PDF下载 分享
[1]胡 洁,巩远发.1984-2013年青藏高原地气温差的时空变化特征[J].成都信息工程大学学报,2020,35(04):455-463.[doi:10.16836/j.cnki.jcuit.2020.04.015]
 HU Jie,GONG Yuanfa.The Characteristics of Spatiotemporal Changes of the Tibetan Plateau Ground-air Temperature Difference from 1984 to 2013[J].Journal of Chengdu University of Information Technology,2020,35(04):455-463.[doi:10.16836/j.cnki.jcuit.2020.04.015]
点击复制

1984-2013年青藏高原地气温差的时空变化特征

参考文献/References:

[1] 周秀骥,赵平,陈军明,等.青藏高原热力作用对北半球气候影响的研究[J].中国科学(D辑:地球科学),2009,39(11):1473-1486.
[2] Yeh T C.The circulation of the high troposphere over China in the winter of 1945-1946[J].Tellus,1950,2(3):173-183.
[3] Flohn H.Contributions to a Meteorology of the Tibetan Highlands[M].Collins:Atmos.Sci, 1968:130.
[4] Yanai M,Li C,Song Z.Seasonal heating of the Tibetan Plateau and its effects of the evolution of the Asian summer monsoon[J].J.Meteor.Soc.Japan,1992,70:319-351.
[5] Ye D Z,Wu G X.The role of the heat source of the Tibetan Plateau in the general circulation[J].Meteor.Atmos.Phys,1998,67:181-198.
[6] 胡江林,朱乾根.青藏高原感热加热对7月份大气环流和亚洲夏季风影响的数值试验[J].热带气象学报,1993,9(1):78-84.
[7] 朱乾根,管兆勇.青藏高原感热加热异常与夏季低频环流的数值研究[J].南京气象学院学报,1997,20(2):186-192.
[8] 吴国雄,刘屹岷,刘新,等.青藏高原加热如何影响亚洲夏季的气候格局[J].大气科学,2005,29(1):47-58.
[9] 江灏,王可丽.青藏高原地表热状况的卫星资料分析[J].高原气象,2000(3):468.
[10] Yang K,Guo X F,Wu B Y.Recent trends in surface sensible heat flux on the Tibetan Plateau[J].Sci China Earth Sci,2010,54(1):19-28.
[11] Zhu X Y,Liu Y M,Wu G X.An assessment of summer sensible heat flux on the Tibetan Plateau from eight datasets[J].Sci China Earth Sci,2012,55(5):779-786.
[12] Zhou L T,Huang R H.Regional differences in surface sensible and latent heat fluxes in China[J].Theor Appl Climatol,2014,116(3/4):625-637.
[13] Ma Y M,Han C B,Zhong L,et al.Using MODIS and AVHRR datato determine regional surface heating field and heat flux distributions over the heterogeneous landscape of the Tibetan Plateau[J].Theor Appl Climatol,2014,117(3/4):643-652.
[14] Shi Q,Liang S.Surface-sensible and latent heat fluxes over the Tibetan Plateau from ground measurements,reanalysis,and satellite data[J].Atmos Chem Phys,2014,14(11):5659-5677.
[15] Chen X,Su Z,Ma Y,et al.Development of a 10-year(2001-2010)0.1_data set of land-surface energy balance for mainland China[J].Atmos Chem Phys,2014,14:13097-13117.
[16] 解晋,余晔,刘川,等.青藏高原地表感热通量变化特征及其对气候变化的响应[J].高原气象,2018,37(1):28-42.
[17] Duan A M,Wu G X.Weakening trend in the atmospheric heat source over the Tibetan Plateau during recent decades.Part I:Observations[J].J Climate,2008,21(13):3149-3164.
[18] Wang M R,Zhou S W,Duan A M. Trend in the atmospheric heat source over the central and eastern Tibetan Plateau during recent decades:Comparison of observations and reanalysis data[J].Chin Sci Bull,2012,57(5):548-557.
[19] 叶笃正,高由禧.青藏高原气象学[M].北京:科学出版社,1979:122-126.
[20] 季国良,姚兰昌,袁福茂,等.1982年冬季青藏高原地面和大气的加热场特征[J].中国科学(B辑),1986,2:214-224.
[21] 张文纲,李述训,吴通华,等.青藏高原地气温差变化分析[J].地理学报,2006,61(9):899-910.
[22] 陈忠明,闵文彬.青藏高原地面加热场与四川主汛期降水及伏旱的关系[J].成都气象学院学报,1999,14(1):1-7.
[23] 王澄海,崔洋.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,2011,16(5):586-596.
[24] 申紫薇,田荣湘,张超.青藏高原地气温差与印度洋海气温差的相互影响[J].浙江大学学报,2018,45(5):576-588.
[25] 宋敏红,吴统文,钱正安.高原地区NCEP热通量再分析资料的检验及在夏季降水预测中的应用[J].高原气象,2000,19(4):467-475.
[26] 柏晶榆,徐祥德,周玉淑,等.春季青藏高原感热异常对长江中下游夏季降水影响的初步研究[J].应用气象学报,2003,14(3):363-368.
[27] 宁亮,钱永甫.北非和青藏高原感热振荡特征及与我国东部夏季降水的关系[J].高原气象,2006,25(3):357-365.
[28] 岑思弦,巩远发,赖欣.青藏高原及其周围地区大气热源对川渝盆地夏季降水的影响[J].高原气象,2014,33(5):1182-1189.
[29] 施晓辉,温敏.中国持续性暴雨特征及青藏高原热源的影响[J].高原气象,2015,34(3):611-620.
[30] 周俊前,刘新,李伟平,等.青藏高原春季地表感热异常对西北地区东部降水变化的影响[J].高原气象,2016,35(4):845-853.
[31] 姚慧茹,李栋梁.1971-2012年青藏高原春季风速的年际变化及对气候变暖的响应[J].气象学报,2016,74(1):60-75.
[32] 李栋梁,陈丽萍.青藏高原地面加热场强度与东亚环流及西北初夏旱的关系[J].应用气象学报,1990(4):383-391.
[33] 徐祥德,赵天良,施晓辉,等.青藏高原热力强迫对中国东部降水和水汽输送的调制作用[J].气象学报,2015,73(1):20-35.

