[1]Chen X, Tung K K, 2014.Varying planetary heat sink led to global-warming slowdown and acceleration[J].Science, 345(6199): 897-903.DOI: 10.1126/science.1254937.
[2]Dai A, Fyfe J C, Xie S P, al et, 2015.Decadal modulation of global surface temperature by internal climate variability[J].Nature Climate Change, 5(6): 555-559.DOI: 10.1038/nclimate2605.
[3]Davini P, Cagnazzo C, Gualdi S, al et, 2012.Bidimensional diagnostics, variability and trends of Northern Hemisphere blocking[J].Journal of Climate, 25(19): 6496-6509.DOI: 10.1175/JCLI-D-12-00032.1.
[4]Dole R, Hoerling M, Perlwitz J, al et, 2011.Was there a basis for anticipating the 2010 Russian heat wave?[J].Geophysical Research Letters, 38(6): L06702.DOI: 10.1029/2010GL046582.
[5]England M H, McGregor S, Spence P, al et, 2014.Recent intensification of wind-driven circulation in the Pacific and the ongoing warming hiatus[J].Nature Climate Change, 4(3): 222-227.DOI: 10.1038/nclimate2106.
[6]Foster G, Rahmstorf S, 2011.Global temperature evolution 1979 -2010[J].Environmental Research Letters, 6(4): 526-533.DOI: 10.1088/1748-9326/6/4/044022.
[7]Guan X, Huang J, Guo R, al et, 2015.The role of dynamically induced variability in the recent warming trend slowdown over the Northern Hemisphere[J].Scientific Reports, 5(1): 12669.DOI: 10.1038/ srep12669.
[8]Higuchi K, Huang J, Shabbar A, 1999.A wavelet characterization of the North Atlantic oscillation variation and its relationship to the North Atlantic sea surface temperature[J].International Journal of Climatology, 19(10): 1119-112.DOI: 10.1002/(SICI)1097-0088(199908)19: 103.0.CO; 2-7.
[9]Huang J, Higuchi K, Shabbar A, 1998.The relationship between the North Atlantic Oscillation and El Ni?o-Southern Oscillation[J].Geophysical Research Letters, 25(14): 2707-2710.DOI: 10. 1029/98GL01936.
[10]Huang J, Xie Y, Guan X, al et, 2016.The dynamics of the warming hiatus over the Northern Hemisphere[J].Climate Dynamics, 48(1/2): 1-18.DOI: 10.1007/s00382-016-3085-8.
[11]Hu X, Sejas S A, Cai M, al et, 2018.Decadal evolution of the surface energy budget during the fast warming and global warming hiatus periods in the ERA-interim[J].Climate Dynamics, 50: 1-12.DOI: 10.1007/s00382-018-4232-1.
[12]IPCC, 2013.Climate Change 2013: The physical science basis: Summary for policymakers[R].Working Group I Contribution to the IPCC 15th Assessment Report.Cambridge University Press.
[13]Jevrejeva S, Moore J C, Grinsted A, 2010.How will sea level respond to changes in natural and anthropogenic forcings by 2100?[J].Geophysical Research Letters, 37: L07703.DOI: 10.1029/2010GL042947.
[14]Ji F, Wu Z, Huang J, al et, 2014.Evolution of land surface air temperature trend[J].Nature Climate Change, 4(6): 462-466.DOI: 10.1038/nclimate2223.
[15]Katsman C A, Oldenborgh G J V, 2011.Tracing the upper ocean’s “missing heat”[J].Geophysical Research Letters, 38(14): L14610.DOI: 10.1029/2011GL048417.
[16]Kaufmann R K, Kauppi H, Mann M L, al et, 2011.Reconciling anthropogenic climate change with observed temperature 1998 -2008[J].Proceedings of the National Academy of Sciences, 108(29): 11790-11793.DOI: 10.1073/pnas.1102467108.
[17]Knight J, Kenneby J J, Folland C, al et, 2009.Do global temperature trends over the last decade falsify climate predictions? In state of the climate in 2008[J].Bulletin of the American Meteorological Society, 90(8): 22-23.
[18]Kosaka Y, Xie S P, 2013.Recent global-warming hiatus tied to equatorial Pacific surface cooling[J].Nature, 501(7467): 403-407.DOI: 10.1038/nature12534.
[19]Lejenas H, Okland H, 1983.Characteristics of northern hemisphere blocking as determined from long time series of observational data[J].Tellus A: Dynamic Meteorology and Oceanography, 35(5): 350-362.DOI: 10.3402/tellusa.v35i5.11446.
[20]Meehl G A, Teng H, 2014.CMIP5 multi-model hindcasts for the mid-1970s shift and early 2000s hiatus and predictions for 2016-2035[J].Geophysical Research Letters, 41(5): 1711-1716.DOI: 10.1002/2014GL059256.
[21]Ogi M, Yamazaki K, Tachibana Y, 2005.The summer northern annular mode and abnormal summer weather in 2003[J].Geophysical Research Letters, 32: 1-4.DOI: 10.1029/2004GL021528.
