Articles | Volume 17, issue 11
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Historic maps as a data source for socio-hydrology: a case study of the Lake Balaton wetland system, Hungary
Balaton Limnological Institute, Centre for Ecological Research, Hungarian Academy of Sciences, Klebelsberg Kuno út 3, 8237 Tihany, Hungary
Department of Geodesy and Geoinformation, Vienna University of Technology, Gußhausstraße 27–29, 1040 Wien, Austria
Invited contribution by A. Zlinszky, recipient of the EGU Young Scientist Outstanding Poster Paper Award 2010.
Department of Geophysics and Space Science, Institute of Geography and Earth Sciences, Eötvös Loránd University, Pázmány Péter Sétány 1/c, 1117 Budapest, Hungary
A. Zlinszky, G. Timár, R. Weber, B. Székely, C. Briese, C. Ressl, and N. Pfeifer
Solid Earth, 5, 355–369,
A. Zlinszky, G. Timár, R. Weber, B. Székely, C. Briese, C. Ressl, and N. Pfeifer
Solid Earth, 5, 355–369,
Related subject area
Subject: Rivers and Lakes | Techniques and Approaches: Instruments and observation techniquesAssessing the influence of lake and watershed attributes on snowmelt bypass at thermokarst lakesInfluence of vegetation maintenance on flow and mixing: case study comparing full cut with high-coverage conditionsTechnical note: Analyzing river network dynamics and the active length–discharge relationship using water presence sensorsTechnical note: Efficient imaging of hydrological units below lakes and fjords with a floating, transient electromagnetic (FloaTEM) systemDrastic decline of flood pulse in the Cambodian floodplains (Mekong River and Tonle Sap system)Seasonality of density currents induced by differential coolingImplications of variations in stream specific conductivity for estimating baseflow using chemical mass balance and calibrated hydrograph techniquesEnhanced flood hazard assessment beyond decadal climate cycles based on centennial historical data (Duero basin, Spain)Contrasting hydrological and thermal intensities determine seasonal lake-level variations – a case study at Paiku Co on the southern Tibetan PlateauTechnical note: Mobile open dynamic chamber measurement of methane macroseeps in lakesA Fast-Response Automated Gas Equilibrator (FaRAGE) for continuous in situ measurement of CH4 and CO2 dissolved in waterTechnical note: Greenhouse gas flux studies: an automated online system for gas emission measurements in aquatic environmentsEvolution and dynamics of the vertical temperature profile in an oligotrophic lakeLong-term changes in central European river discharge for 1869–2016: impact of changing snow covers, reservoir constructions and an intensified hydrological cycleReliable reference for the methane concentrations in Lake Kivu at the beginning of industrial exploitationSmall dams alter thermal regimes of downstream waterOxycline oscillations induced by internal waves in deep Lake IseoTurbulent mixing and heat fluxes under lake ice: the role of seiche oscillationsNew profiling and mooring records help to assess variability of Lake Issyk-Kul and reveal unknown features of its thermohaline structureEvaluation of lacustrine groundwater discharge, hydrologic partitioning, and nutrient budgets in a proglacial lake in the Qinghai–Tibet Plateau: using 222Rn and stable isotopesLong-term temporal trajectories to enhance restoration efficiency and sustainability on large rivers: an interdisciplinary studyActive heat pulse sensing of 3-D-flow fields in streambedsTechnical note: False low turbidity readings from optical probes during high suspended-sediment concentrationsEffectiveness of distributed temperature measurements for early detection of piping in river embankmentsCitizen observations contributing to flood modelling: opportunities and challengesDead Sea evaporation by eddy covariance measurements vs. aerodynamic, energy budget, Priestley–Taylor, and Penman estimatesTechnical note: Stage and water width measurement of a mountain stream using a simple time-lapse cameraIdentifying, characterizing and predicting spatial patterns of lacustrine groundwater dischargeInformation content of stream level class data for hydrological model calibrationHydrology of inland tropical lowlands: the Kapuas and Mahakam wetlandsTechnical Note: Monitoring of unsteady open channel flows using the continuous slope-area methodApplication of CryoSat-2 altimetry data for river analysis and modellingTechnical Note: Advances in flash flood monitoring using unmanned aerial vehicles (UAVs)Using radon to understand parafluvial flows and the changing locations of groundwater inflows in the Avon River, southeast AustraliaInfluence of environmental factors on