Lake pulses driven by glacier melting and climate variability by Songtao Ai, Shoukat Ali Shah, Yi Cai, Jiajun Ling, Xinde Chu, Shijin Wang, Yuande Yang, Runchuan Ouyang, Jiachun An, Wolfgang Rack

“…Understanding glacier-fed hydrological systems is essential for predicting water availability and formulating climate adaptation strategies. …”
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L'eau et le développement durable : un couple en rupture sans gouvernance sociétale et coopération décentralisée by Bernard Guesnier

“…Hydrological cycle should be treated as a whole by societal governance, probably the only way which could guarantee the future of the couple water-sustainable development, with the participation of governments and citizens. …”
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Analysis of Variation Characteristics of the Annual Maximum Flood Flow of Main Streams in Guangdong Province by LIANG Yuanyuan

“…In order to understand the variation characteristics of the annual maximum flood flow at the main hydrological stations in Guangdong province and reduce the production,living,and ecological environment problems caused by floods,the annual maximum flood flow series from 1977 to 2014 at seven hydrological stations in Guangdong province,namely,Sanshui Station,Makou Station,Gaoyao Station,Shijiao Station,Boluo Station,Huazhou Station,and Chaoan Station,are studied.MK test and Pettitt test are used to carry out study or wavelet analysis on the characteristics of the trend,variability,and cycle changes of the annual maximum flood flow at typical stations in the main streams of Guangdong province.The results show that:① the annual maximum flood flow at Boluo Station and Chaoan Station decreases slightly,while that at the other five stations increases,with that at Shijiao Station and Sanshui Station rising significantly.② Four of the seven stations have variability,and they are Gaoyao Station (in 1991 and 1992),Shijiao Station (in 1992,2011,and 2012),Makou Station (in 1993),and Sanshui Station (in 1993),and the variability occurs more than once at Gaoyao and Shijiao stations.In terms of spatial and temporal distribution,the four stations with variability mostly belong to the Xijiang and Beijiang river systems in the 1980s,1990s,and the 21st century.③ Sanshui Station has two main cycles of 2~10 a and 20~30 a,and Makou Station has cycles of 2~9 a and 9~27 a.Gaoyao Station experiences a cycle of 4~10 a and 10~24 a,and Shijiao Station owns a cycle of 2~12 a and 12~20 a.Boluo Station has a cycle of 5~12 a and 12~24 a.In addition,Huazhou Station experiences three cycles of 3~7 a,7~18 a,and 18~26 a,and Chaoan Station experiences cycles of 3~10 a,10~14 a,and 14~23 a,respectively.…”
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Do peixe com farinha à macarronada com frango: uma análise das transformações na rede urbana no Alto Solimões pela perspectiva dos padrões alimentares. by Tatiana Schor, Moisés Augusto Tavares-Pinto, Francisco Carlos da Costa Avelino, Marina Lelis Ribeiro

“…This network is strongly defined by the hydrological cycle. This article brought new elements to the understanding of economic and alimentary dynamics in the tri-border Brazil-Peru-Colombia, looking at flows of food and local production and their importance in the supply of cities in the region. …”
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Ecological Water Level Determination and Safeguard Measures for Rivers in Northern Jiangsu Plain by WANG Zhenqi, FANG Hongyuan, XU Guangdong, ZHU Ye, WANG Chengjie

“…Effective methods of calculating the threshold of river ecological flow (water level) need to be employed to obtain measures of controlling the ecological state of rivers in a plain river network and to build a robust long-term mechanism of ecological flow control.The Zongliutang River in the river network area of Northern Jiangsu Plain is divided into upper,middle,and lower reaches according to its objective environment and its actual operation and management situation.Then,the controlling condition of the ecological water level of each reach is analyzed respectively.Considering the hydrological characteristics,hydrodynamic characteristics,and observed hydrological data conditions of rivers in this river network area,several methods are utilized to calculate the ecological water level threshold of the middle reach of the river respectively.Those methods include the annual minimum water level method with a 90% guarantee rate,the wetted perimeter method,the minimum monthly average water level method,and the lowest survival water depth method.Through the comparative analysis of actual river operation and management schemes,the ecological water level targets of the upper,middle,and lower reaches of the river are comprehensively determined as 17.40 m,8.96 m,and 7.50 m respectively.After the control value of the ecological water level of the river is obtained by comprehensive analysis,the actual operation and management situation of the river is taken into account to propose specific safeguard measures for maintaining the ecological water level (flow) target of the river from multiple perspectives.Some of the measures are constructing a robust and feasible ecological flow control system,accelerating the construction of an information monitoring system of ecological flow and water intake and an early warning system safeguarding the ecological water level target,and strengthening the supervision and assessment of the implementation of river and lake ecological flows (water levels).…”
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Modeling the Effects of Land-Cover Change on Rainfall-Runoff Relationships in a Semiarid, Eastern Mediterranean Watershed by Noa Ohana-Levi, Arnon Karnieli, Roey Egozi, Amir Givati, Aviva Peeters

“…A 1989 Landsat TM-derived classification map was used as input for a Kinematic Runoff and Erosion (KINEROS) hydrological model along with the precipitation data of an extreme rainfall event. …”
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Plant Adaptation and Soil Shear Strength: Unraveling the Drought Legacy in <i>Amorpha fruticosa</i> by Hao Jiang, Xiaoqing Chen, Gang Xu, Jiangang Chen, Dongri Song, Ming Lv, Hanqing Guo, Jingyi Chen

