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青藏高原季风对我国西北干旱区气候的影响

荀学义 胡泽勇 崔桂凤 张和平 胡英华 杨保成

荀学义, 胡泽勇, 崔桂凤, 张和平, 胡英华, 杨保成. 青藏高原季风对我国西北干旱区气候的影响[J]. 气候与环境研究, 2018, 23(3): 311-320. doi: 10.3878/j.issn.1006-9585.2017.17024
引用本文: 荀学义, 胡泽勇, 崔桂凤, 张和平, 胡英华, 杨保成. 青藏高原季风对我国西北干旱区气候的影响[J]. 气候与环境研究, 2018, 23(3): 311-320. doi: 10.3878/j.issn.1006-9585.2017.17024
Xueyi XUN, Zeyong HU, Guifeng CUI, Heping ZHANG, Yinghua HU, Baocheng YANG. The Effect of Tibetan Plateau Monsoon on the Climate in the Arid Area of Northwest China[J]. Climatic and Environmental Research, 2018, 23(3): 311-320. doi: 10.3878/j.issn.1006-9585.2017.17024
Citation: Xueyi XUN, Zeyong HU, Guifeng CUI, Heping ZHANG, Yinghua HU, Baocheng YANG. The Effect of Tibetan Plateau Monsoon on the Climate in the Arid Area of Northwest China[J]. Climatic and Environmental Research, 2018, 23(3): 311-320. doi: 10.3878/j.issn.1006-9585.2017.17024

青藏高原季风对我国西北干旱区气候的影响

doi: 10.3878/j.issn.1006-9585.2017.17024
基金项目: 

中国科学院战略性先导科技专项 XDA2006010101

国家自然科学基金项目 91537101

国家自然科学基金项目 41661144043

中国科学院寒旱区陆面过程与气候变化重点实验室开放基金项目 LPCC201306

详细信息
    作者简介:

    荀学义, 男, 1979年出生, 高工, 主要从事区域气候与陆面过程研究。E-mail:xunmengfei8@163.com

  • 中图分类号: P462.4+1

The Effect of Tibetan Plateau Monsoon on the Climate in the Arid Area of Northwest China

Funds: 

Strategic Priority Research Program of Chinese Academy of Sciences XDA2006010101

National Natural Science Foundation of China 91537101

National Natural Science Foundation of China 41661144043

Key Laboratory Program of Land Surface Process and Climate Change in Cold and Arid Regions, Chinese Acadmy Sciences LPCC201306

  • 摘要: 基于ERA-Interim逐月再分析资料及同期高原和我国西北干旱区观测站温度与降水资料,分析高原季风与西北干旱区气候的关系,对比高原典型强弱季风年平均大尺度环流和水汽输送条件的差异,探讨高原强弱季风年西北干旱区气候差异形成的原因。研究结果表明:高原季风与我国西北干旱区气候相关关系显著;高原强弱季风年对应的大尺度环流和垂直环流系统存在明显差异;水汽条件和抬升条件好坏与降水量多寡配合得较好,即强高原季风年,高原北部边缘水汽条件和抬升条件更有利于降水,而弱高原季风年,高原北部边缘水汽条件和抬升条件偏差,对应降水量较常年同期偏少。
  • 图  1  标准化动态高原季风指数(夏季指数)变化曲线

    Figure  1.  Interannual variation of normalized dynamic plateau monsoon index

    图  2  夏季指数与我国西北干旱区(a)温度和(b)降水量相关系数空间分布

    Figure  2.  Correlation coefficients of the normalized plateau monsoon index with (a) temperature and (b) precipitation in the arid area of Northwest China

    图  3  (a, b)100 hPa和(c, d)500 hPa平均高度场(实线,单位:dagpm)与距平场(阴影区):(a、c)强高原季风年;(b、d)弱高原季风年

    Figure  3.  Average geopotential height (solid lines, units: dagpm) and its anomalies (coloured) at (a, b) 100 hPa and (c, d) 500 hPa: (a, c) Strong plateau monsoon years; (b, d) weak plateau monsoon years

