地球科学进展 ›› 2015, Vol. 30 ›› Issue (5): 517 -529. doi: 10.11867/j.issn.1001-8166.2015.05.517

   下一篇

冰冻圈及其变化的脆弱性与适应研究体系
杨建平 1( ), 丁永建 1, 2, 方一平 3, 秦大河 1, 4   
  1. 1.中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室, 甘肃 兰州 730000
    2. 中国科学院寒区旱区环境与工程研究所水土资源研究室,甘肃 兰州 730000
    3. 中国科学院水利部成都山地灾害与环境研究所, 四川 成都 610041
    4. 中国气象局,北京 100081
  • 出版日期:2015-06-09
  • 基金资助:
    科技部全球变化重大科学研究计划重大科学目标导向项目“ 冰冻圈变化及其影响研究”(编号:2013CBA01800);国家自然科学基金项目“疏勒河流域生态—社会经济系统受冰川变化影响的脆弱性研究”(编号:41271088)资助

Research Frame of Vulnerability and Adaptation for the Cryosphere and its changes

Jianping Yang 1, Yongjian Ding 1, 2, Yiping Fang 3, Dahe Qin 1, 4   

  1. 1.State Key Laboratory of Cryospheric Science,Cold & Arid Regions Environmental & Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000, China
    2. Key Laboratory of Eco-hydrology of Inland River Basin, Cold and Arid Regions Environmental and Engineering Research Institute(CAREERI), Chinese Academy of Sciences(CAS) , Lanzhou, 730000, China
    3. Institute of Mountain Disaster & Environment, Chinese Academy of Sciences, Chengdu, 610041, China
    4. China Meteorological Administration, Beijing, 100081,China)
  • Online:2015-06-09 Published:2015-05-06

冰冻圈及其变化的脆弱性与适应研究是以探索冰冻圈及其变化的脆弱性概念为前提和基础,以冰冻圈变化的自然影响为链接点,以社会经济影响研究为突破,以脆弱性研究为桥梁与纽带,以应对与适应冰冻圈变化影响、风险为目的的冰冻圈科学领域的新兴研究方向。探讨了冰冻圈及其变化的脆弱性概念,并以影响—脆弱性—适应为主线,针对冰冻圈变化的社会经济影响研究、脆弱性研究、适应研究内容及其关键科学问题、脆弱性评估模型、尺度问题进行了较为详细的阐述,初步搭建了中国冰冻圈及其变化的脆弱性与适应研究体系。基于冰冻圈要素的多样性、变化影响的复杂性与显著的区域差异性,从2个梯度勾绘了冰冻圈及其变化的脆弱性与适应研究格局与空间布局。中国冰冻圈及其变化的脆弱性与适应研究除深化冰冻圈变化的影响与脆弱性研究之外,应加强不同利益相关者协同设计、共同参与的冰冻圈变化适应应用研究,并关注冰冻圈灾害风险、渐变风险研究。

Vulnerability and adaptation study of the cryosphere and its changes is a novel research direction in the field of cryospheric research. The exploration and understanding of vulnerability concept of the cryosphere and its changes is the prerequisite and foundation of the study system. In addition, the research content includes social and economic impacts of cryospheric changes, which is the breakthrough point, the vulnerability and adaptation assessments of the different scales of human-environment systems to the effects of cryospheric changes, which is the bridge between impact and adaptation, and the option and pathway of coping with and adapting to the effects and risk of cryospheric changes, which is the goal. In this paper, the vulnerability concept of Chinese cryosphere and its changes is firstly defined and discussed. Impact, vulnerability and adaptation as a main line, the research contents and their respective key scientific issues of social and economic impacts, vulnerability and adaptation of cryosphere change, vulnerability assessment model, and study scale are elaborated. Thus, a research frame of the vulnerability and adaptation is initially built in the kingdom of Chinese cryospheric sciences. The component of Chinese cryosphere is various, including glacier, frozen ground, snow, river ice, lake ice, and sea ice. The variations and impacts of these elements are complicated, and different from one region to another. The vulnerability and adaptation study pattern and spatial layout of Chinese cryosphere and its changes are determined in the paper on the basis of the consideration of abovementioned diversity, complexity and regional differences. The applied study on cryosphere change adaptation of co-design and joint participation for different stakeholders should be strengthened and cryospheric disaster risk, especially gradient risk should also be paid high attention to in addition to the further study of the impact and vulnerability of the cryosphere change.

