[1]Chen B D, Chao W C, Liu X.2003.Enhanced climatic warming in the Tibetan Plateau due to doubling CO<sub>2</sub>:a model study[J].Climate Dyn, 20(4):401-413.
[2]Chen S B, Liu Y F.Axel Thomas.2006.Climatic change on the Tibetan Plateau:potential evapotranspiration trends from 1961-2000[J].Climatic Change, 76(3-4):291-319.
[3]Chen T, Rossow W B, Zhang Y C.2000.Radiative effects of cloud-type variations[J].J Climate, 13(1):264-268.
[4]Duan A M, Wu G X.2005.Role of the Tibetan Plateau thermal forcing in the summer climate patterns over subtropical Asia[J].Climate Dyn, 24(7-8):793-807.
[5]Duan A M, Wu G X.2006.Change of cloud amount and the climate warming on the Tibetan Plateau[J].Geophys Res Lett, 33(22):217-234.
[6]Easterling D R, Horton B, Jones P D, et al.1997.Maximum and minimum temperature trends for the globe[J].Science, 277(5324):364-367.
[7]Hansen J, Ruedy R, Sato M, et al.2010.Global surface temperature change[J].Rev Geophys, 48(4):7362-7388.
[8]IPCC.2013.Climate Change 2013:The Physical Science Basis[R].Working Group I Contribution to the 15<sup>th</sup> Assessment Report of the Intergovernmental Panel on Climate Change.
[9]Jones P D, Raper S C B, Bradley R S, et al.1986.Northern Hemisphere surface air temperature variations:1851-1984[J].J Climate Appl Meteor, 25(2):161-179.
[10]Kaiser D P.1998.Analysis of total cloud amount over China, 1951-1994[J].Geophys Res Lett, 25(19):3599-3602.
[11]Kaiser D P.2000.Decreasing cloudiness over China:An updated analysis examining additional variables[J].Geophys Res Lett, 27(15):2193-2196.
[12]Karl T R, Kukla G, Razuvayev V N, et al.1991.Global warming:Evidence for asymmetric diurnal temperature change[J].Geophys Res Lett, 18(12):2253-2256.
[13]Kaufman Y J, Koren I.2006.Smoke and pollution aerosol effect on cloud cover[J].Science, 313(5787):655-658.
[14]Li Y Q, Liu X D, Chen B D.2006.Cloud type climatology over the Tibetan Plateau:A comparison of ISCCP and MODIS/TERRA measurements with surface observations[J].Geophys Res Lett, 33(17):130-142.
[15]Lin B, Wielicki B A, Chambers L H, et al.2002.The iris hypothesis:A negative or positive cloud feedback?[J].J Climate, 15(1):2713-2715.
[16]Lindzen R S, Chou M D, Hou A Y.2001.Does the earth have an adaptive infrared iris?[J].Bull Amer Meteor Soc, 82(3):417-432.
[17]Liu J Y, Tian H Q, Liu M L, et al.2005.China's changing landscape during the 1990s:Large-scale land transformations estimated with satellite data[J].Geophys Res Lett, 32(2):L02405.DOI:10.1029/2004GL021649.
[18]Liu X D, Chen B D.2000.Climatic warming in the Tibetan Plateau during recent decades[J].Int J climatol, 20(14):1729-1742.
[19]Manabe S, Broccoli A J.1990.Mountains and arid climates of middle latitudes[J].Science, 247(4939):192-195.
[20]Ramanathan V, Cess R D, Harrison E F, et al.1989.Cloud-radiative forcing and climate:Results from the Earth Radiation Budget Experiment[J].Science, 243(4887):57-63.
[21]Rangwala I, Miller J R, Russell G L, et al.2010.Using a global climate model to evaluate the influences of water vapor, snow cover and atmospheric aerosol on warming in the Tibetan Plateau during the twenty-first century[J].Climate Dyn, 34(6):859-872.
[22]Rossow W B, Schiffer R A.1999.Advances in understanding clouds from ISCCP[J].Bull Amer Meteor Soc, 80(11):2261-2287.
[23]Stephens G L.2005.Cloud feedbacks in the climate system:A critical review[J].J Climate, 18(2):237-273.
