Journal articles: 'Hydromorphologie'

1

Redeker, Marq. "Workshop Hydromorphologie III — Erfolgsfaktoren der Gewässerentwicklung." WASSERWIRTSCHAFT 106, no. 7-8 (July 25, 2016): 60–61. http://dx.doi.org/10.1007/s35147-016-0122-9.

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Weigelhofer, G., J. Fuchsberger, B. Teufl, N. Kreuzinger, S. Muhar, S. Preis, K. Schilling, and T. Hein. "Einfluss der Hydromorphologie auf den Nährstoffrückhalt in Weinviertler Bächen – Schlussfolgerungen für das Gewässermanagement." Österreichische Wasser- und Abfallwirtschaft 63, no. 9-10 (October 2011): 183–89. http://dx.doi.org/10.1007/s00506-011-0337-z.

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Cluzel, Philippe. "Étude pour la réduction de l’impact des éclusées sur le fleuve Aude." E3S Web of Conferences 346 (2022): 02009. http://dx.doi.org/10.1051/e3sconf/202234602009.

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Avec un bassin versant de près de 5 500 km2, l’Aude constitue le fleuve côtier le plus important de la Région Occitanie. Il est soumis à un régime d’éclusées ayant pour origine la production d’énergie hydroélectrique de pointe et, en période d’étiage estival, le placement de l’eau au service des sports d’eaux vives et de l’agriculture. Ces éclusées se traduisent par une fluctuation des débits instantanés, liée à des lâchers d’eau limités dans le temps se superposant au débit de base naturel. Ce fonctionnement est générateur de perturbations sur le milieu (hydromorphologie, physico-chimie, biologie), et les phénomènes de marnages posent des difficultés de gestion pour les différentes catégories d’usagers, notamment les préleveurs. Ce phénomène pourrait être aggravé à moyen terme puisque la mise en place d’un système complémentaire de compensation des prélèvements multi-usagers depuis des ressources sécurisées est en discussion. Dans ce contexte, le Syndicat Mixte des Milieux Aquatiques et des Rivières (SMMAR) mène une étude spécifique dont l’objectif est de mieux comprendre les phénomènes d’éclusées et leurs incidences, afin de proposer des solutions d’aménagement et de gestion visant à respecter les objectifs de bon état des milieux imposés par la Directive Cadre, tout en garantissant les usages.

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Malavoi, Jean-René, and Jean-Paul Bravard. "Éléments d'hydromorphologie fluviale. Édité par l'Onema (Office national de l'eau et des milieux aquatiques), 2010, 224 p.En ligne sur : http://www.onema.fr/hydromorphologie-fluviale." Physio-Géo, Volume 5 (January 3, 2011): 1. http://dx.doi.org/10.4000/physio-geo.1532.

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Vogel, Richard M. "Hydromorphology." Journal of Water Resources Planning and Management 137, no. 2 (March 2011): 147–49. http://dx.doi.org/10.1061/(asce)wr.1943-5452.0000122.

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Radice, Alessio, and Barbara Zanchi. "Multicamera, Multimethod Measurements for Hydromorphologic Laboratory Experiments." Geosciences 8, no. 5 (May 10, 2018): 172. http://dx.doi.org/10.3390/geosciences8050172.

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Orr, H. G., A. R. G. Large, M. D. Newson, and C. L. Walsh. "A predictive typology for characterising hydromorphology." Geomorphology 100, no. 1-2 (August 2008): 32–40. http://dx.doi.org/10.1016/j.geomorph.2007.10.022.

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8

Chalov, R. S., and S. R. Chalov. "Channel Processes Disconnectivity in Rivers Hydromorphology." Izvestiya Rossiiskoi Akademii Nauk Seriya Geograficheskaya 87, no. 2 (March 1, 2023): 234–49. http://dx.doi.org/10.31857/s2587556623020036.

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The present paper deals with five main structural levels of channel processes and channel patterns due to disconnectivity of fluvial processes. River braiding is related to existence of point, bar, channel (island), anabranching and large distributary channels (located in the deltas of large and largest rivers). Meandering is related to sinuosity of the flow and formation of complex loop and large meanders, the dimensions of which are larger than those corresponding to the water content of the river, and the meanders of the meandering belts. Due to the instability of the straight flow, the structural levels of the straight single channel are distinguished by their size: pool hollows on the riffles, reaches between adjacent bends and segments of braided channel, sections between single branches and stretched stretch areas along the bedrock banks or in the incised channel. Each structural level is related to the previous one forming scaling sequence (middle and side channels are the basis for the formation of branches and bends, etc.), representing genetic series, although in some cases they may have a different origin (intra-floodplain intercepts, relics of delta branches, etc.). The meandering process happens over various scales in both braided and straight channels. The formation of structural levels is governed by river size, geology, effective discharges and local drivers.

