论我国夏季风影响过渡区及其陆—气相互作用问题

doi:10.11867/j.issn.1001-8166.2017.10.1009

地球科学进展 ›› 2017, Vol. 32 ›› Issue (10): 1009 -1019. doi: 10.11867/j.issn.1001-8166.2017.10.1009

张强 ^1, ^2, ³(

), 张红丽 ^1, ^3, ^*(

), 张良 ^1, ², 岳平 ^1, ^2, ³

1.中国气象局兰州干旱气象研究所/甘肃省干旱气候变化与减灾重点实验室/中国气象局干旱气候变化与减灾重点开放实验室,甘肃兰州 730020
2.甘肃省气象局,甘肃兰州 730020
3.兰州大学大气科学学院, 甘肃兰州 730000

收稿日期:2017-07-28 修回日期:2017-09-01 出版日期:2017-12-20
通讯作者: 张红丽 E-mail:zhangqiang@cma.gov.cn;zhanghl13@lzu.edu.cn
基金资助:
国家自然科学基金重点项目“我国典型夏季风影响过渡区陆—气相互作用及其对夏季风响应研究”(编号:41630426)资助.

Study on Summer Monsoon Transition Zone and Its Land-Air Interaction

Qiang Zhang ^1, ^2, ³( ), Hongli Zhang ^1, ^3, ^*( ), Liang Zhang ^1, ², Ping Yue ^1, ^2, ³

1.Institute of Arid Meteorology, China Meteorological Administration, Key Laboratory of Arid Climatic Change and Reducing Disaster of Gansu Province; Key Open Laboratory of Arid Climatic Change and Disaster Reduction of CMA, Lanzhou 730020, China
2.Gansu Provincial Meteorological Bureau, Lanzhou 730020, China
3.College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China

Received:2017-07-28 Revised:2017-09-01 Online:2017-12-20 Published:2017-10-20
Contact: Hongli Zhang E-mail:zhangqiang@cma.gov.cn;zhanghl13@lzu.edu.cn
About author:
First author:Zhang Qiang(1965-),male,Jingyuan County, Gansu Province, Professor. Resaearch areas include atmospheric boundary layer,landsurface process and arid climate.E-mail:zhangqiang@cma.gov.cn
Supported by:
Project supported by the National Natural Science Foundation of China “Study on interaction between land-atmosphere over Typical Summer Monsoon Edgy region and its response to summer monson characteristics”(No.41630426).

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我国季风影响过渡区既是典型的生态过渡区和生态环境脆弱带,也是我国干旱和水土流失最为严重的区域,其陆—气相互作用在天气气候演变过程中扮演着重要角色,所以该特殊区域陆—气相互作用研究是一个重要的科学问题。为此,国家自然科学基金重点资助“我国典型夏季风影响过渡区陆—气相互作用及其对夏季风响应研究”课题专门针对此问题开展研究。在归纳我国夏季风活动的特点、夏季风影响过渡区的形成及其气候环境特征的基础上,总结了目前夏季风影响过渡区及其陆—气相互作用研究进展,综合分析了该地区陆—气相互作用的特殊性。并且提出了该领域研究存在的主要科学问题及未来的研究方向。这对今后深入研究我国夏季风影响过渡区陆—气相互作用问题具有科学指导意义。

关键词: 夏季风影响过渡区, 陆—气相互作用, 夏季风

The Summer Monsoon Transition Zone is a typical area, which is a transitional zone and has a fragile ecological environment. The area also has the most serious drought and soil erosion disaster. Its land-air interaction plays an important role on evolution of weather and climate, and research on land-air interaction in this zone is an important scientific problems. Therefore, a key project, “land-air interaction of the typical summer monsoon transition zone and its response to the summer monsoon”, by National Natural Science Foundation of China aims at this problem. This study summarized the advances about current summer monsoon transition zone and its land-air interaction. Then, based on the characteristics of summer monsoon activities, the formation of this typical area, its advances of climate and environment characteristics were concluded. Peculiarity of land-air interaction in the area was also analyzed comprehensively. Furthermore, the main problems and direction of scientific research in this field are brought forward. It will have scientific guiding significance for in-depth study of land-air interaction in summer monsoon transition zone in future.

Key words: Summer monsoon transition zone, Land-air interaction, Monsoon.