中图分类号: 

图1 冰冻圈科学树
Fig.1 Sketch showing the tree of Cryospheric Sciences
图2 中国冰冻圈及其变化的脆弱性概念框架
Fig.2 The concept framework of the vulnerabilities of Chinese Cryosphere and its changes
图3 冰冻圈及其变化的脆弱性与适应研究内容与关键科学问题
Fig.3 The research content and the key scientific questions on the vulnerabilities and adaptations of Chinese Cryosphere and its changes
图4 冰冻圈及其变化的脆弱性与适应研究尺度
Fig.4 The study scales of the vulnerabilities and adaptations of Chinese Cryosphere and its changes
图5 中国冰冻圈作用区、脆弱性与适应典型研究地区/流域示意图
Fig.5 Sketch map showing the range of Chinese Cryosphere action area, vulnerability and adaptation typical study areas and basins in China
[1] IPCC. Climate change 2007: The physical science basis[M]∥Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge and New York: Cambridge University Press, 2007.
[2] Climate and cryosphere[EB/OL]. (2014-03-10)[2014-08-25].
URL    
[3] Ding Yongjian, Xiao Cunde.Challenges in the study of cryospheric changes and their impacts[J].Advances in Earth Science, 2013, 28(10):1 067-1 076.
[丁永建,效存德.冰冻圈变化及其影响研究的主要科学问题概论[J].地球科学进展, 2013, 28(10):1 067-1 076.]
[4] IPCC. Climate change: The IPCC impacts assessment[M]∥Contribution of Working Group Ⅱ to the First Assessment Report of the Intergovernmental Panel on Climate Change. Canberra: Australian Government Publishing Service Press, 1990.
[5] IPCC. Climate change 1995: Impacts, adaptations and mitigation of climate change: Scientific-technical analyses[M]∥Contribution of Working Group Ⅱ to the Second Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, New York, and Australia: Cambridge University Press, 1996.
[6] IPCC. Climate change 2001: Impacts, adaptation, and vulnerability of climate change[M]∥Contribution of Working Group Ⅱ to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press, 2001.
[7] IPCC.Climate change 2007:Impacts,adaptation and vulnerability[M]∥Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change.Cambridge, UK and New York, USA:Cambridge University Press, 2007.
[8] IPCC. Climate change 2014: Impacts, adaptation and vulnerability[M]∥Contribution of Working Group Ⅱ to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, United Kingdom and New York, NY, USA: Cambridge University Press, 2014.
[9] Shi Yafeng, Liu Chaohai, Wang Zongtai,et al.A Concise China Glacier Inventory[M].Shanghai:Shanghai Science Popularization Press, 2005.
[施雅风, 刘潮海, 王宗太,等.简明中国冰川编目[M].上海:上海科学普及出版社, 2005.]
[10] Zhou Youwu, Guo Dongxin, Qiu Guoqing, et al.Geocryology in China[M]. Beijing: Science Press, 2000.
[周幼吾, 郭东信, 邱国庆, 等. 中国冻土[M]. 北京:科学出版社, 2000.]
[11] IPCC. Summary for policymakers[M]∥Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, United Kingdom and New York, NY, USA: Cambridge University Press, 2013.
[12] Ren Jiawen. Updating assessment results of global cryospheric change from SPM of IPCC WGI fifth assessment report[J]. Journal of Glaciology and Geocryology, 2013, 35(5):1065-1 067.
[任贾文. 全球冰冻圈现状和未来变化的最新评估:IPCC WGI AR5 SPM发布[J].冰川冻土,2013, 35(5):1065-1 067]
[13] Wang Dan,Zhang Hao.Impact of the Arctic passage’s opening on Chinese northern ports and China’s response[J].China Soft Science, 2014(3):16-31.
[王丹,张浩. 北极通航对中国北方港口的影响及其应对策略研究[J]. 中国软科学, 2014(3):16-31.]
[14] Norway the official site in China[EB/OL]. [2015-01-19]..
URL    
[15] Peng Zhenwu, Wang Yunchuang.Significance and domestic impact of navigable Arctic channel[J]. Port & Waterway Engineering, 2014,(7): 86-89.
[彭振武, 王云闯. 北极航道通航的重要意义及对我国的影响[J]. 水运工程,2014,(7): 86-89.]
