line gale

line gale的基本解释

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二分点风暴

与line gale相关的网络例句 [注：此内容来源于网络，仅供参考]

Based on the new generation weather radar data,Micaps data,Auto-station observation data and MM5 products,a squall line gale process with disaster gale,weak precipitation and local hail occurred in Linyi on April 28,2006 is analyzed.

利用临沂新一代天气雷达观测资料，结合MICAPS资料、加密自动气象站观测资料、MM5模式数值预报产品，对2006年4月28日发生在临沂的一次以灾害性大风为主、有弱降水相伴随、局部还有冰雹发生的飑线天气过程进行了分析。

Using conventional survey and ground encryption observations and T213 amount prediction product and fy-2c/2d infrared satellite cloud chart data, weather power diagnosis and mesoscale analysis of gale and strong sandstorm process initiated by squall line are carried on May 2, 2008 in east of Hexi corridor.

利用常规探测、地面加密观测、T213数值预报产品和fy-2c/2 d红外卫星云图资料对2008年5月2日河西走廊东部飑线引发的强沙尘暴过程进行了天气动力诊断和中尺度分析。

The result showed that the strong storm followed by mesoscale squall line was primary cause of strong sandstorm producing, steps and ladders short wave trough of 500 hPa was great criterion triggering system for the mesoscale squall line producing, the essential dynamic condition was provided by distortion field and the mesoscale low pressure of 700 hPa for the strong sandstorm forming and maintaining in mid-west of Hexi Corridor, the deep vertical circulation development condition was basic power that urged squall line to occur and sand dust to curl up, which was provided for the deep convection development by superimposition of lifting movement before ground cold front and ascendant current of secondary circulation in upper air jet entrance region, temperature and the barometric gradient around the cold front was enlarged by enhancement of ground thermal low and temperature diurnalvariation of afternoon, by which essential thermal energy unstable condition was provided for the gale and strong sandstorm eruption, the strong sandstorm appeared in downstream of -200 m^2s^(-2) center of vertical helicity, the vertical helicity had good instruction significance for development of squall line and landing region of sandstorm, the mesoscale squall line occurred in unstable stratification, basic condition of potential energy transforming as kinetic energy was provided by strong unstable stratification for the strong sandstorm forming and developing.

结果表明：中尺度飑线所伴随的强风暴是产生强沙尘暴的主要原因；500 hPa阶梯短波槽是中尺度飑线产生的大尺度触发系统，河西走廊中西部700 hp变形场、中尺度低压为强沙尘暴形成和维持提供了必要的动力条件；地面冷锋前上升运动与高空急流入口区次级环流的上升气流的叠加，为深对流发展提供了深厚的垂直环流发展条件，是促使飑线发生和沙尘卷起的基本动力；地面热低压的加强和午后气温的日变化加大了冷锋前后的温度和气压梯度，为大风、强沙尘暴爆发提供了必要的热力不稳定条件；强沙尘暴出现在垂直螺旋度为－200平方公尺/s^2中心的下游，垂直螺旋度对飑线的发展和沙尘暴的落区具有较好的指示意义；中尺度飑线发生在不稳定层结内，较强的不稳定层结为强沙尘暴形成、发展提供了位能转化为动能的基本条件。

与line gale相关的网络解释 [注：此内容来源于网络，仅供参考]

freshet：春汛 ;暴漲 ;暴漲溪

强风 fresh gale; line blow; strong breeze | 春汛;暴涨;暴涨溪 freshet | 淡水 frest water

fresh gale; line blow; strong breeze：强风

清风 fresh breeze; fresh wind | 强风 fresh gale; line blow; strong breeze | 春汛;暴涨;暴涨溪 freshet

line gale; line storm：二分风暴

二分风暴 line gale; line storm | 线积分 line integral | 远近线 line of apsides