spectral characteristics of chromophoric dissolved organic matter (CDOM) in Inner Mongolia Plateau, ChinaDAHITI – an innovative approach for estimating water level time series over inland waters using multi-mission satellite altimetryThe Global Network of Isotopes in Rivers (GNIR): integration of water isotopes in watershed observation and riverine researchA 2600-year history of floods in the Bernese Alps, Switzerland: frequencies, mechanisms and climate forcingTechnical Note: Semi-automated effective width extraction from time-lapse RGB imagery of a remote, braided Greenlandic riverCharacterization of sediment layer composition in a shallow lake: from open water zones to reed belt areasMorphological, hydrological, biogeochemical and ecological changes and challenges in river restoration – the Thur River case studyDynamics of auto- and heterotrophic picoplankton and associated viruses in Lake GenevaSpatio-temporal heterogeneity of riparian soil morphology in a restored floodplainFlood discharge measurement of a mountain river – Nanshih River in TaiwanHydrochemical variability at the Upper Paraguay Basin and Pantanal wetlandMeasurement of spatial and temporal fine sediment dynamics in a small riverTechnical Note: How image processing facilitates the rising bubble technique for discharge measurementDischarge estimation in a backwater affected meandering riverEphemeral stream sensor design using state loggersEvidence for double diffusion in temperate meromictic lakes
Evan J. Wilcox, Brent B. Wolfe, and Philip Marsh
Hydrol. Earth Syst. Sci., 26, 6185–6205,Short summary
We estimated how much of the water flowing into lakes during snowmelt replaced the pre-snowmelt lake water. Our data show that, as lake depth increases, the amount of water mixed into lakes decreased, because vertical mixing is reduced as lake depth increases. Our data also show that the water mixing into lakes is not solely snow-sourced but is a mixture of snowmelt and soil water. These results are relevant for lake biogeochemistry given the unique properties of snowmelt runoff.
Monika Barbara Kalinowska, Kaisa Västilä, Michael Nones, Adam Kiczko, Emilia Karamuz, Andrzej Brandyk, Adam Kozioł, and Marcin Krukowski
Hydrol. Earth Syst. Sci. Discuss.,
Revised manuscript accepted for HESSShort summary
Vegetation is commonly found in rivers and channels. Using field investigations, we evaluated the influence of different vegetation coverages on the flow and mixing in the small naturally vegetated channel. The obtained results are expected to be helpful for practitioners, enlarge our still limited knowledge, and show the further required scientific directions for a better understanding of the influence of vegetation on the flow and mixing of dissolved substances in real natural conditions.
Francesca Zanetti, Nicola Durighetto, Filippo Vingiani, and Gianluca Botter
Hydrol. Earth Syst. Sci., 26, 3497–3516,Short summary
River networks are highly dynamical. Characterizing expansion and retraction of flowing streams is a significant scientific challenge. Electrical resistance sensors were used to monitor stream network patterns in an alpine catchment. Our data show the presence of spatial heterogeneity in network dynamics and that the active length is more sensitive than discharge to small rain events. The study unravels potentials and limitations of the sensors for the characterization of temporary streams.
Pradip Kumar Maurya, Frederik Ersted Christensen, Masson Andy Kass, Jesper B. Pedersen, Rasmus R. Frederiksen, Nikolaj Foged, Anders Vest Christiansen, and Esben Auken
Hydrol. Earth Syst. Sci., 26, 2813–2827,Short summary
In this paper, we present an application of the electromagnetic method to image the subsurface below rivers, lakes, or any surface water body. The scanning of the subsurface is carried out by sailing an electromagnetic sensor called FloaTEM. Imaging results show a 3D distribution of different sediment types below the freshwater lakes. In the case of saline water, the system is capable of identifying the probable location of groundwater discharge into seawater.
Samuel De Xun Chua, Xi Xi Lu, Chantha Oeurng, Ty Sok, and Carl Grundy-Warr
Hydrol. Earth Syst. Sci., 26, 609–625,Short summary
We found that the annual flood at the Cambodian floodplains decreased from 1960 to 2019. Consequently, the Tonle Sap Lake, the largest lake in Southeast Asia, is shrinking. The results are worrying because the local fisheries and planting calendar might be disrupted. This drastic decline of flooding extent is caused mostly by local factors, namely water withdrawal for irrigation and channel incision from sand mining activities.
