[1]冯椰林,贺中华,焦树林,等.基于CMIP6气候模式的贵州省极端降水情景预估[J].水土保持研究,2023,30(01):282-290.[doi:10.13869/j.cnki.rswc.20220621.004]
 FENG Yelin,HE Zhonghua,JIAO Shulin,et al.Scenario Prediction of Extreme Precipitation in Guizhou Province Based on CMIP6 Climate Model[J].Research of Soil and Water Conservation,2023,30(01):282-290.[doi:10.13869/j.cnki.rswc.20220621.004]
点击复制

基于CMIP6气候模式的贵州省极端降水情景预估

参考文献/References:

[1] Huang J, Zhang G, Zhang Y, et al. Global desertification vulnerability to climate change and human activities[J]. Land Degradation & Development, 2020,31(11):1380-1391.
[2] Munich Reinsurance Company. Topics Geo, Natural Catastrophes 2009:Analysis, Assessment, Positions [R]. Munich, Germany, 2010.
[3] Allen M R, Ingram W J. Constraints on future changes in climate and the hydrologic cycle[J]. Nature, 2002,419(6903):224-232.
[4] Zhang Q, Li J, Singh V P, et al. Spatio-temporal relations between temperature and precipitation regimes: Implications for temperature-induced changes in the hydrological cycle[J]. Global and Planetary Change, 2013,111:57-76.
[5] 王少平,姜逢清,吴小波,等.1961—2010年西北干旱区极端降水指数的时空变化分析[J].冰川冻土,2014,36(2):318-326.
[6] 任正果,张明军,王圣杰,等.1961—2011年中国南方地区极端降水事件变化[J].地理学报,2014,69(5):640-649.
[7] 顾西辉,张强,孔冬冬.中国极端降水事件时空特征及其对夏季温度响应[J].地理学报,2016,71(5):718-730.
[8] 岳溪柳,黄玫,徐庆勇,等.贵州省喀斯特地区泥石流灾害易发性评价[J].地球信息科学学报,2015,17(11):1395-1403.
[9] 张克新,王娟娟,彭娇婷,等.贵州省降水集散程度时空变化及其影响因素分析[J].贵州师范大学学报:自然科学版,2020,38(2):10-18.
[10] 周超,常鸣,徐璐,等.贵州省典型城镇矿山地质灾害风险评价[J].武汉大学学报:信息科学版,2020,45(11):1782-1791.
[11] 龙万学,谭勇鸿,林剑.基于GIS的贵州省地质灾害危险性评价[J].地理空间信息,2009,7(6):24-27.
[12] 周天军,邹立维,陈晓龙.第六次国际耦合模式比较计划(CMIP6)评述[J].气候变化研究进展,2019,15(5):445-456.
[13] Pu Y, Liu H B, Yan R J, et al. CAS FGOALS-g3 Model Datasets for the CMIP6 Scenario Model Intercomparison Project(ScenarioMIP)[J]. Advances in Atmospheric Sciences, 2020,37(10):1081-1092.
[14] Eyring V, Bony S, Meehl G A, et al. Overview of the Coupled Model Intercomparison Project Phase 6(CMIP6)experimental design and organization[J]. Geoscientific Model Development, 2016,9(5):1937-1958.
[15] 胡一阳,徐影,李金建,等.CMIP6不同分辨率全球气候模式对中国降水模拟能力评估[J].气候变化研究进展,2021,17(6):730-743.
[16] 黄禄丰,朱再春,黄萌田,等.基于CMIP6模式优化集合平均预估21世纪全球陆地生态系统总初级生产力变化[J].气候变化研究进展,2021,17(5):514-524.
[17] Maurer E P, Wood A W, Adam J C, et al. A long-term hydrologically based dataset of land surface fluxes and states for the conterminous United States[J]. Journal of Climate, 2002,15(22):3237-3251.
[18] Ning L, Bradley R S. Snow occurrence changes over the central and eastern United States under future warming scenarios[J]. Scientific Reports, 2015,5(1):17073.
[19] Wood A W, Maurer E P, Kumar A, et al. Long-range experimental hydrologic forecasting for the eastern United States[J]. Journal of Geophysical Research-Atmospheres, 2002,107(D20):6-15.
[20] Maurer E P, Wood A W, Adam J C, et al. A long-term hydrologically based dataset of land surface fluxes and states for the conterminous United States[J]. Journal of Climate, 2002,15(22):3237-3251.
[21] 关颖慧.长江流域极端气候变化及其未来趋势预测[D].陕西杨凌:西北农林科技大学,2015.
[22] King A D, Alexandera L V, Donata M G. The efficacy of using gridded data to examine extreme rainfall characteristics: A case study for Australia[J]. International Journal of Climatology, 2013,33(10):2376-2387.
[23] Zolina O, Kapala A, Simmer C, et al. Analysis of extreme precipitation over Europe from different reanalyses:A comparative assessment[J]. Global and Planetary Change, 2004,44:129-161.
[24] Swain, S., Hayhoe, K. CMIP5 projected changes in spring and summer drought and wet conditions over North America[J]. Climate Dynamics, 2015,44:2737-2750.
[25] Park C K, Byun H R, Deo R et al. Drought prediction till 2100 under RCP 8.5 climate change scenarios for Korea[J]. Journal of Hydrology, 2015,526:221-230.
[26] 雷享勇,高路,马苗苗,等.鄱阳湖流域极端降水时空分布和非平稳性特征[J].应用生态学报,2021,32(9):3277-3287.
[27] 唐明秀,孙劭,朱秀芳,等.基于CMIP6的中国未来暴雨危险性变化评估[J].地球科学进展,2022,37(5):519-534.
[28] 徐晓明,张雪芹.1961—2019年深圳市极端降水变化[J].自然灾害学报,2021,30(3):43-51.
[29] 许玉凤,陈宸,黄娟.贵州省无雨日和最长连续无雨日数时空分布特征[J].人民珠江,2019,40(4):59-64,81.
[30] 韩会庆,张娇艳,苏志华,等.2011—2050年贵州省极端气候指数时空变化特征[J].水土保持研究,2018,25(2):341-346.

