宁夏春季沙尘暴暴发的环流及OLR场特征分析-自然灾害学报.PDF

宁夏春季沙尘暴暴发的环流及OLR场特征分析-自然灾害学报.PDF

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宁夏春季沙尘暴暴发的环流及OLR场特征分析-自然灾害学报

17 4 Vo.l 17, No. 4 2008 8 JOURNAL OF NATURAL D ISASTERS Aug. , 2008 : 1004-4574( 2008) 04- 0059- 07 OLR 1 1, 2 1 1 陈 楠 , 赵光平 , 陈豫英 , 陈晓光 ( 1. , 750002; 2. , 7 0020) : 1970- 200 , NCEP/NCAR ( OLR), ( - 5) OLR : , , 500hPa , 200hPa; , , OLR , , , , ; , OLR : ; ; OLR; : P425. 5. 5 : A Character analysis of circulation and OLR field w ith regard to spring sandstorm breakout in Ningxia 1 1, 2, * 1 1 CHEN Nan , ZHAO Guang-p ing , CHEN Yu-ying , CHEN X iao-guang ( 1K ey Laboratory ofM eteorolog icalD isaster Prevention and Reduction of N ingx ia, Y inchuan 750002, China; 2 Gansu AridM eteorology Institute, CMA, Lanzhou 7 0020, China) Abstract: U sing the sandstorm data ofN ingxia in 1970- 200 , the global monthly mean NCEP /NCAR reanalyzed data and themonthly mean OLR, the comparative diagnostic analysis of the height fields in h igh and low leve,l the cross fields of zonal flow and the difference of OLR field for the sandstorm freguently and rarely occurring years in N ingxia in spring (M arch-M ay) w as conducted. Resu lts show that the positions and intensity of geopotential height fields and the number of sandstorms is closely related. In the yearw ith more sandstorm s, there is a negative anom a- ly area at 500hPa height field inMongolia andw est part ofH ex,i jet at 200hPa locates in north ofHetao, and in the area of Bekal Lake there is a negativeOLR anomaly

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