Review of Advances in World Dryland Climate Research (Ⅱ):Main Investigation Progress

QIAN Zheng'an; SONG Minhong; WU Tongwen; CAI Ying

doi:10.7522/j.issn.1000-0534.2017.00076

Plateau Meteorology >

2017 , Vol. 36 >Issue 6: 1457 - 1476

DOI: https://doi.org/10.7522/j.issn.1000-0534.2017.00076

Review of Advances in World Dryland Climate Research (Ⅱ):Main Investigation Progress

QIAN Zheng'an ,
SONG Minhong ,
WU Tongwen ,
CAI Ying

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Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, Gansu, China;Chengdu University of Information Technology, Chengdu 610225, Sichuan, China;National Climate Center, China Meteorological Administration, Beijing 100081, China

Received date: 2017-04-24

Online published: 2017-12-28

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Abstract

As the continued paper of the review (Ⅰ), the paper (Ⅱ) will further review the main progresses in world dryland climate, including drought indices, arid-and semiarid-zone dividing and their distribution, dryland climate changes, forming causes and projecting. The main points are as follows:(1) More than dozens availability drought "indices" have already put out in various countries, they are well-used in home and abroad. Say, the PDSI, SPI and NDVI indices and so on in the US. (2) Nowdays more researchers utilize the "moisture availability as the "criteria" in dividing the dry areas. Among nearly 10 existed arid-and semiarid-zone maps have been published, the map of Hulme and Marsh is more closer to the real world. On the average, the arid-and semiarid-area make totally up 35% of the global land area, they cover the 8 major arid areas:ie, the North Africa, Australia and China-Mongolia ones and so on; there are the home of about 20 billion people of the globe. (3) The global climate changes in past 1 000 (especially in the recent 100) years are mainly characterized by global warming of the surface air temperature and the larger temporal-and spatial-changes of precipitation climate. Due to the increased CO₂ and CH₄ greenhouse gasses, the global mean temperature increased 0.56~0.92℃ in the past 100 years. In contrast, beyond the East Asia and North Africa, the precipitation climate change links among other dry zones are not so close to each other. There are two combination partterns for temperature and precipitation change in various dry zone in the past. (4) There are many ways for the drought causes across the world arid zones. From the recent discussions about North Africa and China-Mongolia drought causes, it is seemely that the global arid climate forming may classified briefly in two types only:namely global tropical warm SST and mountain topography impact ones. North Africa and China-Mongolia arid areas are the respectively representation of the two types. The discussions show:for the former, it is caused by mainly the global warm SST, especially in the tropical zone and secondly by the land-air interaction; for the latter, by mainly the Qinghai-Xizang Plateau topography and secondly by the circulation. (5) The key point of the arid climate prediction is the one of the decodal drought. There are long road to go for the arid climate prediction.

Key words： Dryland climate adva; drought indices; drought area distrib; dryland climate chan; drought forming caus

Cite this article

QIAN Zheng'an , SONG Minhong , WU Tongwen , CAI Ying . Review of Advances in World Dryland Climate Research (Ⅱ):Main Investigation Progress[J]. Plateau Meteorology, 2017 , 36(6) : 1457 -1476 . DOI: 10.7522/j.issn.1000-0534.2017.00076