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Solari, L., M. Van Oorschot, B. Belletti, D. Hendriks, M. Rinaldi, and A. Vargas-Luna. "Advances on Modelling Riparian Vegetation-Hydromorphology Interactions." River Research and Applications 32, no. 2 (May 22, 2015): 164–78. http://dx.doi.org/10.1002/rra.2910.

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Kilic, Batuhan, Fatih Gulgen, Meltem Celen, Mehmet Salim Oncel, Halil Nurullah Oruc, and Sinem Vural. "The role of topographic maps in river hydromorphology." Abstracts of the ICA 3 (December 13, 2021): 1–2. http://dx.doi.org/10.5194/ica-abs-3-149-2021.

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11

Belletti, B., M. Rinaldi, A. D. Buijse, A. M. Gurnell, and E. Mosselman. "A review of assessment methods for river hydromorphology." Environmental Earth Sciences 73, no. 5 (August 2, 2014): 2079–100. http://dx.doi.org/10.1007/s12665-014-3558-1.

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12

Pelte, Th, and S. Stroffek. "Évaluation de l’état hydromorphologique. Cas des milieux fortement modifiés." Techniques Sciences Méthodes, no. 2 (2007): 30–37. http://dx.doi.org/10.1051/tsm/200702030.

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13

Davy-Bowker, John, and Mike T. Furse. "Hydromorphology – major results and conclusions from the STAR project." Hydrobiologia 566, no. 1 (August 2006): 263–65. http://dx.doi.org/10.1007/s10750-006-0091-6.

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14

Allaire, Maura C., Richard M. Vogel, and Charles N. Kroll. "The hydromorphology of an urbanizing watershed using multivariate elasticity." Advances in Water Resources 86 (December 2015): 147–54. http://dx.doi.org/10.1016/j.advwatres.2015.09.022.

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15

Li, Jianhua, Stephan Hoerbinger, Clemens Weissteiner, Lingmin Peng, and Hans Peter Rauch. "River restoration challenges with a specific view on hydromorphology." Frontiers of Structural and Civil Engineering 14, no. 5 (August 2020): 1033–38. http://dx.doi.org/10.1007/s11709-020-0665-9.

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16

Delgado-Lemus, Tzitzi Sharhí, and Ana Isabel Moreno-Calles. "Agroforestry Contributions to Urban River Rehabilitation." Sustainability 14, no. 13 (June 23, 2022): 7657. http://dx.doi.org/10.3390/su14137657.

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The context of urban rivers is one of pollution of their courses, the degradation of riparian habitats, the loss of biodiversity, and the marginalization of the human populations that live next to them. Due to urban growth, the hydrological dynamics in entire basins and the hydromorphology of rivers are changing. This situation increases flooding, decreases the availability of water for human use, and disconnects the rivers from the dynamics of the city. Agroforestry is the integration of cultural, wild, and domesticated diversity with use, conservation, and restoration objectives. These practices in cities can contribute to addressing the problems mentioned. We analyze agroforestry practices and the socio-ecological contributions to urban river rehabilitation. We review 37 experiences worldwide. Agroforestry practices included in the review are trees and hedgerows; wetland agroforestry; aquatic, botanical, edible, educational, and rain gardens; bioswales; green parking lots; food forestry; vegetation in alleys and streets; vertical terrace walls, among others. Agroforestry contributes to efforts to solve urban river problems, improve water quality and access, restore riparian habitats, enhance river hydromorphology, support local economies, and create a river culture. We emphasize promoting multi-relational people–river interactions based on theoretical and practical frameworks that integrate diverse disciplines, perspectives, and experiences.

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17

Martí, Eugènia, Paula Fonollà, Daniel von Schiller, Francesc Sabater, Alba Argerich, Miquel Ribot, and Joan Lluís Riera. "Variation in stream C, N and P uptake along an altitudinal gradient: a space-for-time analogue to assess potential impacts of climate change." Hydrology Research 40, no. 2-3 (April 1, 2009): 123–37. http://dx.doi.org/10.2166/nh.2009.090.

