1970-2016年冈底斯山冰川变化

doi:10.11821/dlxb201907005

地理学报 ›› 2019, Vol. 74 ›› Issue (7): 1333-1344.doi: 10.11821/dlxb201907005

1970-2016年冈底斯山冰川变化

刘娟¹,姚晓军¹(),刘时银^2,³,郭万钦²,许君利⁴

1.西北师范大学地理与环境科学学院,兰州 730070
2.中国科学院西北生态环境资源研究院冰冻圈科学国家重点实验室,兰州 730000
3.云南大学国际河流与生态安全研究院,昆明 650091
4.盐城师范学院,盐城 224051

收稿日期:2018-05-14 修回日期:2019-05-01 出版日期:2019-07-25 发布日期:2019-07-23
通讯作者: 姚晓军
作者简介:刘娟(1993-), 女, 甘肃定西人, 硕士生, 研究方向为环境科学与地理信息系统。E-mail: liujuan_qx@163.com
基金资助:
国家自然科学基金项目(41561016);国家自然科学基金项目(41861013);国家自然科学基金项目(41801052);科技部科技基础性工作专项(2013FY111400);西北师范大学青年教师科研能力提升计划项目(NWNU-LKQN-14-4)

Glacier changes in the Gangdisê Mountains from 1970 to 2016

LIU Juan¹,YAO Xiaojun¹(),LIU Shiyin^2,³,GUO Wanqin²,XU Junli⁴

1.College of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, China
2.State Key Laboratory of Cryosphere Sciences, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou 730000, China
3.Institute of International Rivers and Eco-Security, Yunnan University, Kunming 650091, China
4.Yancheng Teachers University, Yancheng 224051, Jiangsu, China

Received:2018-05-14 Revised:2019-05-01 Online:2019-07-25 Published:2019-07-23
Contact: YAO Xiaojun
Supported by:
National Natural Science Foundation of China(41561016);National Natural Science Foundation of China(41861013);National Natural Science Foundation of China(41801052);National Basic Work Program of MST(2013FY111400);Youth Scholar Scientific Capability Promoting Project of Northwest Normal University(NWNU-LKQN-14-4)

摘要/Abstract

摘要：

基于修订后的中国两次冰川编目数据及2015-2016年Landsat OLI遥感影像,对冈底斯山1970-2016年的冰川时空变化特征进行分析,并利用相应时段的气温和降水数据,对冰川变化原因进行探讨,为全面认识冈底斯山在气候变暖背景下冰川的响应规律及区域水资源合理利用提供科学依据。结果表明：① 2015-2016年冈底斯山共有冰川3953条,面积1306.45 km ²,冰储量约58.16 km ³;冰川数量以面积< 0.5 km ²的冰川为主,面积则以介于0.1~5 km ²的冰川为主。② 1970-2016年冈底斯山冰川面积共减少854.05 km ²（-39.53%）,冰川面积变化相对速率高达-1.09%/a,消融期气温升高是导致该山区冰川退缩的最主要原因。与中国西部其他山系冰川变化相比,冈底斯山是冰川退缩最为强烈的地区,且近年来冰川退缩呈加快趋势。③ 冈底斯山冰川面积减少主要集中在海拔5600~6100 m之间,海拔6500 m以上区域基本没有变化。除南朝向和东南朝向外,冈底斯山其他朝向冰川数量和面积均呈减少趋势,其中北朝向冰川面积减少最多,西北朝向冰川面积变化最快。④ 冈底斯山冰川面积变化自西向东呈加快趋势,其中东段冰川面积变化相对速率高达-1.72%/a,中段次之（-1.67%/a）,西段仅为-0.83%/a。

关键词: 冰川变化, 冰川编目, 气候变化, 冈底斯山

Abstract:

