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Journal articles on the topic 'Hydrology'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Meng, Xiao, Wu Qun Cheng, and Xian Bing Wu. "Application of Progressive Teaching Model in Engineering Hydrology and Hydrologic Calculation." Advanced Materials Research 919-921 (April 2014): 2185–88. http://dx.doi.org/10.4028/www.scientific.net/amr.919-921.2185.

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Engineering hydrology and hydrologic calculation is a core professional course of agricultural hydrologic engineering, in order to realize the implementation of quality education in higher school teaching purposes, with the teaching practice of engineering hydrology and hydrologic calculation, puts forward the progressive teaching mode of engineering hydrology and hydrologic calculation, and applied in teaching activities. The conception of progressive teaching mode and practice was summarized from four aspects of progressive teaching objective, teaching content, gradual progressive teaching m

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2

Zhao, Ying, Jianguo Zhang, Jianhua Si, Jie Xue, and Zhongju Meng. "Special Issue: Soil Hydrological Processes in Desert Regions: Soil Water Dynamics, Driving Factors, and Practices." Water 14, no. 17 (2022): 2635. http://dx.doi.org/10.3390/w14172635.

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3

Wagener, T., C. Kelleher, M. Weiler, et al. "It takes a community to raise a hydrologist: the Modular Curriculum for Hydrologic Advancement (MOCHA)." Hydrology and Earth System Sciences Discussions 9, no. 2 (2012): 2321–56. http://dx.doi.org/10.5194/hessd-9-2321-2012.

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Abstract. Protection from hydrological extremes and the sustainable supply of hydrological services in the presence of climate change and increasing population pressure are the defining societal challenges for hydrology in the 21st century. A review of the existing literature shows that these challenges and their educational consequences for hydrology were foreseeable and were predicted by some. Surveys of the current educational basis, however, also clearly demonstrate that hydrology education is not yet prepared to deal with this challenge. We present our own vision of the necessary future e

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4

Wagener, T., C. Kelleher, M. Weiler, et al. "It takes a community to raise a hydrologist: the Modular Curriculum for Hydrologic Advancement (MOCHA)." Hydrology and Earth System Sciences 16, no. 9 (2012): 3405–18. http://dx.doi.org/10.5194/hess-16-3405-2012.

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Abstract. Protection from hydrological extremes and the sustainable supply of hydrological services in the presence of changing climate and lifestyles as well as rocketing population pressure in many parts of the world are the defining societal challenges for hydrology in the 21st century. A review of the existing literature shows that these challenges and their educational consequences for hydrology were foreseeable and were even predicted by some. However, surveys of the current educational basis for hydrology also clearly demonstrate that hydrology education is not yet ready to prepare stud

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5

MORI, Kazuki. "Hydrologic science: Hydrology as a fundamental science." Journal of Japanese Association of Hydrological Sciences 47, no. 1 (2017): 17–21. http://dx.doi.org/10.4145/jahs.47.17.

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6

Liu, Dengfeng, Hui Liu, and Xianmeng Meng. "Advanced Hydrologic Modeling in Watershed Scale." Water 15, no. 4 (2023): 691. http://dx.doi.org/10.3390/w15040691.

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7

Day-Lewis, Frederick D., and Arpita P. Bathija. "Introduction to this special section: Hydrogeophysics." Leading Edge 41, no. 8 (2022): 518. http://dx.doi.org/10.1190/tle41080518.1.

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Hydrogeophysics is a crossdisciplinary field integrating hydrogeology with geophysics for more efficient, cost-effective, and minimally invasive characterization and monitoring. Hydrogeophysics aims to provide basic insight to guide understanding of hydrologic processes and applied insight to support the assessment and (or) management of water resources and ecosystem services across multiple scales, as reviewed by Binley et al. (2015) . As in geophysical investigations for mineral and fossil energy resources, geophysical applications to hydrologic problems seek to characterize subsurface struc

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8

Dan-Jumbo, Nimi G., and Marc Metzger. "Relative Effect of Location Alternatives on Urban Hydrology. The Case of Greater Port-Harcourt Watershed, Niger Delta." Hydrology 6, no. 3 (2019): 82. http://dx.doi.org/10.3390/hydrology6030082.

