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1)  floating dust weather
浮尘天气
1.
It was found that the impact systems of the floating dust weather were West Siberia cold eddy,Okhotsk warm high and Tibetan Plateau high ridge at the level of 500 hPa;the dry-cold air at the level of 700 hPa transferred to Beijing ceaselessly,and the cold advection and baroclinic instability were strong,the gale and dust storm occurred in the strong cold advection area;the we.
使用NCEP/NCAR再分析资料对2006年4月7~11日北京浮尘天气过程的持续性进行分析,指出此次浮尘天气过程主要受500 hPa西西伯利亚冷涡、鄂霍次克海暖高压以及青藏高原高压脊影响;700 hPa有干冷空气不断向北京地区输送,冷平流和斜压性都很强,大风和沙尘暴发生在强冷平流区域;由于华北南部地区近地面至中低层存在弱的不稳定层结,容易产生弱的上升运动。
2)  air dust;airborne dust
气浮尘末
3)  Dusty weather
沙尘天气
1.
Based on the retrieval principles of aerosol optical property and combination with surface observational data, some interesting results and elementary classification criteria of different dusty weather according to aerosol optical depth (AOD) had been obtained and were presented a.
同时结合我国已有的沙尘气溶胶光学特性的研究成果,初步提出了依据气溶胶光学厚度判断沙尘天气强度的标准。
2.
During dusty weather the strong wind brings sand-dust but blows chemical pol.
本文阐述了北京沙尘天气的总体概况。
3.
The paper touches upon the dusty weather which has caused serious influence on the northern part of China, especially the sandstorm disaster and its harm.
论述了我国北方地区造成严重影响的沙尘天气 ,特别是沙尘暴及其危害及研建完成的“沙尘暴的卫星遥感监测与灾情评估系统”及其监测评估实例。
4)  Dust weather
沙尘天气
1.
Evolvement characteristics of dust weather events in Northwest China and the Tibetan Plateau;
中国西北及青藏高原沙尘天气演变特征
2.
Observation of Sand-Dust Weather by Lidar in the Spring of 2005 at Beijing;
激光雷达观测2005年春季北京沙尘天气
3.
The dust weather of Northwest China during the Qing Dynasty;
清代西北地区的沙尘天气
5)  sand-dust weather
沙尘天气
1.
Relation between riverbed alluvial deposits in the Harbin reach of the Songhuajiang River and sand-dust weather;
松花江哈尔滨段河床冲积物与沙尘天气关系的讨论
2.
The changing characteristic of sand-dust weather in recent 54 years and future trend forecast in the southern margin of Tarim Basin
塔里木盆地南缘近54年沙尘天气的变化特征及其未来趋势预测
3.
Material composition of city surface soil in Harbin in relation to sand-dust weather
哈尔滨城市地表土的物质组成与沙尘天气
6)  dust storm
沙尘天气
1.
Temporal variation of air pollution and influence of dust storms and other meteorological factors on air pollution in Xi'an City have been investigated by using data of annual mean concentration of TSP, SO_(2) and NO_(x) from 1981 to 2000, data of weekly reports and daily reports of environmental monitoring from 1998 to 2000 as well as data of routine surface and upper air observation.
通过对西安市1981—2000年TSP、SO2和NOx年平均浓度资料,1998—2000年周报和日报环境监测资料以及相应的地面、高空常规气象观测资料的统计分析,研究了该市空气污染的时间变化特点以及沙尘天气等几种气象条件对其浓度变化的影响。
2.
Results show that Mongolia was the initial source of the dust storm influencing Korea,where it occurred between high pressure and cold front.
利用气象卫星、天气形势场和NCEP/NCAR再分析资料,分析了2002年3月21—22日影响韩国沙尘天气的原因。
3.
Base characteristics of the anomalous spring dust storm in 2006 have been analyzed in this paper,and it is found that the spring dust storm in 2006 happened frequently and is stronger than the usual.
作者概述了2006年春季我国北方地区沙尘天气异常的观测特征。
补充资料:虫豸诗·浮尘子
【诗文】:
可叹浮尘子,纤埃喻此微。宁论隔纱幌,并解透绵衣。
有毒能成痏,无声不见飞。病来双眼暗,何计辨雰霏。
乍可巢蚊睫,胡为附蟒鳞。已微于蠢蠢,仍害及仁人。
动植皆分命,毫芒亦是身。哀哉此幽物,生死敌浮尘。
但觉皮肤憯,安知琐细来。因风吹薄雾,向日误轻埃。
暗啮堪销骨,潜飞有祸胎。然无防备处,留待雪霜摧。



【注释】:



【出处】:
全唐诗:卷399-7
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