Based on the revised First and Second Chinese Glacier Inventory and Landsat OLI remote sensing images during 2015-2016, we analyzed the spatial-temporal variation characteristics of glaciers in the Gangdisê Mountains during 1970-2016. The results of this study provide a scientific basis for the rational use of water resources in this region. The results showed that there were 3953 glaciers with a total area of 1306.45 km ² and ice volume of ~58.16 km ³ in the Gangdisê Mountains during 2015-2016. The glaciers in sizes of 0.1-5 km ² and < 0.5 km ² had the largest area and the greatest number of glaciers in the Gangdisê Mountains, respectively. In the past five decades, the area of glaciers decreased by 854.05 km ² (-1.09%/a), accounting for 39.53% of the total area of glaciers in the region in 1970. The increase of temperature in the ablation period was the most important cause of glacier retreat. Compared to other mountains in western China, the Gangdisê Mountains was the region with the strongest glacier retreat and had an accelerating tendency in recent years. The decrease of glacier area was mainly concentrated at elevations of 5600-6100 m a.s.l. and there was no change in elevation above 6500 m a.s.l. in the Gangdisê Mountains. Except for the south and southeast orientations, the number and area of glaciers were decreasing in all the orientations. Specifically, the north orientation suffered the largest area loss of glaciers and the northwest orientation witnessed the fastest retreat of glacier area. A significant feature of spatial variation showed that the rate of glacier retreat was faster from west to east in the Gangdisê Mountains. The relative change of glacier rate in the eastern section was high at -1.72%/a, followed by the middle section (-1.67%/a), and that in the western section was only -0.83%/a.

Key words: glacier change, glacier inventory, climate change, Gangdisê Mountains;

刘娟,姚晓军,刘时银,郭万钦,许君利. 1970-2016年冈底斯山冰川变化[J]. 地理学报, 2019, 74(7): 1333-1344.

LIU Juan,YAO Xiaojun,LIU Shiyin,GUO Wanqin,XU Junli. Glacier changes in the Gangdisê Mountains from 1970 to 2016[J]. Acta Geographica Sinica, 2019, 74(7): 1333-1344.

