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Recent Research Advances on the Interannual-interdecadal Variations of Drought/Flood in South China and Associated Causes
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摘要: 基于气候变暖背景下中国南方旱涝时空格局发生变化的基本事实，回顾了中国南方降水的主要模态和旱涝年际年代际尺度变化特征及其成因的主要研究进展。研究指出，El Niño发展年，中国南方大部地区降水偏少，尤其在长江及其以南地区，而El Niño衰减年则相反。强调热带印度洋海盆一致偏暖使西太平洋副热带高压增强，位置偏南，导致西北太平洋反气旋异常的形成和维持，有利于中国南方降水加强。青藏高原冬春季积雪多，春夏季高原感热和上升运动较弱，导致夏季风偏弱，有利于长江流域降水偏多易涝，反之亦然。关于多因子协同作用对南方旱涝影响，指出南方旱涝是多因子协同影响的结果, 如菲律宾反气旋受冬季青藏高原积雪、El Niño与前期春季印度洋海温等多因子协同影响。南方旱涝与影响因子发生了年际关系的年代际变化，在气候变暖背景下，随着后者的年代际转型，其对前者的影响关系也发生了年代际变化。因此，提出了应该关注南方旱涝的预测策略与方法，提高旱涝预测技巧。Abstract: Based on changes of spatial-temporal distribution of flood and drought in South China under global warming, the recent research progress on characteristics of inter-annual and inter-decadal variations of drought/flood and associated causes are reviewed. It's found there will be less precipitation in South China especially for the Yangtze valley in the developing phase of El Niño, while more precipitation in the decay phase. During the above process, the basin wide warming in tropical Indian Ocean are found to intensify the Northwestern Pacific subtropical high and shift it to a more southward position, leading to the occurrence of low-level anticyclone circulation over Northwestern Pacific, which would affect the precipitation of South China through adjusting the southerly and moisture transportation. The snow cover of the Tibet Plateau is also found as a key factor, when more snow cover occurs in spring-winter, the sensible heat flux is too weak to heat troposphere, which would reduce the meridional temperature gradient to cause a weak summer monsoon and more precipitation over the Yangtze valley, and vice versa. For synergistic effects of multi-factors on the occurrence of flood and drought in South China, results indicate it's impacted by multiple factors and cannot be dominated by one single factor. For example, the Philippine anticyclone can be impacted by the winter Tibet Plateau snow cover, El Niño and basin wide warming of tropical Indian Ocean. For the inter-decadal variation of the inter-annual relationship between flood and drought in South China and their influencing factors, strong inter-decadal variation on the relationship between the influencing factors and flood/drought are found, when these factors exhibit a strong inter-decadal variation. For example, the relationship between tropical Pacific Ocean and South China precipitation is found loose in recent decades, while the influence of Indian Ocean sea surface temperature anomaly on South China is intensified. Based on the aforementioned results, it suggests more attentions being focused on the prediction strategy and method for South China to improve the predictability of drought and flood.
