-
A sauna weather event in northern China in July 2009 is numerically simulated and diagnostically analyzed. The atmospheric circulation characteristics, the horizontal and vertical distributions of temperatures and moistures, and the distribution of potential vorticities are studied. It is found that anticyclone dominates the upper troposphere during the sauna weather event. In the horizontal chart, the relative humidity in the lower troposphere is large. From the vertical sections, descending airflow dominates the moist and warm sectors at the middle and lower levels. There are clear humidity gradient, evident vertical gradient of temperature, and slanting distribution of potential vorticity. The sauna weather event occurs in the generally high-temperature environment of summertime, so it is difficult to dynamically identify and diagnose the sauna weather depending on some single factor, e.g., temperature or moisture. According to the high-temperature, large-moisture, and strong-potential vorticity characteristics during the sauna weather in northern China, a moist thermal potential vorticity parameter MTPV, may be expressed as ▽ q (▽ ▽ Q), where q is the sum of water vapor and all hydrometeors including cloud water, rain water, cloud ice, snow and graupel; is potential temperature; Q is potential vorticity) which is appropriate for sauna weather, is introduced. Then it is used to dynamically diagnose sauna weather event. And it is simplified by calculation analysis in case study. It is found that the MTPV anomaly is accompanied by the sauna weather process. Although high temperature, large moisture and strong slanting potential vorticity development present in the sauna weather process in northern China in July 2009, their coverages for these single variables are larger than our target region of this sauna weather event. While for the MTPV and its simplified form combining these variables, their anomalies maintain in the lower troposphere around Beijing and its peripheral areas in northern China, viewing from either zonal or meridional section. Therefore, both MTPV and its simplified form can better dynamically identify this high-temperature and high-humidity sauna weather event.
-
Keywords:
- sauna weather /
- high temperature and high moisture /
- moist thermal potential vorticity parameter
[1] Kalkstein L S 1993 Lancet 342 1379
[2] Gaffen D J, Ross R J 1998 Nature 396 529
[3] [4] [5] McGeehin M A, Mirabelli M 2001 Environ Health Perspect 109 185
[6] [7] Karl T R, Trenberth K E 2003 Science 302 1719
[8] [9] Meehl G A, Tebaldi C 2004 Science 305 994
[10] Li W, Zhu Y F 2007 Meteorological Monthly. 33 108 (in Chinese) [李威, 朱艳峰 2007 气象 33 108]
[11] [12] Xie Z, Cao H X 1996 Acta. Meteor. Sinica 54 501 (in Chinese) [谢庄, 曹鸿兴 1996 气象学报 54 501]
[13] [14] Zheng S H, Wang S R, Wang Y M 2000 Acta. Geographica. Sinica (Supplement) 55 119 (in Chinese) [郑水红, 王守荣, 王有民 2000 地理学报 55(增刊) 119]
[15] [16] [17] Wang Y C, Ge G Q, Tao Z Y 2003 Meteorological Monthly 29 23 (in Chinese) [王迎春, 葛国庆, 陶祖钰 2003 气象 29 23]
[18] [19] Gao S T, Zhou Y S, Lei T, Sun J H 2005 Sci. China (Series D) 35 107 (in Chinese) [高守亭, 周玉淑, 雷霆, 孙建华 2005 中国科学D辑 35 107]
[20] Ertel H 1960 Gerlands Beitr. Geophys. 69 357
[21] [22] [23] Zdunkowski W, Bott A 2003 Dynamics of the Atmosphere: A Course in Theoretical Meteorology (1st Ed.) (United Kindom: Cambridge University Press), pp268-270
[24] Wang D H, Yang S, Zhong S X, Han Y 2009 Chinese J. Atmos. Sci. 33 1238 (in Chinese) [王东海, 杨帅, 钟水新, 韩瑛 2009 大气科学 33 1238]
[25] [26] [27] [28] [29] [30] [31] [32] [33] [34] [35] [36] [37] [38] [39] [40] [41] [42] [43] [44] [45] [46] [47] [48] [49] -
[1] Kalkstein L S 1993 Lancet 342 1379
[2] Gaffen D J, Ross R J 1998 Nature 396 529
[3] [4] [5] McGeehin M A, Mirabelli M 2001 Environ Health Perspect 109 185
[6] [7] Karl T R, Trenberth K E 2003 Science 302 1719
[8] [9] Meehl G A, Tebaldi C 2004 Science 305 994
[10] Li W, Zhu Y F 2007 Meteorological Monthly. 33 108 (in Chinese) [李威, 朱艳峰 2007 气象 33 108]
[11] [12] Xie Z, Cao H X 1996 Acta. Meteor. Sinica 54 501 (in Chinese) [谢庄, 曹鸿兴 1996 气象学报 54 501]
[13] [14] Zheng S H, Wang S R, Wang Y M 2000 Acta. Geographica. Sinica (Supplement) 55 119 (in Chinese) [郑水红, 王守荣, 王有民 2000 地理学报 55(增刊) 119]
[15] [16] [17] Wang Y C, Ge G Q, Tao Z Y 2003 Meteorological Monthly 29 23 (in Chinese) [王迎春, 葛国庆, 陶祖钰 2003 气象 29 23]
[18] [19] Gao S T, Zhou Y S, Lei T, Sun J H 2005 Sci. China (Series D) 35 107 (in Chinese) [高守亭, 周玉淑, 雷霆, 孙建华 2005 中国科学D辑 35 107]
[20] Ertel H 1960 Gerlands Beitr. Geophys. 69 357
[21] [22] [23] Zdunkowski W, Bott A 2003 Dynamics of the Atmosphere: A Course in Theoretical Meteorology (1st Ed.) (United Kindom: Cambridge University Press), pp268-270
[24] Wang D H, Yang S, Zhong S X, Han Y 2009 Chinese J. Atmos. Sci. 33 1238 (in Chinese) [王东海, 杨帅, 钟水新, 韩瑛 2009 大气科学 33 1238]
[25] [26] [27] [28] [29] [30] [31] [32] [33] [34] [35] [36] [37] [38] [39] [40] [41] [42] [43] [44] [45] [46] [47] [48] [49]
Catalog
Metrics
- Abstract views: 6005
- PDF Downloads: 451
- Cited By: 0