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青藏高原与东亚地区暖季MCSs统计特征的对比分析
  • ISSN号:1000-0534
  • 期刊名称:高原气象
  • 时间:2013.8.1
  • 页码:929-943-
  • 分类:P458.2[天文地球—大气科学及气象学]
  • 作者机构:[1]沈阳农业大学农学院,辽宁沈阳110866, [2]中国气象科学研究院灾害天气国家重点实验室,北京100081, [3]永州市气象局,湖南永州425000, [4]空军气象中心,北京100843
  • 相关基金:财政部/科技部公益性行业(气象)科研专项(GYHY201006014,GYHY201206039,GYHY201306005); 国家自然科学基金项目(41175064)
  • 相关项目:一种正交地形追随坐标系的理论构建及其模拟研究
中文摘要:

利用1996-2010年逐时红外云顶亮温(TBB)数据,对青藏高原(下称高原)和东亚地区暖季(3-9月)中尺度对流系统(MCSs)进行了普查,获得MCSs各项特征数据集;结合CMORPH降水资料对MCSs降水特征进行了分析,在此基础上又对高原和东亚地区的MCSs特征进行了对比分析。结果表明:(1)高原是东亚地区MCSs高频发生区域,高原MCSs的平均发生频次远高于东亚25°N以北地区,是东亚25°N以北地区唯一的MCSs活动高频区。高原腹地是高原地区MCSs发生的高频区,在31°N,88°E附近MCSs的发生频次最高。(2)高原地区MCSs分布有明显的月际变化,春季主要出现在高原北部,夏季主要出现在高原中东部和南部。高原地区MCSs的月际变化特征与东亚地区基本一致,东亚夏季风是其月际变化的重要影响因子。(3)高原地区MCSs存在明显的单峰型日变化特征,但春、夏季日变化特征略有不同,高原MCSs的日变化较东亚地区更为显著。(4)高原地区MCSs的降水频次为5.6%,降水贡献率为10.1%,最大降水频次为12%,最大降水贡献率为27%;与东亚地区相比,高原的MCSs降水偏小。(5)高原地区的MCSs大多为向东移动且移速缓慢以及短生命史的MβCS,平均生命史为4.6h,平均面积约为11.2×10-4km2,平均移速为31.5km.h-1,东移的MCSs占59.4%;与整个东亚地区的MCSs相比,高原的MCSs面积和尺度都较小,生命史略短且移速慢,云顶平均TBB和平均最低TBB均偏高。

英文摘要:

Based on the hourly equivalent temperature of black body(TBB) data of GMS-5,FY-2C and FY-2E from 1996 to 2010,the mesoscale convective systems(MCSs) in warm season(from March to September) over the Qinghai-Xizang Plateau(QXP) and East Asia regions were investigated.The results show that:(1) The QXP is one of the high-frequency area of MCSs in East Asia,where is higher average frequency in East Asia to the north of 25°N.The hinterland of the QXP is the high-frequency concentration area of MCSs,and its nearby(31°N,88°E) is the highest frequency area.(2) There are obvious monthly variation characteristics of MCSs over the QXP,that the MCSs often occur in the northern and eastern areas of the QXP in spring and in the middle-eastern and southern areas in summer.The monthly variation in the QXP is similar with that of East Asia,and the summer monsoon of East Asia is the important factor.(3) The daily variation of MCSs over the QXP appears single peak distribution,but there are a few differences between spring and summer,that daily variation of MCSs over the QXP is more obvious than eastern Asia in some respects.(4) The precipitation frequency of MCSs is 5.6%,the contribution rate of precipitation is 10.1%,the frequency of maximum MCSs precipitation is 12% and the contribution rate of maximum MCSs precipitation is 27%.Comparing with the East Asian region,MCSs precipitation in the QXP is smaller.(5) The most of MCSs over the QXP are eastward low-speed and short life cycle MβCS.The average life cycle of MCS is 4.6 h with 11.2×10-4 km2 of average area,whose average speed is 31.5 km·h-1 and 59.4% of them are eastward.Comparing with the MCSs in East Asian,the MCSs over the QXP show the different characteristics: Smaller scale and area,shorter life cycle,lower speed,and average TBB and average lowest TBB are highter.

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期刊信息
  • 《高原气象》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院
  • 主办单位:中国科学院 寒区旱区环境与工程研究所
  • 主编:文军
  • 地址:甘肃省兰州市天水中路8号
  • 邮编:730000
  • 邮箱:gybjb@lzb.ac.cn gyqx@lzb.ac.cn
  • 电话:0931-82600935
  • 国际标准刊号:ISSN:1000-0534
  • 国内统一刊号:ISSN:62-1061/P
  • 邮发代号:54-43
  • 获奖情况:
  • 中国自然科学核心期刊,1995年获甘肃省编校质量达标优秀期刊,中国期刊方阵“双效”期刊
  • 国内外数据库收录:
  • 美国剑桥科学文摘,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:19859