中图分类号:

P404

图1 气候平均的气象要素逐侯变化(据参考文献[9]改绘)
(a)假相当位温( T>340 K);(b)标准化可降水量( P>0.618);(c)西南风( u>0 m/s, v>2 m/s);(d)东南风( u<0 m/s, v>2 m/s)

Fig.1 Pentad change of meteorological elements(modified after reference[9])
(a)Pseudoe quivalent potential temperature( T>340 K); (b)Standardized precipitation( P>0.618); (c)Southwest winds ( u>0 m/s, v>2 m/s) and (d) Southeast winds( u<0 m/s, v>2 m/s)

图2 不同经度季风北边缘的年际波动方差(据参考文献[9]改绘)

Fig.2 Interannual fluctutation variance of northernmost margin of the Asian Summer monsoon in different longitude(modified after reference[9])

图3 夏季风影响过渡区的分布特征(据参考文献[9]改绘)
色标表示气候干燥度

Fig.3 Distribution of summer monsoon transition zone (modified after reference[9])
Color bar is dry degree

图4 夏季(a)平均降水量(据参考文献[11]改绘,单位:mm)和(b)鲍恩比 ^{[

17
]}(单位:1)的水平空间分布

Fig.4 The spatial distribution of average rainfall in summer (a) (modified after reference[11], unit: mm) and Bowen ratio ^{[

17
]} (b) (unit: 1)

图5 季风影响过渡区(a)生态植被(引自中国科学院资源环境科学数据中心)和(b)潜在蒸发量(据参考文献[19]改绘)空间分布特征

Fig.5 The distribution of (a)vegetation (citation from Resources and Environment Science Data Center,Chinese Academy of Sciences) and (b) potential evapotranspiration(modified after reference[19]) in summer monsoon transition zone

图6 夏季风影响过渡区夏季晴天对流层边界层厚度(a)和陆面感热通量日最大值(b)由西向东的降低趋势(据参考文献[4]改绘)

Fig.6 The reducing trend of sunny summer tropospheric boundary layer thickness (a) and the maximum land surface sensible heat flux (b) (modified after reference[4]) in summer monsoon transition zone

图7 夏季风驱动下区域气候与陆面过程和边界层过程之间相互作用的基本物理框架

Fig.7 The basic physics frameworks of interaction between regional climate and processes of land surface and boundary layer