References

[1]Alley W M, 1984. The Palmer Drought Severity Indices:Limitations and assumptions[J]. J Climate Appl Meteor, 23:1100-1109.
[2]Booth W, 2002. US wildfires are a symptom of a bigger problem:Drought[M]. Washington:the Washington Post, 5.
[3]Bradley R S, Diaz H F, Eischeid K, et al, 1987. Precipitation fluctuation over northern hemisphere land areas since the mid-19th century[J]. Science, 237(4811):171-175.
[4]Bruins H J, 2012. Ancient desert agriculture in the Negev and climate-zone boundary changes during average wet and drought years[J]. J Arid Environment, 86:28-42.
[5]Charney J G, 1975. Dynamics of deserts and drought in the Sahel[J]. Quart J Roy Meteor Soc, 101(428):193-202.
[6]Chen F H, Yuan Y J, Wei W, 2011. Climatic response of Pice crassifolia tree-ring parameters and precipitation reconstruction in the western Qilian Mountains, China[J]. J Arid Environ, 75:1121-1128.
[7]Cook E R, Meko D M, Stahle D W, et al, 1999. Drought reconstruction for the continental United States[J]. J Climate, 12:1145-1162.
[8]Folland C K, Owen J A, Ward M N, et al, 1991. Prediction of seasonal rainfall in the Sahel region of Africa using empirical and dynamical method[J]. J Forecasting, 10:21-56.
[9]Folland C K, Palmer T N, Parker D E, 1986. Sahel rainfall and worldwide sea temperatures, 1901-85[J]. Nature, 320:602-606.
[10]Fye F K, Stahle D W, Cook E R, 2003. Paleoclimatic analogs to twentieth-century moisture regimes across the United States[J]. Bull Amer Meteor Soc, 84(7):901-909.
[11]Giannini A, Saravanan R, Chang P, 2003. Oceanic forcing of Sahel rainfall on interannual to interdecadal time scale[J]. Science, 302:1027-1030.
[12]Gibbs W J, 1987. A drought watch system, WCP-134[J]. Geneva:World Meteorological Organization, 1-23.
[13]Giorgi F, Coppola E, Solmon F, et al, 2012. RegCM4 model description and preliminary test over multile CORDEX domain[J]. Clim Res, 52:7-29.
[14]Heim R R Jr, 2002. A review of twentieth-century drought indices used in the United States[J]. Bull Amer Meteor Soc, 83 (8):1149-1165.
[15]Hulme M, 1996. Recent climatic change in the world' drylands[J]. Geophys Res Lett, 23(1):61-64.
[16]IPCC, 2007. Climate change 2007:The physical science basic:Contribution of working group I to the assessment report of the intergovernment Panel on climate change[J]. Cambridge:Cambridge University Press, 235-336.
[17]Keyantash J, Dracup J A, 2002. The quantification of drought:An evaluation of drought indices[J]. Bull Amer Meteor Soc, 83(8):1167-1180.
[18]Kogan F N, 1995. Drought of the late 1980s in the United States as derived from NOAA polar-orbiting satellite data[J]. Bull Amer Meteor Soc, 76:655-668.
[19]Kutzbach J E, Prell W L, Ruddiman W F, 1993. Sensitivity of eurasian climate to surface uplift of the Tibetan Plateau[J]. J Geol, 101:177-190.
[20]Lawrimore J, Heim Jr R R, Svoboda M, et al, 2002. Beginning a new era of drought monitoring across North America[J]. Bull Amer Meteor Soc, 83(8):1191-1198.
[21]Li J B, Cook E R, Chen F H, et al, 2010. An extreme drought event in the central Tianshan area in the year 1945[J]. J Arid Environ, 74:1225-1231.
[22]Li J B, Gou X H, Cook E R, et al, 2006. Tree-ring based drought reconstruction for the central Tien Shan area in Northwest China[J]. Geophy Res Lett, 33, L07715, DOI:10.1029/02006GL25803.
