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| Global Solar Radiation over Different Underlying Surfaces in the Taklimakan Desert |
| Jin Lili1, He Qing1,2, Li Zhenjie3, Ali Mamtimin1,2 |
1. College of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing 210044, China;
2. Taklimakan Desert Atmosphere and Environment Observation Experiment Station, Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China;
3. Lincang Meteorological Bureau, Lincang 677099, Yunnan, China |
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Abstract The global solar radiation data collected in observation station in Xiaotang (40 48'N,84°18'E), Hade (40°46'N,83°42'E) and Tazhong (38°58'N,83°39'E) from 2010 to 2011 were used to analyze the characteristics of the diurnal variation of the global solar radiation over different underlying surfaces in the Taklimakan Desert. The results show that the annual total global solar radiation is 5 666.4 MJ·m-2, 5 774.5 MJ·m-2 and 6 515.0 MJ·m-2 in Xiaotang, Hade and Tazhong station, respectively. The seasonal change of the global solar radiation of Tazhong is higher than Xiaotang and Hade, and it is similar in Xiaotang and Hade. The maximum global solar radiation is in summer in the three stations, and minimum in winter, it is higher in spring than in autumn. The maximum/minimum values of monthly total global solar radiation are in June/December in Tazhong, but the maximum/minimum values reach the peaks/troughs in July/December in Xiaotang and Hade. The global solar radiation in Tazhong is higher than in Xiaotang and Hade, the difference values are 99.4 MJ·m-2 and 81.9 MJ·m-2, respectively. The peak value of mean global solar radiation appears at 12:00, and the lowest value appears in the morning or evening. The diurnal variation of global solar radiation is irregular on sand-storm day because the global solar radiation is obviously influenced by sand-storm. The peak values of global solar radiation decrease on sand-storm day by 40.3%, 56.2% and 53.0% in Xiaotang, Hade and Tazhong, respectively, and the daily total global solar radiation is reduced by 41.6%, 57.8% and 61.2%, respectively. The attenuation of global solar radiation is still apparent after sandstorm day, and the daily curve shows previous state when the sandstorm process stop. Sand-dust process can increase/decrease low-value/high-value (especially global solar radiation >500 W·m-2)probability distribution to influence the global solar radiation obviously. The global solar radiation increases with the solar zenith angle. The value of global solar radiation is high on clear day but small on sand-dust day at the same solar zenith angle.
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Received: 08 April 2013
Published: 20 March 2014
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2014, Vol. 34 