图/表 11

图1

表1

图2

表2

表3

图3

图4

图5

图6

图7

表4

参考文献 50

[1]	Kargel J S, Leonard G J, Bishop M P , et al. Global Land Ice Measurements from Space. Heidelberg: Springer, 2014.
[2]	Shi Yafeng . Estimation of the water resources affected by climatic warming and glacier shrinkage before 2050 in west China. Journal of Glaciology and Geocryology, 2001,23(4):333-341.
	[ 施雅风 . 2050年前气候变暖冰川萎缩对水资源影响情景预估. 冰川冻土, 2001,23(4):333-341.]
[3]	Zhang Jiutian, He Xiaojia, Shangguan Donghui , et al. Impact of intensive glacier ablation on arid regions of northwest China and its countermeasure. Journal of Glaciology and Geocryology, 2012,34(4):848-854.
	[ 张九天, 何霄嘉, 上官冬辉 , 等. 冰川加剧消融对我国西北干旱区的影响及其适应对策. 冰川冻土, 2012,34(4):848-854.]
[4]	Oerlemans J . Quantifying global warming from the retreat of glaciers. Science, 1994,264(5156):243-244. doi: 10.1126/science.264.5156.243
[5]	Immerzeel W W, Van Beek L P, Bierkens M F . Climate change will affect the Asian water towers. Science, 2010,328(5984):1382-1385. doi: 10.1126/science.1183188
[6]	Church J A, White N J, Konikow L F , et al. Revisiting the Earth's sea-level and energy budgets from 1961 to 2008. Geophysical Research Letters, 2013,40(15):4066-4066. doi: 10.1002/grl.50752
[7]	Benn D I, Bolch T, Hands K , et al. Response of debris-covered glaciers in the Mount Everest region to recent warming, and implications for outburst flood hazards. Earth-Science Reviews, 2012,114(1):156-174. doi: 10.1016/j.earscirev.2012.03.008
[8]	Wang W, Xiang Y, Gao Y , et al. Rapid expansion of glacial lakes caused by climate and glacier retreat in the Central Himalayas. Hydrological Processes, 2015,29(6):859-874. doi: 10.1002/hyp.v29.6
[9]	Wu K P, Liu S Y, Bao W J , et al. Recent glacier mass balance and area changes in the Kangri Karpo Mountains from DEMs and glacier inventories. Cryosphere, 2018,12(1):103-121. doi: 10.5194/tc-12-103-2018
[10]	Qiu J . China: The third pole. Nature, 2008,454(7203):393-396. doi: 10.1038/454393a
[11]	You Lianyuan, Yang Jingchun. Geomorphology in China. Beijing: Science Press, 2013.
	[ 尤联元, 杨景春 . 中国地貌. 北京:科学出版社, 2013.]
[12]	Pu Jianchen, Yao Tandong, Wang Ninglian , et al. Fluctuations of the glaciers on the Tibetan Plateau during the Past Century. Journal of Glaciology and Geocryology, 2004,26(5):517-522.
	[ 蒲健辰, 姚檀栋, 王宁练 , 等. 近百年来青藏高原冰川的进退变化. 冰川冻土, 2004,26(5):517-522.]
[13]	Li Zhiguo, Yao Tandong, Ye Qinghua , et al. Monitoring glacial variations based on remote sensing in the Luozha region, eastern Himalayas, 1980-2007. Geographical Research, 2011,30(5):939-953.
	[ 李治国, 姚檀栋, 叶庆华 , 等. 1980-2007年喜马拉雅东段洛扎地区冰川变化遥感监测. 地理研究, 2011,30(5):939-953.]
[14]	Ye Qinghua, Chen Feng, Yao Tandong , et al. Tupu of glacier variations in the Mt. Naimona Nyi region, western Himalayas, in the last three decades. Journal of Remote Sensing, 2007,11(4):511-520. doi: 10.11834/jrs.20070471
	[ 叶庆华, 陈锋, 姚檀栋 , 等. 近30年来喜马拉雅山脉西段纳木那尼峰地区冰川变化的遥感监测研究. 遥感学报, 2007,11(4):511-520.] doi: 10.11834/jrs.20070471
[15]	Liu Shiyin, Shangguan Donghui, Ding Yongjian , et al. Glacier variations since the early 20th century in the Gangrigabu Range, southeast Tibetan Plateau. Journal of Glaciology and Geocryology, 2005,27(1):55-63.
	[ 刘时银, 上官冬辉, 丁永建 , 等. 20世纪初以来青藏高原东南部岗日嘎布的冰川变化. 冰川冻土, 2005,27(1):55-63.]
[16]	Shangguan Donghui, Liu Shiyin, Ding Liangfu , et al. Variation of glaciers in the western Nyainqetanglha range of Tibetan Plateau during 1970-2000. Journal of Glaciology and Geocryology, 2008,30(2):204-210.
	[ 上官冬辉, 刘时银, 丁良福 , 等. 1970-2000年念青唐古拉山脉西段冰川变化. 冰川冻土, 2008,30(2):204-210.]
