[1] 周幼吾,郭东信,邱国庆,等. 中国冻土[M]. 北京:科学出版社, 2000. [Zhou Y W,Guo D X,Qiu G Q, et al . Geocryology in China[M].Beijing:Science Press,2000.] [2] Zhang T,Barry R G,Knowles K, et al . Statistics and chara-cteristics of permafrost and ground ice distribution in Northern Hemisphere[J]. Polar Geography ,1999,23(2):132-154. [3] 郭玲鹏,李兰海,徐俊荣,等. 天山巩乃斯河谷积雪深度及季节冻土温度对气温变化的响应[J]. 资源科学,2012,34(4):636-643. [Guo L P,Li L H,Xu J R, et al . Responses of snow depth and seasonal frozen ground temperature to enhances air temperature in Kunges Valley,Tianshan Mountains[J]. Resources Science ,2012,34(4):636-643.] [4] 王秋香,李红军,魏荣庆,等. 1961-2002年新疆季节冻土多年变化及突变分析[J]. 冰川冻土,2005,27(6):820-826. [Wang Q X,Li H J,Wei R Q, et al . Annual change and abrupt change of the seasonal frozen soil in Xinjiang,China during 1961- 2002[J]. Journal of Glaciology and Geocryology ,2005,27(6):820-826.] [5] 陈光宇,李栋梁. 东北及邻近地区累积积雪深度的时空变化规律[J]. 气象,2011,37(5):513-521. [Chen G Y,Li D L. Temporal-spatial characteristics of cumulative snow depth in northeast China and its vicinity[J]. Meteorological Monthly ,2011,37(5):513-521.] [6] 李玲萍,李岩瑛. 石羊河流域冬季冻土深度变化趋势及原因[J]. 土壤通报,2012,43(3):587-593. [Li L P,Li Y Y. Changing trend and reasons of winter maximum frozen soil depth in Shiyang River Basin[J]. Chinese Journal of Soil Science ,2012,43(3):587-593.] [7] 赵庆云,李栋梁,吴洪宝. 西北区东部近40年地面气温变化的分析[J]. 高原气象,2006,25(4):643-650. [Zhao Q Y,Li D L,Wu H B. Analyses on surface air temperature change in east part of northwest China in last 40years[J]. Plateau Meteorology ,2006,25(4):643-650.] [8] 王兴菊,许士国,李文义,等. 扎龙湿地季节性冻土冻融规律及其生态水文功能研究[J]. 大连理工大学学报,2008,48(6):897-903. [Wang X J,Xu S G,Li W Y, et al . Freezing-thawing rule of seasonal frozen soil and its eco-hydrological function in Zhalong Wetland[J]. Journal of Dalian University of Technology ,2008,48(6):897-903.] [9] 陈博,李建平. 近50年来中国季节性冻土与短时冻土的时空变化特征[J]. 大气科学,2008,32(3):432-443. [Wang B,Li J P. Characteristics of spatial and temporal variation of seasonal and short-term frozen soil in China in recent 50 years[J]. Chinese Journal of Atmospheric Sciences ,2008,32(3):432-443.] [10] 王澄海,董文杰,韦志刚. 青藏高原季节性冻土年际变化的异常特征[J]. 地理学报,2001,56(5):523-531. [Wang C H,Dong W J,Wei Z G. The feature of seasonal frozen soil in Qinghai-Tibet Plateau[J]. Acta Geographica Sinica ,2001,56(5):523-531.] [11] 高荣,董文杰,韦志刚. 青藏高原季节性冻土的时空分布特征[J]. 冰川冻土,2008,30(5):740-744. [Gao R,Dong W J,Wei Z G. The features of temporal and spatial distributions of seasonal frozen soil in the Tibetan Plateau[J]. Journal of Glaciology and Geocryology ,2008,30(5):740-743.] [12] 符传博,丹利,吴涧,等. 全球变暖背景下新疆地区近45A来最大冻土深度变化及其突变分析[J]. 冰川冻土,2013,35(6):1410-1418. [Fu C B,Dan L,Wu J, et al . Variation and abrupt change of maximum depth of frozen soil over Xinjiang under the background of global warming,1961-2000[J]. Journal of Glaciology and Geocryology ,2013,35(6):1410-1418.] [13] 张山清,普宗朝,李景林,等. 1961-2010年新疆季节性最大冻土深度对冬季负积温的响应[J]. 冰川冻土,2013,35(6):1419-1427. [Zhang S Q,Pu Z C,Li J L, et al . Response of the maximum depth of seasonal freezing to the Xinjiang[J]. Journal of Glaciology and Geocryology ,2013,35(6):1419-1427.] [14] 李海花,刘大锋,段淑芳,等. 