[24]Svensmark H, Friis-Christensen E.1997.Variation of cosmic ray flux and global cloud coverage-a missing link in solar-climate relationships[J].Journal of Atmospheric and Solar-Terrestrial Physics, 59(11):1225-1232.
[25]Wang C H, Guo Y P.2012.Precipitable water conversion rates over the Qinghai-Xizang (Tibet) Plateau:changing characteristics with global warming[J].Hydrological Processes, 26(10):1509-1516.
[26]Wang C H, Yu L, Huang B.2012.The impact of warm pool SST and general circulation on increased temperature over the Tibetan Plateau[J].Adv Atmos Sci, 29(2):274-284.DOI:10.1007/s00376-011-1034-3.
[27]Wang C H, Zhang Z F, Tian W S.2011.Factors affecting the surface radiation trends over China between 1960 and 2000[J].Atmos Environ, 45(14):2379-2385.
[28]Wu G X.1984.The nonlinear response of the atmosphere to large-scale mechanical and thermal forcing[J].Atmos Sci, 41(16):2456-2476.
[29]Yanai M, Li C F, Song Z S.1992.Seasonal heating of the Tibetan Plateau and its effects on the evolution of the Asian summer monsoon[J].J Meteor Soc Japan, 70(1B):319-351.
[30]You Q L, Kang S C, Aguilar E, et al.2008.Changes in daily climate extremes in the eastern and central Tibetan Plateau during 1961-2005[J].J Geophys Res, 113(D7):1639-1647.
[31]Yu R C, Wang B, Zhou T J.2004.Climate effects of the deep continental stratus clouds generated by the Tibetan Plateau[J].J Climate, 17(13):2702-2713.
[32]Zhang Y, Klein S A, Boyle J, et al.2010.Evaluation of tropical cloud and precipitation statistics of Community Atmosphere Model version 3 using CloudSat and CALIPSO data[J].J Geophys Res, 115(D12):1256-1268.
[33]丁守国, 石广玉, 赵春生.2004.利用ISCCP D2资料分析近20年全球不同云类云量的变化及其对气候可能的影响[J].科学通报, 49(11):1105-1111.Ding Shouguo, Shi Guangyu, Zhao Chunsheng.2004.Analyzing global trends of different cloud types and the their potential impacts on climate by using the ISCCP D2 dataset[J].Chinese Science Bulletin, 49(12):1301-1306.
[34]丁守国, 赵春生, 石广玉, 等.2005.近20年全球总云量变化趋势分析[J].应用气象学报, 16(5):670-677.Ding Shouguo, Zhao Chunsheng, Shi Guangyu, et al.2005.Analysis of global total cloud amount variation over the past 20 years[J].J Appl Meteor Sci, 16(5):670-678.
[35]杜川利, 余兴, 李星敏, 等.2012.过去60年中国秦岭地区云量变化及原因分析[J].高原气象, 31(5):446-455.Du Chuanli, Yu Xing, Li Xingmin, et al.2012.Analysis on cloudiness change in Qinling Mountain Region and its possible reason in past 60 years[J].Plateau Meteor, 31(5):446-455.
[36]段玮, 段旭, 徐开, 等.2015.从水汽角度对青藏高原东南侧高空探测布局的分析[J].高原气象, 34(2):307-317, Duan Wei, Duan Xu, Yang Jiakang, et al.2015.Research about radiosonde stations composition in southeast side of Qinghai-Xizang Plateau based on its water vapor[J].Plateau Meteor, 34(2):307-317.DOI:10.7522/j.issn.1000-0534.2014.00024.
[37]刘洪利, 朱文琴, 宜树华, 等.2003.中国地区云的气候特征分析[J].气象学报, 61(4):466-473.Liu Hongli, Zhu Wenqin, Yi Shuhua, et al.2003.Climatic analysis of the cloud over China[J].Acta Meteor Sinica, 61(4):466-473.
[38]刘健.2013.利用卫星数据分析青藏高原云微物理特性[J].高原气象, 32(1):38-45.Liu Jian.2013.Analysis on cloud microphysical property over Qinghai-Xizang Plateau using satellite data[J].Plateau Meteor, 32(1):38-45.DOI:10.7522/j.issn.1000-0534.2013.00005.
