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On the Mechanism of a Terrain-Influenced Snow Burst Event during Midwinter in Northeast China 被引量:6
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作者 Na LI Baofeng JIAO +2 位作者 Lingkun RAN Xinyong SHEN Yanbin QI 《Advances in Atmospheric Sciences》 SCIE CAS CSCD 2021年第5期800-816,共17页
Short-duration snow bursts with heavy snow represent one type of hazardous weather in winter which can be easily missed by the winter weather warnings but often results in great hazards.In this paper,the mechanism for... Short-duration snow bursts with heavy snow represent one type of hazardous weather in winter which can be easily missed by the winter weather warnings but often results in great hazards.In this paper,the mechanism for the occurrence of such events was investigated with the aid of a localized terrain-influenced snow burst event in Northeast China.The snow burst was produced by an eastward-moving cold-frontal snowband which encountered the downstream complex terrain of the Changbai Mountains and intensified.To ascertain the role of orography on the snow burst,numerical experiments,together with a parallel sensitivity experiment removing Changbai Mountains,were performed to attempt to distinguish the contributions of cold-frontal system and orographic effects to produce the heavy snow.Diagnosis showed that without the influence of Changbai Mountains,the release of conditional instability(CI)and inertial instability(II)within a weak frontogenetical environment was responsible for the snowband maintenance.Orographic effects played important roles in enhancing the snowband and increasing the snowfall intensities.The enhancement mechanism was related to the interactions of the cold-frontal snowband and the topography.On the one hand,orographic frontogenesis and persistent ascent,created by orographic gravity waves over the terrain,greatly enhanced the orographic lifting.The intensification of the lifting promoted the release of CI and thus enhanced the snowfall.On the other hand,pre-existing orographic instabilities were released due to the passing of the cold-frontal snowband,which could also serve to intensify the snowband over terrain and thus increase the snowfall. 展开更多
关键词 terrain-influenced snow burst snowband INSTABILITY LIFTING
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结合Ka和X波段双偏振雷达对北京一次锋面降雪过程雪带的观测分析 被引量:10
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作者 武静雅 毕永恒 +1 位作者 孙强 吕达仁 《大气科学》 CSCD 北大核心 2021年第5期931-942,共12页
本文设计了中国科学院大气物理研究所位于同一观测站内的一部单发双收Ka波段双偏振雷达和一部双发双收X波段双偏振雷达高效结合观测的方法,并首次将Ka和X波段双偏振雷达结合应用在降雪过程的观测中,对2019年2月14日锋面气旋系统在北京... 本文设计了中国科学院大气物理研究所位于同一观测站内的一部单发双收Ka波段双偏振雷达和一部双发双收X波段双偏振雷达高效结合观测的方法,并首次将Ka和X波段双偏振雷达结合应用在降雪过程的观测中,对2019年2月14日锋面气旋系统在北京地区降雪过程中雪带的形成、发展、消亡过程的宏微观结构进行了分析。结果表明,雪带的垂直结构符合以往对层状云垂直分层的物理认识,类似但不同于雨带由凝结增长层、丛集层、淞附层、融化层组成的四层结构,雪带只包含由上层“播种”至下层的冰晶形成的凝结增长层、丛集层和淞附层三层。由于各层水平风速不同,雪带的三层结构并非垂直排列。多个雪带不断生成发展维持降雪,直至冰晶凝结生长层变空,云从冰晶凝结生长层分裂为多层云后各自消散。证明了Ka和X波段双偏振雷达结合的必要性和高效性,丰富了对锋面气旋系统雪带的认识,补充了Ka波段和X波段雷达对降雪的观测研究。 展开更多
关键词 Ka和X波段双偏振雷达 同步观测 锋面气旋系统 雪带结构
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