新疆阿勒泰地区1963-2012年最大冻土深度的时空分布及其对气温变化的响应[J]. 干旱地区农业研究,2014,(5):251-258. [Li H H,Liu D F,Duan S F, et al . The spatial-temporal distribution change of maximum frozen soil depth and temperature change in Altay region of Xinjiang Province from 1963 to 2012[J]. Agricultural Research in the Arid Areas ,2014,(5):251-258.] [15] 郝振纯,王晓燕,侯艳茹,等. 黄河源区季节冻土最大冻结深度估算方法[J]. 水电能源科学,2013,(5):73-76. [Hao Z C,Wang X Y,Hou Y R, et al . Estimation method for maximum frozen depth of seasonal frozen soil in source region of the Yellow River[J]. Water Resources and Power ,2013,(5):73-76.] [16] 李忠辉,韦晓丽,王秀娟,等. 吉林省春季土壤温度及化冻深度研究[J]. 土壤通报,2016,(2):334-338. [Li Z H,Wei X L,Wang X J, et al . Study of soil temperature and thaw depth during spring in Jilin Province[J]. Chinese Journal of Soil Science ,2016,(2):334-338.] [17] 王学佳,杨梅学,万国宁. 藏北高原D105点土壤冻融状况与温湿特征分析[J]. 冰川冻土,2012,34(1):56-63. [Wang X J,Yang M X,Wan G N. Processes of soil thawing-freezing and features and moisture at D105 on the northern of ground tempera-ture Tibetan Plateau[J]. Journal of Glaciology and Geocryology ,2012,34(1):56-63.] [18] 付强,侯仁杰,王子龙,等. 冻融期积雪覆盖下土壤水热交互效应[J]. 农业工程学报,2015,(15):101-107. [Fu Q,Hou R J,Wang Z L, et al . Soil moisture thermal interaction effects under snow cover during freezing and thawing period[J]. Transactions of the Chinese Society of Agricultural Engineering ,2015,(15):101-107.] [19] 习阿幸,刘志辉,卢文君. 干旱区季节性冻土冻融状况及对融雪径流的影响[J]. 水土保持研究,2016,23(2):333-339. [Xi A X,Liu Z H,Lu W J. Processes of seasonal frozen soil freezing-thawing and impact on snowmelt runoff in arid area[J]. Research of Soil and Water Conservation ,2016,23(2):333-339.] [20] 赵显波,刘铁军,许士国,等. 季节冻土区黑土耕层土壤冻融过程及水分变化[J]. 冰川冻土,2015,37(1):233-240. [Zhao X B,Liu T J,Xu S G, et al . Freezing thawing process and soil moisture migration within the black soil plow layer in seasonally frozen ground regions[J]. Journal of Glaciology and Geocryology ,2015,37(1):233-240.] [21] 冯波,章光新,李峰平.松花江流域季节性气象干旱特征及风险区划研究[J]. 地理科学,2016,36(3):466-474. [Feng B,Zhang G X,Li F P. Characteristics of seasonal meteorological drought and risk regionalization in Songhua River Basin[J]. Scientia Geographica Sinica ,2016,36(3):466-474.] [22] 于敏. 松花江流域水环境管理系统[D]. 上海:同济大学,2008. [Yu M. Water Environment Management System of Songhua River Basin[D]. Shanghai:Tongji University,2008.] [23] 中国气象数据网[EB/OL].http//data.cma.cn. [China Meteoro-logical Data Network [EB/OL].http://cdc.cma.gov.cn.] [24] 寒区旱区科学数据中心[EB/OL]. http:// westdc.westgis.ac.cn.[ Cold and arid regions Science Data Center[EB/OL]. http:// westdc.westgis.ac.cn.] [25] 王喜峰,周祖昊,贾仰文,等. 几何插值法在大尺度长系列降雨插值中的比较和改进[J]. 水电能源科学,2010,28(12):1-3. [Wang X F,Zhou Z H,Jia Y W, et al . Comparison and improvement of geometry interpolation methods in rainfall interpolation with large-scale long-series data[J]. Water Resources and Power ,2010,28(12):1-3.] [26] 杨晓玲,马中华,马玉山,等. 石羊河流域季节性冻土的时空分布及对气温变化的响应[J]. 资源科学,2013,35(10):2104-2111. [Yang X L,Ma Z H,Ma Y S, et al . The spatial-temporal distribution state of seasonal frozen soil and responses to temper-ature change in the Shiyang River Basin[J]. Resources Science ,2013,35(10):2104-2111.] |