相似文献/References:

[1]柴素盈,曹 言,窦小东,等.1964-2017年南盘江流域主要极端气候事件时空演变特征[J].水土保持研究,2020,27(01):151.
 CHAI Suying,CAO Yan,DOU Xiaodong,et al.Analysis Temporal and Spatial Changes of Extreme Climatic Events in Nanpan River Basin from 1964 to 2017[J].Research of Soil and Water Conservation,2020,27(01):151.
[2]肖薇薇,安 彬,贾 丹.1955—2017年安康市极端气候事件时序变化特征[J].水土保持研究,2021,28(05):212.
 XIAO Weiwei,AN Bin,JIA Dan.Temporal Variation Characteristics of Extreme Weather Events in Ankang from 1955 to 2017[J].Research of Soil and Water Conservation,2021,28(01):212.
[3]慎璐璐,杨艳芬,吴 晶,等.黄河流域极端气候事件时空变化规律[J].水土保持研究,2022,29(02):231.
 SHEN Lulu,YANG Yanfen,WU Jing,et al.Spatial and Temporal Variation Characteristics of Extreme Climate Events in the Yellow River Basin[J].Research of Soil and Water Conservation,2022,29(01):231.
[4]张海宁,周 旗,毛雨唯,等.渭河流域极端降水特性指标分析[J].水土保持研究,2022,29(03):128.
 ZHANG Haining,ZHOU Qi,MAO Yuwei,et al.Analysis of Extreme Precipitation Characteristics in Weihe River Basin[J].Research of Soil and Water Conservation,2022,29(01):128.
[5]刘 敏,厉 悦,何 冰,等.青藏高原草地植被秋季物候动态及其对极端降水的敏感性分析[J].水土保持研究,2023,30(03):353.[doi:10.13869/j.cnki.rswc.2023.03.050]
 LIU Min,LI Yue,HE Bing,et al.Spatiotemporal Dynamics of Grassland Phenology and Sensitivity to Extreme Precipitation in Autumn in Qinghai-Tibetan Plateau[J].Research of Soil and Water Conservation,2023,30(01):353.[doi:10.13869/j.cnki.rswc.2023.03.050]
[6]豆明玉,段克勤,石培宏,等.基于CMIP6多模式的黄土高原气温变化模拟评估及情景预估[J].水土保持研究,2024,31(02):158.
 Dou Mingyu,Duan Keqin,Shi Peihong,et al.Historical Evaluation and Scenario Prediction of Temperature Changes the Loess Plateau Based on CMIP6 Multimodels[J].Research of Soil and Water Conservation,2024,31(01):158.

备注/Memo

收稿日期:2021-10-11 修回日期:2021-10-24
资助项目:国家自然科学基金(u1612441); 国家自然科学基金(41471032); 贵州省水利厅自然科研基金(KT201402)
第一作者:冯椰林(1998—),男(苗族),重庆彭水人,硕士研究生,研究方向:喀斯特水文水资源与遥感。E-mail:1329032804@qq.com
通信作者:贺中华(1976—),男,贵州兴义人,博士,教授,研究方向:喀斯特水文水资源与遥感研究。E-mail:zhonghuahe@gznu.edu.cn

更新日期/Last Update: 2023-01-10