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图 1 中国夏季 (6—8月) 主要雨带年代际变化
Fig. 1 The interdecadal variation of summertime (JJA) main rain belt in China
图 2 东亚夏季风 (a) 与长江中下游夏季降水指数 (b) 经验模型拟合 (1979—2006年)、后报 (2007—2009年) 与预测 (2010—2012年)[119]
Fig. 2 East Asian Summer Monson index (a) and summer (JJA) rainfall index (b) over the middle reaches of the Yangtze predicted by the NAO-ENSO based empirical model (1979-2006 is the period for the model fitting, 2007-2009 for the hindcasts, 2010-2012 for the prediction)(from reference [119])
表 1 1960—2012年5—8月的PSAC指数与前期冬季TPSD指数、Niño3.4指数以及春季TIO指数的相关系数[93]
Table 1 Correlations of the monthly PSAC index from May to August with the previous winter TPSD index, Niño3.4 SST index, and spring TIO SST index from 1960 to 2013(from reference[93])
指数 PSAC指数 5月 6月 7月 8月 TPSD指数 0.16 0.39*** 0.02 0.17 Niño3.4指数 0.54*** 0.30** 0.50*** 0.29** TIO指数 0.55*** 0.27** 0.34** 0.41*** 注:*表示达到0.1显著性水平，**表示达到0.05显著性水平，***表示达到0.01显著性水平。 
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[1] Fu C B.An Aridity Trend in China in Association with Global Warming.Climate-Biosphere Interaction:Biogenic Emission and Environment Effects of Climate Change, 1994:1-18. [2] 马柱国.我国北方干湿演变规律及其与区域增暖的可能联系.地球物理学报, 2005, 48(5):1011-1018. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX200505005.htm [3] Dai A.Increasing drought under global warming in observations and models.Nature Clim Change, 2013, 3(1):52-58. http://adsabs.harvard.edu/abs/2013NatCC...3...52D [4] Jin D, Guan Z, Tang W.The extreme drought event during winter-spring of 2011 in East China:Combined influences of teleconnection in midhigh latitudes and thermal forcing in maritime continent region.J Climate, 2013, 26(20):8210-8222. doi: 10.1175/JCLI-D-12-00652.1 [5] Wang Y, Ren F, Zhang X.Spatial and temporal variations of regional high temperature events in China.Int J Climatol, 2014, 34(10):3054-3065. doi: 10.1002/joc.2014.34.issue-10 [6] 王艳姣, 高蓓, 周兵, 等.2013年全球重大天气气候事件及其成因.气象, 2014, 40(6):759-768. doi: 10.7519/j.issn.1000-0526.2014.06.013 [7] 李清泉, 王安乾, 周兵, 等.2014年全球重大天气气候事件及其成因.气象, 2015, 41(4):497-507. doi: 10.7519/j.issn.1000-0526.2015.04.013 [8] Lu E, Liu S, Luo Y, et al.The atmospheric anomalies associated with the drought over the Yangtze River basin during spring 2011.J Geophys Res, 2014, 119(10):5881-5894. https://www.researchgate.net/publication/262026436_The_atmospheric_anomalies_associated_with_the_drought_over_the_Yangtze_River_basin_during_spring_2011 [9] Lu E, Zeng Y, Luo Y, et al.Changes of summer precipitation in China:The dominance of frequency and intensity and linkage with changes in moisture and air temperature.J Geophys Res, 2014, 119(22):12. https://www.researchgate.net/publication/267761988_Changes_of_summer_precipitation_in_China_The_dominance_of_frequency_and_intensity_and_linkage_with_changes_in_moisture_and_air_temperature [10] Lu E, Zhao W, Gong L, et al.Determining starting time and duration of extreme precipitation events based on intensity.Clim Res, 2015, 63(1):31-41. doi: 10.3354/cr01280 [11] Ma Z, Fu C.Interannual characteristics of the surface hydrological variables over the arid and semi-arid areas of northern China.Global & Planetary Change, 2003, 37(3):189-200. http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.692.982 [12] 《第二次气候变化国家评估报告》编写委员会.