2010
DOI: 10.1007/s11430-010-4104-y
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Characteristics of the lower layer of sandstorms in the Minqin desert-oasis zone

Abstract: By measuring the sand-dust flux, vertical deposition, and the wind velocity throughout 19 sandstorms in the Minqin region, we quantitatively analyzed the horizontal distribution and vertical variation in sandstorm characteristics under different land cover conditions. The effect of different land cover on mitigating sandstorms was also investigated. The results indicated that, in the surface layer ranging from 0-50 m, the intensity of sand-dust horizontal flux and concentration of sand-dust decreased with the … Show more

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Cited by 13 publications
(7 citation statements)
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“…There were obvious differences in wind speed, wind direction, and eolian sediment flux inside and outside shelterbelt in the northeastern edge of Ulan Buh Desert. The results were consistent with the wind speed distribution characteristics of Minqin Oasis and Badain Jaran Desert on the oasis and desert-oasis region, which increased with the height from 0 to 50 m [37]. During the occurrence of sandstorms, wind speed profile and the migration process of sand and dust particles were affected by the type of underlying surface, thereby affecting the distribution of aeolian sediment flux [38][39][40].…”
Section: Discussionsupporting
confidence: 77%
“…There were obvious differences in wind speed, wind direction, and eolian sediment flux inside and outside shelterbelt in the northeastern edge of Ulan Buh Desert. The results were consistent with the wind speed distribution characteristics of Minqin Oasis and Badain Jaran Desert on the oasis and desert-oasis region, which increased with the height from 0 to 50 m [37]. During the occurrence of sandstorms, wind speed profile and the migration process of sand and dust particles were affected by the type of underlying surface, thereby affecting the distribution of aeolian sediment flux [38][39][40].…”
Section: Discussionsupporting
confidence: 77%
“…One sample from each type of coating was investigated for two different velocities, namely 12.2 and 17.1 m s −1 and four consecutive erosions treatments were applied to every sample, lasting 10 minutes each. The setpoint for dust concentration was 100 mg m −3 as it has been measured in a field study [19] and comparable values have been used for accelerated aging experiments already [20,8]. However this setpoint was constantly exceeded by a factor of around There was an additional water jet cleaning applied in the end, to check on the effectiveness of the ultrasonic cleaning.…”
Section: Testing and Cleaning Proceduresmentioning
confidence: 98%
“…It is of high scientific importance and potential value to study the inversion of atmospheric temperature and humidity profile using microwave radiometer data [10]. However, the brightness temperature (BT) data from different channels of the MWR are disturbed by precipitation and cloud factors, resulting in abnormal values [11][12][13]. Meanwhile, when the sun is in the observation direction of the MWR, the BT data will be abnormally increased due to the influence of solar radiation, especially those used in low latitudes [14].…”
Section: Introductionmentioning
confidence: 99%