地球科学 |
|
|
|
|
青藏高原地气温差与印度洋海气温差的相互影响 |
申紫薇, 田荣湘, 张超 |
浙江大学 地球科学学院, 气象信息与灾害研究所, 浙江 杭州 310027 |
|
A study on the interaction between ground-air temperature differences over the Qinghai-Tibet Plateau and sea surface-air temperature differences over the Indian Ocean |
SHEN Ziwei, TIAN Rongxiang, ZHANG Chao |
Institute of Meteorological Information and Disaster, School of Earth Sciences, Zhejiang University, Hangzhou 310027, China |
[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. ZHOU X J, ZHAO P,CHEN J M, et al. Impacts of thermodynamic process over the Tibetan plateau on the northern hemispheric climate[J].Science in China (Ser D:Earth Sci), 2009,39(11):1473-1486.
|
[2] |
李国平. 青藏高原动力气象学[M]. 北京:气象出版社, 2002. LI G P.Dynamic Meteorology of the Qinghai Tibetan Plateau[M]. Beijing:China Meteorological Press,2002.
|
[3] |
白虎志, 董文杰, 马振锋. 青藏高原及邻近地区的气候特征[J]. 高原气象, 2004, 23(6):890-897. BAI H Z, DONG W J, MA Z F.Climatic characteristics of Qinghai-Xizang Plateau and its surrounding[J].Plateau Meteorology,2004,23(6):890-897.
|
[4] |
DUAN A, LI F, WANG M, et al. Persistent weakening trend in the spring sensible heat source over the Tibetan Plateau and its impact on the Asian summer monsoon[J].Journal of Climate, 2011, 24(21):5671-5682.
|
[5] |
周宁芳, 秦宁生, 屠其璞,等. 近50 a青藏高原地面气温变化的区域特征分析[J]. 高原气象, 2005, 24(3):344-349. ZHOU N F, QIN N S,TU Q P, et al. Analyse on region characteristics of temperature changes over Qinghai-Xizang Plateau in recent 50 years[J].Plateau Meteorology,2005,24(3):344-349.
|
[6] |
赵平, 陈隆勋. 35 a来青藏高原大气热源气候特征及其与中国降水的关系[J]. 中国科学(D辑:地球科学),2001, 31(4):327-332. ZHAO P, CHEN L X. The climatic characteristics of the atmospheric heat source in the Qinghai-Tibetan Plateau for the past 35 years and its relationship with precipitation in China[J].Science in China(Ser D:Earth Sci),2001,31(4):327-332.
|
[7] |
DUAN A, LI F, WANG M, et al. Persistent weakening trend in the spring sensible heat source over the Tibetan Plateau and its impact on the Asian summer monsoon[J].Journal of Climate, 2011, 24(21):5671-5682.
|
[8] |
YANAI M, LI C. Mechanism of heating and the boundary layer over the Tibetan Plateau[J].Monthly Weather Review, 1994, 122(2):305-323.
|
[9] |
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. ZHANG W G, LI S X, WU T H, et al. Changes of the differences between ground and air temperature over the Qinghai-Xizang Plateau[J].Acta Geographica Sinica,2006,61(9):899-910.
|
[10] |
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. WANG C H, CUI Y. 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].Climatic and Environmental Research,2011,16(5):586-596.
|
[11] |
刘颖, 徐祥德, 施晓晖. 春季地气温差分布及其与长江中下游旱涝的关系[C]//中国气象学会2008年会. 济南:中国气象学会, 2008. LIU Y, XU X D, SHI X H. Distribution of ground and air temperature difference in spring and its relationship with drought and flood in the middle and lower reaches of the Yangtze River[C]//2008 Meeting of Chinese Meteorological Society. Jinan:Chinese Meteorological Society,2008.
|
[12] |
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. CHEN Z M, MIN W B. Relation between surface heating fields over Tibetan Plateau of season and late-summer drought in Sichuan province[J]. Journal of Chengdu Institute of Meteorology, 1999,14(1):1-7.
|
[13] |
LATIF M, DOMMENGET D, DIMA M, et al. The role of Indian Ocean sea surface temperature in forcing East African rainfall anomalies during December-January 1997/1998[J]. Journal of Climate, 1999, 12(12):3497-3504.
|
[14] |
ANNAMALAI H, XIE S P, MCCREARY J P, et al. Impact of Indian Ocean sea surface temperature on developing El Niño[J].Journal of Climate, 2004, 18(2):302-319.
|
[15] |
肖子牛, 晏红明, 李崇银. 印度洋地区异常海温的偶极振荡与中国降水及温度的关系[J]. 热带气象学报, 2002, 18(4):335-344. XIAO Z N,YAN H M, LI C Y. The relationship between Indian Ocean SSTA dipole index and the precipitation and temperature over China[J].Journal of Tropical Meteorology, 2002,18(4):335-344.