第二次气候变化国家评估报告.北京:科学出版社, 2011. [13] Li D L, Xu D F, Wang H, et al.Characterization and causal analysis of temporal and spatial variation in dry-wet conditions in autumn in Southwest China.J Trop Meteorol, 2015, 21(1):55-66. http://www.cqvip.com/QK/85390X/201501/664472093.html [14] 李维京, 左金清, 宋艳玲, 等.气候变暖背景下我国南方旱涝灾害时空格局变化.气象, 2015, 41(3):261-271. doi: 10.7519/j.issn.1000-0526.2015.03.001 [15] Huang R H, Chen J L, Wang L, et al.Characteristics, processes, and causes of the spatio-temporal variabilities of the East Asian monsoon system.Adv Atmos Sci, 2012, 29:910-942. doi: 10.1007/s00376-012-2015-x [16] Wang B, Li T, Ding Y, et al.Eastern Asian-Western North Pacific Monsoon:A Distinctive Component of the Asian-Australian Monsoon System//The Global Monsoon System:Research and Forecast.WMO/TD No.1266(TMRP Report No.70), 2005:72-94. [17] Zhang R H, Wu B Y, Han J P, et al.Effects on Summer Monsoon and Rainfall Change over China due to Eurasian Snow Cover and Ocean Thermal Conditions//Climate Change-Realities, Impacts Over Ice Cap, Sea Level and Risks.Rijeka:InTech, 2013:227-250. [18] Zhang R H.Natural and human-induced changes in summer climate over the East Asian monsoon region in the last half century:A review.Adv Clim Change Res, 2015, 6:131-140. doi: 10.1016/j.accre.2015.09.009 [19] Zhang R H.Changes in East Asian summer monsoon and summer rainfall over eastern China during recent decades.Sci Bull, 2015, 60:1222-1224. doi: 10.1007/s11434-015-0824-x [20] 魏凤英, 谢宇.近百年长江中下游梅雨的年际及年代际振荡.应用气象学报, 2005, 16(4):492-499. doi: 10.11898/1001-7313.20050410 [21] 吴志伟, 何金海, 韩桂荣, 等.长江中下游梅雨与春季南半球年际模态 (SAM) 的关系分析.热带气象学报, 2006, 22(1):79-85. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200601011.htm [22] 张庆云, 郭恒.夏季长江淮河流域异常降水事件环流差异及机理研究.大气科学, 2014, 38(4):656-669. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK201404005.htm [23] 覃志年, 胡娅敏, 陈丽娟.广西夏季降水的多时间尺度特征及影响因子.应用气象学报, 2013, 24(5):565-575. doi: 10.11898/1001-7313.20130506 [24] Wang Y, Chen X, Yan F.Spatial and temporal variations of annual precipitation during 1960-2010 in China.Quatern Int, 2015, 380:5-13. http://adsabs.harvard.edu/abs/2015QuInt.380....5W [25] 张玉洁, 刘寿东, 任宏利, 等.我国南方夏季低频雨型特征及其年代际变化研究.气象学报, 2014, 72(6):1205-1217. doi: 10.11676/qxxb2014.075 [26] 金炜昕, 李维京, 孙丞虎, 等.夏季中国中东部不同历时降水时空分布特征.气候与环境研究, 2015, 20(4):465-476. http://cdmd.cnki.com.cn/Article/CDMD-10300-1015578914.htm [27] Xu H L, Feng J, Sun C.Impact of preceding summer North Atlantic Oscillation on early autumn precipitation over central China.Atmos Oceanic Sci Lett, 2013, 6(6):417-422. doi: 10.1080/16742834.2013.11447118 [28] Zuo J, Ren H L, Li W.Contrasting impacts of the Arctic Oscillation on surface air temperature anomalies in southern China between early and middle-to-late winter.J Climate, 2015, 28(10):4015-4026. doi: 10.1175/JCLI-D-14-00687.1 [29] 郑菲, 李建平, 刘婷.