[16] Ren Jiawen, Qin Dahe, Kang Shichang, et al.Glacier variations and climate warming and drying in the central Himalayas[J]. Chinese Science Bulletin, 2004, 49:165-169.
[17] Liu Shiyin, Ding Yongjian, Li Jing, et al.Glaciers in response to recent climate warming in western China[J]. 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[J]. 第四纪研究,2006, 26(5):762-771.]
[18] Kang Shichang, Chen Feng, Ye Qinghua, et al. Glacier retreating dramatically on the Mt. Nyainqêntanglha during the last 40 years[J]. Journal of Glaciology and Geocryology, 2007, 29(6): 869-873.
[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[J]. 冰川冻土, 2007, 29(6): 869-873.]
[19] Li Zhongqin, Shen Yongping, Wang Feiteng, et al.Response of glacier melting to climate change —Take rümqi Glacier No.1 as an example[J]. Journal of Glaciology and Geocryology, 2007, 29(3):333-342.
[李忠勤, 沈永平, 王飞腾, 等. 冰川消融对气候变化的响应——以乌鲁木齐河源1号冰川为例[J]. 冰川冻土, 2007, 29(3):333-342.]
[20] Kang Shichang, Xu Yanwei, You Qinglong, et al.Review of climate and cryospheric change in the Tibetan Plateau[J]. Environmental Research Letter, 2010, 5: 015101,doi:10.1088/1748-9326/5/1/015101.
[21] Wang Liping, Xie Zichu, Liu Shiyin, et al.Glacierized area variation and its response to climate change in Qiangtang Plateau during 1970-2000[J]. Journal of Glaciology and Geocryology, 2011, 33(5):979-990.
[王利平, 谢自楚, 刘时银, 等. 1970—2000年羌塘高原冰川变化及其预测研究[J]. 冰川冻土,2011, 33(5):979-990.]
[22] Lan Yongru, Liu Gaohuan, Shao Xuemei.Variation of the Melang Glacier in Mount Kawa Karpo in the past 40 years, based on dendrochronolog[J]. Journal of Glaciology and Geocryology, 2011, 33(6):1 229-1 234.
[蓝永如, 刘高焕, 邵雪梅. 近40a来基于树轮年代学的梅里雪山明永冰川变化研究[J]. 冰川冻土, 2011, 33(6): 1 229-1 234.]
[23] Bie Qiang, Qiang Wenli, Wang Chao, et al.Monitoring glacier variation in the upper reaches of the Heihe River based on remote sensing in 1960-2010[J]. Journal of Glaciology and Geocryology, 2013, 35(3):574-582.
[别强,强文丽,王超,等.1960—2010年黑河流域冰川变化的遥感监测[J].冰川冻土,2013, 35(3):574-582.]
[24] Xiang Lingzhi, Liu Zhihong, Liu Jinbao, et al.Variation of glaciers and its response to climate change in Bomi County of Tibet Autonomous region in 1980-2010[J]. Journal of Glaciology and Geocryology, 2013, 35(3):593-600.
[向灵芝,刘志红,柳锦宝,等. 1980—2010年西藏波密县冰川变化及其对气候变化的响应[J]. 冰川冻土,2013, 35(3):593-600.]
[25] Wang Shaoling, Zhao Xiufeng, Guo Dongxin, et al.Response of permafrost to climate change in the Qinghai-Xizang Plateau[J]. Journal of Glaciology and Geocryology, 1996, 18(Suppl.): 157-165.
[王绍令, 赵秀锋, 郭东信, 等. 青藏高原冻土对气候变化的响应[J]. 冰川冻土, 1996, 18(增刊): 157-165.]
[26] Wang Shaoling.Study of permafrost degradation in the Qinghai-Xizang Plateau[J]. Advances in Earth Science, 1997,12(2): 164-167.
[王绍令. 青藏高原冻土退化的研究[J]. 地球科学进展, 1997, 12(2): 164-167.]
[27] Li Xin, Cheng Guodong.Response model of permafrost in high altitude on global change[J]. Science in China (Series D), 1999, 29(2): 185-192.
[李新, 程国栋. 高海拔多年冻土对全球变化的响应模型[J]. 中国科学:D辑, 1999, 29(2): 185-192.]
[28] Jin Huijun, Li Shuxun, Wang Shaoling, et al.Impacts of climatic change on permafrost and cold regions environments in China[J]. Acta Geographica Sinica, 2000, 55(2): 161-173.
