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  • CN 62-1070/P
  • ISSN 1000-694X
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The Anomaly Characteristics and Causes of Low-level Water Vapor over the Eastern Part of Northwest China

  • Zhao Guangping ,
  • Ren Xiaofang
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  • College of Atmospheric Science, Nanjing University of Information Science & Technology, Nanjing 210044, China

Received date: 2015-01-09

  Revised date: 2015-02-10

  Online published: 2016-05-20

Abstract

By using the ERA-Interim global reanalysis wind and specific humidity data from 1979 to 2012, the evolution characteristics of low-level water vapor are analyzed with the methods of variation rate analysis, Mann-Kendall test and analogy deviation analysis. And based on the wind field difference, the moisture abnormality is preliminarily discussed. Results showed that the annual lower-level water vapor increased in recent 30 years. In the Qinghai Plateau and arid desert region, water vapor happened abrupt change in 1996, while in 1991 for the monsoon region. Furthermore, westerly winds weaken and southerly winds increased significantly after abrupt change occurred. Through quantitative analysis of the impact of wind field change on water vapor, we found that meridional wind positively contributed to water vapor in the Qinghai Plateau region, except negative contribution in summer, and zonal wind showed negative contribution. The meridional and zonal contribution were 0.28 g·kg-1 and -0.46 g·kg-1 in the monsoon region, respectively. In arid desert region, wind's contribution appeared positive in winter and spring, while negative in summer and autumn. Based on the wind's climatic pattern differences in specific regions and typical months, we found that influence of low-level wind field change on the distribution of water vapor was much more different within a single region. However, the configuration of wind fields in adjacent areas in different backgrounds and wind interaction between different areas are the main reasons for the change of water vapor.

Cite this article

Zhao Guangping , Ren Xiaofang . The Anomaly Characteristics and Causes of Low-level Water Vapor over the Eastern Part of Northwest China[J]. Journal of Desert Research, 2016 , 36(3) : 749 -759 . DOI: 10.7522/j.issn.1000-694X.2015.00040

References

[1] 张强,胡隐樵,曹晓彦,等.论西北干旱气候的若干问题[J].中国沙漠,2000,20(4):357-362.
[2] 杨金虎,王鹏祥,等.中国西北降水年内非均匀性特征分析[J].气候变化研究,2007,3(5):276-281.
[3] Zhou S W,Wu P,Wang C H,et al.Spatial distribution of atmospheric water vapor and its relationship with precipitation in summer over the Tibetan Plateau[J].Journal of Geographical Sciences,2012,22(5):795-809.
[4] 王秀荣,徐祥德,王国维.西北地区春、夏季降水的水汽输送特征[J].高原气象,2007,26(4):749-758.
[5] 翟盘茂,周琴芳.中国大气水分气候变化研究[J].应用气象学报,1997,8(3):342-351.
[6] 张学文.可降水量与地面水汽压力的关系[J].气象,2004,30(2):9-11.
[7] 魏娜,巩远发,孙娴,等.西北地区近50 a降水变化及水汽输送特征[J].中国沙漠,2010,30(6):1450-1457.
[8] 韩彩军,周顺武,刘伟.华北地区夏季水汽含量变化特征及影响因子分析[J].气象与环境学报,2012,28(6):32-37.
[9] 姚俊强,杨青,胡文峰,等.天山山区空中水汽含量及与气候因子的关系[J].地理科学,2013,33(7):859-864.
[10] 李栋梁,魏丽,蔡英,等.中国西北现代气候变化事实与未来趋势展望[J].冰川冻土,2003,25(2):135-142.
[11] 宋连春,张存杰.20世纪西北地区降水量变化特征[J].冰川冻土,2003,25(2):143-148.
[12] 陈晓光,苏占胜,郑广芬,等.宁夏气候变化的事实分析[J].干旱区资源与环境,2005,19(6):43-47.
[13] 王宝鉴,黄玉霞,陶建红,等.西北地区大其水汽的区域分布特征及其变化[J].冰川冻土,2006,28(1):15-21.
[14] 陈豫英,冯建民,陈楠,等.西北地区东部可利用降水的时空变化特征[J].干旱区地理,2012,35(1):56-66.
[15] 陈楠,陈豫英,范小明,等.西北地区东部沙尘暴转型的额环流演变及差异特征分析[J].干旱区地理,2010,33(5):676-683.
[16] Kousari M R,Ahani H.An investigation of near surface wind speed trends in arid and semiarid regions of Iran[J].Theoretical Applied Climatology,2013,114:153-168.
[17] McVicar T R,Roderick M L,Donohue R J,et al.Global review and synthesis of trends in observed terrestrial near-surface wind speeds:implications for evaporation[J].Journal of Hydrology,2012,416:182-205.
[18] 贾丽伟,李维京,陈德亮.东北地区降水与大气环流关系[J].应用气象学报,2006,17(5):557-566.
[19] Yao S Q,Huang Y Z,Zhou X.The simulation of water vapor transport in East Asia using a regional air-sea coupled model[J].Journal Geophysical Research-Atmospheres,2013,118:1585-1600.
[20] 俞亚勋,王劲松,李青燕.西北地区空中水汽时空分布及变化趋势分析[J].冰川冻土,2003,25(2):49-56.
[21] 赵光平,马丽.1953-2012年中国西北地区东部低层气旋性风场演变特征及成因[J].中国沙漠,2014,34(5):1343-1352.
[22] 姜旭,赵光平.中国西北地区东部雨日的气候特征及其与低空风场的相关性研究[J].中国沙漠,2013,33(3):888-895.
[23] 赵光平,施新民,丁永红.宁夏暴雨动力相似预报系统[J].气象,2000,26(7):32-35.
[24] 王遂缠,王锡稳,李栋梁,等.相似离度在甘肃省冬春季强沙尘暴天气入型判别和预报中的应用研究[J].中国沙漠,2004,24(6):724-728.
[25] 丛芳,刘黎平.新一代天气雷达与地面雨量资料的综合分析[J].气象,2011,37(5):532-539.
[26] 何邓新,邵爱梅.判断大气要素长相似度的相似面积比方法[J].高原气象,2014,33(3):658-665.
[27] Lu E,Takle E S,Manoj J.The relationships between climatic and hydrological changes in the upper Mississippi River basin:a SWAT and multi-GCM study[J].Journal of Hydrometeorology,2010,11:437-451.
[28] 孙悦,李栋梁.1975-2011年渭河上游径流演变规律及对气候驱动因子的响应[J].冰川冻土,2014,36(2):413-423.
[29] Chen H P,Sun J Q,Chen X L,et al.CGCM projections of heavy rainfall events in China[J].International Journal of Climatology,2012,32:441-450.
[30] Drumond A,Nieto R,Gimeno L.On the contribution of the Tropical Western Hemisphere Warm Pool source of moisture to the Northern Hemisphere precipitation through a Lagrangian approach[J].Journal of Geophysical Research:Atmospheres,2011,116(D21).
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