[22]Rex D F, 1950.Blocking action in the middle troposphere and its effect upon regional climate[J].Tellus, 2(3): 196-211.DOI: 10.3402/tellusa.v2i4.8603.
[23]Solomon S, Rosenlof K H, Portmann R W, al et, 2010.Contributions of stratospheric water vapor to decadal changes in the rate of global warming[J].Science, 327(5970): 1219-1223.DOI: 10.1126/science.1182488.
[24]Stott P A, Stone D A, Allen M R, 2004.Human contribution to the European heatwave of 2003[J].Nature, 432: 610-614.DOI: 10.1038/nature03089.
[25]Tibaldi S, Molteni F, 1990.On the operational predictability of blocking[J].Tellus A: Dynamic Meteorology and Oceanography, 42(3): 343-365.DOI: 10.3402/tellusa.v42i3.11882.
[26]Treidl R A, Birch E C, Sajecki P, 1981.Blocking action in the northern hemisphere: A climatological study[J].Atmosphere-Ocean, 19(1): 1-23.DOI: 10.1080/07055900.1981.9649096.
[27]Trenberth K E, Fasullo J T, Branstator G, al et, 2014.Seasonal aspects of the recent pause in surface warming[J].Nature Climate Change, 4(10): 911-916.DOI: 10.1038/nclimate2341.
[28]Wallace J M, Fu Q, Smoliak B V, al et, 2012.Simulated versus observed patterns of warming over the extratropical Northern Hemisphere continents during the cold season[J].Proceedings of the National Academy of Sciences, 109(36): 14337-14342.DOI: 10.1073/pnas.1204875109.
[29]Wu Z, Huang N E, 2009.Ensemble empirical mode decomposition: A noise-assisted data analysis method[J].Advances in Adaptive Data Analysis, 1(1): 1-41.DOI: 10.1142/S1793536909000047.
[30]Zhao L, Ding R, Moore J C, 2016.The high mountain Asia glacier contribution to sea-level rise from 2000 to 2050[J].Annals of Glaciology, 57(71): 223-231.DOI: 10.3189/2016AoG71A049.
[31]曹杨, 陈洪滨, 李军, 等, 2017.利用再分析与探空资料对0 ℃层高度和地面气温变化特征及其相关性的分析[J].高原气象, 36(6): 1608-1618.DOI: 10.7522/j.issn.1000-0534.2017.00011.
[32]陈少勇, 王劲松, 郭俊庭, 等, 2012.中国西北地区1961 -2009年极端高温事件的演变特征[J].自然资源学报, 27(5): 832-844.DOI: 10.3760/j.issn: 1001-7097.2006.01.007.
[33]仇永炎, 1985.中期天气预报[M].北京: 科学出版社.
[34]季明霞, 黄建平, 王绍武, 等, 2008.冬季中高纬地区阻塞高压活动及其气候影响[J].高原气象, 27(2): 415-421.
[35]金荣花, 李艳, 王式功, 2009.四种客观定量表征阻塞高压方法的对比分析[J].高原气象, 28(5): 1121-1128.
[36]刘菊菊, 游庆龙, 周毓荃, 等, 2018.基于ERA-Interim的中国云水量时空分布和变化趋势[J].高原气象, 37(6): 1590-1604.DOI: 10.7522/j.issn.1000-0534.2018.00059.
[37]李黎, 吕世华, 范广洲, 2019.夏季青藏高原地表能量变化对高原低涡生成的影响分析[J].高原气象, 38(6).DOI: 10.7522/j.issn.1000-0534.2018.00074.
[38]李红梅, 李林, 2015.2 ℃全球变暖背景下青藏高原平均气候和极端气候事件变化[J].气候变化研究进展, 11(3): 157-164.DOI: 10.3969/j.issn.1673-1719.2015.03.00.
[39]李宗省, 何元庆, 辛惠娟, 等, 2010.我国横断山区1960 -2008年气温和降水时空变化特征[J].地理学报, 65(5): 563-579.DOI: 10.11821/xb201005006.
[40]吕晶, 李忠贤, 李跃清, 等, 2018.峨眉山及其周边地区降水气候特征研究[J].高原气象, 37(6): 1544-1562.DOI: 10.7522/j.issn.1000-0534.2018.00049.
[41]秦大河, 2014.气候变化科学与人类可持续发展[J].地理科学进展, 33(7): 874-883.DOI: 10.11820/dlkxjz.2014.07.002.
[42]魏萌, 乔方利, 2016.CMIP5气候模式模拟的1850 -2014年全球温度变化的集合经验模态分解[J].中国科学: 地球科学, 46(12): 1675-1688.DOI: 10.1007/s11430-015-5465-y.
[43]杨朝虹, 张镭, 苑广辉, 等, 2018.东亚和北美地区温度和降水变化特征[J].高原气象, 37(3): 662-674.DOI: 10.7522/j.issn. 1000-0534.2017.00083.
[44]张渊萌, 程志刚, 2014.青藏高原增暖海拔依赖性研究进展[J].高原山地气象研究, 34(2): 91-96.DOI: 10.3969/j.issn.1674-2184.2014.02.018.