[1]	Qian W, Ding T, Hu H,et al. An overview of dry-wet climate variability among monsoon-westerly regions and the monsoon northernmost marginal active zone in China[J]. Advances in Atmospheric Scineces,2009,26(4):630-641.
[2]	Lin Xiang, Qian Weihong.Review of the global monsoon and monsoon marginal zones[J]. Advances in Earth Science, 2012, 27(1):26-34.
	[林祥, 钱维宏. 全球季风和季风边缘研究[J]. 地球科学进展, 2012, 27(1):26-34.]
[3]	Bao Y, Kang S, Ljungqvist F C, et al. Drought variability at the northern fringe of the Asian summer monsoon region over the past millennia[J].Climate Dynamics, 2014, 43(3/4):845-859.
[4]	Zhang Qiang, Zhang Jie, Qiao Juan,et al. Study on deeply atmospheric boundary layer and its relationship with the land surface thermal process in arid area of China[J]. Science in China (Series D),2011,41(9):1 365-1 374.
	[张强, 张杰, 乔娟,等. 我国干旱区深厚大气边界层与陆面热力过程的关系研究[J]. 中国科学:D辑, 2011,41(9):1 365-1 374.]
[5]	Shi Zhengtao, Zhang Linyuan, Su Guiwu.Natural disasters and their formation causes on Chinese monsoon marginal belt[J]. Journal of Catastrophology, 1994, 9(4): 59-64.
	[史正涛, 张林源, 苏桂武. 中国季风边缘带的自然灾害及成因[J]. 灾害学, 1994, 9(4):59-64.]
[6]	Hao Lisheng, Ding Yihui.Progress of precipitation research in North China[J]. Progress in Geography, 2012,31(5):593-601.
	[郝立生, 丁一汇. 华北降水变化研究进展[J].地理科学进展, 2012, 31(5):593-601.]
[7]	Guan Yinghui, Zheng Fenlin, Zhang Peng, et al. Spatial and temporal changes of meteorological disasters in China during 1950-2013[J]. Natural Hazards, 2015, 75(3):2 607-2 623.
[8]	Tang Xu, Chen Baode, Liang Ping, et al. Definition and features of the north edge of Asian summer monsoon[J]. Acta Meteorologica Sinica, 2010, 24(1): 43-49.
[9]	Hu Haoran, Qian Weihong.Identification of the northernmost boundary of East Asia summer monsoon[J].Progress in Natural Science, 2007,17(1):57-65.
	[胡豪然,钱维宏. 东亚夏季风北边缘的确认[J].自然科学进展,2007,17(1):57-65.]
[10]	Qian W, Shan X, Chen D, et al. Droughts near the northern fringe of the East Asian summer monsoon in China during 1470-2003[J]. Climatic Change, 2012, 110(1):373-383.
[11]	Huang Fei, Li Dongliang, Tang Xu, et al. Determination on the north boundary of summer monsoon in East Asian with soaking rainfall[J].Journal of Applied Meteorological Science, 2009, 20(5): 530-538.
	[黄菲, 李栋梁, 汤绪,等. 用过程透雨量确定的东亚夏季风北边缘特征[J].应用气象学报, 2009, 20(5):530-538.]
[12]	Li Chun, Han Xiao.Relationship of northern boundary of East Asian summer monsoon and summer precipitation in eastern part of China[J].Plateau Meteorology,2008, 27(2): 325-330.
	[李春, 韩笑. 东亚夏季风北界与我国夏季降水关系的研究[J]. 高原气象, 2008, 27(2):325-330.]
[13]	Zhu Qian’gen, Yang Song.The northward advance and oscillation of the East-Asian summer monsoon[J]. Journal of Nanjing Institute of Meteorology,1989, 12(3): 249-257.
	[朱乾根,杨松.东亚副热带季风的北进及其低频振荡[J].南京气象学院学报, 1989, 12(3): 249-257.]
[14]	Wu Changgang, Liu Hongsheng, Xie An.Interdecadal characteristics of the influence of northward shift and intensity of summer monsoon on precipitation over Northern China in summer[J].Plateau Meteorology, 2005, 24(5): 656-665.
	[吴长刚, 刘鸿升, 谢安. 夏季风北推和强度对我国北方夏季降水影响的年代际特征[J]. 高原气象, 2005, 24(5): 656-665.]
[15]	Jia Tiefei.Holocene environmental evolution in the transitional area of monsoon climate and inland climate in Northern China[J]. Journal of Inner Mongolia Normal University, 1995,(1): 64-70.
	[贾铁飞. 中国北方季风气候与内陆气候过渡地带全新世环境演变[J],内蒙古师大学报,1995,(1):64-70.]
[16]	Sun Donghuai, Zhou Jie, Wu Xihao, et al. Preliminary reconstruction of annual rainfall in Loess Plateau and loess-desert transitional regions in suitable climatic period of holocene[J]. Journal of Desert Research, 1995, 15(4): 339-344.
	[孙东怀,周杰,吴锡浩,等. 全新世气候适宜期黄土高原及黄土/沙漠过渡区年降水量的初步恢复[J].中国沙漠,1995, 15(4): 339-344.]
[17]	Zeng Jian, Zhang Qiang, Wang Chunling.Spatial-temporal pattern of surface energy fluxes over the East Asian summer monsoon edge area in China and its relationship with climate[J]. Acta Meteorologica Sinica, 2016, 74(6): 876-888.