“…Concurrently, the stomatal conductance and transpiration rate of leaves decrease, weakening the capacity to augment soil matric suction through transpiration and potentially reducing hydrological reinforcement. Although rewetting treatments aid in recovery, drought legacy effects persist and impact plant functional attributes. …”
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Study on scour simulation and boundary condition conversion technology for a shallow foundation bridge by Gangping Fan, Huanzhe Li, Tianzhuo Wang, Jian Che, Xing Li, Chunyang Dou, Tong Wu

“…To prevent and mitigate scouring risks, this paper investigates the riverbed scouring characteristics of shallow foundation bridges under different hydrological conditions.The study found that under high water levels and flow velocities, scour depth significantly increased.Under extreme hydrological conditions, a horseshoe vortex forms at the base of the front end of the bridge pier, causing scour pits on both sides of the upstream face of the foundation, which is the main cause of foundation voids that first appear at 2580 s with a maximum scour depth of -2.51 m and a void area of 0.5%, continuing to increase over time.Based on simulated scouring data, this study proposes a method for converting boundary conditions from a scouring model to a mechanical model. …”
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Physically-based modelling of UK river flows under climate change by Ben A. Smith, Stephen J. Birkinshaw, Elizabeth Lewis, Eleyna McGrady, Paul Sayers

“…This study presents the model setup and results from the first calibrated, physically-based, spatially-distributed hydrological modelling of combined land cover and climate change impacts on a large sample of UK river catchments. …”
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Cinématique et impacts d’un événement hydrométéorologique : les inondations du 6-7 octobre 2014, Grabels (France méditerranéenne) by Tony Rey, Stéphanie Defossez, Freddy Vinet, Laurent Boissier

“…We identified the floodplain, the development of the flood and others characteristics on morphosedimentary and hydrologics changes. We also estimate damages and impacts on urbanized area.…”
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Runoff of the Lena Basin Rivers in the Trans-Baikal Territory and its Relationship with Atmospheric Precipitation by Natalia V. Rakhmanova, Elena V. Noskova, Irina L. Vakhnina

“…However, the Lena River basin hydrological characteristics within the boundaries of Trans-Baikal Kray have been studied insufficiently.…”

Permeability Properties of Jointed Rock with Periodic Partially Filled Fractures by Fei Ye, Jun-Chao Duan, Wen-Xi Fu, Xing-Yu Yuan

“…Rock fractures always influence the hydrological properties of a rock mass. To investigate the seepage characteristics of a rock mass with partly filled fractures, a mathematical model is established. …”
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Aide au suivi du phénomène de dénitrification naturelle pour une gestion durable de la ressource en eau du Béthunois by José Luis Martin-Bordes, Éric Henry, Cherif Boulemia, François-Xavier Masson

“…In this article, we propose the setting-up of a control panel thanks to a GIS platform coupled with a hydrological model. Our research work is applied to the SIVOM of the Béthunois.…”
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Diversité régionale de la prise en compte des zones humides et de leurs dynamiques by Magalie Franchomme, Claude Kergomard

“…Nevertheless, the local and regional planning gradually integrates them, because small areas wetlands have different hydrological and biological functions. The wetlands constitute a new development contribution, despite contradictions between their protection and their uses. …”
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Role of Barystatic Sea Level Change in Global Mass Conservation and Its Excitation to Length‐Of‐Day Variations by Qiqi Shi, Yonghong Zhou, Cancan Xu, Xueqing Xu

“…The barystatic sea level exhibits the most significant amplitude in mass‐induced LOD variations, compensating for most land hydrological excitation, but shows no clear correlation with the atmosphere. …”
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Runoff Change in Upper Watershed of Tangwang River Based on CMIP-6 Climate Model by ZHAO Yusu, SUN Yingna, HUANG Xihao

“…In addition, future runoff change was estimated according to the soil and water assessment tool (SWAT) hydrological model. The maximum and minimum air temperatures and precipitation will increase in the future (2015–2100), but the growth rate varies in different situations, involving 0.65 °C/10a, 0.65 °C/10a,12.23 mm/10a (SSP1-2.6), 0.25 °C/10a, 0.39 °C/10a, 11.14 mm/10a (SSP2-4.5), and 0.81 °C/10a,0.86 °C/10a, 23.57 mm/10a (SSP5-8.5). …”
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Morphological Model for Erosion Prediction of India’s Largest Braided River Using MIKE 21C Model by Kuldeep Pareta

“…Model runs were conducted to predict design variables across these river reaches, encompassing different hydrological scenarios and development-planning scenarios. …”
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Groundwater Quality on the Adriatic Karst Island of Mljet (Croatia) and Its Implications on Water Supply by Staša Borović, Josip Terzić, Marco Pola

“…Water sampling and chemical analyses were performed during hydrological minimum and maximum with regard to groundwater levels in 2005/2006 and minimum in 2016. …”
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Predicting Future Surface Runoff Delivered to the Euphrates River Using LARSWG and SWAT Models: (Sahiliya Valley in the Iraqi Western    Desert as a Case Study) by Wisam Abdulabbas Abidalla, Basim Sh. Abed

“… The Weather Generation Model “LARSWG” and hydrological Model “SWAT” used in this study to estimate the quantity of future surface runoff in the Sahiliya Valley located within the Iraqi western desert. …”
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Lower grass stomatal conductance under elevated CO2 can decrease transpiration and evapotranspiration rates despite carbon fertilization by Sate Ahmad, Charilaos Yiotis, Weimu Xu, Jan Knappe, Laurence Gill, Jennifer McElwain

“…The combined effect of these responses on the total plant transpiration and on evapotranspiration (ET) has a wide range of implications on local, regional, and global hydrological cycles, and thus needs to be better understood. …”
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