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A space-for-time substitution approach was used to evaluate potential effects of climate change on stream nutrient uptake by examining the relationship between stream environmental parameters and carbon (C), nitrogen (N) and phosphorus (P) uptake along an altitudinal gradient. The study was carried out in 14 streams located in the Central Pyrenees (NE Spain) draining calcareous catchments that cover an altitudinal range of 700–2,100 m a.s.l. In these streams, uptake of inorganic (soluble reactive phosphorus (SRP), ammonium and nitrate) and organic (acetate and glycine) nutrients was estimated. Additionally, several physical, chemical and biological parameters were measured. Results showed higher uptake for both SRP, a potentially limiting nutrient in these streams, and glycine, a labile source of dissolved organic N, than for the rest of the nutrients. Uptake of SRP, nitrate, glycine and acetate varied along stream environmental gradients associated with changes in stream hydromorphology, SRP availability and epilithic biomass. However, these gradients did not vary with altitude. These results indicate that climate change effects on stream nutrient uptake are more likely to be driven by indirect effects on hydromorphology and nutrient availability induced by shifts in the precipitation and run-off regime than by direct modifications in the thermal regime.

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18

Urbanič, Gorazd, Zlatko Mihaljević, Vesna Petkovska, and Maja Pavlin Urbanič. "Disentangling the Effects of Multiple Stressors on Large Rivers Using Benthic Invertebrates—A Study of Southeastern European Large Rivers with Implications for Management." Water 12, no. 3 (February 25, 2020): 621. http://dx.doi.org/10.3390/w12030621.

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Predicting anthropogenic actions resulting in undesirable changes in aquatic systems is crucial for the development of effective and sustainable water management strategies. Due to the co-occurrence of stressors and a lack of appropriate data, the effects on large rivers are difficult to elucidate. To overcome this problem, we developed a partial canonical correspondence analyses (pCCA) model using 292 benthic invertebrate taxa from 104 sites that incorporated the effects of three stressors groups: hydromorphology, land use, and water quality. The data covered an environmental gradient from near-natural to heavily altered sites in five large rivers in Southeastern Europe. Prior to developing the multi-stressor model, we assessed the importance of natural characteristics on individual stressor groups. Stressors proved to be the dominant factors in shaping benthic invertebrate assemblages. The pCCA among stressor-groups showed that unique effects dominated over joint effects. Thus, benthic invertebrate assemblages were suitable for disentangling the specific effect of each of the three stressor groups. While the effects of hydromorphology were dominant, both water quality and land use effects were nearly equally important. Quantifying the specific effects of hydromorphological alterations, water quality, and land use will allow water managers to better understand how large rivers have changed and to better define expectations for ecosystem conditions in the future.

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19

YILMAZ, Seher Gulcın, Abdul CHAUDHARY, and Rakesh KANDA. "Impacts of Extreme Weather Events on Hydromorphology of UK Rivers." Turkish Journal of Water Science and Management 5, no. 1 (January 20, 2021): 116–56. http://dx.doi.org/10.31807/tjwsm.819574.

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20

Langhans, Simone D., Judit Lienert, Nele Schuwirth, and Peter Reichert. "How to make river assessments comparable: A demonstration for hydromorphology." Ecological Indicators 32 (September 2013): 264–75. http://dx.doi.org/10.1016/j.ecolind.2013.03.027.

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21

Miler, Oliver, and Mario Brauns. "Hierarchical response of littoral macroinvertebrates to altered hydromorphology and eutrophication." Science of The Total Environment 743 (November 2020): 140582. http://dx.doi.org/10.1016/j.scitotenv.2020.140582.

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22

NEWSON, M., D. SEAR, and C. SOULSBY. "Incorporating hydromorphology in strategic approaches to managing flows for salmonids." Fisheries Management and Ecology 19, no. 6 (February 7, 2012): 490–99. http://dx.doi.org/10.1111/j.1365-2400.2011.00822.x.

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23

O'Briain, R., S. Shephard, and B. Coghlan. "A river vegetation quality metric in the eco-hydromorphology philosophy." River Research and Applications 34, no. 3 (January 23, 2018): 207–17. http://dx.doi.org/10.1002/rra.3244.

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24

Hseu, Zeng-Yei, and Zueng-Sang Chen. "Quantifying Soil Hydromorphology of a Rice-Growing Ultisol Toposequence in Taiwan." Soil Science Society of America Journal 65, no. 1 (January 2001): 270–78. http://dx.doi.org/10.2136/sssaj2001.651270x.

