Comparison of Precipitation in Yunnan from GPS Observation Data and Three Reanalysis Data

  • REN Juzhang ,
  • SUN Jihua ,
  • LI Jian ,
  • XU Kai
Expand
  • Yunnan Research Institute of Meteorology, Kunming 650034, China;2. Dali Observatory, Dali 630020, China;3. Chinese Academy of Meteorological Sciences, China Meteorological Administration, Beijing 100081, China

Received date: 2012-10-24

  Online published: 2014-12-28

Abstract

By using GPS observation data, the NCEP/NCAR reanalysis data, the NCEP/DOE reanalysis data and the JRA-25 reanalysis data, the features of precipitation in the eastern Yunnan in 2009 is investigated. The results show that the annual mean precipitation in 2009 is decreasing from south side to north side in Yunnan, and the annual characteristics of the monthly mean precipitation in 2009 present the unimodal distribution. The difference among the values of precipitation estimated by these four data is clear in every month, and the values of precipitation estimated by three reanalysis data are all less than that by GPS observation in every month. Analyzing the daily mean precipitation by the four kinds of data, the trend of the precipitation increases from south side to north side in the eastern Yunnan. But it is difficult to present the procedure of precipitation boosting from south side to north side in Yunnan at the beginning of the rainy season period by three reanalysis data. From the case study, the precipitation variation by the JRA-25 reanalysis data is same as that by GPS observation in the short time scale, so the precipitation of JRA-25 reanalysis data is more reliable than the other reanalysis data.

Cite this article

REN Juzhang , SUN Jihua , LI Jian , XU Kai . Comparison of Precipitation in Yunnan from GPS Observation Data and Three Reanalysis Data[J]. Plateau Meteorology, 2014 , 33(6) : 1480 -1489 . DOI: 10.7522/j.issn.1000-0534.2013.00114

References

[1]Kalnay E, Kanamitsu M, Kistler R, et al. The NCEP/NCAR 40-year reanalysis project[J]. Bull Amer Meteor Soc, 1996, 77: 437-471.
[2]Kistler R, Kalnay E, Collins W, et al. The NCEP/NCAR 50-year reanalysis: monthly means CD-ROM and documentation[J]. Bull Amer Mereor Soc, 2001, 82: 247-267.
[3]Kanamitsu M, Ebisuzaki W, Woollen I, et al. NCEP/DOE AM IP-Ⅱ Reanalysis(R-2)[J]. Bull Amer Meteor Soc, 2002, 83: 1631-1643.
[4]Onogi K, Tsutsui J, Koide H, et al. The JRA-25 reanalysis[J]. J Meteor Soc Japan, 2007, 85(3): 369-432.
[5]Hu Zengzhen. Interdecadal variability of summer climate over East Asia and its association with 500 hPa height and global sea surface temperature[J]. J Geophys Res, 1997, 102: 19403-19412.
[6]周长艳, 蒋兴文, 李跃清, 等. 高原大部及邻近地区空中水汽资源的气候变化特征[J]. 高原气象, 2009, 28(1): 55-63.
[7]Chang C P, Zhang Y, Li T. Interannual and interdecadal variations of the East Asian summer monsoon and tropical Pacific SSTs, Part I: Roles of the subtropical ridge[J]. J Climate, 2000, 13: 4310-4325.
[8]Chang C P, Zhang Y, Li T. Interannual and interdecadal variations of the East Asian summer monsoon and tropical Pacific SSTs. Part II: Meridional structure of the monsoon[J]. J Climate, 2000, 13: 4326-4340.
[9]Wang Huijun. The weakening of the Asian monsoon circulation after the end of 1970s[J]. Adv Atmos Sci, 2001, 17: 376-385.
[10]赵天保, 符淙斌. 中国区域ERA-40、NCEP-2再分析资料与观测资料的初步比较与分析[J]. 气候与环境研究, 2006, 11(1): 14-32.
[11]施晓辉, 徐祥德, 谢立安. NCEP/NCAR再分析风速、表面气温距平在中国区域气候变化研究中的可信度分析[J]. 气象学报, 2006, 64(6): 709-722.
[12]赵天保, 符淙斌. 几种再分析地表气温资料在中国区域的适用性评估[J]. 高原气象, 2009, 28(3): 594-606.
[13]李瑞青, 吕世华, 韩博, 等. 青藏高原东部三种再分析资料与地面气温观测资料的对比分析[J]. 高原气象, 2012, 31(6): 1488-1502.
[14]魏丽, 李栋梁. 青藏高原地区NCEP新再分析地面通量资料的检验[J]. 高原气象, 2003, 22(5): 479-487.
[15]Businger S, Chiswell S R, Bevis M, et al. The promise of GPS in atmospheric monitoring[J]. Bull Amer Meteor Soc, 1996, 77: 5-18.
[16]郭虎, 段丽, 杨波, 等. 0679香山局地大暴雨的中小尺度天气分析[J]. 应用气象学报, 2008, 19(3): 265-275.
[17]袁招洪, 丁金才, 陈敏. GPS观测资料应用于中尺度数值预报模式的初步研究[J]. 气象学报, 2004, 62(2): 200-211.
[18]梁宏, 刘晶淼, 李世奎. 青藏高原及周边地区大气水汽资源分布和季节变化特征分析[J]. 自然资源学报, 2006, 21(4): 526-534.
[19]梁宏, 刘晶淼, 章建成, 等. 青藏高原大气总水汽量的反演研究[J]. 高原气象, 2006, 25(6): 1055-1063.
[20]宾振, 吴瑶, 邱璐, 等. 江西地基GPS遥感大气可降水量变化特征及精度[J]. 高原气象, 2013, 32(5): 1503-1509, doi: 10.7522/j.issn.1000-0534.2012.00140.
[21]蔡英, 钱正安, 吴统文, 等. 青藏高原及周围地区大气可降水量的分布、变化与各地多变的降水气候[J]. 高原气象, 2004, 23(1): 3-12.
[22]符睿, 段旭, 刘建宇, 等. 云南地基GPS观测大气可降水量变化特征[J]. 气象科技, 2010, 38(4): 456-462.
[23]赵天保, 符淙斌, 柯宗建, 等. 全球大气再分析资料的研究现状与进展[J]. 地球科学进展, 2010, 25(3): 242-254.
Outlines

/