| 基于CloudSat资料分析北疆强降雪天气的云结构特征 |
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| 引用本文： | 王智敏,冯婉悦,李圆圆,储长江,徐文霞,陈勇航.基于CloudSat资料分析北疆强降雪天气的云结构特征[J].干旱区地理,2019,42(2):244-251. |
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| 作者姓名： | 王智敏 冯婉悦 李圆圆 储长江 徐文霞 陈勇航 |
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| 作者单位： | （1 新疆维吾尔自治区人工影响天气办公室，新疆 乌鲁木齐 830002；2 新疆维吾尔自治区气象技术装备保障中心，新疆 乌鲁木齐 830002；
3 新疆气象局，新疆 乌鲁木齐 830002；4 东华大学环境科学与工程学院，上海 201620） |
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| 基金项目： | 新疆维吾尔自治区气象局青年基金课题（Q201810）,中亚大气科学基金项目（CAAS201919）共同资助 |
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| 摘 要： | 利用NASA发布的2008—2015年CloudSat卫星的2B-CWC-RO、2B-CLDCLASS、2C-SNOW-PROFILE和地面气象站的观测资料，对北疆沿天山及其周边区域内21次强降雪天气降雪前和降雪期间卫星过境时云宏微观特征进行了对比分析。本文将研究区域分为了北疆沿天山西部和中部地区，分析结果表明：（1）降雪前和降雪期间的云类型以层云、积云、高层云和深对流云为主。（2）降雪前冰粒子等效半径均值分布在58.65~67.29 μm之间，冰粒子数浓度的均值在41.2~76.5 L-1之间，冰水含量的均值在25.4~135.1 mg·m-3之间，雪水含量均值在28.0~88.0 mg·m-3之间，降雪强度均值在0.08~0.36 mm·h-1之间。（3）降雪前冰粒子等效半径、冰粒子数浓度、冰水含量、雪水含量和降雪强度均值分别比降雪期间大2.9 %、6.2 %、34.4 %、36.4 %和18.7 %，且高值区主要集中在北疆沿天山西部地区。
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| 关 键 词： | CloudSat 强降雪 宏微观物理量 北疆区域 |
Cloud structure characteristics in heavy snowfall days in northern Xinjiang using Cloudsat satellite data |
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| WANG Zhi-min,FENG Wan-yue,LI Yuan-yuan,CHU Chang-jiang,XU Wen-xia,CHENG Yong-hang.Cloud structure characteristics in heavy snowfall days in northern Xinjiang using Cloudsat satellite data[J].Arid Land Geography,2019,42(2):244-251. |
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| Authors: | WANG Zhi-min FENG Wan-yue LI Yuan-yuan CHU Chang-jiang XU Wen-xia CHENG Yong-hang |
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| Institution: | （ 1 Xinjiang Weather Modification Office，Urumqi 830002，Xinjiang，China；2 Meteorological and Technical Equipment Support Center of Xinjiang Uygur Autonomous Region, Urumqi 830002，Xinjiang，China；3 Xinjiang Meteorological Bureau, Urumqi 830002，Xinjiang，China；;
4 College of Environmental Science and Engineering，Donghua University Shanghai，Shanghai 201620,China） |
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| Abstract: | The CloudSat observational dataset provides an important opportunity to study snowfall, and there have been numerous investigations making use of CloudSat for snowfall-related research. Based on the data of 2B-CLDCLASS, 2B-CWC-RVOD and 2C-SNOW-PROFILE and the precipitation data of the ground observation stations, the macro and micro physical properties of the clouds before and during the snowfall were compared and analyzed in 21 heavy snowfall events in the northern Xinjiang, China. In the paper, the northern Xinjiang was divided into the western and the central region along Tianshan Mountains. Firstly, all the sites which had precipitation reached to heavy snowstorm in 24 hours were selected in the northern Xinjiang from 2008 to 2015. Then, according to the specific dates of the snowfall and the latitude and longitude of the sites, those sites which had CloudSat passed their territory were selected as the research object and there were 21 cases obtained. Out of the 21 cases there were 12 cases with the satellite passing their territories while the snowfall was occurring, and 9 cases with the satellite passing their territories before snowfall. The distributions of microphysical properties, which include ice effective radius (IER), ice number concentration (INC), ice water content (IWC), snow water content (SWC) and snow rate (SR), were revealed through analyzing the clouds, cloud types of heavy snowfall and the relationship between cloud microphysical properties and snowfall. Before the heavy snowfall and during the heavy snowfall, the main cloud types were altostratus clouds, cumulus clouds, nimbostratus, stratus clouds, the convective clouds between altostratus clouds and deep stratus. The maximum of IER was 296.5 μm and the minimum was 28.4 μm. The mean of IER of ice cloud was 64.1 μm before the snowfall, and 62.3 μm in the snowfall. The IER before the snowfall was 7.1 % larger than that in the snowfall. The largest INC is 768.4 L-1, and the values of geometric mean range of INC were 41.2-76.5 L-1 before the snowfall, and 28.1-73.0 L-1 during the snowfall. The values of geometric mean range of IWC of ice cloud were 25.4-135.1 mg·m-3 before the snowfall, and 12.0-77.7 mg·m-3 during the snowfall. The largest IWC was 701.8 mg·m-3, and the smallest IWC was 1.0 mg·m-3. The mean values of SWC and SR were 28.0~88.0 mg·m-3 and 0.08~0.36 mm·h-1 respectively. The mean values of IER, INC, IWC, SWC and SR before the snowfall were respectively 2.9 %, 6.2 %, 34.4 %, 36.4 % and 18.7 % higher than those during the snowfall. The areas with larger values of the micro physical cloud properties are mainly concentrated in the western part of northern Xinjiang. This study had presented a comprehensive analysis of cloud vertical structures and regional variations before and during the heavy snowfall. The analysis of ice effective radius, ice number concentration, ice water content, snow water content and snow rate also helps understand the artificial snow augmentation. |
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| Keywords: | Cloudsat heavy snowfall macro and micro physical properties northern Xinjiang |
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