南半球环状模气候影响的若干研究进展.Acta Meteor Sinica, 2014, 72(5):926-939. doi: 10.11676/qxxb2014.074 [30] Wu Z W, Dou J, Lin H.Potential influence of the November-December Southern Hemisphere annular mode on the East Asian winter precipitation:A new mechanism.Climate Dyn, 2015, 44(5-6):1215-1226. doi: 10.1007/s00382-014-2241-2 [31] Zheng F, Li J, Wang L, et al.Cross-seasonal influence of the December-February Southern Hemisphere annular mode on March-May meridional circulation and precipitation.J Climate, 2015, 28(17):6859-6881. doi: 10.1175/JCLI-D-14-00515.1 [32] Wang B, Zhang Q.Pacific-East teleconnection.PartⅡ:How the Philippine Sea anomalous anticyclone is estabilished during El Niño development.J Climate, 2002, 15(22):3252-3265. doi: 10.1175/1520-0442(2002)015<3252:PEATPI>2.0.CO;2 [33] 李超, 张庆云.春季长江中下游旱涝的环流特征及对前期海温异常的响应.气象学报, 2013, 71(3):452-461. doi: 10.11676/qxxb2013.033 [34] 司东, 袁媛, 崔童, 等.2013年海洋和大气环流异常及对中国气候的影响.气象, 2014, 40(4):494-501. doi: 10.7519/j.issn.1000-0526.2014.04.012 [35] Si D, Hu Z Z, Kumar A, et al.Is the interdecadal variation of the summer rainfall over eastern China associated with SST?Climate Dyn, 2015(1-12):135-146. https://www.researchgate.net/publication/291329132_Is_the_interdecadal_variation_of_the_summer_rainfall_over_eastern_China_associated_with_SST [36] 郭维栋, 马柱国, 王会军.土壤湿度——一个跨季度降水预测中的重要因子及其应用探讨.气候与环境研究, 2007, 12(1):20-28. http://www.cnki.com.cn/Article/CJFDTOTAL-QHYH200701002.htm [37] 马柱国, 魏和林, 符淙斌.中国东部区域土壤湿度的变化及其与气候变率的关系.气象学报, 2000, 58(3):278-287. doi: 10.11676/qxxb2000.029 [38] 孙丞虎, 李维京, 张祖强, 等.淮河流域土壤湿度异常的时空分布特征及其与气候异常关系的初步研究.应用气象学报, 2005, 16(2):129-138. doi: 10.11898/1001-7313.20050217 [39] 左志燕, 张人禾.中国东部夏季降水与春季土壤湿度的联系.科学通报, 2007, 52(14):1722-1724. doi: 10.3321/j.issn:0023-074x.2007.14.021 [40] Meng L, Long D, Quiring S M, et al.Statistical analysis of the relationship between spring soil moisture and summer precipitation in East China.Int J Climatol, 2014, 34:1511-1523. doi: 10.1002/joc.2014.34.issue-5 [41] Zhang R H, Zuo Z Y.Impact of spring soil moisture on surface energy balance and summer monsoon circulation over East Asia and precipitation in East China.J Climate, 2011, 24:3309-3322. doi: 10.1175/2011JCLI4084.1 [42] Zuo Z Y, Zhang R H.Influence of soil moisture in eastern China on the East Asian summer monsoon.Adv Atmos Sci, 2016, 33:151-163. doi: 10.1007/s00376-015-5024-8 [43] Wu B Y, Zhang R H, Wang B, et al.On the association between spring Arctic sea ice concentration and Chinese summer rainfall.Geophy Res Lett, 2009, Vol.35, L09501, doi: 10.1029/2009GL037299. [44] Wu B Y, Yang K, Zhang R H.Eurasian snow cover variability and its association with summer rainfall in China.Adv Atmos Sci, 2009, 26:31-44. doi: 10.1007/s00376-009-0031-2 [45] Wu G X, Duan A M, Liu Y M, et al.Tibetan Plateau climate dynamics:Recent research progress and outlook.Nature Geosciences, 2015, 2:100-116, doi: 10.1093/nsr/nwu045. [46] Wu G X, Liu Y M.Revisiting Asian monsoon formation and change associated with Tibetan Plateau forcing:Ⅰ.Formation.Clim Dyn, 2012, 39:1169-1181. doi: 10.1007/s00382-012-1334-z [47] Si D, Ding Y.Decadal change in the correlation pattern between the Tibetan Plateau winter snow and the East Asian summer precipitation during 1979-2011.J Climate, 2013, 26(19):7622-7634. doi: 10.1175/JCLI-D-12-00587.1 [48] 陈丽娟, 袁媛, 杨明珠, 等.