参考文献/References:
[1] VOOGT J A, OKE T R. Thermal remote sensing of urban climates [J]. Remote Sensing of Environment, 2003, 86(3):370-384.
[2] 欧阳斌,车涛,戴礼云,等.基于MODIS LST产品估算青藏高原地区的日平均地表温度[J].冰川冻土,2012,34(2):296-303. [OUYANG Bin, CHE Tao, DAI Liyun, et al. Estimating mean daily surface temperature over the Tibetan Plateau based on MODIS LST products [J]. Journal of Glaciology and Geocryology, 2001, 34(2):296-303]
[3] 高懋芳,覃志豪,徐斌.用MODIS数据反演地表温度的基本参数估计方法[J].干旱区研究,2007,24(1): 113-119.[GAO Maofang, QIN Zhihao, XU Bin. Estimation of the basic parameters for deriving surface temperature from MODIS data [J]. Arid Zone Research, 2007, 24(1): 113-119]
[4] 冯松,汤懋苍,王冬梅.青藏高原是我国气候变化启动区的新证据[J].科学通报,1998,43(6):633-636. [FENG Song, TANG Maocang, WANG Dongmei. New evidence for the Qinghai-Xizang(Tibet)Plateau as a pilot region of climatic fluctuation in China [J].Chinese Science Bulletin, 1998, 43(6):633-636]
[5] 叶笃正,罗四维,朱抱真.西藏高原及其附近的流场结构和对流层大气的热量平衡[J].气象学报,1957,28(2):108-121.[YEH Tucheng, LO Szuwei, CHU Paochen. The wind structure and heat balance in the lower troposphere over Tibetan plateau and its surrounding [J]. Acta Meteorologica Sinica, 1957, 28(2):108-121]
[6] 吴国雄,张永生.青藏高原的热力和机械强迫作用以及亚洲季风的爆发*I.爆发地点[J].大气科学,1998,22(6):825-838.[WU Guoxiong, ZHANG Yongsheng. Thermal and mechanical forcing of the Tibetan plateau and the Asian monsoon onset Part I situating of the onset [J]. Scientia Atmosphererica Sinica, 1998, 22(6):825-838]
[7] 黄培培,南卓铜.基于Wavelet-ANFIS和MODIS地表温度产品的青藏高原0cm土壤温度估算方法[J].冰川冻土,2013,35(1):74-83.[HUANG Peipei, NAN Zhuotong. Estimation of 0-cm soil temperature over the Tibetan Plateau based on the wavelet analysis and adaptive net-work-fuzzy inference system [J]. Journal of Glaciology and Geocryology, 2013, 35(1):74-83]
[8] 薛纪善.气象卫星资料同化的科学问题与前景[J].气象学报,2009,67(6):903-911.[XUE Jishan. Scientific issues and perspective of assimilation of meteorological satellite data [J]. Acta Meteorologica Sinica, 2009, 67(6): 903-911]
[9] BENGTSSON L, SHUKLA J. Integration of space and in situ observations to study global climate change [J]. Bulletin of the American Meteorological Society, 1998, 69(10):1130-1143.
[10] KISTLER R, KALNAY E, COLLINS W, et al. The NCEP-NCAR 50-Year reanalysis: monthly means CD-ROM and documentation [J]. Bulletin of the American Meteorological Society, 2001, 82(2):247-268.
[11] 赵天保,符淙斌.中国区域ERA-40、NCEP-2再分析资料与观测资料的初步比较与分析[J].气候与环境研究,2006,11(1):14-32. [ZHAO Tianbao, FU Congbin. Preliminary comparison and analysis between ERA-40, NCEP-2 reanalysis and observations over China [J]. Climatic and Environmental Research, 2006, 11(1):14-32]
[12] 秦艳慧,吴通华,李韧,等.ERA-Interim地表温度资料在青藏高原多年冻土区的适用性[J].高原气象,2015,34(3):666-675.[QIN Yanhui, WU Tonghua, LI Ren, et al. Application of ERA product of land surface temperature in permafrost regions of Qinghai-Xizang Plateau [J]. Plateau Meteorology, 2015, 34(3):666-675]
[13] GAO Lu, HAO Lu, CHEN Xingwei. Evaluation of ERA-Interim monthly temperature data over the Tibetan Plateau [J]. Journal of Mountain Science, 2014, 11(05):1154-1168.
[14] YOU Qinglong, FRAEDRICH K, REN Guoyu, et al. Variability of temperature in the Tibetan Plateau based on homogenized surface stations and reanalysis data [J]. International Journal of Climatology, 2013, 33: 1337-1347.