	[曾剑,张强,王春玲. 东亚夏季风边缘摆动区陆面能量时空分布规律及其与气候环境的关系[J]. 气象学报,2016, 74(6):876-888.]
[18]	Shen Baizhu, Lin Zhongda, Lu Riyu, et al. Circulation anomalies associated with interannual variation of early and late-summer precipitation in Northeast China[J]. Science in China (Series D),2011,41(3):402-412.
	[沈柏竹, 林中达, 陆日宇,等. 影响东北初夏和盛夏降水年际变化的环流特征分析[J]. 中国科学:D辑, 2011,41(3):402-412.]
[19]	Yin Y, Wu S, Du Z,et al. Radiation calibration of FAO56 Penman-Monteith model to estimate reference crop evapotranspiration in China[J]. Agricultural Water Management, 2008, 95(1):77-84.
[20]	Zhang Hongli, Zhang Qiang, Liu Xiaoyun.Study on the main factors of aridity in Hetao area of North China[J].Climate Change Research,2016, 12(1):20-27.
	[张红丽, 张强, 刘晓云. 华北河套地区气候干燥度的影响因素研究[J]. 气候变化研究进展, 2016, 12(1):20-27.]
[21]	Huang Jianping, Ran Jinjiang, Ji Mingxia.Preliminary analysis of the flood disaster over the arid and semi-arid regions in China[J]. Acta Meteorologica Sinica, 2014, 72(6): 1 096-1 107.
	[黄建平,冉津江,季明霞. 中国干旱半干旱区洪涝灾害的初步分析[J]. 气象学报,2014,72(6): 1 096-1 107.]
[22]	Yang Jianping, Ding Yongjian, Cheng Rensheng, et al. The fluctuations of dry and wet climate boundary and its causal analyses in China[J]. Acta Meteorologica Sinica, 2004, 18(2):211-226.
[23]	Yang Jianping, Ding Yongjian, Chen Rensheng, et al. Fluctuations of the semi-arid zone in China, and consequences for society[J]. Climatic Change, 2005, 72(1/2):171-188.
[24]	Bi Shuoben, Qu Ying, Bi Shengjie, et al. Multi-scale impacts of the Pacific SST and PDO on the summer precipitation of North-Central China from 1870 to 2002[J]. Theoretical Applied Climatology, 2017,(24):1-11.
[25]	Zhang Lansheng, Fang Xiuqi, Ren Guoyu, et al. Environmental changes in the North China farming-grazing transitional zone[J]. Earth Science Frontiers, 1997, 4(1/2): 127-136.
	[张兰生, 方修琦, 任国玉,等. 我国北方农牧交错带的环境演变[J]. 地学前缘, 1997, 4(1/2):127-136.]
[26]	Zhang Qiang, Wang Sheng, Zhang Jie,et al. The progresses on land surface processes and atmospheric boundary layer in arid regions[J]. Advances in Earth Science, 2009, 24(11): 1 185-1 194.
	[张强,王胜,张杰,等.干旱区陆面过程和大气边界层研究进展[J]. 地球科学进展, 2009, 24(11):1 185-1 194.]
[27]	Zhang Qiang, Huang Jing, Zhang Liang,et al. Warming and dryingclimate over Loess Plateau area in China and its effect on land surface energy exchange[J]. Acta Physica Sinica, 2013, 62(13): 139 201-139 212.
	[张强,黄菁,张良,等. 黄土高原区域气候暖干化对地表能量交换特征的影响[J]. 物理学报,2013,62(13): 139 201-139 212.]
[28]	Gibbard S, Caldeira K, Bala G, et al. Climate effects of global cover change[J]. Geophysical Research Letters, 2005, 32(23):308-324.
[29]	Sun Lan, Wu Guoxiong.The impact of land surface evapotranspiration on climate change[J]. Science in China (Series D), 2001, 31(1):59-69.
	[孙岚, 吴国雄. 陆面蒸散对气候变化的影响[J]. 中国科学:D辑, 2001, 31(1):59-69.]
[30]	Herrmann S M, Anyamba A, Tucker C J.Recent trends in vegetation dynamics in the African sahel and their relationship to climate[J]. Global Environmental Change, 2005, 15: 394-404.
[31]	Wang Y, Wen C, Zhang J, et al. Relationship between soil temperature in may over Northwest China and the East Asian summer monsoon precipitation[J]. Journal of Meteorological Research, 2013, 27(5):716-724.
[32]	Myoung B, Choi Y, Choi S, et al. Impact of vegetation on land-atmosphere coupling strength and its implication for desertification mitigation over East Asia[J]. Journal of Geophysical Research Atmospheres, 2012, 117(D12):2 870-2 883.
[33]	Meng Weiguang, Li Jiangnan, Wang Anyu, et al. Effect of condensation heating and surface fluxes on the development of a south China Mesoscale Convective System(MCS)[J]. Journal of Tropical Meteorology, 2005, 21(4):368-376.
	[蒙伟光, 李江南, 王安宇,等. 凝结加热和地表通量对华南中尺度对流系统(MCS)发生发展的影响[J]. 热带气象学报, 2005, 21(4):368-376.]