Tomy Doda, Cintia L. Ramón, Hugo N. Ulloa, Alfred Wüest, and Damien Bouffard
Hydrol. Earth Syst. Sci., 26, 331–353,Short summary
At night or during cold periods, the shallow littoral region of lakes cools faster than their deeper interior. This induces a cold downslope current that carries littoral waters offshore. From a 1-year-long database collected in a small temperate lake, we resolve the seasonality of this current and report its frequent occurrence from summer to winter. This study contributes to a better quantification of lateral exchange in lakes, with implications for the transport of dissolved compounds.
Hydrol. Earth Syst. Sci., 26, 183–195,Short summary
Using specific conductivity (SC) to estimate groundwater inflow to rivers is complicated by bank return waters, interflow, and flows off floodplains contributing to baseflow in all but the driest years. Using the maximum SC of the river in dry years to estimate the SC of groundwater produces the best baseflow vs. streamflow trends. The variable composition of baseflow hinders calibration of hydrograph-based techniques to estimate groundwater inflows.
Gerardo Benito, Olegario Castillo, Juan A. Ballesteros-Cánovas, Maria Machado, and Mariano Barriendos
Hydrol. Earth Syst. Sci., 25, 6107–6132,Short summary
Climate change is expected to increase the intensity of floods, but changes are difficult to project. We compiled historical and modern flood data of the Rio Duero (Spain) to evaluate flood hazards beyond decadal climate cycles. Historical floods were obtained from documentary sources, identifying 69 floods over 1250–1871 CE. Discharges were calculated from reported flood heights. Flood frequency using historical datasets showed the most robust results, guiding climate change adaptation.
Yanbin Lei, Tandong Yao, Kun Yang, Lazhu, Yaoming Ma, and Broxton W. Bird
Hydrol. Earth Syst. Sci., 25, 3163–3177,Short summary
Lake evaporation from Paiku Co on the TP is low in spring and summer and high in autumn and early winter. There is a ~ 5-month lag between net radiation and evaporation due to large lake heat storage. High evaporation and low inflow cause significant lake-level decrease in autumn and early winter, while low evaporation and high inflow cause considerable lake-level increase in summer. This study implies that evaporation can affect the different amplitudes of lake-level variations on the TP.
Frederic Thalasso, Katey Walter Anthony, Olya Irzak, Ethan Chaleff, Laughlin Barker, Peter Anthony, Philip Hanke, and Rodrigo Gonzalez-Valencia
Hydrol. Earth Syst. Sci., 24, 6047–6058,Short summary
Methane (CH4) seepage is the steady or episodic flow of gaseous hydrocarbons from subsurface reservoirs that has been identified as a significant source of atmospheric CH4. The monitoring of these emissions is important and despite several available methods, large macroseeps are still difficult to measure due to a lack of a lightweight and inexpensive method deployable in remote environments. Here, we report the development of a mobile chamber for measuring intense CH4 macroseepage in lakes.
Shangbin Xiao, Liu Liu, Wei Wang, Andreas Lorke, Jason Woodhouse, and Hans-Peter Grossart
Hydrol. Earth Syst. Sci., 24, 3871–3880,Short summary
To better understand the fate of methane (CH4) and carbon dioxide (CO2) in freshwaters, dissolved CH4 and CO2 need to be measured with a high temporal resolution. We developed the Fast-Response Automated Gas Equilibrator (FaRAGE) for real-time in situ measurement of dissolved gases in water. FaRAGE can achieve a short response time (CH4: t95 % = 12 s; CO2: t95 % = 10 s) while retaining a high equilibration ratio and accuracy.
Nguyen Thanh Duc, Samuel Silverstein, Martin Wik, Patrick Crill, David Bastviken, and Ruth K. Varner
Hydrol. Earth Syst. Sci., 24, 3417–3430,Short summary
Under rapid ongoing climate change, accurate quantification of natural greenhouse gas emissions in aquatic environments such as lakes and ponds is needed to understand regulation and feedbacks. Building on the rapid development in wireless communication, sensors, and computation technology, we present a low-cost, open-source, automated and remotely accessed and controlled device for carbon dioxide and methane fluxes from open-water environments along with tests showing their potential.
