1) heary dustfall
特大尘暴
2) Desposition of the extremely severe sandstorm
特大沙尘暴降尘
3) heavy dust storm
特强沙尘暴
1.
Based on FY-2 infrared images and the reanalysis data for six hours of NCEP(1°×1°),the heavy dust storm process occurred on 13 April 2007 in the middle west part of Hexi corridor is analyzed,particularly the cloud head of the descending jet was tracked and the gravitational instability,conditional symmetric instability and conditional instability are diagnosed in detail.
2007年4月13日在河西走廊中西部发生了特强沙尘暴,极大风速25m/s,最小能见度50m。
2.
Based on the past research works we theoretically analyzed the formation mechanism of heavy dust storm and discussed the action of atmospheric strong advection to heavy dust storm (black wind).
在总结过去研究结果的基础上,对特强沙尘暴的发生机制进行了进一步的理论分析,探讨了大气强对流对特强沙尘暴(黑风)形成的作用;从物理上系统解释了特强沙尘暴天气的沙尘壁特征;概述了特强沙尘暴的大气沙尘粒子尺度和垂直分布;定性评估了沙尘暴的直接和间接、短期和长期气候效应;最后,还讨论了沙尘暴研究中存在的一些关键科学问题。
4) severe sandstorm
特强沙尘暴
1.
In this paper the heavy sandstorms are that whose shortest visibility is less than 500 m, and the severe sandstorms less than 200 m.
从陕西1954—2003年所有沙尘暴记录所对应的3次或4次定时能见度观测资料中挑出最小能见度小于500m的作为强沙尘暴记录,小于200m的作为特强沙尘暴记录。
6) gale and duststorm
大风沙尘暴
1.
This paper statistically analyzed the data of gale and duststorms from 1960 to 2004 observed at the six weather stations in Zhangye City in central Hexi Corridor during the past 45 years,then analyzed in detail the space-time distribution and forming cause of gale and duststorm weather,and has concluded their formative atmospheric circulation situation characteristics and influencing system.
统计了1960—2004年甘肃河西走廊中部张掖市6个气象站近45 a的实测大风沙尘暴资料,详细分析了该市大风沙尘暴天气的时空分布及形成原因,并归纳出其形成的大气环流形势特征和影响系统。
补充资料:尘暴
尘暴 dust storm 大量尘土沙粒被强劲阵风或大风吹起,飞扬于空中而使空气混浊、水平能见度小于1千米的现象。又称沙暴。中国新疆南部和河西走廊的强沙暴,有时可使能见度接近于零,这时白昼如同黑夜,当地人称为黑风。尘暴一般发生在土地干燥、土质松散而无植被覆盖的地区,中国在春季较常出现,以西北、内蒙古、华北和东北等地区最多。尘暴形成时,一般风速在10米/秒以上,且空气热力不稳定。严重的尘暴可导致沙漠迁移、毁坏良田、掩埋作物和交通中断。采取植树种草、固沙固土的措施,是防止尘暴侵袭的有效措施。 |
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