[17]	Kang Shichang, Chen Feng, Ye Qinghua , et al. Glacier retreating dramatically on the Mt. Nyainqentaglha during the last 40 years. Journal of Glaciology and Geocryology, 2007,29(6):863-873.
	[ 康世昌, 陈锋, 叶庆华 , 等. 1970-2007年西藏念青唐古拉峰南、北坡冰川显著退缩. 冰川冻土, 2007,29(6):863-873.]
[18]	Wang Congqiang, Yang Taibao, Ji Qin , et al. Remote sensing monitoring of glacier changes in the middle region of Tanggula Mountain. Arid Land Geography (Chinese Version), 2016,39(3):504-512.
	[ 王聪强, 杨太保, 冀琴 , 等. 1990-2015年唐古拉山中段冰川变化遥感监测. 干旱区地理(汉文版), 2016,39(3):504-512.]
[19]	Gardelle J, Berthier E, Arnaud Y . Slight mass gain of Karakoaram glaciers in the early twenty-first century. Nature Geoscience, 2012,5(5):322-325. doi: 10.1038/ngeo1450
[20]	Kääb A, Treichler D, Nuth C , et al. Brief communication: Contending estimates of 2003-2008 glacier mass balance over the Pamir-Karakoram-Himalaya. Cryosphere, 2015,7(4):1263-1286.
[21]	Gardelle J, Berthier E, Arnaud Y , et al. Region-wide glacier mass balances over the Pamir-Karakoram-Himalaya during 1999-2011. The Cryosphere, 2013,9(2):557-564.
[22]	Liu Shiyin, Ding Yongjian, Li Jing , et al. Glaciers in response to recent climate warming in western China. Quaternary Sciences, 2006,26(5):762-771.
	[ 刘时银, 丁永建, 李晶 , 等. 中国西部冰川对近期气候变暖的响应. 第四纪研究, 2006,26(5):762-771.]
[23]	Yao T, Thompson L, Yang W , et al. Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings. Nature Climate Change, 2012,2(9):663-667. doi: 10.1038/nclimate1580
[24]	Xu Qiang, Ding Lin . Paleoelevation research on Gangdisê Mountains and Tibetan Plateau. China Science Foundation, 2015(1):54-59.
	[ 许强, 丁林 . 冈底斯山的隆升过程与青藏高原古高度研究. 中国科学基金, 2015(1):54-59.]
[25]	Yang Qinye, Zheng Du . On the significance of the boundary line-The Gandisi-Nyainqentanglna Range. Geographical Research, 1985,4(2):36-44.
	[ 杨勤业, 郑度 . 冈底斯山—念青唐古拉山线自然地理意义的探讨. 地理研究, 1985,4(2):36-44.]
[26]	Li Jijun, Zheng Benxing, Yang Xijin , et al. Tibet Glacier. Beijing: Science Press, 1986.
	[ 李吉均, 郑本兴, 杨锡金 , 等. 西藏冰川. 北京:科学出版社, 1986.]
[27]	Shi Yafeng, Liu Shiyin . Pre-estimation for the response of China glaciers to global warming in the 21st century. Chinese Science Bulletin, 2000,45(4):434-438.
	[ 施雅风, 刘时银 . 中国冰川对21世纪全球变暖响应的预估. 科学通报, 2000,45(4):434-438.]
[28]	Shi Yafeng. A Concise China Glacier Inventory. Shanghai: Shanghai Science Popular Press, 2005.
	[ 施雅风 . 简明中国冰川目录. 上海: 上海科学普及出版社, 2005.]
[29]	Liu Shiyin, Yao Xiaojun, Guo Wanqin , et al. The contemporary glaciers in China base on the Second Chinese Glacier Inventory. Acta Geographica Sinica, 2015,70(1):3-16.
	[ 刘时银, 姚晓军, 郭万钦 , 等. 基于第二次冰川编目的中国冰川现状. 地理学报, 2015,70(1):3-16.]
[30]	Guo W, Liu S, Xu J , et al. The second Chinese glacier inventory: Data, methods and results. Journal of Glaciology, 2015,61(226):357-372. doi: 10.3189/2015JoG14J209
[31]	Hall D K, Bayr K J, Schnöer W , et al. Consideration of the errors inherent in mapping historical glacier positions in Austria from ground and space (1893-2001). Remote Sensing of Environment, 2003,86(4):566-577. doi: 10.1016/S0034-4257(03)00134-2
[32]	Williams R S, Hall D K, Sigurosson O . Comparison of satellite-derived with ground-based measurements of the fluctuations of the margins of Vatnajökull, Iceland, 1973-92. Annals of Glaciology, 1997,24(3):72-80. doi: 10.3189/S0260305500011964
[33]	Shangguan Donghui . Glacier changes in Tarim Interior River Basin using 3S [D]. Cold and Arid Regions Environmental and Engineering Research Institute. Lanzhou: Chinese Academy of Science, 2007.
	[ 上官冬辉 . 基于3S的塔里木河流域冰川应用研究[D]. 兰州: 中国科学院寒区旱区环境与工程研究所, 2007.]