[金会军, 李述训,王绍令, 等. 气候变化对中国多年冻土和寒区环境的影响[J]. 地理学报, 2000, 55(2): 161-173.]
[29] Jian N.A simulation of biomes on the Tibetan Plateau and their responses to global climate change[J]. Mountain Research and Development, 2002, 20(1): 80-89.
[30] Nan Zhuotong, Li Shuxun, Liu Yongzhi.Mean annual ground temperature distribution on the Tibetan Plateau: Permafrost distribution mapping and further application[J]. Journal of Glaciology and Geocryology, 2002, 24(2): 142-148.
[南卓铜, 李述训, 刘永智. 基于年平均地温的青藏高原冻土分布制图及应用[J]. 冰川冻土, 2002, 24(2): 142-148.]
[31] Nan Zhuotong, Li Shuxun, Cheng Guodong.Prediction of permafrost distribution on the Qinghai-Tibetan Plateau in the next 50 and 100 years[J]. Science in China (Series D), 2005, 48(6):797-804.
[32] Wu Qingbai, Lu Zijian, Liu Yongzhi.Permafrost monitoring and its recent changes in Qinghai-Tibet Plateau[J]. Advances in Climate Change Research, 2005, 1(1): 26-28.
[吴青柏, 陆子建, 刘永智. 青藏高原多年冻土监测及近期变化[J]. 气候变化研究进展,2005, 1(1): 26-28.]
[33] Jin Huijun, Yu Shaopeng, Lü Lanzhi, et al. Degradation of permafrost in the Da and Xiao Hinggan Mountains, Northeast China, and preliminary assessment of its trend[J]. Journal of Glaciology and Geocryology, 2006, 28(4):467-476.
[金会军, 于少鹏, 吕兰芝, 等. 大小兴安岭多年冻土退化及其趋势初步评估[J]. 冰川冻土,2006, 28(4):467-476.]
[34] Luo Dongliang, Jin Huijun, Lin Lin, et al.Degradation of permafrost and cold-environments on the interior and eastern Qinghai Plateau[J]. Journal of Glaciology and Geocryology, 2012, 34(3):538-546.
[罗栋梁, 金会军, 林林, 等. 青海高原中、东部多年冻土及寒区环境退化[J]. 冰川冻土,2012, 34(3):538-546.]
[35] Zhang Zhongqiong, Wu Qingbai. Predicting changes of active layer thickness on the Qinghai-Tibet Plateau as climate warming[J]. Journal of Glaciology and Geocryology, 2012, 34(3): 505-511.
[张中琼, 吴青柏. 气候变化情景下青藏高原多年冻土活动层厚度变化预测[J]. 冰川冻土, 2012, 34(3): 505-511.]
[36] Wu Qingbai, Niu Fujun.Permafrost changes and engineering stability in Qinghai-Xizang Plateau[J]. Chinese Science Bulletin, 2013, 58(2):115-130.
[吴青柏, 牛富俊. 青藏高原多年冻土变化与工程稳定性[J]. 科学通报, 2013, 58(2):115-130.]
[37] Ren Guoyu.Climate change and the engineering projects of the Qinghai-Tibet Plateau[J]. Engineering Science, 2012, 14(9):84-95.
[任国玉. 气候变化与青藏高原工程设计[J]. 中国工程科学,2012, 14(9):84-95.]
[38] Zhao Lin, Ding Yongjian, Liu Guangyue, et al.Estimates of the reserves of ground ice in permafrost regions on the Tibetan Plateau[J]. Journal of Glaciology and Geocryology, 2010, 32(1): 1-9.
[赵林,丁永建,刘广岳, 等. 青藏高原多年冻土层中地下冰储量估算及评价[J]. 冰川冻土,2010, 32(1): 1-9.]
[39] Wang Genxu, Li Yuanshou, Wu Qingbai, et al.Impacts of permafrost changes on alpine ecosystem in Qinghai-Tibet Plateau[J]. Science in China(Series D), 2006, 36(8):743-754.
[王根绪,李元寿,吴青柏,等. 青藏高原冻土区冻土与植被的关系及其对高寒生态系统的影响[J]. 中国科学:D辑,2006,36(8):743-754.]
[40] Zhao Yonghua, Du Erji, Liu Guangyue, et al. Study of soil methane production rate from marsh meadow in permafrost regions on Tibetan Plateau[J]. Journal of Glaciology and Geocryology, 2011, 33(5): 999-1 005.