[23]Li J F, Yuan Y J, Zhou W S, 1989. Xinjiang dendrohydrological research[J]. Beijing:China Meteorlogical Press, 1-57.
[24]Liu X D, Dong B W, 2013. Influence of Tibetan Plateau uplift on the Asian monsoon-arid environment evolution[J]. China Sci Bull, 58(34):4277-4291.
[25]Liu X D, Guo Q C, Guo Z T, et al, 2015a. Where were the monsoon regions and arid zones in Asian prior to the Tibetan Plateau uplift?[J]. National Science Review, 2(4):411-414.
[26]Liu X D, Sun H, Miao Y F, et al, 2015b. Impact of uplift of Northern Tibetan Plateau and formation of Asian inland deserts on regional climate and environment[J]. Quaternary Science Reviews, 116:1-14.
[27]Mamtimin B, Et-TanTawi A M, Schaeter D, et al, 2011. Recent trends of temperature change under hot and cold desert climate:Comparing the Sahera (Libya) and Central Asia (Xinjiang, China)[J]. J Arid Environ, 75:1105-1113.
[28]Manabe S, Broccolli A J, 1990. Mountains and arid climates of middle latitudes[J]. Science, 247:192-195.
[29]Mckee T B, Doesken N J, Kleist J, 1993. The relationship of drought frequency and duration to time scales[R]. Preprints, Eighth Conf on Applied Climatology, Anaheiml, CA, Amer Meteor Soc, 179-184.
[30]Nicholls N, 1985. Towards the prediction of major Australian drought[J]. Austri Met Mag, 33:161-166.
[31]Nicholls N, 2004. The changing nature of Australian droughts[J]. Climatic Change, 63(3):323-336.
[32]Nicholson S E, 1980. The nature of rainfall flectuations in subtropical West Africa[J]. Mon Wea Rev, 108(4):473-487.
[33]Nicholson S E, 1988. Land surface and atmosphere interaction:Physical processes and surface changes and their impact[J]. Prog Phy Geogr, 12:36-65.
[34]Nicholson S E, Some B, Kone B, 2000. An analysis of recent in West Africa, including the rainy seasons of the 1997 El Nino and the 1998 La Nina years[J]. J Climate, 13:2628-2640.
[35]Olapid E O, 1985. A comparative performance analysis of three meteorological drought indexes[J]. J Climate, 5:655-644.
[36]Palmer W C, 1965. Meteorological drought[J]. US Weather Bureau Research Paper, 45, 58.
[37]Pederson N, Jacoby G C, D'Arrigo R D, et al, 2001. Hydrometeorological reconstructions for Northeastern Mongolia derived from tree rings:1651-1995[J]. J Climate, 14:873-881.
[38]Prospero J M, Nees R T, 1986. Impact of the North African drought and El Nino on mineral dust in Barodos trade winds[J]. Nature, 320:735-738.
[39]Redmond K T, 2002. The depiction of drought-a commentary[J]. Bull Amer Meteor Soc, 83(8):1143-1165.
[40]Rowell D P, Folland C K, Maskell K, et al, 1992. Modeling the influence of global sea temperatures on the variability and predicability of seasonal Sahel rainfall[J]. Geophy Res Lett, 19(9):905-908.
[41]Sheffield J, Wood E F, Roderick M L, 2012. Little change in Global drought over the past 60 years[J]. Nature, 491(7424):435-438.
[42]Shinoda M, 1990. Long-term Sahelian drought from the late 1960's to the mid-1980's and its relation to the atmospheric circulation[J]. J Meteor Soc Japan, 68(5):613-624.
[43]Streten N A, 1981. Southern Hemisphere sea surface temperature variability and apparent association with Australian rainfall[J]. J Geophys Res, 86(c1):485-497.
[44]Streten N A, 1983. Circulation contrasts in the Southern hemisphere winters of 1972 and 1973[J]. Austri Meteor Mag, 31:161-170.
[45]Sud Y C, Smith W E, 1985. The influence of surface roughness of deserts on the July circulation[J]. Prog Phy Geogr, 12:36-65.