海温异常对东亚夏季风影响机理的研究进展.应用气象学报, 2013, 24(5):521-532. doi: 10.11898/1001-7313.20130502 [49] 李维京, 郑志海, 孙丞虎.近年来我国短期气候预测中动力相似预测方法研究与应用进展.大气科学, 2013, 37(2):341-350. doi: 10.3878/j.issn.1006-9895.2012.12311 [50] 刘景鹏, 陈丽娟, 李维京, 等.月尺度气温可预报性对资料长度的依赖及可信度.应用气象学报, 2015, 26(2):151-159. doi: 10.11898/1001-7313.20150203 [51] 王绍武, 叶瑾琳, 龚道溢, 等.中国东部夏季降水型的研究.应用气象学报, 1998, 9(增刊Ⅰ):65-73. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200904017.htm [52] 竺夏英, 何金海, 吴志伟.江淮梅雨期降水经向非均匀分布及异常年特征分析.科学通报, 2007, 52(8):951-957. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200708016.htm [53] 陈旭.气候变暖背景下江淮梅雨由典型向非典型演变的统计特征及其成因分析.南京:南京信息工程大学, 2015. [54] 黄嘉佑.准两年周期振荡在我国月降水量中的表现.大气科学, 1988, 12(2):267-273. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK198803005.htm [55] 王志伟, 翟盘茂, 唐红玉, 等.中国南方近半个世纪的雨涝变化特征.自然灾害学报, 2005, 14(3):56-60. http://www.cnki.com.cn/Article/CJFDTOTAL-ZRZH200503010.htm [56] 吴志伟, 李建平, 何金海, 等.大尺度大气环流异常与长江中下游夏季长周期旱涝急转.科学通报, 2006, 51(14):1717-1724. doi: 10.3321/j.issn:0023-074X.2006.14.016 [57] 詹丰兴, 刘芸芸, 何金海.江南春季降水的准2 a振荡及其与热带海温异常的关系.地理科学, 2013, 33(8):1006-1013. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKX201308017.htm [58] 章开美, 李丽平, 项连东, 等.华南前汛期极端降水气候变化特征及其与太平洋海温相关关系研究.气象与减灾研究, 2015, 38(1):1-7. http://www.cnki.com.cn/Article/CJFDTOTAL-HXQO201501001.htm [59] Ding Y, Wang Z, Sun Y.Inter-decadal variation of the summer precipitation in East China and its association with decreasing Asian summer monsoon.Part Ⅰ:Observed evidences.Int J Climatol, 2008, 28(9):1139-1161. doi: 10.1002/joc.v28:9 [60] Zhou T, Gong D, Li J, et al.Detecting and understanding the multi-decadal variability of the East Asian Summer Monsoon-Recent progress and state of affairs.Meteor Z, 2009, 18(4):455-467. doi: 10.1127/0941-2948/2009/0396 [61] Wu R, Wen Z, Yang S, et al.An interdecadal change in southern China summer rainfall around 1992/93.J Climate, 2010, 23(9):2389-2403. doi: 10.1175/2009JCLI3336.1 [62] Xu Z, Fan K, Wang H.Decadal variation of summer precipitation over China and associated atmospheric circulation after the late 1990s.J Climate, 2015, 28(10):4086-4106. doi: 10.1175/JCLI-D-14-00464.1 [63] Zhang M, He J, Wang B, et al.Extreme drought changes in Southwest China from 1960 to 2009.J Geogr Sci, 2013, 23(1):3-16. doi: 10.1007/s11442-013-0989-7 [64] Zou X, Zhai P, Zhang Q.Variations in droughts over China:1951-2003.Geophys Res Lett, 2005, 32(4):L04707. http://adsabs.harvard.edu/abs/2005GeoRL..32.4707Z [65] 赵振国.厄尔尼诺现象对北半球大气环流和中国降水的影响.大气科学, 1996, 20(4):422-428. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK604.005.htm [66] 陶诗言, 张庆云.亚洲冬夏季风对ENSO事件的响应.大气科学, 1998, 22(4):399-407. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK804.001.htm [67] 金祖辉, 陶诗言.ENSO循环与中国东部地区夏季和冬季降水关系的研究.大气科学, 1999, 23(6):663-672. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK199906003.htm [68] 陈文.E1 Niño和La Niña事件对东亚冬, 夏季风循环的影响.大气科学, 2002, 26(5):595-606. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200205001.htm [69] Chang C, 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 Climate, 2000, 13(24):4310-4325. doi: 10.1175/1520-0442(2000)013<4310:IAIVOT>2.0.CO;2 [70] Wang B, Wu R, Fu X.Pacific-East Asian teleconnection:How does ENSO affect East Asian climate?J Climate, 2000, 13(9):1517-1536. doi: 10.1175/1520-0442(2000)013<1517:PEATHD>2.0.CO;2 [71] Chou C, Tu J Y, Yu J Y.Interannual variability of the western North Pacific summer monsoon:Differences between ENSO and non-ENSO years.J Climate, 2003, 16(13):2275-2287. doi: 10.1175/2761.1 [72] Lau N C, Nath M J.ENSO modulation of the interannual and intraseasonal variability of the East Asian monsoon-A model study.J Climate, 2006, 19(18):4508-4530. doi: 10.1175/JCLI3878.1 [73] Zhang R H, Sumi A, Kimoto M.Impact of El Niño on the East Asia Monsoon:A diagnostic study of the '86/87 and '91/92 events.J Meteor Soc Japan, 1996, 74:49-62. https://www.researchgate.net/publication/258514352_Impact_of_El_Nino_on_the_East_Asian_Monsoon_A_diagnostic_study_of_the_%278687_and_%279192_events [74] Zhang R H, Sumi A, Kimoto M.A diagnostic study of the impact of El Niño on the precipitation in China.Adv Atmos Sci, 1999, 16:229-241. doi: 10.1007/BF02973084 [75] Li S, Lu J, Huang G, et al.Tropical Indian Ocean basin warming and East Asian summer monsoon:A multiple AGCM study.J Climate, 2008, 21(22):6080-6088. doi: 10.1175/2008JCLI2433.1 [76] Xie S P, Hu K, Hafner J, et al.Indian Ocean capacitor effect on Indo-western Pacific climate during the summer following El Niño.J Climate, 2009, 22(3):730-747. doi: 10.1175/2008JCLI2544.1 [77] Yang J, Liu Q, Liu Z.Linking observations of the Asian monsoon to the Indian Ocean SST: Possible roles of Indian Ocean basin mode and dipole mode.J Climate, 2010, 23(21):5889-5902. doi: 10.1175/2010JCLI2962.1 [78] 吴国雄, 刘平, 刘屹岷, 等.印度洋海温异常对西太平洋副热带高压的影响——大气中的两级热力适应.气象学报, 2000, 58(5):513-522. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200005000.htm [79] Wei W, Zhang R, Wen M, et al.Interannual variation of the South Asian high and its relation with Indian and East Asian summer monsoon rainfall.J Climate, 2015, 28(7):2623-2634. doi: 10.1175/JCLI-D-14-00454.1 [80] Wu Z, Wang B, Li J, et al.An empirical seasonal prediction model of the East Asian summer monsoon using ENSO and NAO.J Geophys Res, 2009, 114(D18):85-86. [81] Zuo J, Li W, Sun C, et al.Impact of the North Atlantic sea surface temperature tripole on the East Asian summer monsoon.Adv Atmos Sci, 2013, 30(4):1173-1186. doi: 10.1007/s00376-012-2125-5 [82] Wu R, Kirtman B P.Observed relationship of spring and summer East Asian rainfall with winter and spring Eurasian snow.J Climate, 2007, 20(7):1285-1304. doi: 10.1175/JCLI4068.1 [83] 陈兴芳, 宋文玲.冬季高原积雪和欧亚积雪对我国夏季旱涝不同影响关系的环流特征分析.大气科学, 2000, 24(5):585-592. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200005001.htm [84] 陈烈庭, 阎志新. 青藏高原冬春季积雪对大气环流和我国南方汛期降水的影响//中长期水温气象预报文集 (第一集). 北京: 水电出版社, 1979: 194-195. [85] 郭其蕴, 王继琴.青藏高原的积雪及其对东亚季风的影响.高原气象, 1986, 5(2):116-123. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX198602001.htm [86] 吴统文, 钱正安.青藏高原冬春积雪异常与中国东部地区夏季降水关系的进一步分析.