[34]	Charney J G.Dynamics of deserts and drought in the Sahel[J]. Quarterly Journal of the Royal Meteorological Society, 1975, 101: 193-202.
[35]	Parasnis S S.The convective boundary layer during active and break conditions of summer monsoon[J].Journal of the Atmospheric Sciences, 1991, 48(7):999-1 004.
[36]	Li Weiping, Wu Guoxiong, Liu Hui.A numerical simulation study of the impacts of surface albedo on the summer time North Africa subtropical high[J]. Acta Meteorologica Sinica, 2000, 58(1): 26-39.
	[李伟平,吴国雄, 刘辉. 地表反照率的改变影响夏季北非副热带高压的数值模拟[J].气象学报,2000,58(1): 26-39.]
[37]	Claussen M, Bathiany S, Brovkin V, et al. Simulated climate-vegetation interaction in semi-arid regions affected by plant diversity[J]. Nature Geosciences Letters,2013,6: 954-958.
[38]	Tetsuzo Y.Role of land-atmosphere interaction on Asian monsoon climate[J]. Journal of the Meteorological Society of Japan, 2007, 85(7):55-75.
[39]	Xue Y.The impact of desertification in the Mongolian and the Inner Mongolian grass land on the regional climate[J]. Journal of Climate, 1996,9(9):2 173-2 189.
[40]	Yuan Renmin, Sun Jianning, Yao Keya, et al. A laboratory simulation of atmospheric boundary layer analyses of temperature structure in the entrainment zone[J]. Chinese Journal of Atmospheric Sciences, 2002, 26(6): 773-780.
	[袁仁民,孙鉴泞,姚克亚,等.大气边界层的室内模拟研究——夹卷层温度场结构分析[J].大气科学,2002,26(6):773-780.]
[41]	Tan Zhemin, Fang Juan, Wu Rongsheng.Ekman boundary layer fynamic theories[J]. Acta Meteorologica Sinica, 2005, 63(5): 543-555.
	[谈哲敏, 方娟,伍荣生.Ekman边界层动力学的理论研究[J].气象学报,2005,63(5):543-555.]
[42]	Li Yushan.The properties of water cycle in soil and their effect on water cycle for land in the Loess region[J]. Acta Ecologica Sinca, 1983, 3(2):125-132.
	[李玉山. 黄土区土壤水分循环特征及其对陆地水分循环的影响[J]. 生态学报, 1983, 3(2):125-132.]
[43]	Qian W, Lin X, Zhu Y, et al. Climatic regime shift and decadal anomalous events in China[J]. Climatic Change, 2007, 84: 167-189.
[44]	Gettelman A, Kinnison D E, Dunkerton T J, et al. Impact of monsoon circulations on the upper troposphere and lower stratosphere[J]. Journal of Geophysical Research, 2004, 109: 51-67.
[45]	Wang Sheng, Zhang Qiang, Li Hongyu, et al. Comparison of the water and heat characteristics of bare soil in different climate region of the Loess Plateau[J]. Journal of Desert Research, 2013,33(4):1 166-1 173.
	[王胜, 张强, 李宏宇,等. 黄土高原不同气候区裸地水热特征对比[J].中国沙漠,2013,33(4):1 166-1 173.]
[46]	Huang Q, Marsham J H, Parker D J, et al. A comparison of roll and nonroll convection and the subsequent deepening moist convection: An LEM case study based on SCMS data[J]. Monthly Weather Review, 2009, 137: 350-365.
[47]	Goutorbe J P, Lebel T, Dolman A J,et al. An overview of HAPEX-Sahel: A study in climate and desertification[J]. Journal of Hydrology, 1997, 188: 4-17.
[48]	Xia Lu, Zhang Qiang.Plateau surface energy balance components and interannual variability in response to climate fluctuations[J]. Acta Physica Sinica, 2014, 63(11): 119 201.
	[夏露,张强. 黄土高原地表能量平衡分量年际变化及其对气候波动的响应[J]. 物理学报,2014,63(11):119 201.]
[49]	Wei J, Su H, Yang Z L.Impact of moisture flux convergence and soil moisture on precipitation: A case study for the southern United States with implications for the globe[J]. Climate Dynamics, 2016, 46(1/2):467-481.
[50]	Hao Lisheng, Ding Yihui, Min Jinzhong.Relationship between summer monsoon change in East Asia and abnormal summer rainfall in North China[J]. Plateau Meterology,2016,35(5): 1 280-1 289.
	[郝立生, 丁一汇, 闵锦忠. 东亚夏季风变化与华北夏季降水异常的关系[J]. 高原气象, 2016, 35(5):1 280-1 289.]
[51]	Zhang H, Zhang Q, Yue P, et al. Aridity over a semi-arid zone in Northern China and responses to the East Asian summer monsoon[J]. Journal of Geophysical Research Atmospheres, 2016, 121:13 901-139 181.

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