[46]Sun H, Pan Z T, Liu X D, 2012. Numerical simulation of spacial-temporal distribution of dust aero and its direct radiative effects on East Asian Climate[J]. J Geophys, 117:D13206.
[47]Sun J M, Liu T S, 2006. The age of Takimakan Desert[J]. Science, 312:1621.
[48]Svoboda M, LeComte D, Hayes M, et al, 2002. The drought monitor[J]. Bull Amer Meteor Soc, 83(8):1181-1190.
[49]Tanaka T Y, Chiba M, 2005. Global simulation of dust aerosol with a chemical transport model, MASINGAR[J]. J Meteor Soc Japan, 83A:255-278.
[50]Tannehill I R, 1947. Drought-Its causes and effects[M]. Princeton:Princeton University Press, 1-264.
[51]Thomas D S G, 1997. Arid zone geomorphology——Process, form and change in dryland[M]. 2nd Edition. New York:John Wiley & Sons Press, 5-12.
[52]Trenberth K E, 1998. Atmospheric moisture residence times and cycling:Implication for rainfall rates and climate changes[J]. Climatic Change, 39:667-694.
[53]Voice M E, Hunt B G, 1984. Study of the dynamics of drought initiation using a global general circulation model[J]. J Geophy Res, 89(D6):9504-9520.
[54]Washington R, Preston A, Todd M. 2003. The role of Indian and Pacific Ocean SSTs in African rainfall variability[J]. Bull Amer Meteor Soc, 84(7):899-900.
[55]WMO, 1975. Drought and agriculture[R]. WMO Technical Note No 138, WMO-No 392, Geneva, Switzerland, 113, 127.
[56]An S Q, 1985. Revised Palmer index[J]. Meteor Mon, 11(12):5-11. 安顺清, 1985.修正的Palmer指数[J].气象, 11(12):5-11.
[57]Bai Z Y, Xu G C, Chen Q, et al, 1988. Weather of Northwest China[M]. Beijing:China Meteorology Press, 1-442. 白肇烨, 徐国昌, 陈乾, 等, 1988.中国西北天气[M].北京:气象出版社, 1-442.
[58]Cai Y, Qian Z A, 2003. Contrast analyses on water vapor and EASM between dry and wet years of Northwest and North China[J]. Plateau Meteor, 22(1):14-25. 蔡英, 钱正安, 2003.华北和西北区干湿年间水汽场和东亚夏季风的对比分析[J].高原气象, 22(1):14-25.
[59]蔡英, 宋敏红, 钱正安, 等, 2015.西北旱区夏季强干、湿事件环流及水汽输送的再分析[J].高原气象, 34(3):597-610.
[60]Cai Y, Song M H, Qian Z A, et al, 2005. Reanalyses of circulation and water vapor transport between strong dry and wet years of Northwest China in summer[J]. Plateau Meteor, 34(3):597-610.
[61]Chen X C, Xu Y, Xu C H, et al. 2014. Assessment of precipitation simulations in China by CMIP5 multi-models[J]. Progressus Inquisitiones De Mutatione Climatis, 10(3):217-225. 陈晓晨, 徐影, 许崇海, 等, 2014.CMIP5全球气候模式对中国地区降水模拟能力的评估[J].气候变化研究进展, 10(3):217-225.
[62]Chen Y Y, Chen N, Qian Z A, et al, 2011. Temporal and spatial change features of precipitation over CMASA(Ⅱ):Synthetical climate subregions of the CMASA and further analyses of periodic change of precipitation in its various ones[J]. Plateau Meteor, 30(1):13-21. 陈豫英, 陈楠, 钱正安, 等, 2011.中蒙干旱半干旱区降水时空变化特征分析(Ⅱ):综合气侯分区及各分区降水时间变化的进一步分析[J].高原气象, 30(1):13-21.
[63]Chen Y Y, Chen N, Wang S G, et al, 2010. Temporal and spatial change features of precipitation over CMASA(Ⅰ):Features of annual precipitation and REOF of precipitation from May to September[J]. Plateau Meteor, 29(1):33-43. 陈豫英, 陈楠, 王式功, 等, 2010.中蒙干旱半干旱区降水的时空变化特征(Ⅰ):年降水的特征及5-9月降水的REOF分析[J].高原气象, 29(1):33-43.
[64]Dai J X, Zhou L S, Wu Y S, et al, 1990. Climate of Tibetan Plateau[M]. Beijing:China Meteorology Press, 1-356. 戴加洗, 周陆生, 吴永森, 等, 1990.青藏高原气候[M].北京:气象出版社, 1-356.