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25

Billi, Paolo, Biadgilgn Demissie, Jan Nyssen, Girma Moges, and Massimiliano Fazzini. "Meander hydromorphology of ephemeral streams: Similarities and differences with perennial rivers." Geomorphology 319 (October 2018): 35–46. http://dx.doi.org/10.1016/j.geomorph.2018.07.003.

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26

Garcia, X. F., I. Schnauder, and M. T. Pusch. "Complex hydromorphology of meanders can support benthic invertebrate diversity in rivers." Hydrobiologia 685, no. 1 (November 9, 2011): 49–68. http://dx.doi.org/10.1007/s10750-011-0905-z.

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27

Scheifhacken, Nicole, Ulrike Haase, Lesya Gram-Radu, Roman Kozovyi, and Thomas U. Berendonk. "How to assess hydromorphology? A comparison of Ukrainian and German approaches." Environmental Earth Sciences 65, no. 5 (September 6, 2011): 1483–99. http://dx.doi.org/10.1007/s12665-011-1218-2.

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28

Vaughan, I. P., M. Diamond, A. M. Gurnell, K. A. Hall, A. Jenkins, N. J. Milner, L. A. Naylor, D. A. Sear, G. Woodward, and S. J. Ormerod. "Integrating ecology with hydromorphology: a priority for river science and management." Aquatic Conservation: Marine and Freshwater Ecosystems 19, no. 1 (January 2009): 113–25. http://dx.doi.org/10.1002/aqc.895.

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29

Ijaz, Muhammad Wajid, Altaf Ali Siyal, Rasool Bux Mahar, Waqas Ahmed, and Muhammad Naveed Anjum. "Detection of Hydromorphologic Characteristics of Indus River Estuary, Pakistan, Using Satellite and Field Data." Arabian Journal for Science and Engineering 42, no. 6 (April 24, 2017): 2539–58. http://dx.doi.org/10.1007/s13369-017-2528-9.

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30

Verdonschot, Piet FM. "Impact of Hydromorphology and Spatial Scale on Macroinvertebrate Assemblage Composition in Streams." Integrated Environmental Assessment and Management 5, no. 1 (2009): 97. http://dx.doi.org/10.1897/ieam_2008-028.1.

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31

KILINÇ, SERHAT FATİH. "Determination of the Most Suitable Assessment Methods of River Hydromorphology for Turkey." Turkish Journal of Water Science and Management 2, no. 2 (July 11, 2018): 110–48. http://dx.doi.org/10.31807/tjwsm.322489.

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32

VAUGHAN, I. P., D. G. NOBLE, and S. J. ORMEROD. "Combining surveys of river habitats and river birds to appraise riverine hydromorphology." Freshwater Biology 52, no. 11 (November 2007): 2270–84. http://dx.doi.org/10.1111/j.1365-2427.2007.01837.x.

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33

Rowan, J. S., S. J. Greig, C. T. Armstrong, D. C. Smith, and D. Tierney. "Development of a classification and decision-support tool for assessing lake hydromorphology." Environmental Modelling & Software 36 (October 2012): 86–98. http://dx.doi.org/10.1016/j.envsoft.2011.09.006.

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34

Boon, Philip, Christine Argillier, Angela Boggero, Marzia Ciampittiello, Judy England, Monika Peterlin, Snežana Radulović, John Rowan, Hanna Soszka, and Gorazd Urbanič. "Developing a standard approach for assessing the hydromorphology of lakes in Europe." Aquatic Conservation: Marine and Freshwater Ecosystems 29, no. 4 (February 6, 2019): 655–69. http://dx.doi.org/10.1002/aqc.3015.

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35

Stefanidis, Konstantinos, Theodora Kouvarda, Anna Latsiou, George Papaioannou, Konstantinos Gritzalis, and Elias Dimitriou. "A Comparative Evaluation of Hydromorphological Assessment Methods Applied in Rivers of Greece." Hydrology 9, no. 3 (February 24, 2022): 43. http://dx.doi.org/10.3390/hydrology9030043.

