Characteristics of the Moist Pool over the Qinghai-Tibetan Plateau and its variation are analyzed by using ERA-Interim reanalysis data from 1979-2011.The result shows that, under the climate average state, to the global middle-high levels, there exists an entire layer of high humidity area over the Tibetan Plateau from June to September, which is known as the Qinghai-Tibetan Plateau Moist Pool in this paper. The vertical features of the Plateau Moist Pool are studied through the relative zonal difference of specific humidity. It is found that, during June and September, the Plateau Moist Pool is a vertical, deep and maximum center of the water vapor content to other parts of the globe at the same latitude. The value of water vapor content at different level inside the Moist Pool is above one time to three times of the zonal average. The high value areas of the relative zonal difference of specific humidity inside the Plateau Moist Pool are obviously extending obliquely to the downstream regions with the increase of the altitude and can reach 120°E and the areas east to it. The empirical orthogonal function (EOF) analysis shows that the Plateau Moist Pool in summer has three modes in spatial distribution as follows: the same signs in the whole, the reverse signs in the western and eastern, and the reverse signs in the southern and northern. The summer intensity index of the Plateau Moist Pool is defined in this paper, and it is found the Moist Pool has a significant increase trend in summer from 1979 to 2011, mainly with the oscillation cycle of 3~4 years and 7~8 years. The Plateau Moist Pool in summer has changed significantly around 1997.Since 1998, the Plateau Moist Pool in summer enhanced significantly, and the increase trend in the western is more stronger than that in the eastern. In the west of the Moist Pool, the increase trend of the upper air is stronger than that near the surface, and the maximum center is located near the 400~200 hPa. Finally, the results with three kinds of reanalysis data and the relating researches using sounding data and satellite data are integrated to analyze the applicability of the data in the study, and the analysis shows that the data for this study is applicable, and the results based on ERA-Interim reanalysis data in this paper are credible.
[1]Bao X, Zhang F.2013.Evaluation of NCEP-CFSR, NCEP-NCAR, ERA-Interim, and ERA-40 reanalysis datasets against independent sounding observations over the Tibetan Plateau[J].J Climate, 26(1): 206-214.
[2]Feng Lei, Zhou Tian jun.2012.Water vapor transport for summer precipitation over the Tibetan Plateau: Multi-dataset analysis[J].J Geophys Res Atmos, 117(D20): 85-99.
[3]Liu Ge, Zhao Ping, Wu Renguang, et al.2012.Potential flaws of interdecadal changes over eastern China around the early 1990s in the National Centers for Environmental Prediction-National Center for Atmospheric Research reanalyses[J].J Geophys Res Atmos, 117(D2): 262-269.
[4]Rienecker M M, Suarez M J, Gelaro R, et al.2011.MERRA: NASA's Modern-Era retrospective analysis for research and applications[J].J Climate, 24(14): 3624-3648.
[5]Yang Xu chao, Zhang Yi li, Zhang Wei, et al.2006.Climate change in Mt.Qomolangma region since 1971[J].Journal of Geographical Sciences, 16(3): 326-336.
[6]Zhang Y, Wang D, Zhai P, et al.2013.Spatial distributions and seasonal variations of tropospheric water vapor content over the Tibetan Plateau[J].J Climate, 26(15): 5637-5654.
[7]蔡英, 钱正安, 吴统文, 等.2004.青藏高原及周边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, 23(1): 1-10.
[8]Cai Ying, Qian Zheng'an, Wu Tongwen, et al.2004.Distribution changes of atmospheric precipitable water over Qinghai-Xizang Plateau and its surroundings and their changeable precipitation climate[J].Plateau Meteor, 23(1): 1-10.
[9]韩军彩, 周顺武, 吴萍, 等.2012.青藏高原上空夏季水汽含量的时空分布特征[J].干旱区研究, 29(3): 457-463.
[10]Han Juncai, Zhou Shunwu, Wu Ping, et al.2012.Spatial distribution of water vapor content over the Qinghai-Tibet Plateau in summer[J].Arid Zone Res, 29(3): 457-463.
[11]江吉喜, 范梅珠.2002.青藏高原夏季TBB场与水汽分布关系的初步研究[J].高原气象, 21(1): 20-24.
[12]Jiang Jixi, Fan Meizhu.2002.A primary study of the relationship between TBB fields and water vapor distribution over Qinghai-Xizang Plateau in summer[J].Plateau Meteor, 21(1): 20-24.
[13]梁宏, 刘晶淼, 李世奎.2006.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, 21(4): 526-534.
[14]Liang Hong, Liu Jingmiao, Li Shikui.2006.Analysis of precipitable water vapor source distribution and its seasonal variation characteristics over Tibetan Plateau and its surroundings[J].J Natural Resour, 21(4): 526-534.
[15]梁宏, 刘晶淼, 章建成, 等.2006.青藏高原大气总水汽量的反演研究[J].高原气象, 25(6): 1055-1063.
[16]Liang Hong, Liu Jingmiao, Zhang Jiancheng, et al.2006.Research on retrieval of the amount of atmospheric water vapor over Qinghai-Xizang Plateau[J].Plateau Meteor, 25(6): 1055-1063.
[17]刘宪锋, 任志远, 林志慧, 等.2013.2000-2011年三江源区植被覆盖时空变化特征[J].地理学报, 68(7): 897-908.
[18]Liu Xianfen, Ren Zhi yuan, Lin Zhihui, et al.2013.The spatial-temporal changes of vegetation coverage in the Three-River Headwater Region during 2000 and 2011[J].Acta Geographica Sinica, 68(7): 897-908.