气象学报, 2000, 58(5):570-581. doi: 10.11676/qxxb2000.059 [87] Chen L T, Wu R G.Interannual and decadal variations of snow cover over Qinghai-Xizang Plateau and their relationships to summer monsoon rainfall in China.Adv Atmos Sci, 2000, 17(1):18-30. doi: 10.1007/s00376-000-0040-7 [88] Wu T W, Qian Z A.The relation between the Tibetan winter snow and the Asian summer monsoon and rainfall: An observational investigation.J Climate, 2003, 16(12):2038-2051. doi: 10.1175/1520-0442(2003)016<2038:TRBTTW>2.0.CO;2 [89] 张顺利, 陶诗言.青藏高原积雪对亚洲夏季风影响的诊断及数值研究.大气科学, 2001, 25(3):372-390. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200103008.htm [90] 陈乾金, 高波等.青藏高原冬季雪盖异常与冬夏季风变异及其相互联系的物理诊断研究.大气科学, 2000, 24(4):477-492. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200004004.htm [91] 朱玉祥, 丁一汇, 刘海文.青藏高原冬季积雪影响我国夏季降水的模拟研究.大气科学, 2009, 33(5):903-915. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200905004.htm [92] 李永华, 卢楚翰, 徐海明, 等.夏季青藏高原大气热源与西南地区东部旱涝的关系.大气科学, 2011, 35(3):422-434. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK201103004.htm [93] Ren H C, Li W, Ren H L, et al.Distinct linkage between winter Tibetan Plateau snow depth and early summer Philippine Sea anomalous anticyclone.Atmos Sci Lett, 2016, doi: 10.1002/asl.646. [94] 翟盘茂, 周琴芳.北半球雪盖变化与我国夏季降水.应用气象学报, 1997, 8(2):231-235. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19970231&flag=1 [95] 李震坤, 武炳义, 朱伟军.春季欧亚积雪异常影响中国夏季降水的数值试验.气候变化研究进展, 2009, 5(4):196-201. http://www.cnki.com.cn/Article/CJFDTOTAL-QHBH200904005.htm [96] 穆松宁, 周广庆.欧亚北部冬季增雪"影响"我国夏季气候异常的机理研究——陆面季节演变异常的"纽带"作用.大气科学, 2012, 36(2):297-315. doi: 10.3878/j.issn.1006-9895.2011.11015 [97] 张人禾, 武炳义, 赵平, 等.中国东部夏季气候20世纪80年代后期的年代际转型及其可能成因.气象学报, 2008, 66(5):697-706. doi: 10.11676/qxxb2008.064 [98] Gao H, Wang Y G, He J H.Weakening significance of ENSO as a predictor of summer precipitation in China.Geophys Res Lett, 2006, 33(9):L09807. https://www.researchgate.net/publication/260274815_Weakening_significance_of_ENSO_as_a_predictor_of_precipitation_in_China [99] Ashok K, Behera S K, Rao S A, et al.El Niño Modoki and its possible teleconnection.J Geophys Res, 2007, 112:C11007. doi: 10.1029/2006JC003798 [100] Feng J, Li J.Influence of El Niño Modoki on spring rainfall over south China.J Geophys Res, 2011, 116(D1302), doi: 10.1029/2010JD015160. [101] Feng J, Wang L, Chen W, et al.Different impacts of two types of Pacific Ocean warming on Southeast Asian rainfall during boreal winter.J Geophys Res, 2010, 115:D24122. https://www.researchgate.net/publication/251428343_Different_impacts_of_two_types_of_Pacific_Ocean_warming_on_Southeast_Asian_rainfall_during_boreal_winter [102] 袁媛, 李崇银, 杨崧.与厄尔尼诺和拉尼娜相联系的中国南方冬季降水的年代际异常特征.气象学报, 2014, 72(2):237-255. doi: 10.11676/qxxb2014.014 [103] Huang G, Hu K, Xie S P.Strengthening of tropical Indian Ocean teleconnection to the Northwest Pacific since the mid-1970s:An atmospheric GCM study.J Climate, 2010, 23(19):5294-5304. doi: 10.1175/2010JCLI3577.1 [104] Xie S P, Du Y, Huang G, et al.Decadal shift in El Niño influences on Indo-Western Pacific and East Asian climate in the 1970s.J Climate, 2010, 23(12):3352-3368. doi: 10.1175/2010JCLI3429.1 [105] Qu X, Huang G.Impacts of tropical Indian Ocean SST on the meridional displacement of East Asian jet in boreal summer.Int J Climatol, 2012, 32(13):2073-2080. doi: 10.1002/joc.v32.13 [106] Hu K, Huang