[赵拥华,杜二计, 刘广岳, 等. 青藏高原多年冻土区沼泽草甸土壤CH4产生速率研究[J]. 冰川冻土,2011, 33(5): 999-1 005.]
[41] Li Lin, Wang Zhenyu, Xu Weixin, et al.Response of growth of typical plateau meadow on Tibetan Plateau to climate change[J]. Journal of Glaciology and Geocryology,2011, 33(5): 1 006-1 013.
[李林, 王振宇, 徐维新, 等. 青藏高原典型高寒草甸植被生长发育对气候和冻土环境变化的响应[J]. 冰川冻土,2011, 33(5): 1 006-1 013.]
[42] Zhang Zhongqiong,Wu Qingbai. Freeze-thaw hazard zonation and climate change in Qinghai-Tibet Plateau permafrost[J]. Nat Hazards, 2012, 61:403-423.
[43] Zhang Zhongqiong, Wu Qingbai.Thermal hazards prediction on Qinghai-Tibet Plateau permafrost region[J]. Journal of Jilin University(Earth Science Edition), 2012, 42(2):454-461.
[张中琼,吴青柏. 青藏高原多年冻土热融灾害发展预测[J]. 吉林大学学报:地球科学版, 2012, 42(2):454-461.]
[44] Reid W V, Bréchignac C, Lee Y. Earth system research priorities[J]. Science,2009, 325(5 938): 245.
[45] Reid W V, Chen D, Goldfarb L, et al.Earth system science for global sustainability: Grand challenges[J]. Science, 2010, 330:916-917.
[46] Futurearth Research for Global Sustainability[EB/OL].(2014-03-07)[2014-09-20].
URL    
[47] Yang Jianping, Zhang Tingjun.An overview of cryospheric vulnerability and its assessment methods in China[J]. Journal of Glaciology and Geocryology, 2010, 32(6): 1 084-1 096.
[杨建平,张廷军. 我国冰冻圈及其变化的脆弱性与评估方法[J]. 冰川冻土, 2010, 32(6): 1 084-1 096.]
[48] Fang Y P, Qin D H, Ding Y J.Frozen soil change and adaptation of animal husbandry: A case of the source regions of Yangtze and Yellow Rivers[J]. Environmental Science & Policy, 2011, 14(5):555-568.
[49] Biagini B, Bierbaum R, Stults M, et al.A typology of adaptation actions: A global look at climate adaptation actions financed through the global environment facility[J]. Global Environmental Change, 2014, 25:97-108.
[50] Yang Jianping, Li Man, Yang Suiqiao, et al.Vulnerability of the glaciers to climate change in China:Current situation and evaluation[J].Journal of Glaciology and Geocryology, 2013,35(5):1 077-1 087.
[杨建平,李曼,杨岁桥,等.中国冰川脆弱性现状评价与未来预估[J].冰川冻土,2013,35(5):1 077-1 087.]
[51] Yang Jianping, Yang Suiqiao, Li Man, et al.Vulnerbaility of frozen ground to climate change in China[J]. Journal of Glaciology and Geocryology, 2013, 35(6):1 436-1 445.
[杨建平,杨岁桥,李曼,等. 中国冻土对气候变化的脆弱性[J].冰川冻土,2013,35(6):1 436-1 445.]
[52] Sun Xike, Zhou Lihua, Ma Yonghuan, et al.The adaptive countermeasures against permafrost degradation in Northeast China[J]. Journal of Glaciology and Geocryology, 2009, 31(3):532-539.
[孙希科,周立华,马永欢,等. 我国东北地区多年冻土退化情景下的适应对策[J]. 冰川冻土, 2009, 31(3):532-539.]
[53] Fang Yiping, Qin Dahe, Ding Yongjian.Frozen soil change and adaptation of animal husbandry: A case of the source regions of Yangtze and Yellow rivers[J]. Environmental Science & Policy, 2011, doi:10.1016/j.envsci.2011.03.012.
[54] Fang Yiping, Qin Dahe, Ding Yongjian, et al.Adaptation management of mountain tourism service: The case of the source regions of the Yangtze and Yellow rivers[J]. Journal of Mountain Science, 2009, 6(3):299-310.
