, ecology, public health, and the environment [4][5][6][7][8][9][10][11][12][13][14][15]. One of the methods for measuring LST is to use satellite data and thermal remote sensing techniques.…”
Section: Introductionmentioning
confidence: 99%
“…The lowest elevation of the area is 1400 m and the highest elevation is 3800 m from the sea level. Average precipitation for the whole study area is 150 mm, while the amount comes to 60 mm in low elevation places and 230 mm in higher places [42][43][44][45][46][47]. The highest percentage of vegetation coverages are clustered in the regions where villages and gardens are located (brown color regions).…”
Section: Study Areamentioning
confidence: 99%