[1]LIU Le,YUE Dapeng,ZHAO Jingbo,et al.Flood Disasters and Climate Characteristics in Tang Dynasty in the Middle South of Loess Plateau in Shaanxi[J].Research of Soil and Water Conservation,2022,29(06):284-289,297.
Copy

Flood Disasters and Climate Characteristics in Tang Dynasty in the Middle South of Loess Plateau in Shaanxi

References:
[1] 郑景云,刘洋,郝志新,等.过去2000年气候变化的全球集成研究进展与展望[J].第四纪研究,2021,41(2):309-322,308.
[2] 胡畔,陈波,史培军.中国暴雨洪涝灾情时空格局及影响因素[J].地理学报,2021,76(5):1148-1162.
[3] 郑景云,郝志新,张学珍,等.中国东部过去2000年百年冷暖的旱涝格局[J].科学通报,2014,59(30):2964-2971.
[4] Hao Z X, Wu M W, Zheng J Y, et al. Patterns in data of extreme droughts/floods and harvest grades derived from historical documents in eastern China during 801—1910[J]. Climate of the Past, 2020,16(1):101-116.
[5] 叶建春,田以堂,匡尚富,等.中国水旱灾害防御公报2019[R].北京:中华人民共和国水利部,2019.
[6] Sánchez-García C, Schulte L, Carvalho F, et al. A 500-year flood history of the arid environments of southeastern Spain: The case of the Almanzora River[J]. Global and Planetary Change,2019,181:102987.
[7] Ota Y, Kawahata H, Sato T, et al. Flooding history of Lake Nakaumi, western Japan, inferred from sediment records spanning the past 700 years[J]. Journal of Quaternary Science, 2017,32(8),1063-1074.
[8] 何则,何元庆,王世金,等.基于历史文献的1470—2008年中国西北地区气候干湿序列分区重建[J].中国沙漠,2016,36(5):1278-1285.
[9] 刘威,杨煜达.过去600年中国西南地区极端旱涝事件的重建与分析[J].第四纪研究,2021,41(2):368-378.
[10] 赵景波,顾静,邵天杰.唐代渭河流域与泾河流域涝灾研究[J].自然灾害学报,2009,18(2):50-55.
[11] 靳俊芳,殷淑燕,王学佳.汉江上游北宋时期洪水事件的沉积记录和文献记录对比[J].山地学报,2016,34(3):266-273.
[12] Chen X Y, Quan Q, Zhang K, et al. Spatiotemporal characteristics and attribution of dry/wet conditions in the Weihe River Basin within a typical monsoon transition zone of East Asia over the recent 547 years[J]. Enviromental Modelling and Software, 2021,143:105116.
[13] 张强,岳平,张良,等.夏季风过渡区的陆-气相互作用:述评与展望[J].气象学报,2019,77(4):758-773.
[14] 陕西省地方志编纂委员会.陕西省志第五卷黄土高原志[M].西安:陕西人民出版社,1995.
[15] 李双双,孔锋,韩鹭,等.陕北黄土高原区极端降水时空变化特征及其影响因素[J].地理研究,2020,39(1):140-151.
[16] 葛全胜.中国历朝气候变化[M].北京:科学出版社,2011.
[17] 刘俊文.唐代水害史论[J].北京大学学报:哲学社会科学版,1988(2):50-56,64.
[18] 张德二.中国三千年气象记录总集[M].南京:江苏教育出版社,2013.
[19] 翟佑安.中国气象灾害大典·陕西卷[M].北京:气象出版社,2005.
[20] 袁祖亮.中国灾害通史·隋唐五代卷[M].郑州:郑州大学出版社,2008.
[21] 袁林.西北灾荒史[M].兰州:甘肃人民出版社,1994.
[22] 殷淑燕,徐潇悦,党群.陕西省明代水旱灾害与干湿特征[J].干旱区资源与环境,2020,34(1):115-122.
[23] Chen X B, Yin L R, Fan Y L, et al. Temporal evolution characteristics of PM2.5 concentration based on continuous wavelet transform[J]. Science of the Total Environment, 2020,699:134244.
[24] 郝志新,刘可邦,张学珍,等.地球系统模式CESM模拟的ENSO变率与中国东部降水格局[J].自然资源学报,2016,31(12):1984-1994.
[25] 马柱国,邵丽娟.中国北方近百年干湿变化与太平洋年代际振荡的关系[J].大气科学,2006,30(3):464-474.
[26] 韩健夫,杨煜达.过去千年黄土高原干湿变化和极端干旱事件与太平洋年代际振荡[J].中国历史地理论丛,2017,32(2):5-12.
[27] 铜川市地方志编纂委员会.铜川市志[M].西安:陕西师范大学出版社,1997.
[28] Zheng J Y, Wang W C, Ge Q S, et al. Precipitation variability and extreme events in eastern China during the past 1 500 years[J]. Terrestrial Atmospheric and Oceanic Sciences, 2006,17(3):579-592.
[29] 郑景云,文彦君,方修琦.过去2000年黄河中下游气候与土地覆被变化的若干特征[J].资源科学,2020,42(1):3-19.
[30] 李兆元,李莉,全小伟.西安地区(380—1983年)旱涝气候变化[J].地理研究,1988,7(4):64-69.
[31] 吴宏岐,党安荣.隋唐时期气候冷暖特征与气候波动[J].第四纪研究,1998(1):31-38.
[32] 费杰,侯甬坚,刘晓东,等.基于黄土高原南部地区历史文献记录的唐代气候冷暖波动特征研究[J].中国历史地理论丛,2001,16(4):75-82,129.
[33] Zhang H L, Zhang Q, Yue P, et al. Aridity over a semiarid zone in northern China and responses to the East Asian summer monsoon[J]. Journal of Geophysical Research: Atmospheres, 2016,121(23):13901-13918.
[34] 刘欢,潘威.黄土高原地区1766—1950年雨季开始时间及其对夏季风的响应[J].地球环境学报,2014,5(6):378-384.
[35] Zhang P Z, Cheng H, Edwards R L, et al. A test of climate, sun, and culture relationships from an 1 810-year Chinese cave record[J]. Science, 2008,322(5903):940-942.
Similar References:

Memo

-

Last Update: 2022-10-20

Online:10089       Total Traffic Statistics:27428403

Website Copyright: Research of Soil and Water Conservation Shaanxi ICP No.11014090-10
Tel: 029-87012705 Address: Editorial Department of Research of Soil and Water Conservation, No. 26, Xinong Road, Yangling, Shaanxi Postcode: 712100