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新疆层云和层积云冰粒子属性的季节变化

王昀 王旭 赵笑颜 马禹 王式功 陈勇航

干旱区地理2017,Vol.40Issue(3):589-597,9.
干旱区地理2017,Vol.40Issue(3):589-597,9.

新疆层云和层积云冰粒子属性的季节变化

Seasonal variations of microphysical properties of ice particles for stratus and stratocumulus in Xinjiang

王昀 1王旭 2赵笑颜 1马禹 3王式功 1陈勇航4

作者信息

  • 1. 兰州大学大气科学学院,甘肃省干旱与减灾重点实验室,甘肃兰州 730000
  • 2. 新疆维吾尔自治区人工影响天气办公室,新疆乌鲁木齐830002
  • 3. 新疆维吾尔自治区气候中心,新疆乌鲁木齐830002
  • 4. 东华大学环境科学与工程学院,上海 201620
  • 折叠

摘要

Abstract

The vertical distributions and seasonal variations of microphysical quantities for stratus and stratocumulus were analyzed in term of ice particle equivalent radius (IER),the number concentration of ice particles (INC),ice water content (IWC) by using CloudSat satellite data.The results were of great significance for carrying out artificial precipitation operation.The occurrence frequencies of the small particles (0-50 μm),medium particles (50-80 μn),large particles (over 80 μm) in stratus (stratocumulus) were 18.7% (16.3%),77.6%(62.6%) and 3.7% (21.2%),respectively.In the vertical distribution of IER,small and medium particles distributed over the stratus and more frequently appeared in the middle parts,while large particles mainly distributed in the bottom parts.Meanwhile,for stratocumulus,except for winter,the distribution of IER were observed over the clouds;more small particles appeared in the upper part,more medium and large particles appeared in the middle parts.In the vertical direction,the stratification for stratus was obvious while it for stratocumulus was not obvious.The occurrence frequencies of ice number concentration (INC) in low value (0-50 L-1),median value (50-100 L-1) and high value (more than 100 L-1) for stratus (stratocumulus) were 90.1% (76.5%),9.6%(19.5%) and 0.3% (4.1%),respectively.In the vertical distributions of INC,the low value of INC distributed over the stratus,and the distributions of medium value was in middle and upper parts while the distributions of low and median value appeared more frequently in middle parts.At the same time,the distribution of low value of INC was over the stratocumulus,the distribution of medium value was in middle and upper parts while the distribution of low and median value ofINC appeared more frequently in middle and upper part.The occurrence frequencies of ice water content (IWC) in low value (0-50 mg· m-3),median value (50-100 mg·m-3) and high value (more than 100 mg·m-3) for stratus (stratocumulus) were 96.7% (82.8%),3.2% (13.4%),0.1% (3.7%),respectively.In the vertical distributions of IWC,the low value of IWC distributed over the stratus,and the distributions of medium value of IWC was in middle parts,the distribution of low value of IWC appeared more frequently in middle parts.At the same time,the distributions of low value and medium value of IWC were over the stratocumulus,high value was in the upper parts,low and median values appeared more frequently in the middle and upper parts.

关键词

CloudSat/层云/层积云/微物理属性/季节变化

Key words

CloudSat/stratus/stratocumulus/microphysical property/seasonal change

分类

天文与地球科学

引用本文复制引用

王昀,王旭,赵笑颜,马禹,王式功,陈勇航..新疆层云和层积云冰粒子属性的季节变化[J].干旱区地理,2017,40(3):589-597,9.

基金项目

新疆维吾尔自治区人民政府重大专项《新疆吐鲁番哈密地区空中云水资源开发利用》课题(降水现象及其历时蕴含的人工增水潜力分析、新疆三大山系水汽总量的遥感监测与评估)资助 (降水现象及其历时蕴含的人工增水潜力分析、新疆三大山系水汽总量的遥感监测与评估)

干旱区地理

OA北大核心CSCDCSTPCD

1000-6060

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