[15] 范科科,张强,史培军,等.基于卫星遥感和再分析数据的青藏高原土壤湿度数据评估[J].地理学报,2018,73(09):1778-1791. [FAN Keke, ZHANG Qiang, SHI Peijun, et al.Evaluation of remote sensing and reanalysis soil moisture products on the Tibetan Plateau[J]. Acta Geographica Sinica, 2018, 73(09):1778-1791]
[16] 崔园园,敬文琪,覃军.基于TIPEX Ⅲ资料对CLDAS-V2.0和GLDAS-NOAH陆面模式产品在青藏高原地区的适用性评估[J].高原气象,2018,37(5):1143-1160. [CUI Yuanyuan, JING Wenqi, QIN Jun. Applicability evaluation of merged soil moisture in GLDAS-NOAH and CLDAS-V2.0 products over Qinghai-Tibetan Plateau of 2015 based on TIPEX Ⅲ observations[J].Plateau Meteorology, 2018, 37(5):1143-1160]
[17] 徐影,丁一汇,赵宗慈.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,2001,12(3):337-347.[XU Ying, DING Yihui, ZHAO Zongci. Confidence analysis of NECP/NCAR 50-year global reanalyzed data in climate change research in China [J]. Quarterly Journal of Applied Meteorology, 2001, 12(3):337-347]
[18] 李川,张廷军,陈静.近40年青藏高原地区的气候变化-NCEP和ECMWF地面气温及降水再分析和实测资料对比分析[J].高原气象,2004,V23(Z1):97-103.[ LI Chuan, ZHANG Tinjun, CHEN Jing. Climatic change of Qinghai Xizang Plateau region in recent 40 year reanalysis and surface observation data-contrast of observation data and NCEP, ECMWF surface air temperature and precipitation [J]. Plateau Meteorology, 2004, V23(Z1):97-103]
[19] 赵天保,艾丽坤,冯锦明.NCEP再分析资料和中国站点观测资料的分析与比较[J].气候与环境研究,2004,9(2):278-294. [ZHAO Tianbao, AI Likun, FENG Jinming. An intercomparison between NCEP reanalysis and observed data over China [J]. Climatic and Environmental Research, 2004, 9(2):278-294]
[20] 施晓晖,徐祥德,谢立安.NCEP/NCAR再分析风速、表面气温距平在中国区域气候变化研究中的可信度分析[J].气象学报,2006,64(6):709-722.[SHI Xiaohui, XU Xiangde, XIE Li'an. Reliability analysis of anomalies of NECP/NCAR reanalysis wind speed and surface temperature in climate change research in China [J]. Acta Meteorological Sinica, 2006, 64(6):709-722]
[21] 周青,赵凤生,高文华.NCEP/NCAR逐时分析与中国实测地表温度和地面气温对比分析[J].气象,2008,34(2):83-91. [ZHOU Qing, ZHAO Fengsheng, GAO Wenhua. Comparison and analysis between NCEP/NCAR every-6-hours analysis land surface and air temperature and 753 Chinese stations' observation in 2005 [J]. Meteorological Monthly, 2008, 34(2):83-91]
[22] 朱智,师春香,张涛,等.多种再分析地表温度资料在中国区域的适用性分析[J].冰川冻土,2015,37(3):614-624.[ZHU Zhi, SHI Chunxiang, ZHANG Tao, et al. Applicability analysis of various reanalyzed land surface temperature datasets in China [J]. Journal of Glaciology and Geocryology, 2015, 37(3):614-624]
[23] 何冬燕,田红,邓伟涛.三种再分析地表温度资料在青藏高原区域的适用性分析[J].大气科学学报,2013,36(4):458-465. [HE Dongyan, TIAN Hong, DENG Weitao. Applicability analysis of three reanalysis surface temperature data over the Tibetan Plateau [J]. Transactions of Atmospheric Sciences, 2013, 36(4): 458-465]
[24] 田柳茜,李卫忠,张尧,等.青藏高原1979-2007年间的积雪变化[J].生态学报,2014,34(20):5974-5983.[TIAN Liuxi, LI Weizhong, ZHANG Yao, et al. The analysis of snow information from 1979 to 2007 in Qinghai-Tibetan Plateau [J]. Acta Ecologica Sinica, 2014, 34(20):5974-5983]
[25] 除多,杨勇,罗布坚参,等.1981-2010年青藏高原积雪日数时空变化特征分析[J].冰川冻土,2015,37(6):1461-1472. [CHU Duo, YANG Yong, LUOBU Jiancan, et al. The variations of snow cover days over the Tibetan Plateau during 1981-2010 [J]. Journal of Glaciology and Geocryology, 2015, 37(6):1461-1472]
[26] 唐志光,王建,王欣,等.基于MODIS数据的青藏高原积雪日数提取与时空变化分析[J].山地学报,2017,35(3):412-419. [TANG Zhiguang, WANG Jian, WANG Xin, et al. Extraction and spatiotemporal analysis of snow covered days over tibetan plateau based on MODIS Data [J]. Mountain Research, 2017, 35(3):412-419]
相似文献/References:
[1]蓝永超,胡兴林,丁宏伟,等.河西内陆河流域山区近50余年来气温变化的多尺度特征和突变分析[J].山地学报,2014,(02):163.
