[1]Bengtsson L, Hagemann S, Hodges K I, 2004. Can climate trends be calculated from reanalysis data?[J]. Journal of Geophysical Research Atmospheres, 109 (D11):839-856.
[2]Burrows M T, Schoeman D S, Buckley L B, et al, 2011. The pace of shifting climate in marine and terrestrial ecosystems[J]. Science, 334(6056):652-655.
[3]Christy J R, Spencer Roy W, McNider, et al, 1995. Reducing Noise in the MSU Daily Lower-Tropospheric Global Temperature Dataset[J]. Journal of Climate, 8(4):888-896.
[4]Fu Q, Johanson C M, 2005. Satellite-derived vertical dependence of tropical tropospheric temperature trends[J]. geophysical research letters, 32:L10703.
[5]Ji F, Wu Z, Huang J, et al, 2014. Evolution of land surface air temperature trend[J]. Nature Climate Change, 4(6):462-466.
[6]Liu X D, Chen B D, 2000. Climatic warming in the Tibetan Plateau during recent decades[J]. International Journal of Climatology, 20(14):1729-1742.
[7]Liu X D, Zhang M F, 1998. Contemporary climatic change over the Qinghai-Xizang (Tibet) Plateau and its response to the greenhouse effect[J]. Chinese Geographical Science, 8(4):289-298.
[8]Kanamitsu M, Ebisuzaki W, Woollen J, et al, 2002. NCEP-DOE AMIP-Ⅱ Reanalysis (R-2), BAMS, 1631-1643.
[9]Pepin N C, Seidel D J, 2005. A global comparison of surface and free-air temperatures at high elevations[J]. Journal of Geophysical Research Atmospheres, 110:D03104.
[10]Randel W J, Smith A K, Wu F, et al, 2016. Stratospheric temperature trends over 1979-2015 derived from combined SSU, MLS, and SABER satellite observations[J]. Climate, 29:4843-4859.
[11]Simmons A, Uppala S, Dee D, et al, 2007. ERA-Interim:New ECMWF Reanalysis Products from 1989 Onwards[J]. ECMWF Newsletter, 110:29-35.
[12]Wu Z, Huang N E, 2008. Ensemble Empirical Mode Decomposition:a noise assisted data analysis method[J]. Advances in Adaptive Data Analysis, 1(1):1-41.
[13]Yanai M, Li C F, Song Z S, et al, 1992. Seasonal heating of the Tibetan Plateau and its effects of the evolution of the Asian summer monsoon[J]. Journal of the Meteorological Society of Japan, 70:319-351.
[14]Ye D Z, Wu G X, 1998. The role of the heat source of the Tibetan Plateau in the general circulation[J]. Meteorology and Atmospheric Physics, 67(1/4):181-198.
[15]You Q, Kang S, Pepin N, et al, 2010. Relationship between temperature trend magnitude, elevation and mean temperature in the Tibetan Plateau from homogenized surface stations and reanalysis data[J]. Global and Planetary Change, 71(1/2):124-133.
[16]Zhang Q, Kang S, Yan Y, 2006. Characteristics of spatial and temporal variations of monthly mean surface air temperature over Qinghai-Tibet Plateau[J]. Chinese Geographical Science, 16 (4):351-358.
[17]Zou C Z, Wang W, 2011. Intersatellite calibration of AMSU-A observations for weather and climate applications[J]. Journal of Geophysical Research Atmospheres, 116(D23):2053-2056.
[18]Zou C Z, Qian H F, 2016. Stratospheric temperature climate data record from merged SSU and AMSU-A Observations[J]. Journal of Geophysical Research, 33(9):1967-1984. doi:10.1175/jtech-d-16-0018.1.
[19]Zou C Z, Qian H, Wang W, et al, 2014. Recalibration and merging of SSU observations for stratospheric temperature trend studies[J]. Journal of Geophysical Research, 119(23):13180-13205.
[20]Zou C Z, Li J, 2015. NOAA MSU/AMSU-A mean layer temperature, climate algorithm theoretical basis document (C-ATBD), NOAA/NESDIS.
[21]边多, 杜军, 2006.近40年西藏"一江两河"流域气候变化特征[J].应用气象学报, 17(2):169-175.
[22]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(5):464-470.
[23]程译萱, 范广洲, 张永莉, 等, 2018.青藏高原及周边地区垂直温度梯度特征及其成因分析[J].高原气象, 37(2):333-348. DOI:10.7522/j.issn.1000-0534.2017.00057.