G, Zheng X T, et al.Interdecadal variations in ENSO influences on Northwest Pacific-East Asian early summertime climate simulated in CMIP5 Models.J Climate, 2014, 27(15):5982-5998. doi: 10.1175/JCLI-D-13-00268.1 [107] Hong C C, Chang T C, Hsu H H.Enhanced relationship between the tropical Atlantic SST and the summertime western North Pacific subtropical high after the early 1980s.J Geophys Res, 2014, 119(7):3715-3722. https://www.researchgate.net/publication/261330989_Enhanced_Relationship_between_the_Tropical_Atlantic_SST_and_the_Summertime_Western_North_Pacific_Subtropical_High_after_the_early_1980s [108] Wu Z, Li J, Jiang Z, et al.Possible effects of the North Atlantic Oscillation on the strengthening relationship between the East Asian summer monsoon and ENSO.Int J Climatol, 2012, 32(5):794-800. doi: 10.1002/joc.v32.5 [109] 左金清, 李维京, 任宏利, 等.春季北大西洋涛动与东亚夏季风年际关系的转变及其可能成因分析.地球物理学报, 2012, 55(2):384-395. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201202002.htm [110] Kripalani R, Kulkarni A.Climatology and variability of historical Soviet snow depth data: Some new perspectives in snow-Indian monsoon teleconnections.Climate Dyn, 1999, 15(6):475-489. doi: 10.1007/s003820050294 [111] Dash S, Singh G, Shekhar M, et al.Response of the Indian summer monsoon circulation and rainfall to seasonal snow depth anomaly over Eurasia.Climate Dyn, 2005, 24(1):1-10. doi: 10.1007/s00382-004-0448-3 [112] Liu X, Yanai M.Influence of Eurasian spring snow cover on Asian summer rainfall.Int J Climatol, 2002, 22(9):1075-1089. doi: 10.1002/(ISSN)1097-0088 [113] Gu W, Li C, Wang X, et al.Linkage between Mei-yu precipitation and North Atlantic SST on the decadal timescale.Adv Atmos Sci, 2009, 26:101-108. doi: 10.1007/s00376-009-0101-5 [114] Sun J, Wang H.Changes of the connection between the summer North Atlantic Oscillation and the East Asian summer rainfall.J Geophys Res, 2012, 117(D8):393-407. https://www.researchgate.net/profile/Jianqi_Sun/publication/258663056_Changes_of_the_connection_between_the_summer_North_Atlantic_Oscillation_and_the_East_Asian_summer_rainfall/links/5466e42f0cf2397f7829e717.pdf [115] Li J P, Wang J X.A new North Atlantic Oscillation index and its variability.Adv Atmos Sci, 2003, 20(5):661-676. doi: 10.1007/BF02915394 [116] Nan S, Li J.The relationship between the summer precipitation in the Yangtze River valley and the boreal spring Southern Hemisphere annular mode.Geophys Res Lett, 2003, 30(24):2266. https://www.researchgate.net/publication/260696540_The_relationship_between_the_summer_precipitation_in_the_Yangtze_River_valley_and_the_boreal_spring_Southern_Hemisphere_annular_mode [117] 南素兰, 李建平.春季南半球环状模与长江流域夏季降水的关系:Ⅱ印度洋和南海海温的"海洋桥"作用.气象学报, 2005, 63(6):847-856. doi: 10.11676/qxxb2005.081 [118] 郑菲, 李建平.前冬南半球环状模对春季华南降水的影响及其机理.地球物理学报, 2012, 55(11):3542-3557. doi: 10.6038/j.issn.0001-5733.2012.11.004 [119] 李建平, 任荣彩, 齐义泉, 等.亚洲区域海-陆-气相互作用对全球和亚洲气候变化的作用研究进展.大气科学, 2013, 37(2):518-538. doi: 10.3878/j.issn.1006-9895.2012.12322 [120] 李维京, 李怡, 陈丽娟, 等.我国冬季气温与影响因子关系的年代际变化.应用气象学报, 2013, 24(4):385-396. doi: 10.11898/1001-7313.20130401 -
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