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The ecological assessment of all surface water bodies in Europe according to the Water Framework Directive involves the monitoring of biological, physicochemical and hydromorphological quality elements. For the hydromorphological assessment in particular, there are numerous methods that have been developed and adopted by EU member countries. With this study, we compared three different methods (River Habitat Survey, Morphological Quality Index and River Hydromorphology Assessment Technique) applied in 122 river reaches that are part of the National Monitoring Network of Greece. The main objectives were (a) to identify whether different assessment systems provide similar classifications of hydromorphological status and (b) to distinguish strengths and weaknesses associated with the implementation of each method. Our results show that the River Hydromorphology Assessment Technique (RHAT) and the Morphological Quality Index (MQI) resulted in the same classification for 58% of the studied reaches, while 34% of the remaining cases differed by only one quality class. Correlations between the two indices per river type (ICT) showed that the two indices were strongly correlated for water courses located at low altitudes. Concerning the HMS index of the River Habitat Survey (RHS), which is an index that reflects the overall hydromorphological pressure, it showed larger differences with the other two indices, mainly because it classified more sites as “Poor” and “Bad” quality classes. Based on our results, we recommend that the two indices, RHAT and MQI, can be implemented complementary to the RHS for providing a rather easy and quick assessment of the overall hydromorphological status, at least until a national hydromorphological database is compiled that will allow for the proper adaptation of the Habitat Quality Assessment (HQA) index.

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36

Chong, Xin Yi, Damià Vericat, Ramon J. Batalla, Fang Yenn Teo, Karen Suan Ping Lee, and Christopher N. Gibbins. "A review of the impacts of dams on the hydromorphology of tropical rivers." Science of The Total Environment 794 (November 2021): 148686. http://dx.doi.org/10.1016/j.scitotenv.2021.148686.

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37

Lin, Qiaoyan, Yixin Zhang, Rob Marrs, Raju Sekar, Xin Luo, and Naicheng Wu. "Evaluating ecosystem functioning following river restoration: the role of hydromorphology, bacteria, and macroinvertebrates." Science of The Total Environment 743 (November 2020): 140583. http://dx.doi.org/10.1016/j.scitotenv.2020.140583.

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38

Scorpio, V., A. Loy, M. Di Febbraro, A. Rizzo, and P. Aucelli. "Hydromorphology Meets Mammal Ecology: River Morphological Quality, Recent Channel Adjustments and Otter Resilience." River Research and Applications 32, no. 3 (October 8, 2014): 267–79. http://dx.doi.org/10.1002/rra.2848.

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39

Gilvear, David J., Corine Davids, and Andrew N. Tyler. "The use of remotely sensed data to detect channel hydromorphology; River Tummel, Scotland." River Research and Applications 20, no. 7 (December 2004): 795–811. http://dx.doi.org/10.1002/rra.792.

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40

Åkesson, Anna, and Anders Wörman. "Stage-dependent hydraulic and hydromorphologic properties in stream networks translated into response functions of compartmental models." Journal of Hydrology 420-421 (February 2012): 25–36. http://dx.doi.org/10.1016/j.jhydrol.2011.11.015.

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41

Økland, R. H. "Studies in SE Fennoscandian mires, with special regard to the use of multivariate techniques and the scaling of ecological gradients." Sommerfeltia 2, s2 (January 1, 1990): 1–28. http://dx.doi.org/10.2478/som-1990-0004.

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Abstract The study presents the results from an integrated approach to hydromorphology, species distribution, and ecological conditions in SE Fennoscandian bogs and poor fens. Patterns of distribution are observed on spatial scales ranging from 0.25 m2 to whole mires (1 km2), and the scope of the study extended to include the regional perspective. Detailed ecological studies studies are performed within a restricted part (0.3 km2) of one mire complex, N. Kisselbergmosen, R{lkienes, SE Norway, while the distribution of plant species and hydromorphological mire types is studied within parts (1000 km2) of Akershus and Østfold counties, SE Norway. Patterns are interpreted by use of multivariate techniques, in particular ordination by detrended correspondence analysis (DCA). On the scale of one mire, four complex-gradients are shown to account for most of the vegetational variation. The relative merits of different sampling procedures and classification systems are discussed. On a broader scale, gradient relationships of vegetation, hydromorphology and species distributions can mostly be ascribed to variation in thermal and hygric factors, often operating in conjunction. Their effects on the vegetation are often mediated by differential water supply. Structuring factors in boreal mires are discussed, and interspecfic interaction as well as abiotic factors are important. The importance of interactions is higher in the bottom layer in the field layer. On a fine scale, boreal mires are considered to conform to the patch dynamics theory of non-equilibrium coexistence of species. On a broad scale, boreal mires appear to be in a dynamic equilibrium with present climatic conditions east of the limit for the onset of erosion. The common conceptual basis for descriptive biogeography and vegetation ecology is emphasized. Arguments in favour of scaling ecological gradients in units of compositional turnover are forwarded, and the properties of one such scaling method, the nonlinear rescaling procedure in DCA ordination, is outlined. The advantage of an integrated approach to ecological problems is emphasized.