Zvjezdana B. Klaić, Karmen Babić, and Mirko Orlić
Hydrol. Earth Syst. Sci., 24, 3399–3416,Short summary
Fine-resolution lake temperature measurements (2 min, 15 depths) show different lake responses to atmospheric forcings: (1) continuous diurnal oscillations in the temperature in the first 5 m of the lake, (2) occasional diurnal oscillations in the temperature at depths from 7 to 20 m, and (3) occasional surface and internal seiches. Due to the sloped lake bottom, surface seiches produced the high-frequency oscillations in the lake temperatures with periods of 9 min at depths from 9 to 17 m.
Erwin Rottler, Till Francke, Gerd Bürger, and Axel Bronstert
Hydrol. Earth Syst. Sci., 24, 1721–1740,Short summary
In the attempt to identify and disentangle long-term impacts of changes in snow cover and precipitation along with reservoir constructions, we employ a set of analytical tools on hydro-climatic time series. We identify storage reservoirs as an important factor redistributing runoff from summer to winter. Furthermore, our results hint at more (intense) rainfall in recent decades. Detected increases in high discharge can be traced back to corresponding changes in precipitation.
Bertram Boehrer, Wolf von Tümpling, Ange Mugisha, Christophe Rogemont, and Augusta Umutoni
Hydrol. Earth Syst. Sci., 23, 4707–4716,Short summary
Dissolved methane in Lake Kivu (East Africa) represents a precious energy deposit, but the high gas loads have also been perceived as a threat by the local population. Our measurements confirm the huge amount of methane and carbon dioxide present, but do not support the current theory of a significant recharge. Direct measurements of gas pressure indicate no imminent danger due to limnic eruptions. A continuous survey is mandatory to support responsible action during industrial exploitation.
André Chandesris, Kris Van Looy, Jacob S. Diamond, and Yves Souchon
Hydrol. Earth Syst. Sci., 23, 4509–4525,Short summary
We found that small dams in rivers alter the thermal regimes of downstream waters in two distinct ways: either only the downstream daily minimum temperatures increase, or both the downstream daily minimum and maximum temperatures increase. We further show that only two physical dam characteristics can explain this difference in temperature response: (1) residence time, and (2) surface area. These results may help managers prioritize efforts to restore the fragmented thermalscapes of rivers.
Giulia Valerio, Marco Pilotti, Maximilian Peter Lau, and Michael Hupfer
Hydrol. Earth Syst. Sci., 23, 1763–1777,Short summary
This paper provides experimental evidence of the occurrence of large and periodic movements induced by the wind at 95 m in depth in Lake Iseo, where a permanent chemocline is located. These movements determine vertical oscillations of the oxycline up to 20 m. Accordingly, in 3 % of the sediment area alternating redox conditions occur, which might force unsteady sediment–water fluxes. This finding has major implications for the internal matter cycle in Lake Iseo.
Georgiy Kirillin, Ilya Aslamov, Matti Leppäranta, and Elisa Lindgren
Hydrol. Earth Syst. Sci., 22, 6493–6504,Short summary
We have discovered transient appearances of strong turbulent mixing beneath the ice of an Arctic lake. Such mixing events increase heating of the ice base up to an order of magnitude and can significantly accelerate ice melting. The source of mixing was identified as oscillations of the entire lake water body triggered by strong winds over the lake surface. This previously unknown mechanism of ice melt may help understand the link between the climate conditions and the seasonal ice formation.
Peter O. Zavialov, Alexander S. Izhitskiy, Georgiy B. Kirillin, Valentina M. Khan, Boris V. Konovalov, Peter N. Makkaveev, Vadim V. Pelevin, Nikolay A. Rimskiy-Korsakov, Salmor A. Alymkulov, and Kubanychbek M. Zhumaliev
Hydrol. Earth Syst. Sci., 22, 6279–6295,Short summary
This paper reports the results of field surveys conducted in Lake Issyk-Kul in 2015–2017 and compares the present-day data with the available historical records. Our data do not confirm the reports of progressive warming of the deep Issyk-Kul waters as suggested in some previous publications. However, they do indicate a positive trend of salinity in the lake’s interior over the last 3 decades. An important newly found feature is a persistent salinity maximum at depths of 70–120 m.
