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24 March 1999, Volume 18 Issue 1   
  • THE INFLUENCE OF ATMOSPHERIC DUST ON THE SURFACE RADIATIVE ENERGY BUDGET IN THE HEIFE AREA
  • SHEN Zhi-Bao;WEI Li
  • 1999 Vol. 18 (1): 1-8. 
  • Abstract ( ) PDF (307KB) ( )
  • The influences of the atmospheric dust on the surface radiative energy budget was analysed and estimated by using the data of the atmospheric turbidity and the surface radiation balance observed at Zhangye (oasis) and Desert stations in the HEIFE area during the period from the third decade of February to the secend decade of May in 1991.The downward components of both short and long wave radiations are affected obviously by the atmospheric dust. There are a good relationship between the atmospheric transmitttance and atmospheric turbidity coefficient. The atmospheric transmittance and surface global radiation decrease as the atmospheric turbidity increase. The surface global radiation at noon decrease 67.6~85.8 W/m 2(7.0%~9.2 %) in April when the atmospheric turbidity increase from 0.1~0.6, in other words, it decrease 1.3%~1.9% as the atmospheric turbidity increase 0.1. This decrease is larger in the desert than that in the oasis. The positive corelation was fund between the downward long wave radiation and the atmospheric turbidity. The downward long wave radiation at noon increase more than 21.6 W/m 2 (9.0%~10.5%)at Desert station and 17.3 W/m 2 (7.6%~12.8%) at Zhangye station respectively in the very turbid days (the atmospheric turbidity coefficient are larger than 0.450) as compared with that in the clear day. The same results were fund in the night. The upward long wave radiation seems to decrease in the turbid day. The influence of the atmospheric dust on the surface radiative energy budget is to decrease the surface net radiation in the day time, but not obvious in the night. The surface net radiation at noon decreases about 43~58 W/m 2 (about 9%~12%) in the very turbid days at Desert station as compared with that in the clear day, but at Zhangye station the results are not the regurarity same as that at Desert station because the surface conditions in the oasss were affected by the irrigation.