[39]孙玉婷, 高庆九, 闵锦忠.2013.再分析温度资料与西藏地区冬, 夏季观测气温的比较[J].高原气象, 32(4):909-920.Sun Yuting, Gao Qingjiu, Min Jinzhong.2013.Comparison of reanalysis data and observation about summer/winter surface air temperature in Tibet[J].Plateau Meteor, 32(4):909-920.DOI:10.7522/j.issn.1000-0534.2012.00087.
[40]田磊, 孙艳桥, 胡文东, 等.2013.银川地区大气水汽, 云液态水含量特性的初步分析[J].高原气象, 32(6):1774-1779.Tian Lei, Sun Yanqiao, Hu Wendong, et al.2013.Preliminary analysis of the characteristics of atmosphere water vapor and cloud liquid water in Yinchuan area[J].Plateau Meteor, 32(6):1774-1779.DOI:10.7522/j.issn.1000-0534.2012.00164.
[41]王澄海, 崔洋.2011.东亚夏季风建立前青藏高原地气温差变化特征[J].气候与环境研究, 16(5):586-596.Wang Chenghai, Cui Yang.2011.Characteristics of the difference of temperature between surface and atmosphere over the Tibetan Plateau in the early stage of east Asian summer monsoon onset[J].Climate Environ Res, 16(5):586-596.
[42]王澄海, 董文杰, 韦志刚.2001.青藏高原季节性冻土年际变化的异常特征[J].地理学报, 56(5):523-531.Wang Chenghai, Dong Wenjie, Wei Zhigang.2001.The feature of seasonal frozen soil in Qinghai-Tibet Plateau[J].Acta Geogeraphica Sinica, 56(5):523-531.
[43]王澄海, 李健, 许晓光.2012.中国近50年气温变化准3年周期的普遍性及气温未来的可能变化趋势[J].高原气象, 31(1): 126-136.Wang Chenghai, Li Jian, Xu Xiaoguang.2012.Universality of quasi-3-year period of temperature in last 50 years and change in next 20 years in China[J].Plateau Meteor, 31(1):126-136.
[44]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.Wei Zhigang, Huang Ronghui, Dong Wenjie.2003.Interannual and interdecadal variations of air temperature and precipitation over the Tibetan Plateau[J].Chinese J Atmos Sci, 27(2):157-170.
[45]魏丽, 钟强.1997.青藏高原云的气候学特征[J].高原气象, 16(1):10-15.Wei Li, Zhong Qiang.1997.Characteristics of cloud clmatology over Qinghai-Xizang Plateau[J].Plateau Meteor, 16(1):10-15.
[46]杨溯, 石广玉, 王标, 等.2013.全球"变暗"和"变亮"时期中国地面温度变化研究[J].高原气象, 32(4):993-999.Yang Shuo, Shi Guangyu, Wang Biao, et al.2013.Characteristics of surface temperature in China during global‘dimming’and‘brightening’periods[J].Plateau Meteor, 32(4):993-999.DOI:10.7522/j.issn.1000-0534.2012.00095.
[47]叶笃正, 高由禧.1979.青藏高原气象学[M].北京:科学出版社, 122-146.Ye Duzheng, Gao Youxi.1979.Meteorology of the Tibetan Plateau[M].Beijing:Science Press, 122-146.
[48]翟盘茂, 任福民.1997.中国近四十年最高最低温度变化[J].气象学报, 55(4):418-429.Zhai Panmao, Ren Fumin.1997.On changes of China smaxmum and minmum temperatures in the recent 40 years[J].Acta Meteor Sinica, 55(4):418-429.
[49]张飞民, 王澄海.2014.利用WRF-3DVAR同化常规观测资料对近地层风速预报的改进试验[J].高原气象, 33(3):675-685.Zhang Feimin, Wang Chenghai.2014.Experiment of surface-layer wind forecast improvement by assimilating conventional data with WRF-3DVAR[J].Plateau Meteor, 33(3):675-685.DOI:10.7522/j.issn.1000-0534.2012.00198.
[50]朱玉祥, 丁一汇, 刘海文.2009.青藏高原冬季积雪影响我国夏季降水的模拟研究[J].大气科学, 33(5):903-915.Zhu Yuxiang, Ding Yihui, Liu Haiwen.2009.Simulation of the influence of winter snow depth over the Tibetan Plateau on summer rainfall in China[J].Chinese J Atmos Sci, 33(5):903-915.
