Articles | Volume 383
https://doi.org/10.5194/piahs-383-327-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/piahs-383-327-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Water replenishment for ecological flow with E-WAS framework: a case study of the Longgang River Basin, Shenzhen, China
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China
Zuhao Zhou
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China
Xuefeng Sang
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China
Hao Wang
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China
Yangwen Jia
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China
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Xudong Zheng, Dengfeng Liu, Shengzhi Huang, Hao Wang, and Xianmeng Meng
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2024-230, https://doi.org/10.5194/hess-2024-230, 2024
Revised manuscript under review for HESS
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Water budget non-closure is a widespread phenomenon among multisource datasets, which undermines the robustness of hydrological inferences. This study proposes a Multisource Datasets Correction Framework grounded in Physical Hydrological Processes Modelling to enhance water budget closure, called PHPM-MDCF. We examined the efficiency and robustness of the framework using the CAMELS dataset, and achieved an average reduction of 49 % in total water budget residuals across 475 CONUS basins.
Pengxiang Wang, Zuhao Zhou, Jiajia Liu, Chongyu Xu, Kang Wang, Yangli Liu, Jia Li, Yuqing Li, Yangwen Jia, and Hao Wang
Hydrol. Earth Syst. Sci., 27, 2681–2701, https://doi.org/10.5194/hess-27-2681-2023, https://doi.org/10.5194/hess-27-2681-2023, 2023
Short summary
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Considering the impact of the special geological and climatic conditions of the Qinghai–Tibet Plateau on the hydrological cycle, this study established the WEP-QTP hydrological model. The snow cover and gravel layers affected the temporal and spatial changes in frozen soil and improved the regulation of groundwater on the flow process. Ignoring he influence of special underlying surface conditions has a great impact on the hydrological forecast and water resource utilization in this area.
Pengxiang Wang, Zuhao Zhou, Jiajia Liu, Chongyu Xu, Kang Wang, Yangli Liu, Jia Li, Yuqing Li, Yangwen Jia, and Hao Wang
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2021-538, https://doi.org/10.5194/hess-2021-538, 2021
Manuscript not accepted for further review
Short summary
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Combining the geological characteristics of the thin soil layer on the thick gravel layer and the climate characteristics of the long-term snow cover of the Qinghai-Tibet Plateau, the WEP-QTP hydrological model was constructed by dividing a single soil structure into soil and gravel. In contrast to the general cold area, the special environment of the Qinghai–Tibet Plateau affects the hydrothermal transport process, which can not be ignored in hydrological forecast and water resource assessment.
Yong Jing and Zuhao Zhou
Proc. IAHS, 383, 111–119, https://doi.org/10.5194/piahs-383-111-2020, https://doi.org/10.5194/piahs-383-111-2020, 2020
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Using 1956~2012 years of river runoff series data of 27 rivers in hilly gully area of Loess Plateau in Shaanxi province 39 hydrological station data, reduction of social and economic water consumption, plotting the annual precipitation and annual runoff double cumulative curve of annual runoff flow series consistency test, the consistency processing of annual runoff data and the quantitative analysis of its influence were also made.
Jingwen Zhang, Ximing Cai, Xiaohui Lei, Pan Liu, and Hao Wang
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2020-304, https://doi.org/10.5194/hess-2020-304, 2020
Preprint withdrawn
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Real-time reservoir flood control operation is controlled manually by reservoir operators based on their experiences and justifications, rather than by computer automatically. We use a human-machine interactive modeling method to combine computer optimization model, human’s consideration, and reservoir stage observations for actual decisions on release for real-time reservoir flood control operation. The proposed method can reduce the flood risk and improve water use benefit simultaneously.
Denghua Yan, Baisha Weng, Tianling Qin, Hao Wang, Xiangnan Li, Yuheng Yang, Kun Wang, Zhenyu Lv, Jianwei Wang, Meng Li, Shan He, Fang Liu, Shanshan Liu, Wuxia Bi, Ting Xu, Xiaoqing Shi, Zihao Man, Congwu Sun, Meiyu Liu, Mengke Wang, Yinghou Huang, Haoyu Long, Yongzhen Niu, Batsuren Dorjsuren, Mohammed Gedefaw, Abel Girma, and Asaminew Abiyu
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2019-224, https://doi.org/10.5194/essd-2019-224, 2020
Publication in ESSD not foreseen
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This paper provides a complete data set of global water withdrawal. There is almost no continuous long series of water withdrawal data globally. Moreover, most of the data released by international organizations is based on national scale and lacks finer regional data. Therefore, appropriate methods are needed to modify the data. This dataset has important practical significance in promoting the harmonious and sustainable development of economy and resources of the world.
Mengtian Lu, Pieter Hazenberg, Xiaohui Lei, and Hao Wang
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2019-356, https://doi.org/10.5194/hess-2019-356, 2019
Revised manuscript not accepted
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Using a newly developed identification procedure, this work identifies the occurrence and duration of observed hydrological extremes (drought and wet spells) within the semi-arid San Pedro basin that experiences a yearly precipitation season. Results, shows that the summertime North American Monsoon a start and reset button, with very few extremes lasting multiple years, and duration dependent on the time until the following monsoon.
Wuxia Bi, Baisha Weng, Denghua Yan, Meng Li, Zhilei Yu, Lin Wang, and Hao Wang
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2019-185, https://doi.org/10.5194/hess-2019-185, 2019
Preprint withdrawn
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This study focuses on solving the
land useand
water usecompetitions between lake-marsh wetland system and its surrounding socio-economic system, also inside the system. An optimal lake-marsh pattern determination method was proposed on considering the ecological services values and water shortage amount. We explored the optimal lake-marsh pattern in both annual and monthly scales. This study could provide references for the ecological spatial management and ecological water control.
Chao Mei, Jiahong Liu, Hao Wang, Weiwei Shao, Lin Xia, Chenyao Xiang, and Jinjun Zhou
Proc. IAHS, 379, 223–229, https://doi.org/10.5194/piahs-379-223-2018, https://doi.org/10.5194/piahs-379-223-2018, 2018
Tingting Wang, Fubao Sun, Hong Wang, Wenbin Liu, and Hao Wang
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2017-151, https://doi.org/10.5194/hess-2017-151, 2017
Revised manuscript not accepted
Short summary
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Accurate estimation of annual evapotranspiration (ET) in humid catchments remains a huge challenge and there is no well accepted explanation so far. We compare the estimated ET and ET + ΔS against ETwb with assumption that annual ΔS is zero, and find that much improvement has been made in ET + S. This provides an acceptable explanation for the poorly annual ET estimation and highlight that the annual ΔS shouldn't be taken as zero in water balance equation in humid catchments.
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