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Globally, cities in developing countries are urbanising at alarming rates, and a major concern to hydrologists and planners are the options that affect the hydrologic functioning of watersheds. Environmental impact assessment (EIA) has been recognised as a key sustainable development tool for mitigating the adverse impacts of planned developments, however, research has shown that planned developments can affect people and the environment significantly due to urban flooding that arises from increased paved surfaces. Flooding is a major sustainable development issue, which often result from incr

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9

Johnson, K. A., and N. Sitar. "Hydrologic conditions leading to debris-flow initiation." Canadian Geotechnical Journal 27, no. 6 (1990): 789–801. http://dx.doi.org/10.1139/t90-092.

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Mitigation of the hazards posed by debris flows requires an understanding of the mechanisms leading to their initiation. The objectives of this study were to evaluate and document the hydrologic response of a potential debris-flow source area to major rainstorms and to evaluate whether traditional models of hillslope hydrology can account for the observed response. A field site in an area of previous debris-flow activity was instrumented and monitored for two winter seasons. Hydrologic responses for a wide variety of antecedent conditions were recorded, including two storm events that produced

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10

Peters-Lidard, Christa D., Martyn Clark, Luis Samaniego, et al. "Scaling, similarity, and the fourth paradigm for hydrology." Hydrology and Earth System Sciences 21, no. 7 (2017): 3701–13. http://dx.doi.org/10.5194/hess-21-3701-2017.

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Abstract. In this synthesis paper addressing hydrologic scaling and similarity, we posit that roadblocks in the search for universal laws of hydrology are hindered by our focus on computational simulation (the third paradigm) and assert that it is time for hydrology to embrace a fourth paradigm of data-intensive science. Advances in information-based hydrologic science, coupled with an explosion of hydrologic data and advances in parameter estimation and modeling, have laid the foundation for a data-driven framework for scrutinizing hydrological scaling and similarity hypotheses. We summarize

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11

Chu, Vena W. "Greenland ice sheet hydrology." Progress in Physical Geography: Earth and Environment 38, no. 1 (2013): 19–54. http://dx.doi.org/10.1177/0309133313507075.

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Understanding Greenland ice sheet (GrIS) hydrology is essential for evaluating response of ice dynamics to a warming climate and future contributions to global sea level rise. Recently observed increases in temperature and melt extent over the GrIS have prompted numerous remote sensing, modeling, and field studies gauging the response of the ice sheet and outlet glaciers to increasing meltwater input, providing a quickly growing body of literature describing seasonal and annual development of the GrIS hydrologic system. This system is characterized by supraglacial streams and lakes that drain

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12

Hall, Caitlyn A., Sheila M. Saia, Andrea L. Popp, et al. "A hydrologist's guide to open science." Hydrology and Earth System Sciences 26, no. 3 (2022): 647–64. http://dx.doi.org/10.5194/hess-26-647-2022.

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Abstract. Open, accessible, reusable, and reproducible hydrologic research can have a significant positive impact on the scientific community and broader society. While more individuals and organizations within the hydrology community are embracing open science practices, technical (e.g., limited coding experience), resource (e.g., open access fees), and social (e.g., fear of weaknesses being exposed or ideas being scooped) challenges remain. Furthermore, there are a growing number of constantly evolving open science tools, resources, and initiatives that can be overwhelming. These challenges

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13

Shen, Chaopeng, Eric Laloy, Amin Elshorbagy, et al. "HESS Opinions: Incubating deep-learning-powered hydrologic science advances as a community." Hydrology and Earth System Sciences 22, no. 11 (2018): 5639–56. http://dx.doi.org/10.5194/hess-22-5639-2018.

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Abstract. Recently, deep learning (DL) has emerged as a revolutionary and versatile tool transforming industry applications and generating new and improved capabilities for scientific discovery and model building. The adoption of DL in hydrology has so far been gradual, but the field is now ripe for breakthroughs. This paper suggests that DL-based methods can open up a complementary avenue toward knowledge discovery in hydrologic sciences. In the new avenue, machine-learning algorithms present competing hypotheses that are consistent with data. Interrogative methods are then invoked to interpr

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14

Si, Bing. "Hydrology." Soil Science Society of America Journal 70, no. 5 (2006): 1820. http://dx.doi.org/10.2136/sssaj2006.0011br.

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15

Rosbjerg, Dan, and Ian Littlewood. "From Nordic Hydrology to Hydrology Research." Hydrology Research 39, no. 1 (2008): i—ii. http://dx.doi.org/10.2166/nh.2008.0001.

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16

Carter, Virginia. "An overview of the hydrologic concerns related to wetlands in the United States." Canadian Journal of Botany 64, no. 2 (1986): 364–74. http://dx.doi.org/10.1139/b86-053.