[55] Deng Maozhi, Liu Shoudong, Zhang Hongguang, et al.A variance analysis of perception on climate change and cryosphere change of different residents in Inland River Basin of arid regions—Taking the Rümqi River Basin as an example[J]. Journal of Glaciology and Geocryology, 2011, 33(5):1 074-1 080.
[邓茂芝, 刘寿东, 张宏广, 等. 干旱区内陆河流域不同特征居民对气候变化及冰冻圈变化的感知差异分析——以乌鲁木齐河流域为例[J]. 冰川冻土, 2011, 33(5):1 074-1 080.]
[56] Yang Suiqiao, Yang Jianping, Wang Shijin, et al.Adaptive capacity evaluation of ecological-economic system to cryospheric change—A case study in the Mount Yulong[J]. Journal of Glaciology and Geocryology, 2012, 34(2):485-493.
[杨岁桥, 杨建平, 王世金, 等. 生态—经济系统对冰冻圈变化的适应能力评价——以玉龙雪山地区为例[J].冰川冻土, 2012, 34(2):485-493.]
[57] He Yong, Wu Yongfeng, Liu Qiufeng.Vulnerability assessment of areas affected by Chinese cryospheric changes in future climate change scenarios[J]. Chinese Science Bulletin, 2012, 57(36):4 784-4 790.
[58] IPCC. Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation:A Special Report of Working Groups I and II of the Intergovemmental Panel on Climate Change[M].Cambridge and New York: Cambridge University Press, 2012.
[1] 原世伟, 李新, 杜二虎. 多主体建模在水资源管理中的应用:进展与展望[J]. 地球科学进展, 2021, 36(9): 899-910.
[2] 韦进, 申重阳, 胡敏章, 江颖, 张晓彤, 刘子维. 连续重力观测站测定的中国大陆潮汐因子空间分布特征[J]. 地球科学进展, 2021, 36(5): 490-499.
[3] 李耀辉, 孟宪红, 张宏升, 李忆平, 王闪闪, 沙莎, 莫绍青. 青藏高原—沙漠的陆—气耦合及对干旱影响的进展及其关键科学问题[J]. 地球科学进展, 2021, 36(3): 265-275.
[4] 崔林丽, 史军, 杜华强. 植被物候的遥感提取及其影响因素研究进展[J]. 地球科学进展, 2021, 36(1): 9-16.
[5] 刘秦玉,张苏平,贾英来. 冬季黑潮延伸体海域海洋涡旋影响局地大气强对流的研究[J]. 地球科学进展, 2020, 35(5): 441-451.
[6] 苗毅, 刘海猛, 宋金平, 戴特奇. 青藏高原交通设施建设及影响评价研究进展[J]. 地球科学进展, 2020, 35(3): 308-318.
[7] 童磊,郑珂,苏飞. 生计脆弱性概念、分析框架与评价方法[J]. 地球科学进展, 2020, 35(2): 209-217.
[8] 康世昌, 郭万钦, 吴通华, 钟歆玥, 陈仁升, 许民, 陈金雷, 杨瑞敏. “一带一路”区域冰冻圈变化及其对水资源的影响[J]. 地球科学进展, 2020, 35(1): 1-17.
[9] 谢彦君, 任福民, 李国平, 王铭杨, 杨慧. 影响中国双台风活动气候特征研究[J]. 地球科学进展, 2020, 35(1): 101-108.
[10] 罗鑫玥,陈明星. 城镇化对气候变化影响的研究进展[J]. 地球科学进展, 2019, 34(9): 984-997.
[11] 王坚红,张萌,任淑媛,王兴,苗春生. 太行山脉地形坡度对下山锋面气旋暴雨影响模拟研究[J]. 地球科学进展, 2019, 34(7): 717-730.
[12] 杨慧,任福民,杨明仁. 不同强度热带气旋对中国降水变化的影响[J]. 地球科学进展, 2019, 34(7): 747-756.
[13] 刘小茜,裴韬,舒华,高锡章. 基于文献计量学的社会—生态系统恢复力研究进展[J]. 地球科学进展, 2019, 34(7): 765-777.
[14] 宁晓菊,张丽君,秦耀辰,刘凯. 60年来我国主要粮食作物适宜生长区的时空分布[J]. 地球科学进展, 2019, 34(2): 191-201.
[15] 孟宪萌,张鹏举,周宏,刘登峰. 水系结构分形特征的研究进展[J]. 地球科学进展, 2019, 34(1): 48-56.
阅读次数
全文


摘要