    图  4  (a、b)100~500 hPa和(c、d)600~850 hPa平均风距平流线图:(a、c)强高原季风年;(b、d)弱高原季风年

    Figure  4.  Wind anomalies streamlines averaged between (a, b) 100-500 hPa and (c, d) 600-850 hPa: (a, c) Strong plateau monsoon years; (b, d) weak plateau monsoon years

    图  5  沿(a、b)80°E和(c、d)90°E经圈平均环流剖面:(a、c)强高原季风年;(b、d)弱高原季风年

    Figure  5.  Vertical profiles of average circulation along (a, b) 80°E and (c, d) 90°E: (a, c) Strong plateau monsoon years; (b, d) weak plateau monsoon years

    图  6  强高原季风年与弱高原季风年(a)500 hPa、(b)600 hPa、(c)700 hPa和(d)850 hPa平均比湿差值场(单位:10-3 g/kg)

    Figure  6.  Differences in average specific humidity at (a) 500 hPa, (b) 600 hPa, (c) 700 hPa, and (d) 850 hPa between strong and weak plateau monsoon years (units: 10-3 kg/kg)

    图  7  强高原季风年和弱高原季风年(a)地面至600 hPa和(b)600 hPa以上垂直积分的水汽通量散度差值场(填色,单位:g s-1 cm-1 hPa-1);流线表示水汽通量差值场

    Figure  7.  Differences in the water vapor flux divergence (color filling, units: g s-1 cm-1 hPa-1) vertically integrated from (a) the surface to 600 hPa and (b) from 600 hPa upward between strong and weak plateau monsoon years; the streamlines stand for differences in the water vapor fluxes

    图  8  强高原季风年与弱高原季风年(a)500 hPa、(b)600 hPa、(c)700 hPa和(d)850 hPa平均散度差值场

    Figure  8.  Differences in the divergence at (a) 500 hPa, (b) 600 hPa, (c) 700 hPa, and (d) 850 hPa between strong and weak plateau monsoon years

  • [1] Akperov M G, Mokhov I I. 2010. A comparative analysis of the method of extratropical cyclone identification[J]. Izvestiya, Atmospheric and Oceanic Physics, 46:574-590, doi: 10.1134/S0001433810050038.
    [2] 白肇烨, 徐国昌, 孙学筠, 等. 1988.中国西北天气[M].北京:气象出版社, 443pp.

    Bai Zhaoye, Xu Guochang, Sun Xuejun, et al. 1988. The Weather in Northwest China (in Chinese)[M]. Beijing:China Meteorological Press, 442pp.
    [3] 蔡英, 李栋梁, 汤懋苍, 等. 2003.青藏高原近50年来气温的年代际变化[J].高原气象, 22:464-470. doi: 10.3321/j.issn:1000-0534.2003.05.006

    Cai Ying, Li Dongliang, Tang Maocang, et al. 2003. Decadal temperature changes over Qinghai-Xizang Plateau in recent 50 years[J]. Plateau Meteorology (in Chinese), 22:464-470, doi: 10.3321/j.issn:1000-0534.2003.05.006.
    [4] 蔡英, 宋敏红, 钱正安, 等. 2015.西北干旱区夏季强干、湿事件降水环流及水汽输送的再分析[J].高原气象, 34:597-610. doi: 10.7522/j.issn.1000-0534.2015.00049

    Cai Ying, Song Minhong, Qian Zheng'an, et al. 2015. Reanalyses of precipitation circulation and vapor transportation of severe dry and wet events in summer in arid region of Northwest China[J]. Plateau Meteorology (in Chinese), 34:597-610, doi: 10.7522/j.issn.1000-0534.2015.00049.
    [5] 符淙斌, 安芷生. 2002.我国北方干旱化研究——面向国家需求的全球变化科学问题[J].地学前缘, 9:271-275. doi: 10.3321/j.issn:1005-2321.2002.02.004