[65]Ding Y H, Sun Y, Liu Y Y, et al, 2013. Interdecadal and interannual variabilities of the Asian summer monsoon and its projection of future change[J]. Chinese J Atmos Sci, 37(2):253-280. 丁一汇, 孙颖, 刘芸芸, 等, 2013.亚洲夏季风的年际和年代际变化及其未来预测[J].大气科学, 37(2):253-279.
[66]Ding Y H, Wang S R. 2001. An introduction to climate and ecological environment in Northwest China[M]. Beijing:China Meteorology Press, 1-154. 丁一汇, 王守荣, 2001.中国西北地区气候与生态环境概论[M].北京:气象出版社, 1-154.
[67]Fu C B, 1994. Studies on the observed abrupt climatic change[J]. Chinese J Atmos Sci, 18(3):373-384. 符淙斌, 1994.气候突变现象的研究[J].大气科学, 18(3):373-384.
[68]Gao G D. 1961. Discussion on the eastern boundary between the Qinghai-Xizang Plateau and arid areas of the Northwest China[J]. Acta Geographica Sinica, 27:80-84. 高国栋, 1961.对我国自然区划中青藏高原区和西北干旱区东部界线问题的探讨[J].地理学报, 27:80-84.
[69]Geng Qichang, et al, eds, 1985. The past and present of the arid climate[M]. Barry R G. The study of global desert. Chongqing:Science and Technology Press, 16-19. 耿其昌, 等译, 1985.干旱气候的过去和现在[M]. Barry R G.世界沙漠研究.重庆:科学技术出版社重庆分社, 16-19.
[70]State Science and Technology Commission, 1990. Climate(No 5 blue book from China Science and Technology)[R]. Beijing:Science and Technology Literature Press, 1-367. 国家科学技术委员会, 1990. 气候(中国科学技术兰皮书第5号)[R]. 北京: 科学技术文献出版社, 1-367.
[71]Huang J P, Ji M X, Liu Y Z, et al. 2013. An overview of arid and semi-arid climate change[J]. Progressus Inquisitiones de Mutatione Climatis, 9(1):9-14. 黄建平, 季明霞, 刘玉芝, 等, 2013.干旱半干旱区气候变化综述[J].气候变化研究进展, 9(1):9-14.
[72]Yoshino J M, 2002. Chinese desertification[M]. Chen W P eds. Beijing:China Science and Technology Press, 1-254. 吉野正敏, 2002. 中国的沙漠化[M]. 陈维平等译. 北京: 中国科学技术出版社, 1-254.
[73]Kang X C, Cheng G D, Kang E S, et al. 2002. Reconstruction of mountain runoff in Heihe for nearly a thousand years using tree ring data[J]. Science of China (Earth Sciences), 32(8):675-685. 康兴成, 程国栋, 康尔泗, 等, 2002.利用树轮资料重建黑河近千年来出山口径流量[J].中国科学(地球科学), 32(8):675-685.
[74]Li D L, Liu D X, 2000. Climate of Gansu[M]. Beijing:China Meteorological Press, 1-378. 李栋梁, 刘德祥, 2000.甘肃气候[M].北京:气象出版社, 1-378.
[75]Li D L, Peng S Q, Yao H, 1995. Climatic features of the mean temperature in Northwest China during winter time[J]. Chinese J Atmos Sci, 19(2):192-199. 李栋梁, 彭素琴, 姚辉, 1995.我国西北地区冬季平均气温的气候特征[J].大气科学, 19(2):192-199.
[76]Li D L, Xie J N, Wang W, 1997. A study of summer precipitation features and anomaly in Northwest China[J]. Chinese J Atmos Sci, 21(3):331-340. 李栋梁, 谢金南, 王文, 1997.中国西北夏季降水特征及其异常研究[J].大气科学, 21(3):331-340.
[77]Li J F, 1991. Climate of Xinjiang[M]. Beijing:China Meteorology Press, 1-302. 李江风, 1991.新疆气候[M].北京:气象出版社, 1-302.
[78]Li J F, Yuan Y J, You X Y, 2000. Research and application of tree ring hydrology[M]. Beijing:Science Press, 186-252. 李江风, 袁玉江, 由希尧, 2000.树木年轮水文学研究与应用[M].北京:科学出版社, 186-252.
[79]Li W Y, Qian Z A, 2005. Temporal and spatial feature analyses of winter and summer surface air temperature in CMASA, part(Ⅰ):January[J]. Plateau Meteor, 24(6):889-898. 李万源, 钱正安, 2005.中蒙干旱半干旱区冬、夏季地面气温时空变化特征分析(Ⅰ):1月[J].高原气象, 24(6):889-898.
[80]Li W Y, Qian Z A, 2006. Temporal and spatial feature analyses of winter and summer surface air temperature in CMASA, part(Ⅱ):July[J]. Plateau Meteor, 25(4):624-632. 李万源, 钱正安, 2006.中蒙干旱半干旱区冬、夏季地面气温时空变化特征分析(Ⅱ):7月[J].高原气象, 25(4):624-632.
[81]Li X Z, Liu X D, Ma Z G, 2004. Analysis on the drought characteristics in the main arid regions in the world since recent hundred-odd years[J]. Arid Zone Res, 21(2):97-103. 李新周, 刘晓东, 马柱国, 2004.近百年来全球主要干旱区的干旱化特征分析[J].干旱研究, 21(2):97-103.