Xin Luo, Xingxing Kuang, Jiu Jimmy Jiao, Sihai Liang, Rong Mao, Xiaolang Zhang, and Hailong Li
Hydrol. Earth Syst. Sci., 22, 5579–5598,
David Eschbach, Laurent Schmitt, Gwenaël Imfeld, Jan-Hendrik May, Sylvain Payraudeau, Frank Preusser, Mareike Trauerstein, and Grzegorz Skupinski
Hydrol. Earth Syst. Sci., 22, 2717–2737,Short summary
In this study we show the relevance of an interdisciplinary study for improving restoration within the framework of a European LIFE+ project on the French side of the Upper Rhine (Rohrschollen Island). Our results underscore the advantage of combining functional restoration with detailed knowledge of past trajectories in complex hydrosystems. We anticipate our approach will expand the toolbox of decision-makers and help orientate functional restoration actions in the future.
Eddie W. Banks, Margaret A. Shanafield, Saskia Noorduijn, James McCallum, Jörg Lewandowski, and Okke Batelaan
Hydrol. Earth Syst. Sci., 22, 1917–1929,Short summary
This study used a portable 56-sensor, 3-D temperature array with three heat pulse sources to measure the flow direction and magnitude below the water–sediment interface. Breakthrough curves from each of the sensors were analyzed using a heat transport equation. The use of short-duration heat pulses provided a rapid, accurate assessment technique for determining dynamic and multi-directional flow patterns in the hyporheic zone and is a basis for improved understanding of biogeochemical processes.
Nicholas Voichick, David J. Topping, and Ronald E. Griffiths
Hydrol. Earth Syst. Sci., 22, 1767–1773,Short summary
This paper describes instances in the Grand Canyon study area and a laboratory experiment in which very high suspended-sediment concentrations result in incorrectly low turbidity recorded with a commonly used field instrument. If associated with the monitoring of a construction or dredging project, false low turbidity could result in regulators being unaware of environmental damage caused by the actually much higher turbidity.
Silvia Bersan, André R. Koelewijn, and Paolo Simonini
Hydrol. Earth Syst. Sci., 22, 1491–1508,Short summary
Backward erosion piping is the cause of a significant percentage of failures and incidents involving dams and river embankments. In the past 20 years fibre-optic Distributed Temperature Sensing (DTS) has proved to be effective for the detection of leakages and internal erosion in dams. This work investigates the effectiveness of DTS for monitoring backward erosion piping in river embankments. Data from a large-scale piping test performed on an instrumented dike are presented and discussed.
Thaine H. Assumpção, Ioana Popescu, Andreja Jonoski, and Dimitri P. Solomatine
Hydrol. Earth Syst. Sci., 22, 1473–1489,Short summary
Citizens can contribute to science by providing data, analysing them and as such contributing to decision-making processes. For example, citizens have collected water levels from gauges, which are important when simulating/forecasting floods, where data are usually scarce. This study reviewed such contributions and concluded that integration of citizen data may not be easy due to their spatio-temporal characteristics but that citizen data still proved valuable and can be used in flood modelling.
Jutta Metzger, Manuela Nied, Ulrich Corsmeier, Jörg Kleffmann, and Christoph Kottmeier
Hydrol. Earth Syst. Sci., 22, 1135–1155,Short summary
This paper is motivated by the need for more precise evaporation rates from the Dead Sea (DS) and methods to estimate and forecast evaporation. A new approach to measure lake evaporation with a station located at the shoreline, also transferable to other lakes, is introduced. The first directly measured DS evaporation rates are presented as well as applicable methods for evaporation calculation. These results enable us to further close the DS water budget and to facilitate the water management.
Pauline Leduc, Peter Ashmore, and Darren Sjogren
Hydrol. Earth Syst. Sci., 22, 1–11,Short summary
We show the utility of ground-based time-lapse cameras for automated monitoring of stream stage and flow characteristics. High-frequency flow stage, water surface width and other information on the state of flow can be acquired for extended time periods with simple local calibration using a low-cost time-lapse camera and a few simple field measurements for calibration and for automated image selection and sorting. The approach is a useful substitute or complement to the conventional stage data.
Christina Tecklenburg and Theresa Blume
Hydrol. Earth Syst. Sci., 21, 5043–5063,Short summary
We characterized groundwater–lake exchange patterns and identified their controls based on extensive field measurements. Our measurement design bridges the gap between the detailed local characterisation and low resolution regional investigations. Results indicated strong spatial variability in groundwater inflow rates: large scale inflow patterns correlated with topography and the groundwater flow field and small scale patterns correlated with grainsize distributions of the lake sediment.