[34]	Gärtner-Roer I, Naegeli K, Huss M , et al. A database of worldwide glacier thickness observations. Global and Planetary Change, 2014,122:330-344. doi: 10.1016/j.gloplacha.2014.09.003
[35]	Radić V, Hock R . Regional and global volumes of glaciers derived from statistical upscaling of glacier inventory data. Journal of Geophysical Research, 2010,115, F01010. doi: 10. 1029/2009JF001373.
[36]	Grinsted A . An estimate of global glacier volume. Cryosphere, 2013,7:141-151. doi: 10.5194/tc-7-141-2013
[37]	Liu S, Sun W, Shen Y , et al. Glacier changes since the Little Ice Age maximum in the western Qilian Shan, northwest China, and consequences of glacier runoff for water supply. Journal of Glaciology, 2003,49(164):117-124. doi: 10.3189/172756503781830926
[38]	Xie Zichu, Liu Chaohai. Introduction to Glaciology. Shanghai: Shanghai Science Popular Press, 2010.
	[ 谢自楚, 刘潮海 . 冰川学导论. 上海: 上海科学普及出版社, 2010.]
[39]	Gao Xiaoqing . Discussion on the relationship between glacial fluctuation and climate change. Plateau Meteorology, 2000,19(1):9-16.
	[ 高晓清 . 冰川变化与气候变化关系的若干探讨. 高原气象, 2000,19(1):9-16.]
[40]	Beedle M J, Menounos B, Wheate R , et al. Glacier change in the Cariboo Mountains, British Columbia, Canada (1952-2005). Cryosphere, 2014,9(1):65-80.
[41]	Liu W, Guo Q H, Wang Y X . Temporal-spatial climate change in the last 35 years in Tibet and its geo-environmental consequences. Environmental Geology, 2008,54(8):1747-1754. doi: 10.1007/s00254-007-0952-y
[42]	Oerlemans J . Extracting a climate signal from 169 glacier records. Science, 2005,308(5722):675-677. doi: 10.1126/science.1107046
[43]	Xu B Q, Cao J J, Hansen J , et al. Black soot and the survival of Tibetan glaciers. Proceedings of the National Academy of Sciences. 2009,106(52):22114-22118.
[44]	Sun M P, Liu S Y, Yao X J , et al. Glacier changes in the Qilian Mountains in the past half century: Based on the revised first and second Chinese glacier inventory. Journal of Geographical Sciences, 2018,28(2):206-220. doi: 10.1007/s11442-018-1468-y
[45]	Yao Xiaojun, Liu Shiyin, Guo Wanqin , et al. Glacier change of Altay Mountain in China from 1960 to 2009: Based on the Second Glacier Inventory of China. Journal of Natural Resources, 2012,27(10):1734-1745.
	[ 姚晓军, 刘时银, 郭万钦 , 等. 近50a来中国阿尔泰山冰川变化: 基于中国第二次冰川编目成果. 自然资源学报, 2012,27(10):1734-1745.]
[46]	Xing Wucheng, Li Zhongqin, Zhang Hui , et al. Spatial-temporal variation of glacier resources in Tianshan Mountains since. Acta Geographica Sinica, 2017,72(9):1594-1605.
	[ 邢武成, 李忠勤, 张惠 , 等. 1959年以来中国天山冰川资源时空变化. 地理学报, 2017,72(9):1594-1605.]
[47]	Zhu Heyong, Yang Taibao, Tian Hongzhen . Glacier variation in the Altun mountains from 1973 to 2010. Geographical Research, 2013,32(8):1430-1438.
	[ 祝合勇, 杨太保, 田洪阵 . 1973-2010年阿尔金山冰川变化. 地理研究, 2013,32(8):1430-1438.]
[48]	Liu Shiyin, Lu Anxin, Ding Yongjian , et al. Glacier fluctuations and the inferred climate changes in the Anymaqn Mountains in the source area of the Yellow River. Journal of Glaciology and Geocryology, 2002,24(6):701-707.
	[ 刘时银, 鲁安新, 丁永建 , 等. 黄河上游阿尼玛卿山区冰川波动与气候变化. 冰川冻土, 2002,24(6):701-707.]
[49]	Li Deping, Wang Liping, Liu Shiyin , et al. Tupu analysis of the spatio-temporal glacier variations in the central and western Qangtang Plateau since the Little Ice Age. Journal of Glaciology and Geocryology, 2009,31(1):40-47.
	[ 李德平, 王利平, 刘时银 , 等. 小冰期以来羌塘高原中西部冰川变化图谱分析. 冰川冻土, 2009,31(1):40-47.]
[50]	Li Xia, Yang Taibao, Tian Hongzhen , et al. Response of glacier in Gongga Mountain to climate change during the last 40 years. Research of Soil and Water Conservation, 2013,20(6):125-129.
	[ 李霞, 杨太保, 田洪阵 , 等. 贡嘎山近40年冰川对气候变化的响应. 水土保持研究, 2013,20(6):125-129.]