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There is a tremendous diversity in wetland types and wetland vegetation in the United States, caused primarily by regional, geologic, topographic, and climatic differences. Wetland hydrology, a primary driving force influencing wetland ecology, development, and persistence, is as yet poorly understood. The interaction between groundwater and surface water and the discharge–recharge relationships in wetlands affect water quality and nutrient budgets as well as vegetative composition. Hydrologic considerations necessary for an improved understanding of wetland ecology include detailed water budg

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17

Cao, Xuejian, Youcun Qi, and Guangheng Ni. "Significant Impacts of Rainfall Redistribution through the Roof of Buildings on Urban Hydrology." Journal of Hydrometeorology 22, no. 4 (2021): 1007–23. http://dx.doi.org/10.1175/jhm-d-20-0220.1.

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AbstractMicrotopography on a building roof will direct rainfall from roofs to the ground through downspouts and transform the rainfall spatial distribution from plane to points. However, the issues on whether and how the building-induced rainfall redistribution (BIRR) influences hydrologic responses are still not well understood despite the numerous downspouts in the urban area. Hence, this study brings the roof layer into a grid-based urban hydrologic model (gUHM) to quantitatively evaluate the impacts of BIRR, aiming to enhance the understanding of building effects in urban hydrology and sub

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18

Singh, Kuldeep. "Stream Order Delineation using SRTM 30 meter Resolution Digital Elevation Model (DEM) and Hydrology Tools in ArcGIS 10.3 and QGIS: Mapping of Drainage Pattern of Mandi District, Himachal Pradesh, India." Asian Review of Civil Engineering 10, no. 2 (2021): 9–17. http://dx.doi.org/10.51983/tarce-2021.10.2.3118.

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The paper describes step by step watershed and stream network delineation based on digital elevation models using the Hydrology tools in ArcGIS and online services for Hydrology and Hydrologic data. The 30-meter resolution SRTM image of Himachal Pradesh was downloaded from open topology website. This was further processed in QGIS and ArcGIS 10.3 software. The different hydrological processes and data management tools were used like, fill, Flow direction; flow accumulation, map algebra, stream orders, stream feature and stream dissolve in order to get the final map of Mandi drainage pattern.

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19

Dai, Chang Lei, Cheng Gang Yu, Lan Lin, Di Fang Xiao, and Hui Yu Li. "Analysis of Characteristics of Hydrology and Water Resources of the Heilong (Amur) River Basin." Advanced Materials Research 550-553 (July 2012): 2525–32. http://dx.doi.org/10.4028/www.scientific.net/amr.550-553.2525.

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As the most remote river in the North of China, Heilong (Amur) River have an abundant precipitation in the basin and a rich runoff. Due to the special transnational spanned geographic location, Heilong (Amur) basin 's borders, water rights, regional water resources development are a big concern. Due to lack of multinational management and information, analysis of characteristic of Heilong (Amur) watershed's hydrology and water resources are not enough. In order to serve the water resources development and water security, and to better understand the state of hydrology and water resources in He

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20

Habib, E., Y. Ma, D. Williams, H. O. Sharif, and F. Hossain. "HydroViz: design and evaluation of a Web-based tool for improving hydrology education." Hydrology and Earth System Sciences 16, no. 10 (2012): 3767–81. http://dx.doi.org/10.5194/hess-16-3767-2012.

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Abstract. HydroViz is a Web-based, student-centered, educational tool designed to support active learning in the field of Engineering Hydrology. The design of HydroViz is guided by a learning model that is based on learning with data and simulations, using real-world natural hydrologic systems to convey theoretical concepts, and using Web-based technologies for dissemination of the hydrologic education developments. This model, while being used in a hydrologic education context, can be adapted in other engineering educational settings. HydroViz leverages the free Google Earth resources to enab

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21

Bogaard, Thom A., and Roberto Greco. "Landslide hydrology: from hydrology to pore pressure." WIREs Water 3, no. 3 (2015): 439–59. http://dx.doi.org/10.1002/wat2.1126.

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22

Williams, Chenille, and Dan Tufford. "Groundwater Recharge Rates in Isolated and Riverine Wetlands: Influencing Factors." Journal of South Carolina Water Resources, no. 2 (June 1, 2015): 86–92. http://dx.doi.org/10.34068/jscwr.02.10.