    Fu Congbin, An Zhisheng. 2002. Study of aridification in northern China——A global change issue facing directly the demand nation[J]. Earth Science Frontiers (in Chinese), 9:271-275, doi: 10.3321/j.issn:1005-2321.2002.02.004.
    [6] 符淙斌, 马柱国. 2008.全球变化与区域干旱化[J].大气科学, 32:752-760. doi: 10.3878/j.issn.1006-9895.2008.04.05

    Fu Congbin, Ma Zhuguo. 2008. Global change and regional aridification[J]. Chinese Journal of Atmospheric Sciences (in Chinese), 32:752-760, doi: 10.3878/j.issn.1006-9895.2008.04.05.
    [7] Hahn D G, Manabe S. 1975. The role of mountains in the South Asian monsoon circulation[J]. J. Atmos. Sci., 32:1515-1541, doi:10.1175/1520-0469(1975)032<1515:TROMIT>2.0.CO;2.
    [8] 黄荣辉, 陈际龙. 2010.我国东、西部夏季水汽输送特征及其差异[J].大气科学, 34:1035-1045. doi: 10.3878/j.issn.1006-9895.2010.06.01

    Huang Ronghui, Chen Jilong. 2010. Characteristics of the summertime water vapor transports over the eastern part of China and those over the western part of China and their difference[J]. Chinese Journal of Atmospheric Sciences (in Chinese), 34:1035-1045, doi: 10.3878/j.issn.1006-9895.2010.06.01.
    [9] 李岩瑛, 钱正安, 薛新玲, 等. 2009.西北干旱区夏半年深厚的混合层与干旱气候形成[J].高原气象, 28:46-54. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gyqx200901006

    Li Yanying, Qian Zheng'an, Xue Xinling, et al. 2009. Deep mixed layer in Northwest China dry area in summer half year and formation of the dry climate[J]. Plateau Meteorology (in Chinese), 28:46-54. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gyqx200901006
    [10] 钱正安, 吴统文, 吕世华, 等. 1998.夏季西北干旱气候形成的数值模拟——高原地形和环流场等的影响[J].大气科学, 22:753-762. doi: 10.3878/j.issn.1006-9895.1998.05.10

    Qian Zheng'an, Wu Tongwen, Lü Shihua, et al. 1998. Numerical simulation of Northwest China arid climate formation-Effects of the Qinghai-Xizang Plateau terrain and circulation field[J]. Scientia Atmospherica Sinica (in Chinese), 22:753-762, doi: 10.3878/j.issn.1006-9895.1998.05.10.
    [11] 史玉光, 孙照渤. 2008.新疆水汽输送的气候特征及其变化[J].高原气象, 27:310-319. http://www.oalib.com/paper/4179756

    Shi Yuguang, Sun Zhaobo. 2008. Climate characteristics of water vapor transportation and its variation over Xinjiang[J]. Plateau Meteorology (in Chinese), 27:310-319. http://www.oalib.com/paper/4179756
    [12] 汤懋苍. 1995.高原季风的年代际振荡及其原因探讨[J].气象科学, 15 (4):64-68. doi: 10.3969/2012jms.00**

    Tang Maocang. 1995. Discussion on inter-decade oscillation of plateau monsoon and its causes[J]. Scientia Meteorologica Sinica (in Chinese), 15 (4):64-68, doi: 10.3969/2012jms.00**.
    [13] 汤懋苍. 1998.青藏高原季风的形成、演化及振荡特征[J].干旱气象, 16 (1):3-16. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=gsqx801.000&dbname=CJFD&dbcode=CJFQ

