squall [skwɔ:l]

squall的基本解释

n.

暴风雪, 狂风, 哇哇器声

• The baby's squall was heard all over the house.
• 满屋子都听到了婴孩的大哭声。

• My plane ran into a squall over the bay.
• 我的飞机在海湾上空遇上了暴风。

• There was an angry squall from the bedroom.
• 卧室里传出一声愤怒的喊叫。

vi.

嚎啕, 狂风吹袭, 哇哇地叫嚷, 起飑

vt.

尖声叫着, 尖叫

squall的同义词

v. wail · howl · squeal · scream · cry · yell · moan · bawl

n. gust · blizzard · gale

squall所属的单词分类

Weather / 天气 [276]

wind shear  ·  weather satellite  ·  tropical storm  ·  tropical disturbance  ·  tropical depression  ·  supercell  ·  snow level  ·  snow flurry  ·  rain shadow  ·  prevailing wind

与squall相关的网络例句 [注：此内容来源于网络，仅供参考]

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。

The strong sandstorm was caused by squall line activity of eastern Hexi Corridor in Apr. to Jun. that was cold front, majority is in May, four times strong sandstorm is accompanied by the squall line in seven times. It was explained that the squall line was suggested easily when the strong cold front moved east to Hexi Corridor where special canyon tube terrain was in, the strong sandstorm which was created by squall line activity have very strong paroxysm that often created serious disaster.

河西走廊东部的飑线活动造成的强沙尘暴出现在4~6月，均为冷锋型，其中5月居多，出现的7次强沙尘暴中有4次伴有飑线，说明5月份强冷锋东移经河西走廊特殊峡管地形时易诱发飑线，飑线活动造成的强沙尘暴爆发性强，往往造成严重灾情。

The results indicate that the squall line systems are stronger with the increasing of water vapor in the lowest kilometer of atmosphere. The decreasing of water vapor in the height of 3 to 5 kilometer lead to a weaker development of squall line system. The decreasing of water vapor above 5 kilometer level has less impact on the development of the squall line system.

根据 Lin and Arakawa( 1997a，b )的研究指出，积云内部空气逸入源主要来自云顶发展高度以下的区域，且可能来自各种不同的环境高度，因此环境水气的垂直分布情形对积云结构的发展有重要影响。

与squall相关的网络解释 [注：此内容来源于网络，仅供参考]

squall：飑

比斯开湾以多风暴著名,猛烈的暴风时速高达113公里(70哩),一年中任何时候均可发生威胁航行的雷飑(squall). 西班牙北部沿海的大风更加变幻莫测,雷飑更多. 尽管这里是危险的海线,仍有许多重要航线通过海湾. 从史前时代以来,

squall：暴风雨

但是南海的天气多变,热带暴风雨(SQUALL)说来就来说去就去,像青纱帐一样. 抓住了的军舰,一转眼就没了. 伊-65已经锁定了的英国舰队就是一场热带暴风雨给弄丢了的. 现在到哪儿去找?19:45分,元山航空队打道回府了,但在20:10分,

squall：暴风

to furl 卷起(帆) | squall 暴风 | gale 大风

squall：狂风

森林气候forest climate | 狂风squall | 烈风strong gale

squall：abbr. sq; 暴风雨,台