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Isolated wetlands and riverine wetlands have been shown to have similar groundwater hydrology despite their difference in topography and surface water hydrology. The current study aimed to address the impact of topography and surface water hydrology on groundwater hydrologic behavior by comparing the groundwater recharge rates of several isolated and riverine wetlands in the Coastal Plain of South Carolina. Study sites contained an isolated wetland, a riverine wetland, and an upland that bisected the two wetland types. Shallow water tables and sandy soils, allowed a rapid response to precipita

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23

Schultz, Richard C., and Kye-Han Lee. "Book Reviews: Forest Hydrology: An Introduction to Water and Forests." Forest Science 49, no. 2 (2003): 336–37. http://dx.doi.org/10.1093/forestscience/49.2.336.

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Abstract In recent years, water resource issues concerning quality, quantity, and timing have been dominating natural resource management discussions around the world. Forest hydrology has historically been an important topic in forest management leading to some of the earliest forest research conducted in the United States. While there are a few textbooks on forest hydrology, there has always been a dilemma in what to include in such books. The hydrologic cycle may be briefly covered in ecology courses. However, without a significant introduction to water resources, most forestry and nonfores

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24

Loucks, Daniel P. "Debates-Perspectives on socio-hydrology: Simulating hydrologic-human interactions." Water Resources Research 51, no. 6 (2015): 4789–94. http://dx.doi.org/10.1002/2015wr017002.

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25

Bauser, Hannes H., Daniel Berg, Ole Klein, and Kurt Roth. "Inflation method for ensemble Kalman filter in soil hydrology." Hydrology and Earth System Sciences 22, no. 9 (2018): 4921–34. http://dx.doi.org/10.5194/hess-22-4921-2018.

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Abstract. The ensemble Kalman filter (EnKF) is a popular data assimilation method in soil hydrology. In this context, it is used to estimate states and parameters simultaneously. Due to unrepresented model errors and a limited ensemble size, state and parameter uncertainties can become too small during assimilation. Inflation methods are capable of increasing state uncertainties, but typically struggle with soil hydrologic applications. We propose a multiplicative inflation method specifically designed for the needs in soil hydrology. It employs a Kalman filter within the EnKF to estimate infl

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26

Javadinejad, Safieh, Rebwar Dara, and Neda Dolatabadi. "Runoff coefficient estimation for various catchment surfaces." Resources Environment and Information Engineering 3, no. 1 (2022): 145–55. http://dx.doi.org/10.25082/reie.2021.01.005.

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The definition of runoff coefficient is the portion of rainfall that turn into direct runoff throughout an occurrence, and it is a significant perception in engineering hydrology and is extensively applied for design and as a diagnostic variable to show runoff creation in catchments. Event runoff coefficients may also be applied in event‐based developed flood frequency models that measure flood frequencies from rainfall frequencies and are valuable for recognizing the flood frequency controls in a specific hydrologic or climatic regime. Only a few previous studies worked on hydrological system

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27

Khan, Muhammad Owais, Saskia D. Keesstra, Ewa Słowik-Opoka, Anna Klamerus-Iwan, and Waqas Liaqat. "Determining the Role of Urban Greenery in Soil Hydrology: A Bibliometric Analysis of Nature-Based Solutions in Urban Ecosystem." Water 17, no. 3 (2025): 322. https://doi.org/10.3390/w17030322.

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Nature-based solutions play an essential role in enhancing urban soil hydrology by improving water retention properties, reducing surface runoff, and improving water infiltration. This bibliometric analysis study reviewed the literature and identified the current trends in research related to nature-based solutions in urban soil hydrology. The study has the potential to highlight current research areas and future hot topics in this specific field. The research used the Scopus database to collect published articles from 1973 to 2023. The keywords (“trees” OR “vegetation” OR “green infrastructur

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28

Harman, C., and P. A. Troch. "Darwinian hydrology: can the methodology Charles Darwin pioneered help hydrologic science?" Hydrology and Earth System Sciences Discussions 10, no. 5 (2013): 6407–44. http://dx.doi.org/10.5194/hessd-10-6407-2013.

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Abstract. There have been repeated calls for a Darwinian approach to hydrologic science or for a synthesis of Darwinian and Newtonian approaches, to deepen understanding the hydrologic system in the larger landscape context, and so develop a better basis for predictions now and in an uncertain future. But what exactly makes a Darwinian approach to hydrology "Darwinian"? While there have now been a number of discussions of Darwinian approaches, many referencing Harte (2002), the term is potentially a source of confusion while its connections to Darwin remain allusive rather than explicit. Here

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29

Tarboton, D. G. "Physical hydrology." Eos, Transactions American Geophysical Union 76, no. 32 (1995): 316. http://dx.doi.org/10.1029/95eo00194.