    Tang Maocang. 1998. The formation, evolution and oscillation characteristics of the Tibetan Plateau monsoon[J]. Journal of Arid Meteorology (in Chinese), 16 (1):3-16. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=gsqx801.000&dbname=CJFD&dbcode=CJFQ
    [14] Tang M C, Reiter E R. 1984. Plateau monsoons of the Northern Hemisphere:A comparison between North America and Tibet[J]. Mon. Wea. Rev., 112:617-637, doi:10.1175/1520-0493(1984)112<0617:PMOTNH>2.0.CO;2.
    [15] 汤懋苍, 沈志宝, 陈有虞. 1979.高原季风的平均气候特征[J].地理学报, 34:33-42. doi: 10.3321/j.issn:0375-5444.1979.01.004

    Tang Maocang, Shen Zhibao, Chen Youyu. 1979. On climatic characteristics of the Xizang Plateau monsoon[J]. Acta Geographica Sinica (in Chinese), 34:33-42. doi: 10.3321/j.issn:0375-5444.1979.01.004
    [16] van den Hurk B, Viterbo P, Beljaars A, et al. 2000. Offline validation of the ERA40 surface scheme[R]. Technical Memorandum No. 295.
    [17] 王志伟, 翟盘茂. 2003.中国北方近50年干旱变化特征[J].地理学报, 58 (S1):61-68. doi: 10.11821/xb20037s007

    Wang Zhiwei, Zhai Panmao. 2003. Climate change in drought over northern China during 1950-2000[J]. Acta Geographica Sinica (in Chinese), 58 (S1):61-68, doi: 10.11821/xb20037s007.
    [18] 徐国昌. 1986.气候变化, 干旱和沙漠化——1986年的世界气象日[J].气象, 12 (3):24-26. doi: 10.7519/j.issn.1000-0526.1986.03.006

    Xu Guochang. 1986. Climate, drought and desertification——the World Meteorological Day in 1986[J]. Meteorological Monthly (in Chinese), 12 (3):24-26, doi:10.7519/j.issn. 1000-0526.1986.03.006.
    [19] 徐国昌, 张志银. 1983.青藏高原对西北干旱气候形成的作用[J].高原气象, 2 (2):9-16. http://mall.cnki.net/magazine/article/GYQX2003S1008.htm

    Xu Guochang, Zhang Zhiyin. 1983. The effect of Qinghai-Xizang Plateau on the formation of dry climate over the Northwest of China[J]. Plateau Meteorology (in Chinese), 2 (2):9-16. http://mall.cnki.net/magazine/article/GYQX2003S1008.htm
    [20] 徐淑英, 高由禧. 1962.西藏高原的季风现象[J].地理学报, 28:111-123. doi: 10.11821/xb196202002

    Xu Shuying, Gao Youxi. 1962. The phenomena of the Tibet Plateau monsoon[J]. Acta Geographica Sinica (in Chinese), 28:111-123, doi: 10.11821/xb196202002.
    [21] 荀学义, 胡泽勇, 崔桂凤, 等. 2015.青藏高原近地层及北侧气压系统的季节性振荡变化[J].冰川冻土, 37:360-368. doi: 10.7522/j.issn.1000-0240.2015.0039

    Xun Xueyi, Hu Zeyong, Cui Guifeng, et al. 2015. Seasonal variations of the pressure systems in surface layer and northern regions of the Tibetan Plateau[J]. Journal of Glaciology and Geocryology (in Chinese), 37:360-368, doi: 10.7522/j.issn.1000-0240.2015.0039.
    [22] Xun X Y, Hu Z Y, Ma Y M. 2012. The dynamic plateau monsoon index and its association with general circulation anomalies[J]. Advances in Atmospheric Sciences, 29:1249-1263, doi: 10.1007/s00376-012-1125-9.
    [23] 荀学义, 胡泽勇, 吴学宏, 等. 2011.三套位势高度再分析资料在青藏高原地区的对比分析[J].高原气象, 30:1444-1452. http://www.cqvip.com/QK/91655X/201106/40289215.html

    Xun Xueyi, Hu Zeyong, Wu Xuehong, et al. 2011. Comparative analyses of three geopotential height reanalysis data in Qinghai-Xizang Plateau[J]. Plateau Meteorology (in Chinese), 30:1444-1452. http://www.cqvip.com/QK/91655X/201106/40289215.html
    [24] 叶笃正, 高由禧. 1979.青藏高原气象学[M].北京:科学出版社.