[19]王霄, 巩远发, 岑思弦.2009.夏半年青藏高原"湿池"的水汽分布及水汽输送特征[J].地理学报, 64(5): 601-608.
[20]Wang Xiao, Gong Yuanfa, Cen Sixian.2009.Characteristics of the moist pool and its moisture transports overQinghai-Xizang Plateau in summer half year[J].Acta Geographica Sinica, 64(5): 601-608.
[21]徐祥德.2009.青藏高原"敏感区"对我国灾害天气气候的影响及其监测[J].中国工程科学, 11(10): 96-107.
[22]Xu Xiangde.2009.The effects of sensitive region over Tibetan Plateau on disastrous weather and climate and its monitoring[J].Engineering Sciences, 11(10): 96-107.
[23]许健民, 郑新江, 徐欢.1996.GMS-5水汽图像所揭示的青藏高原地区对流层上部水汽分布特征[J].应用气象学报, 1996, 7(2): 246-251.
[24]Xu Jianmin Zheng Xinjiang, Xu Huan.1996.Upper tropospheric moisture distribution over the Tibetan Plateau as revealed from GMS-5 vapour Images[J].J Appl Meteor Sci, 7(2): 246-251.
[25]叶笃正, 高由禧.1979.青藏高原气象学[M].北京:科学出版社.
[26]Ye Duzheng, Gao Youxi.1979.Meteorology of the Tibetan Plateau[M].Beijing: Science Press.
[27]殷芳. 2013. 青海省三江源地区气候变化影响草地和牧民收入的机理研究[D]. 北京: 中国科学院大学.
[28]Yin Fang.2013.Impact of climate change on grassland and herdsman's income: a case of three-river headwaters region in Qinghai Province[D].Beijing: University of Chinese Academy of Sciences.
[29]占瑞芬, 李建平.2008.青藏高原地区大气红外探测器 (AIRS) 资料质量检验及揭示的上对流层水汽特征[J].大气科学, 32(2): 242-260.
[30]Zhan Ruifen, Li Jianping.2008.Validation and characteristics of upper tropospheric water vapor over the Tibetan Plateau from AIRS satellite retrieval[J].Chinese J Atmos Sci, 32(2): 242-260.
[31]张清.1999.1998年我国天气气候特点[J].气象, 25(4): 26-29.
[32]Zhang Qing.1999.The weather and climate characteristics of China in 1998[J].Meteor Mon, 25(4): 26-29.
[33]张雨微. 2013. AIRS卫星观测的青藏高原大气水汽资料的评估与分析研究[D]. 北京: 中国气象科学研究院.
[34]Zhang Yuwei.2013.Validation and analysis of AIRS measured water vapor over the Tibetan Plateau[D].Beijing: Chinese Academy of Meteorological Acience.
[35]郑新江, 许建民, 李献洲.1997.夏季青藏高原水汽输送特征[J].高原气象, 16(3): 274-281.
[36]Zheng Xinjiang, Xu Jianmin, Li Xianzhou.1997.Characteristics of water vapour transfer in upper troposphere over Qinghai-Xizang Plateau in summer[J].Plateau Meteor, 16(3): 274-281.
[37]中国气象局国家气候中心.2011.气候系统监测诊断年报 (2010年)[M].北京:气象出版社.
[38]National Climate Center.2011.Climate system monitoring and diagnosis annual report of 2010[M].Beijing: China Meteorological Press.
[39]周顺武, 吴萍, 王传辉, 等.2011.青藏高原夏季上空水汽含量演变特征及其与降水的关系[J].地理学报, 66(11): 1466-1478.
[40]Zhou Shunwu, Wu Ping, Wang Chuanhui, et al.2011.Spatial distribution of atmospheric water vapor and its relationship with precipitation in summer over the Tibetan Plateau[J].Acta Geographica Sinica, 66(11): 1466-1478.
[41]周长艳, 蒋兴文, 李跃清, 等.2009.高原东部及邻近地区空中水汽资源的气候变化特征[J].高原气象, 28(1): 55-63.
[42]Zhou Changyan, Jiang Xingwen, Li Yueqing, et al.2009.Features of climate change of water vapor resource over eastern region of the Tibetan Plateau and its surroundings[J].Plateau Meteor, 28 (1): 55-63.
[43]周长艳, 李跃清, 李薇, 等.2005.青藏高原东部及邻地区水汽输送的气候特征[J].高原气象, 24(6): 880-888.
[44]Zhou Changyan, Li Yueqing, Li Wei, et al.2005.Climatological characteristics of water vapor transport over eastern part of Qinghai-Xizang Plateau and its surroundings[J].Plateau Meteor, 24 (6): 880-888.
[45]朱福康, 陶诗言, 陈联寿, 等.2000.第二次青藏高原大气科学试验理论研究进展 (二)[M].北京:气象出版社, 106-112.
[46]Zhu Fukang, Tao Shiyan, Chen Lianshou, et al.The Second Session of International Workshop on TIPEX (IWTE-I)[M].Beijing: China Meteorological Press, 106-112.
[47]卓嘎, 徐祥德, 陈联寿.2002.青藏高原夏季降水的水汽分布特征[J].气象科学, 22(1): 1-8.
[48]Zhuo Ga, Xu Xiangde, Chen Lianshou.2002.Water vapor feature of summer precipitation on Tibetan Plateau[J].J Meteor Sci, 22(1): 1-8.