[82]Li X Z, Liu X D, 2012. A modeling study on drought trend in the Sino-Monogolian arid and semiarid regions in the 21st century[J]. Arid Zone Res, 29(2):262-272. 李新周, 刘晓东, 2012.21世纪中蒙干旱半干旱区干旱化趋势的模拟研究[J].干旱区研究, 29(2):262-272.
[83]Li Y Y, Qian Z A, Xue X L, et al, 2009. Deep mixed layer in Northwest China dry area in summer half year and formation of the dry climate[J]. Plateau Meteor, 28(1):46-54. 李岩瑛, 钱正安, 薛新玲, 等, 2009.西北干旱区夏半年深厚混合层与干旱气候形成[J].高原气象, 28(1):46-54.
[84]Luan C, 2012.Some statistical study of strong precipitation and comparative analysis of the formation of severe dry and wet years in summer in the west of Northwest China[D]. Lanzhou:Cold Arid Environmental and Engeering Research Institute. 栾晨, 2012. 中国西北区西部夏季强降水若干统计及其干、湿年形成的对比分析[D]. 兰州: 中国科学院寒区旱区环境与工程研究所.
[85]Luo Z X, 2005. Dynamics theory of drought climate in Northwest China[M]. Beijing:China Meteorology Press, 1-232. 罗哲贤, 2005.中国西北干旱气候动力学引论[M].北京:气象出版社, 1-232.
[86]Ma Z G, Huang G, Gan W Q, et al. 2005. Multi-scale temporal characteristics of the dryness/wetness over Northern China during the last century[J]. Chinese J Atmos Sci, 29(5):671-681. 马柱国, 黄刚, 甘文强, 等, 2005.近代中国北方干湿变化趋势的多时段特征[J].大气科学, 29(5):671-681.
[87]Moorezajef A, 1958. Nature Geographic in the People's Republic of Mongolia[M]. Bai Y H, ed. Beijing:Joint Publishing, 1-529. 穆尔扎也夫A, 1958. 蒙古人民共和国自然地理[M]. 柏郁华译. 北京: 三联书店, 1-529.
[88]Qian Z A, Song M H, Li W Y, et al, 2011. Global, China-Mongolia arid-and semiarid-areas(CMASA) and the details of precipitation distribution in part regions of CMASA[J]. Plateau Meteor, 30(1):1-12. 钱正安, 宋敏红, 李万源, 等, 2011.全球及中蒙干旱区部分地区降水分布细节[J].高原气象, 30(1):1-12.
[89]Qian Z A, Wu T W, Liang X Y, 2001a. Feature of mean vertical circulation over the Qinghai-Xizang Plateau and its neighborhood[J]. Chinese J Atmos Sci, 25(4):444-454. 钱正安, 吴统文, 梁潇云, 2001a.青藏高原及周围地区的平均垂直运动场特征[J].大气科学, 25(4):444-454.
[90]Qian Z A, Wu T W, Lü S H, et al, 1998. Numerical simulation of Northwest China arid climate formation-effects of the Qinghai-Xizang Plateau terrain and circulation field[J]. Chinese J Atmos Sci, 22(5):753-763. 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(5):753-763.
[91]Qian Z A, Wu T W, Song M H, et al, 2001b. Arid disaster and advances in arid climate researches over Northwest China[J]. Adv Earth Sci, 16(1):28-38. 钱正安, 吴统文, 宋敏红, 等, 2001b.干旱灾害和我国西北干旱气候的研究进展及问题[J].地球科学进展, 16(1):28-38.
[92]Qian Z A, Song M H, Wu T W, et al, 2017. Review of advances in world dryland climate research (Ⅰ):Development and Contribution of some main dryland countries and the UN[J]. Plateau Meteor, 36(6):1433-1456. DOI:10.7522/j. issn. 1000-0534.2017. 00075. 钱正安, 宋敏红, 吴统文, 等, 2017.世界干旱气候研究动态及进展综述(Ⅰ):若干主要干旱区国家的研究动态及联合国的贡献[J].高原气象, 36(6):1433-1456.
[93]Qin D H, Ding Y H, et al, eds, 2007. Climate in twenty-first century[M]. Beijing:China Meteorology Press, 1-259. 秦大河, 丁一汇, 等译, 2007.21世纪的气候[M].北京:气象出版社, 1-259.
[94]Qu X Z, Yang Y Q, Wang Z, 2009.The six most important in the world about ancient animal fossils in Hezheng[N]. Lanzhou Evening News, July 19, twelfth edition. 瞿学忠, 杨雅琴, 王卓, 2009. 和政古动物化石的六大世界之最[N]. 兰州晚报, 7月19日第12版.
[95]Shao X M, Liang E Y, Huang L, et al, 2006. A reconstructed precipitation series over the past millennium in the Northeastern Qaidam Basin[J]. Adv Climate Change Res, 2(3):122-126. 邵雪梅, 梁尔源, 黄磊, 等, 2006.柴达木盆地东北部过去1437年的降水变化重建[J].气候变化研究进展, 2(3):122-126.