|
[16] |
徐志清, 范可. 冬季和春季印度洋海温异常年际变率模态对中国东部夏季降水的可能影响过程[J]. 大气科学, 2012, 36(5):879-888. XU Z Q,FAN K. Possible process for influences of winter and spring Indian Ocean SST anomalies interannual variability mode on summer rainfall over eastern China[J].Chinese Journal of Atmospheric Sciences,2012,36(5):879-888.
|
[17] |
蒋贤玲, 巩远发, 马柱国,等. 青藏高原-热带印度洋地区大气热源的时空变化特征[J]. 成都信息工程学院学报, 2011,26(6):601-607. JIANG X L, GONG Y F, MA Z G,et al. Characteristics of temporal and spatial variation of atmospheric heat sources over the Tibetan Plateau-Tropical Indian Ocean[J].Journal of Chengdu University of Information Technology,2011,26(6):601-607.
|
[18] |
BOTHE O, FRAEDRICH K, ZHU X H. The large-scale circulations and summer drought and wetness on the Tibetan Plateau[J]. International Journal of Climatology, 2010, 30(6):844-855.
|
[19] |
张平, 陈碧辉, 毛晓亮. 青藏高原东侧降水与印度洋海温的遥相关特征[J]. 高原山地气象研究, 2008, 28(2):15-21. ZHANG P, CHEN B H, MAO X L. The teleconnection characteristics between the precipitation on the east side of Tibetan Plateau and Indian Ocean SST[J].Plateau and Mountain Meteorology Research,2008,28(2):15-21.
|
[20] |
张平, 高丽, 毛晓亮. 青藏高原气温与印度洋海温遥相关的初步研究[J]. 高原气象, 2006, 25(5):800-806. ZHANG P, GAO L, MAO X L. Primary analyses of teleconnection relationship between the Qinghai-Xizang Plateau air temperature and the Indian Ocean SST[J].Plateau Meteorology,2006,25(5):800-806.
|
[21] |
金蕊, 祁莉, 何金海. 春季青藏高原感热通量对不同海区海温强迫的响应及其对我国东部降水的影响[J]. 海洋学报, 2016, 38(5):83-95. JIN R, QI L,HE J H. Effect of oceans to spring surface sensible heat flux over Tibetan Plateau and its influence to East China precipitation[J]. Acta Oceanologica Sinica,2016,38(5):83-95.
|
[22] |
HU J, DUAN A. Relative contributions of the Tibetan Plateau thermal forcing and the Indian Ocean Sea surface temperature basin mode to the interannual variability of the East Asian summer monsoon[J].Climate Dynamics, 2015, 45(9):1-15.
|
[23] |
竺夏英, 刘屹岷, 吴国雄. 夏季青藏高原多种地表感热通量资料的评估[J]. 中国科学(D辑:地球科学), 2012, 42(7):1104-1112. ZHU X Y,LIU Y M,WU G X. An assessment of summer sensible heat flux on the Tibetan Plateau from eight data sets[J]. Science in China(Ser D:Earth Sci),2012,42(7):1104-1112.
|
[24] |
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. LI D L,CHEN L P.The relationship of surface heating fields over the Qinghai-Xizang Plateau to the east Asian circulation and the early summer drought in Northwest of China[J]. Quarterly Journal of Applied Meteorology,1990,1(4):383-391.
|
[25] |
徐祥德, 赵天良, 施晓晖,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. XU X D, ZHAO T L, SHI X H, et al.A study of the role of the Tibetan Plateau's thermal forcing in modulating rainband and moisture transport in Eastern China[J]. Acta Meteorologica Sinica,2015,73(1):20-35.
|
[26] |
MIHALAKAKOU G, LEWIS J O, SANTAMOURIS M. The influence of different ground covers on the heating potential of earth-to-air heat exchangers[J].Renewable Energy, 1996, 7(1):33-46.
|
[27] |
ZHANG T. Influence of the seasonal snow cover on the ground thermal regime:An overview[J].Reviews of Geophysics, 2005, 43(4):589-590.
|
[28] |
李超. 冬、夏季青藏高原地面加热场激发的500 hPa遥相关型[J]. 高原气象, 1994,13(2):122-127. LI C. 500 hPa teleconnection pattern excited by the surface heating field in the Qinghai-Xizang Plateau in winter and summer[J]. Plateau Meteorology,1994,13(2):122-127.
|
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
|
Shared |
|
|
|
|
|
Discussed |
|
|
|
|