相似文献/References:

[1]梁 宁,刘海文,潘丽丽.近40年来西北低涡的统计[J].成都信息工程大学学报,2018,(06):675.[doi:10.16836/j.cnki.jcuit.2018.06.013]
 LIANG Ning,LIU Hai-wen.Statistics of Northwest Vortex in Recent 40 Years[J].Journal of Chengdu University of Information Technology,2018,(04):675.[doi:10.16836/j.cnki.jcuit.2018.06.013]
[2]田 姗,范广洲.,胡德强,等.春季青藏高原南侧低层垂直环流圈的年际变化特征分析[J].成都信息工程大学学报,2016,(02):190.
 TIAN Shan,FAN Guang-zhou-,HU De-qiang,et al.Characteristic of the Vertical Circulation over the Low-level of the South of Tibetan Plateau during Spring[J].Journal of Chengdu University of Information Technology,2016,(04):190.
[3]熊光明,胡德强,陈权亮,等.川渝中部地区夏季强降水年代际变化研究[J].成都信息工程大学学报,2016,(增刊1):37.
[4]周芳存,巩远发,阿米娜.麦图迪尔.中国西北地区土壤湿度的气候特征[J].成都信息工程大学学报,2016,(增刊1):43.
[5]石鹏翔,刘海文,段伯隆,等.影响重庆夏季暴雨的中尺度低涡的气候学特征[J].成都信息工程大学学报,2016,(03):323.
 SHI Peng-xiang,LIU Hai-wen,DUAN Bo-long,et al.The Summery Heavy Rainfall Climatic Characteristics Associated with the Mesocale Low Vortex over Chongqing[J].Journal of Chengdu University of Information Technology,2016,(04):323.
[6]李依瞳,赵琳娜,巩远发,等.春季南支槽与中国降水的关系及成因[J].成都信息工程大学学报,2017,(03):282.[doi:10.16836/j.cnki.jcuit.2017.03.009 ]
 LI Yi-tong,ZHAO Lin-na,GONG Yuan-fa,et al.The Relationship and Formation of Springtime Southern Branch Trough and Precipitation in China[J].Journal of Chengdu University of Information Technology,2017,(04):282.[doi:10.16836/j.cnki.jcuit.2017.03.009 ]
[7]曹永兴,蔡宏珂,薛志航.2010年秋季热带低压引发海南省特大暴雨特征分析[J].成都信息工程大学学报,2017,(04):445.[doi:10.16836/j.cnki.jcuit.2017.04.016]
 CAO Yong-xing,CAI Hong-ke,XUE Zhi-hang.Characteristics Analysis on Super Rainstorm Caused by Tropical Depression in Hainan Province during the Autumn of 2010[J].Journal of Chengdu University of Information Technology,2017,(04):445.[doi:10.16836/j.cnki.jcuit.2017.04.016]
[8]马有绚,时兴合,向亚飞,等.2016年青海省汛期气候预测评估及先兆信号分析[J].成都信息工程大学学报,2017,(05):559.[doi:10.16836/j.cnki.jcuit.2017.05.016]
 MA You-xuan,SHI Xing-he,XIANG Ya-fei,et al.Climate Prediction Assessment and Precursor Signal Analysis in 2016 Flood Season of Qinghai[J].Journal of Chengdu University of Information Technology,2017,(04):559.[doi:10.16836/j.cnki.jcuit.2017.05.016]
[9]宋美洋,顾建峰,刘海文,等.重庆夏季低涡无暴雨的气候学分析[J].成都信息工程大学学报,2016,(04):413.
 SONG Mei-Yang,GU Jian-feng,LIU Hai-wen,et al.The Summery without Heavy Rainfall Climatic Characteristics Associated with the Mesocale Low Vortex over Chongqing[J].Journal of Chengdu University of Information Technology,2016,(04):413.
[10]李琳琳,南素兰,赵 平,等.与南亚高压相联的欧亚大陆-印度洋经向环流[J].成都信息工程大学学报,2021,36(02):185.[doi:10.16836/j.cnki.jcuit.2021.02.010]
 LI Linlin,NAN Sulan,ZHAO Ping,et al.The Meridional Circulation Associated with South Asian High over Eurasia and Indian Ocean[J].Journal of Chengdu University of Information Technology,2021,36(04):185.[doi:10.16836/j.cnki.jcuit.2021.02.010]

备注/Memo

收稿日期:2019-12-05

更新日期/Last Update: 2020-08-30