    Yeh Tucheng, Gao Youxi. 1979. Qinghai-Xizang Plateau Meteorology (in Chinese)[M]. Beijing:Science Press.
    [25] 叶笃正, 罗四维, 朱抱真. 1957.西藏高原及其附近的流场结构和对流层大气的热量平衡[J].气象学报, 28:108-121. doi: 10.11676/qxxb1957.010

    Yeh Tucheng, Luo Siwei, Zhu Baozhen. 1957. The wind structure and heat balance in the lower troposphere over Tibetan Plateau and its surrounding[J]. Acta Meteorologica Sinica (in Chinese), 28:108-121, doi:10.11676/qxxb1957. 010.
    [26] 叶笃正, 杨广基, 王兴东. 1979.东亚和太平洋上空平均垂直环流(一)夏季[J].大气科学, 3 (1):1-11. http://www.oalib.com/paper/4881144

    Yeh Tucheng, Yang Guangji, Wang Xingdong. 1979. The average vertical circulations over the East Asia and the Pacific area, (I) in summer[J]. Scientia Atmospherica Sinica (in Chinese), 3 (1):1-11. http://www.oalib.com/paper/4881144
    [27] 俞亚勋, 王宝灵, 谢金南, 等. 2001.青藏高原东北侧地区干湿年夏季环流异常的对比分析[J].气候与环境研究, 6:103-112. doi: 10.3878/j.issn.1006-9585.2001.01.12

    Yu Yaxun, Wang Baoling, Xie Jinnan, et al. 2001. Contrast on the large scale circulation anomaly over Tibetan Plateau northeastern side for drought and rainy in summer[J]. Climatic and Environmental Research (in Chinese), 6:103-112, doi: 10.3878/j.issn.1006-9585.2001.01.12.
    [28] 张家宝, 邓子风. 1987.新疆降水概论[M].北京:气象出版社, 44-58.

    Zhang Jiabao, Deng Zifeng. 1987. The Introduction to Precipitation in Xinjiang (in Chinese)[M]. Beijing:China Meteorological Press, 44-58.
    [29] 张林源, 蒋兆理. 1992.论我国西北干旱气候的成因[J].干旱区地理, 15 (2):1-12. doi: 10.13826/j.cnki.cn65-1103/x.1992.02.001

    Zhang Linyuan, Jiang Zhaoli. 1992. The genesis of the arid climate of northwestern China[J]. Arid Land Geography (in Chinese), 15 (2):1-12, doi: 10.13826/j.cnki.cn65-1103/x.1992.02.001.
    [30] 郑水红, 王守荣. 2003.西北干旱区水资源供需分析与可持续利用对策研究[J].气候与环境研究, 8:52-59. doi: 10.3878/j.issn.1006-9585.2003.01.07

    Zheng Suihong, Wang Shourong. 2003. Analysis on supply and demand of water resource and study on relevant strategies of sustainable utilization in the arid region of the Northwest China[J]. Climatic and Environmental Research (in Chinese), 8:52-59, doi: 10.3878/j.issn.1006-9585.2003.01.07.
    [31] 朱德琴, 陈文, 刘辉志, 等. 2006.我国西北典型干旱区和高原地区地表辐射能量收支特征的比较[J].气候与环境研究, 11:683-690. doi: 10.3878/j.issn.1006-9585.2006.06.02

    Zhu Deqin, Chen Wen, Liu Huizhi, et al. 2006. The comparison of surface radiation budget between typical arid region in Northwest China and plateau region[J]. Climatic and Environmental Research (in Chinese), 11:683-690, doi: 10.3878/j.issn.1006-9585.2006.06.02.
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  • 收稿日期:  2017-02-18
  • 网络出版日期:  2017-12-23
  • 刊出日期:  2018-05-20

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