[96]Shi N, Chen L W, 2003. Climatic change of global land flood/drought in June-August during 1920-2000[J]. Acta Meteor Sinica, 61(2):237-244. 施能, 陈绿文, 2003.1920-2000年6-8月全球陆地旱涝气候变化[J].气象学报, 61(2):237-244.
[97]Sun A J, Gao B, 2000. A diagnostic analyses of serious flood/drought during summer season in the North China Plane[J]. Chinese J Atmos Science, 24(3):393-402. 孙安健, 高波, 2000.华北平原夏季严重旱涝特征诊断分析[J].大气科学, 24(3):393-402.
[98]Sun G W, Luo Z X, Li Z Y, et al, 1996. Study of drought climate in Northwest China[M]. Beijing:China Meteorology Press, 1-394. 孙国武, 罗哲贤, 李兆元, 等, 1996.中国西北干旱气候研究[M].北京:气象出版社, 1-394.
[99]Wang W G, Feng Z D, Khosbayar P, et al, 2005. The studies of holocene climate changes in Mogolia:A review[J]. Adv Earth Science, 20(2):240-247. 汪卫国, 冯兆东, Khosbayar P, 等, 2005.蒙古全新世气候变化研究进展[J].地球科学进展, 20(2):240-247.
[100]Wang H J, Fan K, 2013. Recent changes in the East Asian monsoon[J]. Chinese J Atmos Sci, 37(2):313-318. 王会军, 范可, 2013.东亚季风近几十年的主要变化特征[J].大气科学, 37(2):313-318.
[101]Wang J S, ed, 2004. Weather and climate in Qinghai[M]. Beijing:China Meteorology Press, 1-616. 王江山主编, 2004.青海天气气候[M].北京:气象出版社, 1-616.
[102]Wang S W, Luo Y, Wen X Y, et al, 2007. Latest advances in studies of the global temperature variations for the last millennium[J]. Adv Climate Change Res, 3(1):14-19. 王绍武, 罗勇, 闻新宇, 等, 2007.近千年全球温度变化研究的新进展[J].气候变化研究进展, 3(1):14-19.
[103]Wang T, Chen G T, Zhao H L, et al, 2003. Desert and desertification in China[M]. Shijiazhuang:Hebei Science and Technology Press, 1-955. 王涛, 陈广庭, 赵哈林, 等, 2003.中国沙漠与沙漠化[M].石家庄:河北科学技术出版社, 1-955.
[104]Wang W H, 1990. Climate of Inner Mongolia[M]. Beijing:China Meteorological Press, 1-273. 王文辉, 1990.内蒙古气候[M].北京:气象出版社, 1-273.
[105]Wei J, Ma Z G, 2003. Comparison of Palmer drought severity index, percentage of precipitation anomaly and surface humid index[J]. Acta Geographica Sinica, 58(7s):117-124. 卫捷, 马柱国, 2003.Palmer干旱指数、地表湿润指数与降水距平的比较[J].地理学报, 58(增刊1):117-124.
[106]Wei F Y, Zhang X G, 2001. Dryness and wetness grades series during 1991-2000 in China[J]. Meteor Mon, 27(3):46-50. 魏凤英, 张先恭, 2001.1991-2000年中国旱涝等级资料[J].气象, 27(3):46-50.
[107]Wu G X, Liu Y M, Liu X, et al, 2005. How the heating over the Tibetan Plateau affects the Asian climate in summer[J]. Chinese J Atmos Sci, 29(1):47-56. 吴国雄, 刘屹岷, 刘新, 等, 2005.青藏高原加热如何影响亚洲夏季的气候格局[J].大气科学, 29(1):47-56.
[108]Wu T W, Qian Z A, 1996a. Comparative analyses of differences between circulation and dynamical effect of Qinghai-Xizang Plateau over Northwest China drought area in dry-and wet-summer[J]. Plateau Meteor, 15(4):387-396. 吴统文, 钱正安, 1996a.夏季西北干旱区干、湿年环流及高原动力影响差异的对比分析[J].高原气象, 15(4):387-396.
[109]Wu T W, Qian Z A, 1996b. The comparative analyses of differences between vertical circulation on north side of Tibetan Plateau in wet and dry summer and thermal effects of the Plateau[J]. Acta Meteor Sinica, 54(5):558-568. 吴统文, 钱正安, 1996b.青藏高原北侧地区干湿年夏季垂直环流差异的对比分析及青藏高原的热力影响[J].气象学报, 54(5):558-568.
[110]Xie J N, ed, 2000. Climatic change and prediction of drought in Northwest China[M]. Beijing:China Meteorolgical Press, Vol 1:1-343; Vol 2:1-308; Vol 3:1-376. 谢金南主编, 2000. 中国西北干旱气候变化与预测研究[M]. 北京: 气象出版社, 第1卷, 1-343;第2卷, 1-308;第3卷, 1-376.
[111]Xu G C, 1997. Climate change in arid and semi-arid regions of China[M]. Beijing:China Meteorological Press, 1-101. 徐国昌, 1997.中国干旱半干旱区气候变化[M].北京:气象出版社, 1-101.