序号	轨道号			获取日期	序号	轨道号		获取日期
序号	Path	Row		获取日期	序号	Path	Row	获取日期
1	138		39	2016-04-27	8	143	38	2016-10-07
2	138		40	2016-04-27	9	143	39	2016-09-05
3	139		39	2016-03-17	10	144	38	2016-06-24
4	140		39	2016-10-18	11	145	37	2016-10-15
5	141		39	2016-05-18	12	145	38	2016-09-03
6	141		40	2015-10-07	13	146	37	2016-09-10
7	142		39	2015-09-28

一级流域 (编码)	二级流域 (编码)	三级流域 (编码)	冰川数量		冰川面积		冰储量
一级流域 (编码)	二级流域 (编码)	三级流域 (编码)	(条)	(%)	(km²)	(%)	(km²)	(%)
恒河(5O)	雅鲁藏布江(5O2)	多雄藏布等(5O26)	1372	34.71	413.65	31.66	16.63	28.65
印度河(5Q)	森格藏布等(5Q1)	森格藏布等(5Q15)	703	17.78	172.36	13.19	7.54	12.99
	朗钦藏布等(5Q2)	朗钦藏布等(5Q22)	227	5.74	40.09	3.07	1.30	2.24
		合计	930	23.52	212.45	16.26	8.84	15.23
青藏高原内流区(5Z)	色林错流域(5Z2)	色林错(5Z22)	43	1.09	15.46	1.18	0.66	1.14
	扎日南木错流域(5Z3)	当惹错等(5Z31)	104	2.63	27.28	2.09	0.93	1.60
		扎日南木错(5Z32)	182	4.61	61.48	4.71	2.52	4.34
		塔惹错等(5Z33)	301	7.61	157.64	12.07	6.80	11.71
		昂仁拉错(5Z34)	531	13.43	343.12	26.26	19.47	33.54
	班公湖流域(5Z4)	班公湖(5Z42)	490	12.40	75.37	5.77	2.20	3.79
	合计		1651	41.78	680.35	52.08	29.72	51.19

市(地区)	冰川数量		冰川面积		冰储量
市(地区)	(条)	(%)	(km²)	(%)	(km³)	(%)
拉萨	46	1.17	22.83	1.75	1.13	1.94
日喀则	1603	40.55	607.87	46.53	27.09	46.58
阿里	2260	57.17	665.13	50.91	29.60	50.89
那曲	44	1.11	10.62	0.81	0.34	0.58