LAN Yongchao,HU Xinglin,DIN Hongwei,et al.Multiple Time Scales Analysis of Jump and Variation of Air Temperature in Mountain Area of Hexi Inland River Basin in the Past More than 50 Years[J].Mountain Research,2014,(01):163.
[2]张宏亮,刘青利,李世杰,等.青藏高原兹格塘错沉积物介形虫壳体同位素[J].山地学报,2014,(03):373.
ZHANG Hongliang,LIU Qingli,LI Shijie,et al.Holocene Environmental Changes Derived from Ostracode Shell Stable Isotopes in the Sediment Core of Zigetang Lake,Tibetan Plateau[J].Mountain Research,2014,(01):373.
[3]花晓波,阎建忠,刘祥,等.定居牧民对草地退化的适应策略——以那曲县为例[J].山地学报,2013,(02):140.
HUA Xiaobo,YAN Jianzhong,Liu Xiang(9).Settled Herdsmen’s Adaptation Strategies to Pasture Degradation——Case Study of Naqu County in Tibet Plateau[J].Mountain Research,2013,(01):140.
[4]鲁嘉濠,牛富俊,程花,等.青藏高原工程走廊冻土分布模型及其变化趋势[J].山地学报,2013,(02):226.
LU Jiahao,NIU Fujun,Cheng Hua,et al.The Permafrost Distribution Model and Its Change Trend of Qinghai-Tibet Engineering Corridor[J].Mountain Research,2013,(01):226.
[5]刘军会,高吉喜,王文杰,等.青藏高原植被覆盖变化及其与气候变化的关系[J].山地学报,2013,(02):234.
LIU Junhui,GAO Jixi,WANG Wenjie().Variations of Vegetation Coverage and Its Relations to Global Climate Changes on the Tibetan Plateau during 1981—2005[J].Mountain Research,2013,(01):234.
[6]何永涛,石培礼,张宪洲,等.当雄念青唐古拉山脉南坡不同海拔垫状点地梅分布特征[J].山地学报,2013,(06):641.
HE Yongtao,SHI Peili,ZHANG Xianzhou,et al.Elevational Distribution of Cushion Plant Androsace tapete in the Southern Slope of Nyainqentanglha Mountains, Tibetan Plateau[J].Mountain Research,2013,(01):641.
[7]赵志龙,张镱锂,刘峰贵,等.青藏高原农牧区干旱灾害风险分析[J].山地学报,2013,(06):672.
ZHAO Zhilong,ZHANG Yili,LIU Fenggui,et al.Drought Disaster Risk Analysis of Tibetan Plateau[J].Mountain Research,2013,(01):672.
[8]陈有超,鲁旭阳,李卫朋,等.藏北典型高寒草原土壤微气候对增温的响应[J].山地学报,2014,(04):401.
CHEN Youchao,LU Xuyang,LI Weipeng,et al.Response of Soil Microclimate to Warming in Alpine Steppe, Northern Tibetan Plateau[J].Mountain Research,2014,(01):401.
[9]姜永见,李世杰,沈德福,等.青藏高原江河源区近40年来气候变化特征及其对区域环境的影响[J].山地学报,2012,(04):461.
JIANG Yongjian,LI Shijie,SHEN Defu,et al.Climate Change and Its Impact on the Regional Environment in the Source Regions of the Yangtze, Yellow and Lantsang Rivers in Qinghai-Tibetan Plateau during 1971—2008[J].Mountain Research,2012,(01):461.
[10]赵尚民,周成虎,程维明,等.青藏高原西北缘地形抬升速率与地质年代的关系[J].山地学报,2011,(05):616.
ZHAO Shangmin,,et al.Relationships between Topographic Uplifting Velocity and Geological Times for the Northwestern Edge of Qinghai-Tibet Plateau[J].Mountain Research,2011,(01):616.