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30

Schulmeister, Marcia K. "Subsurface Hydrology." Ground Water 46, no. 4 (2008): 524. http://dx.doi.org/10.1111/j.1745-6584.2008.00447.x.

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31

Agouridis, Carmen. "Environmental Hydrology." Groundwater 54, no. 5 (2016): 626. http://dx.doi.org/10.1111/gwat.12446.

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32

Anonymous. "Groundwater hydrology." Eos, Transactions American Geophysical Union 70, no. 8 (1989): 114. http://dx.doi.org/10.1029/eo070i008p00114-04.

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33

Gifford, G. F. "Watershed hydrology." Eos, Transactions American Geophysical Union 73, no. 16 (1992): 179. http://dx.doi.org/10.1029/91eo00146.

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34

Feddes, Reinder A. "Soil Hydrology." Soil Science 161, no. 2 (1996): 136–37. http://dx.doi.org/10.1097/00010694-199602000-00009.

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35

Lawrence, Gregory B. "Watershed Hydrology." Soil Science 161, no. 10 (1996): 725. http://dx.doi.org/10.1097/00010694-199610000-00009.

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36

Ritchie, J. C. W. "Urban hydrology." Canadian Journal of Civil Engineering 12, no. 2 (1985): 424–25. http://dx.doi.org/10.1139/l85-050.

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37

Innsbruck, H. Rott. "Hydrology/Snow." Photogrammetria 42, no. 4 (1988): 178–79. http://dx.doi.org/10.1016/0031-8663(88)90051-8.

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38

Slack, J. R., and K. E. Bencala. "Stochastic hydrology." Journal of Hydrology 103, no. 3-4 (1988): 396. http://dx.doi.org/10.1016/0022-1694(88)90150-3.

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39

Haugh, Larry D., Ian B. MacNeill, and Gary J. Umphrey. "Stochastic Hydrology." Statistician 38, no. 1 (1989): 83. http://dx.doi.org/10.2307/2349030.

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40

Kulik, V. "Bushfire hydrology." International Journal of Water Resources Development 6, no. 1 (1990): 44–54. http://dx.doi.org/10.1080/07900629008722449.

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41

Walling, D. E. "Physical hydrology." Progress in Physical Geography: Earth and Environment 9, no. 1 (1985): 97–103. http://dx.doi.org/10.1177/030913338500900108.

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42

Walling, D. E. "Physical hydrology." Progress in Physical Geography: Earth and Environment 10, no. 1 (1986): 69–80. http://dx.doi.org/10.1177/030913338601000104.

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43

Walling, D. E. "Physical hydrology." Progress in Physical Geography: Earth and Environment 11, no. 1 (1987): 112–20. http://dx.doi.org/10.1177/030913338701100106.

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44

Walling, D. E. "Physical hydrology." Progress in Physical Geography: Earth and Environment 11, no. 4 (1987): 590–97. http://dx.doi.org/10.1177/030913338701100407.

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45

Anderson, M. G. "Physical hydrology." Progress in Physical Geography: Earth and Environment 13, no. 1 (1989): 93–102. http://dx.doi.org/10.1177/030913338901300106.

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46

Wilby, R. L. "Greenhouse hydrology." Progress in Physical Geography: Earth and Environment 19, no. 3 (1995): 351–69. http://dx.doi.org/10.1177/030913339501900304.

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Hydrological processes are an integral component of both global climate change arising from increasing concentrations of greenhouse gases and the assessment of subsequent terrestrial impacts. This article examines the potential sensivity of water resources in the UK to climatic change as exemplified by the 1988-92 drought. The representation of hydrological processes at three distinct model scales is then discussed with reference to global hydrology, regional downscaling and catchment-scale responses. A final section speculates on future directions of research for an emerging greenhouse hydrol

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47

House, Andrew. "Physical Hydrology." Hydrological Sciences Journal 60, no. 9 (2015): 1649–50. http://dx.doi.org/10.1080/02626667.2015.1059141.

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48

Court, Arnold. "Heterodox Hydrology." Geographical Analysis 4, no. 2 (2010): 194–96. http://dx.doi.org/10.1111/j.1538-4632.1972.tb00469.x.

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49

McCulloch, J. S. G. "Tracer hydrology." Journal of Hydrology 144, no. 1-4 (1993): 429. http://dx.doi.org/10.1016/0022-1694(93)90183-a.

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50

GOODRICH, DAVID C., and DAVID A. WOOLHISER. "Catchment Hydrology." Reviews of Geophysics 29, S1 (1991): 202–9. http://dx.doi.org/10.1002/rog.1991.29.s1.202.

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