[24]段思汝, 范广洲, 华维, 等, 2015.1979-2013年青藏高原上空温度变化特征[J].成都信息工程学院学报, 30(6):587-591.
[25]高世仰, 张杰, 罗琦, 2017.青藏高原非均匀下垫面热力输送系数的估算[J].高原气象, 36(3):596-609. DOI:10.7522/j.issn.1000-0534.2016.00060.
[26]郭艳君, 丁一汇, 2008.近50年来我国探空温度序列均一化及变化趋势[J].应用气象, 19(6):646-656.
[27]黄荣辉, 1985.夏季青藏高原上空热源异常对北半球大气环流异常的作用[J].气象学报, 43(2):208-220.
[28]江灏, 王可丽, 2000.青藏高原地表热状况的卫星资料分析[J].高原气象, 19(3):323-328.
[29]李刚, 张鹭, 2016.基于微波探测资料的全球大气亮温长期变化趋势研究[J].气象科学, 36(1):10-19.
[30]李生辰, 徐亮, 郭英香, 等, 2006.近34a青藏高原年气温变化[J].中国沙漠, 26(1):27-34.
[31]林振耀, 赵昕奕, 1996.青藏高原降水气温变化的空间特征[J].中国科学(D辑), 26(4):354-358.
[32]刘桂芳, 卢鹤立, 2010.1961-2005年来青藏高原主要气候因子的基本特征[J].地理研究, 29(12):2281-2288.
[33]牛涛, 陈隆勋, 王文, 2002.青藏高原冬季平均温度、湿度气候特征的REOF分析[J].应用气象学报, 13(5):671-681.
[34]马耀明, 胡泽勇, 田立德, 等, 2014.青藏高原气候系统变化及其对东亚区域的影响与机制研究进展[J].地球科学进展, 29(2):207-215.
[35]田红瑛, 田文寿, 雒佳丽, 等, 2014.青藏高原地区上对流层-下平流层区域水汽分布和变化特征[J].高原气象, 33(1):1-13. DOI:10.7522/j.issn.1000-0534.2013.00074.
[36]王前, 赵勇, 陈飞, 等, 2017.南亚高压的多模态特征及其与新疆夏季降水的联系[J].高原气象, 36(5):1209-1220. DOI:10.7522/j.issn.1000-0534.2016.00123.
[37]王荣英, 周顺武, 闫巨盛, 等, 2011.近30年青藏高原上空大气温度变化特征[J].高原山地气象研究, 31(1):1-5.
[38]王腾, 2014.青藏高原上空温度年代际变异特征分析[R].广州: 第31届中国气象学会年会S7中高层大气及其与对流层的耦合, 422-423.
[39]王颖, 任国玉, 2005.中国高空温度变化初步分析[J].气候与环境研究. 10(4):780-790.
[40]韦志刚, 黄荣辉, 董文杰, 2003.青藏高原气温和降水的年际和年代际变化[J].大气科学, 27(2):157-170.
[41]魏凤英, 2007.现代气候统计诊断与预测技术[M].北京:气象出版社, 36-55.
[42]吴国雄, 林海, 邹晓蕾, 等, 2014.全球气候变化研究与科学数据[J].地球科学进展, 29(1):15-22.
[43]徐影, 丁一汇, 赵宗慈, 2001.美国NCEP/NCAR近50年全球再分析资料在我国气候变化研究中可信度的初步分析[J].应用气象学报, 12(3):338-347.
[44]叶笃正, 高由禧, 1979.青藏高原气象学[M].北京:科学出版社, 1-278.
[45]于晓晶, 杜娟, 王敏仲, 等, 2018.青藏高原新增探空资料同化对南疆夏季降水预报的影响[J].高原气象, 37(1):13-27. DOI:10.7522/j.issn.1000-0534.2017.00034.
[46]周顺武, 张人禾, 2009.青藏高原地区上空NCEP/NCA R再分析温度和位势高度资料与观测资料的比较分析[J].气候与环境研究, 14(2):284-292.
[47]赵天保, 符淙斌, 柯宗建, 等, 2010.全球大气再分析资料的研究现状与进展[J].地球科学进展, 25(3):241-254.
[48]朱文琴, 陈隆勋, 周自江, 2001.现代青藏高原气候变化的几个特征[J].中国科学(地球科学), 31(增刊):327-334.
[49]邹成治, 高梅, 2008.交叉定标产生的NOAA卫星长期大气温度观测资料[J].应用气象学报, 19(5):582-587.
[50]邹晓蕾, 2012.极轨气象卫星微波温度探测仪资料的分辨率[J].气象科技进展, 2:38-41.