[112]Xu G C, Zhang Z Y, 1983. The effect of Qinghai-Xizang Plateau in the formation of dry climate over the Northwest of China[J]. Plateau Meteor, 2(2):9-16. 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.
[113]Yaluo M, 2015.The concentration of carbon dioxide in the atmosphere exceeds the warning line[N]. Reference News, November 11, seventh edition. 雅罗·米, 2015. 大气中二氧化碳浓度超过警戒线[N]. 参考消息, 11月11日第7版.
[114]Yang J C, 1958. Practice and prospect of long term weather forecast[J]. Chinese Sci Bull, 9(23):722-724. 杨鑑初, 1958.长期天气预报的实践与前景[J].科学通报, 9(23):722-724.
[115]Ya D Z, Gao Y X, et al, eds, 1979. Meteorology in Qinghai-Xizang Plateau[M]. Beijing:Science Press, 1-278. 叶笃正, 高由禧, 等编, 1979.青藏高原气象学[M].北京:科学出版社, 1-278.
[116]Ye D Z, Huang R H, 1990. Research progress of drought and flood climate[M]. Beijing:China Meteorological Press, 1-156. 叶笃正, 黄荣辉, 1990.旱涝气候研究进展[M].北京:气象出版社, 1-156.
[117]Ye D Z, Huang R H, 1996. Law and cause of drought and flood in the Yellow River and the Yangtze River[M]. Jinan:Shandong Science and Technology Press, 1-387. 叶笃正, 黄荣辉, 1996.长江黄河流域旱涝规律和成因研究[M].济南:山东科学技术出版社, 1-387.
[118]Ye D Z, Zeng Q C, Guo Y F, 1991. Contemporary climate research[M]. Beijing:China Meteorological Press, 1-353. 叶笃正, 曾庆存, 郭裕福, 1991.当代气候研究[M].北京:气象出版社, 1-353.
[119]Zhang J B, Deng Z F, 1987. Introduction of precipitation in Xinjiang[M]. Beijing:China Meteorological Press, 1-410. 张家宝, 邓子风, 1987.新疆降水概论[M].北京:气象出版社, 1-410.
[120]Zhang J C, Lin Z G, 1985. Chinese Climate[M]. Shanghai:Shanghai Technology Press, 1-603. 张家诚, 林之光, 1985.中国气候[M].上海:上海科技出版社, 1-603.
[121]Zhang L, Ding Y H, Sun Y, 2008. Evaluation of precipitation simulation in East Asian monsoon areas by coupled ocean-atmosphere general circulation models[J]. Chinese J Atmos Sci, 32(2):261-276, 张莉, 丁一汇, 孙颖, 2008.全球海气耦合模式对东亚季风降水模拟的检验[J].大气科学, 32(2):261-276.
[122]Zhang Q, Pan X B, Ma Z G, et al, 2009. Drought[M]. Beijing:China Meteorological Press, 1-198. 张强, 潘学标, 马柱国, 等, 2009.干旱[M].北京:气象出版社, 1-198.
[123]Zhang X Y, Zhao Y, 2009.Ancient Gansu-A paradise for dinosaurs[N]. Lanzhou Morning News, July 27, A14 edition. 张馨玉, 赵扬, 2009. 远古甘肃-恐龙生存的乐园[N]. 兰州晨报, 7月27日A14版.
[124]Academy of Meteorological Sciences, China Meteorological Administration, 1981. Atlas of droughts and floods in China in recent 500 years[Z]. Beijing:Map Publishing Press, 1-332. 中国气象局气象科学研究院主编, 1981. 中国近500年旱涝分布图集[Z]. 北京: 地图出版社, 1-332.
[125]Zhou J Q, Cai Y, Qian Z A, et al, 2009a. Simulation on impact of water vapor in various source areas on NWC precipitation summer (Ⅰ):Experiment schemes and contrast run results[J]. Plateau Meteor, 28(6):1211-1219. 周建琴, 蔡英, 钱正安, 等, 2009a.夏季不同源地水汽对西北地区降水影响的数值模拟(Ⅰ):试验个例、方案设计及对照试验结果[J].高原气象, 28(6):1211-1219.
[126]Zhou J Q, Qian Z A, Cai Y, et al, 2009b. Simulation on impact of water vapor in various source areas on NWC precipitation summer (Ⅱ):Sensitive run results of effects of decreasing (increasing) water vapor in various source areas[J]. Plateau Meteor, 28(6):1220-1232. 周建琴, 钱正安, 蔡英, 等, 2009b.夏季不同源地水汽对西北地区降水影响的数值模拟(Ⅱ):减、增各源区水汽影响的敏感性试验[J].高原气象, 28(6):1220-1232.
[127]Zhu K Z, 1973. Preliminary study of climate changes in China in the past five thousand years[J]. Science of China, 3(2):168-189. 竺可桢, 1973.中国近五千年来气候变迁的初步研究[J].中国科学, 3(2):168-189.

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