名称	时间段	面积变化(km²)	面积变化速率(km²/a)	面积变化相对速率(%/a)	资料来源
阿尔泰山	1960-2009年	-104.61	-2.13	-0.94	[45]
天山	1959-2010年	-1619.82	-31.76	-0.40	[46]
阿尼玛卿山	1966-2000年	-21.70	-0.64	-0.56	[47]
阿尔金山	1973-2010年	-54.22	-1.47	-0.46	[48]
祁连山	1956-2010年	-417.15	-7.73	-0.43	[44]
唐古拉山中段	1990-2015年	-115.46	-4.62	-1.00	[18]
羌塘高原中西部	1970-2000年	-5.07	-0.17	-0.03	[49]
冈底斯山	1970-2016年	-854.05	-18.57	-1.09	本研究
念青唐古拉山西段	1970-2000年	-52.10	-1.74	-0.19	[16]
岗日嘎布	1980-2015年	-679.50	-19.41	-0.82	[9]
喜马拉雅东段洛扎地区	1980-2007年	-80.77	-2.99	-0.66	[13]
贡嘎山	1974-2010年	-30.20	-0.84	-0.35	[50]

1970-2016年冈底斯山冰川变化

Glacier changes in the Gangdisê Mountains from 1970 to 2016

RichHTML

PDF (PC)

赞

可视化

摘要/Abstract

引用本文

使用本文

图/表 11

参考文献 50

相关文章 15

Metrics

本文评价

[1]	李哲, 丁永建, 陈艾姣, 张智华, 张世强. 1960—2019年西北地区气候变化中的Hiatus现象及特征[J]. 地理学报, 2020, 75(9): 1845-1859.
[2]	金凯, 王飞, 韩剑桥, 史尚渝, 丁文斌. 1982—2015年中国气候变化和人类活动对植被NDVI变化的影响[J]. 地理学报, 2020, 75(5): 961-974.
[3]	李双双, 汪成博, 延军平, 刘宪锋. 面向事件过程的秦岭南北极端降水时空变化特征[J]. 地理学报, 2020, 75(5): 989-1007.
[4]	田晶, 郭生练, 刘德地, 陈启会, 王强, 尹家波, 吴旭树, 何绍坤. 气候与土地利用变化对汉江流域径流的影响[J]. 地理学报, 2020, 75(11): 2307-2318.
[5]	萧凌波, 闫军辉. 基于地方志的1736-1911年华北秋粮丰歉指数序列重建及其与气候变化的关系[J]. 地理学报, 2019, 74(9): 1777-1788.
[6]	李双双, 延军平, 武亚群, 汪成博. 秦岭—淮河南北供暖格局变化及其影响因素[J]. 地理学报, 2019, 74(9): 1866-1877.
[7]	佟彪, 党安荣, 许剑. 300 BC-1900 AD无定河流域城镇时空格局演变[J]. 地理学报, 2019, 74(8): 1508-1524.
[8]	马丹阳, 尹云鹤, 吴绍洪, 郑度. 中国干湿格局对未来高排放情景下气候变化响应的敏感性[J]. 地理学报, 2019, 74(5): 857-874.
[9]	刘俊,黄莉,孙晓倩,李宁馨,张恒锦. 气候变化对中国观鸟旅游的影响——基于鸟类物候变化的分析[J]. 地理学报, 2019, 74(5): 912-922.
[10]	高江波, 焦珂伟, 吴绍洪. 1982-2013年中国植被NDVI空间异质性的气候影响分析[J]. 地理学报, 2019, 74(3): 534-543.
[11]	唐见,曹慧群,陈进. 生态保护工程和气候变化对长江源区植被变化的影响量化[J]. 地理学报, 2019, 74(1): 76-86.
[12]	李依婵,李育,朱耿睿. 一种新的气候变化敏感区的定义方法与预估[J]. 地理学报, 2018, 73(7): 1283-1295.
[13]	张扬,白红英,苏凯,黄晓月,孟清,郭少壮. 1960-2013年秦岭陕西段南北坡极端气温变化空间差异[J]. 地理学报, 2018, 73(7): 1296-1308.
[14]	邓海军,陈亚宁. 中亚天山山区冰雪变化及其对区域水资源的影响[J]. 地理学报, 2018, 73(7): 1309-1323.
[15]	秦雅,刘玉洁,葛全胜. 气候变化背景下1981-2010年中国玉米物候变化时空分异[J]. 地理学报, 2018, 73(5): 906-916.