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42

Gusarov, A. V., and V. N. Golosov. "INTERNATIONAL SYMPOSIUM “DYNAMICS OF SILT LOAD AND HYDROMORPHOLOGY OF FLUVIAL SYSTEMS” (DUNDEE, SCOTLAND GB)." Geomorphology RAS, no. 2 (August 6, 2015): 106. http://dx.doi.org/10.15356/0435-4281-2007-2-106-108.

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43

Gebler, Daniel, Gerhard Wiegleb, and Krzysztof Szoszkiewicz. "Integrating river hydromorphology and water quality into ecological status modelling by artificial neural networks." Water Research 139 (August 2018): 395–405. http://dx.doi.org/10.1016/j.watres.2018.04.016.

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44

Poppe, Michaela, Jochem Kail, Jukka Aroviita, Mateusz Stelmaszczyk, Marek Giełczewski, and Susanne Muhar. "Assessing restoration effects on hydromorphology in European mid-sized rivers by key hydromorphological parameters." Hydrobiologia 769, no. 1 (October 30, 2015): 21–40. http://dx.doi.org/10.1007/s10750-015-2468-x.

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45

Woodget, Amy S., Robbie Austrums, Ian P. Maddock, and Evelyn Habit. "Drones and digital photogrammetry: from classifications to continuums for monitoring river habitat and hydromorphology." Wiley Interdisciplinary Reviews: Water 4, no. 4 (April 26, 2017): e1222. http://dx.doi.org/10.1002/wat2.1222.

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46

Neglia, Giulia Annalinda. "Urban Morphology and Forms of the Territory: Between Urban and Landscape Design." Land 13, no. 1 (December 28, 2023): 37. http://dx.doi.org/10.3390/land13010037.

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This paper explores the relationship between territory and urban space, discussing the joint development processes of urban and territorial morphologies. The paper argues that territorial structure is a precursor to urban design. It also discusses how landscape architecture can respond to the morphological needs of contemporary urban design as the boundaries between city and territory merge. The introduction and framework review section examines various approaches to studying the relationship between urban morphology and interstitial spaces or unbuilt geographies, which are often still considered empty spaces, physically incorporated but excluded from urban design. It also briefly discusses the role that green spaces and territorial morphologies have played, or not played, in defining urban form from antiquity to modernity. The paper then focuses on the role of hydromorphologies in shaping the urban form of Rome, Boston and Bari. These cities are analyzed as case studies to discuss 20th-century approaches to urban planning in relation to territorial layout. Finally, this study analyzes a marginal area of the metropolitan city of Bari in order to propose possible landscape morphologies of reconnection for the resulting interstitial areas.

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47

Bourdin, L. "Préservation et restauration hydromorphologique des milieux aquatiques, un enjeu majeur sur le bassin Rhône Méditerranée." Techniques Sciences Méthodes, no. 2 (2007): 54–59. http://dx.doi.org/10.1051/tsm/200702054.

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48

Kim, Hyea-Ju, Beom-Kyun Shin, and Won Kim. "A Study on Hydromorphology and Vegetation Features Depending on Typology of Natural Streams in Korea1a." Korean Journal of Environment and Ecology 28, no. 2 (April 30, 2014): 215–34. http://dx.doi.org/10.13047/kjee.2014.28.2.215.

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49

Alcayaga, Hernán, Sebastián Palma, Diego Caamaño, Luca Mao, and Marco Soto-Alvarez. "Detecting and quantifying hydromorphology changes in a chilean river after 50 years of dam operation." Journal of South American Earth Sciences 93 (August 2019): 253–66. http://dx.doi.org/10.1016/j.jsames.2019.04.018.

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50

Keogh, John, Robert Wilkes, and Shane O'Boyle. "A new index for the assessment of hydromorphology in transitional and coastal waters around Ireland." Marine Pollution Bulletin 151 (February 2020): 110802. http://dx.doi.org/10.1016/j.marpolbul.2019.110802.

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Journal articles on the topic 'Hydromorphologie'

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