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Bulletin of Chinese Academy of Sciences (Chinese Version)

Authors

MA Zhuguo, Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; University of Chinese Academy of Sciences, Beijing 100049, China
FU Congbin, Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; University of Chinese Academy of Sciences, Beijing 100049, China; Nanjing University, Nanjing 210093, China
ZHOU Tianjun, Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
YAN Zhongwei, Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; University of Chinese Academy of Sciences, Beijing 100049, China
LI Mingxing, Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
ZHENG Ziyan, Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
CHEN Liang, Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
LV Meixia, Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China

Keywords

the Yellow River Basin; warming and drying climate; decreased streamflow; human water use

Document Type

Article

Abstract

The Yellow River is known as China's Mother River, which fosters the great and profound Chinese civilization. However, the frequent flood and drought disasters have also brought serious disasters to the people who live in the Yellow River Basin. At present, significant changes have taken place in the climate and hydrological processes of the Yellow River Basin due to global warming and human activities. The warming and drying climate and increase of human water use in the Yellow River Basin have led to an increase in hydrological drought. Although the Grain for Green program has greatly improved the vegetation coverage on the Loess Plateau and effectively inhibited severe soil erosion, but also enhanced the soil desiccation and enlarged the dry soil layers in this area. These phenomena are not only the major challenges for ecological protection and high-quality development in the Yellow River Basin, but also the basic scientific issues which related to the coordinated development of climate-water-ecology-society.

First page

52

Last Page

60

Language

Chinese

Publisher

Bulletin of Chinese Academy of Sciences

References

习近平.在黄河流域生态保护和高质量发展座谈会上的讲话.求是, 2019, (20):1-5.

夏军, 彭少明, 王超, 等.气候变化对黄河水资源的影响及其适应性管理.人民黄河, 2014, 36(10):1-15.

刘昌明, 田巍, 刘小莽, 等.黄河近百年径流量变化分析与认识.人民黄河, 2019, 41(10):11-15.

张建云, 贺瑞敏, 齐晶, 等.关于中国北方水资源问题的再认识.水科学进展, 2013, 24(3):303-310.

马柱国.黄河径流量的历史演变规律及成因.地球物理学报, 2005, 48(6):1270-1275.

Lv M X, Ma Z G, Lv M Z. Effects of climate/land surface changes on streamflow with consideration of precipitation intensity and catchment characteristics in the Yellow River Basin. Journal of Geophysical Research-Atmospheres, 2018, 123:1942-1958.

Lv M X, Ma Z G, Li M X, et al. Quantitative analysis of terrestrial water storage changes under the Grain for Green program in the Yellow River basin. Journal of Geophysical Research-Atmospheres, 2019, 124:1336-1351.

Lv M X, Ma Z G, Chen L, et al. Evapotranspiration reconstruction based on land surface models and observed water budget components while considering irrigation. Journal of Hydrometeorology, 2019, 20:2161-2183.

Chen L, Ma Z G, Zhao T B, et al. Simulation of the regional climatic effect of irrigation over the Yellow River Basin. Atmospheric and Oceanic Science Letters, 2017, 10(4):291-297.

傅伯杰, 邱扬, 王军, 等.黄土丘陵小流域土地利用变化对水土流失的影响.地理学报, 2002, 57(6):717-722.

Sun G, Zhou G Y, Zhang Z Q, et al. Potential water yield reduction due to forestation across China. Journal of Hydrology, 2006, 328:548-558.

Sorooshian S, AghaKouchak A, Li J L. Influence of irrigation on land hydrological processes over California. Journal of Geophysical Research-Atmospheres, 2014, 119(23):13137-13152.

Lan C, Zhang Y X, Gao Y H, et al. The impacts of climate change and land cover/use transition on the hydrology in the upper Yellow River Basin, China. Journal of Hydrology, 2013, 502:37-52.

López-M J I, J Zabalza, S M Vicente-Serrano, et al. Impact of climate and land use change on water availability and reservoir management:Scenarios in the Upper Aragón River, Spanish Pyrenees. Science of the Total Environment, 2014, 493:1222-1231.

Nie W M, Yuan Y P, W Kepner, et al. Assessing impacts of Landuse and Landcover changes on hydrology for the upper San Pedro watershed. Journal of Hydrology, 2011, 407:105-114.

Wang R Y, L Kalin, Kuang W H, et al. Individual and combined effects of land use/cover and climate change on Wolf Bay watershed streamflow in southern Alabama. Hydrological Processes, 2014, 28:5530-5546.

Hu Z D, Wang L, Wang Z J, et al. Quantitative assessment of climate and human impacts on surface water resources in a typical semi-arid watershed in the middle reaches of the Yellow River from 1985 to 2006. International Journal of Climatology, 2015, 35:97-113.

Wang J H, Hong Y, Gourley J, et al. Quantitative assessment of climate change and human impacts on long-term hydrologic response:a case study in a sub-basin of the Yellow River, China. International Journal of Climatology, 2010, 30:2130-2137.

Tadanobu N. Simulation of the effect of irrigation on the hydrologic cycle in the highly cultivated Yellow River Basin. Agricultural and Forest Meteorology, 2011, 151:314-327.

Li L, Shen H Y, Dai S, et al. Response of runoff to climate change and its future tendency in the source region of Yellow River. Journal of Geographical Sciences, 2012, 22(3):431-440.

李晓宇, 刘晓燕, 李焯.黄河主要产沙区近年降雨及下垫面变化对入黄沙量的影响.水利学报, 2016, 47(10):1253-1268.

Wang S, Fu B J, Piao S L, et al. Reduced sediment transport in the Yellow River due to anthropogenic changes. Nature Geoscience, 2016, 9(1):38-41.

Chen Y P, Wang K B, Lin Y S, et al. Balancing green and grain trade. Nature Geoscience, 2015, 8:739-741.

Jia X X, Shao M G, Zhu Y J, et al. Soil moisture decline due to afforestation across the Loess Plateau, China. Journal of Hydrology, 2017, 546:113-122.

谢昌卫, 丁永建, 韩海东, 等.黄河源区径流波动变化对气候要素的响应特征.干旱区资源与环境, 2006, 20(4):7-11.

杨建平, 丁永建, 陈仁升, 等.长江黄河源区多年冻土变化及其生态环境效应.山地学报, 2004, 22(3):278-285.

蓝永超, 朱云通, 刘根生, 等.黄河源区气候变化的季节特征与区域差异研究.冰川冻土, 2016, 38(3):741-749.

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