H. J. Ilja van Meerveld, Marc J. P. Vis, and Jan Seibert
Hydrol. Earth Syst. Sci., 21, 4895–4905,Short summary
We tested the usefulness of stream level class data for hydrological model calibration. Only two stream level classes, e.g. above or below a rock in the stream, were already informative, particularly when the boundary was chosen at a high stream level. There was hardly any improvement in model performance when using more than five stream level classes. These results suggest that model based streamflow time series can be obtained from citizen science based water level class data.
Hidayat Hidayat, Adriaan J. Teuling, Bart Vermeulen, Muh Taufik, Karl Kastner, Tjitske J. Geertsema, Dinja C. C. Bol, Dirk H. Hoekman, Gadis Sri Haryani, Henny A. J. Van Lanen, Robert M. Delinom, Roel Dijksma, Gusti Z. Anshari, Nining S. Ningsih, Remko Uijlenhoet, and Antonius J. F. Hoitink
Hydrol. Earth Syst. Sci., 21, 2579–2594,Short summary
Hydrological prediction is crucial but in tropical lowland it is difficult, considering data scarcity and river system complexity. This study offers a view of the hydrology of two tropical lowlands in Indonesia. Both lowlands exhibit the important role of upstream wetlands in regulating the flow downstream. We expect that this work facilitates a better prediction of fire-prone conditions in these regions.
Kyutae Lee, Ali R. Firoozfar, and Marian Muste
Hydrol. Earth Syst. Sci., 21, 1863–1874,Short summary
Accurate estimation of stream/river flows is important in many aspects, including public safety during floods, effective uses of water resources for hydropower generation and irrigation, and environments. In this paper, we investigated a feasibility of the continuous slope area (CSA) method which measures dynamic changes in instantaneous water surface elevations, and the results showed promising capabilities of the suggested method for the accurate estimation of flows in natural streams/rivers.
Raphael Schneider, Peter Nygaard Godiksen, Heidi Villadsen, Henrik Madsen, and Peter Bauer-Gottwein
Hydrol. Earth Syst. Sci., 21, 751–764,Short summary
We use water level observations from the CryoSat-2 satellite in combination with a river model of the Brahmaputra River, extracting satellite data over a dynamic river mask derived from Landsat imagery. The novelty of this work is the use of the CryoSat-2 water level observations, collected using a complex spatio-temporal sampling scheme, to calibrate a hydrodynamic river model. The resulting model accurately reproduces water levels, without precise knowledge of river bathymetry.
Matthew T. Perks, Andrew J. Russell, and Andrew R. G. Large
Hydrol. Earth Syst. Sci., 20, 4005–4015,Short summary
Unmanned aerial vehicles (UAVs) have the potential to capture information about the earth’s surface in dangerous and previously inaccessible locations. Here we present a method whereby image acquisition and subsequent analysis have enabled the highly dynamic and oft-immeasurable hydraulic phenomenon present during high-energy flash floods to be quantified at previously unattainable spatial and temporal resolutions.
Ian Cartwright and Harald Hofmann
Hydrol. Earth Syst. Sci., 20, 3581–3600,Short summary
This paper uses the natural geochemical tracer Rn together with streamflow measurements to differentiate between actual groundwater inflows and water that exits the river, flows through the near-river sediments, and subsequently re-enters the river downstream (parafluvial flow). Distinguishing between these two components is important to understanding the water balance in gaining streams and in managing and protecting surface water resources.
Z. D. Wen, K. S. Song, Y. Zhao, J. Du, and J. H. Ma
Hydrol. Earth Syst. Sci., 20, 787–801,Short summary
The study indicated that CDOM in rivers had higher aromaticity, molecular weight, and vascular plant contribution than in terminal lakes in the Hulun Buir plateau, Northeast China. The autochthonous sources of CDOM in plateau waters were higher than in other freshwater rivers reported in the literature. Study of the optical–physicochemical correlations is helpful in the evaluation of the potential influence of water quality factors on non-water light absorption in plateau water environments.
C. Schwatke, D. Dettmering, W. Bosch, and F. Seitz
Hydrol. Earth Syst. Sci., 19, 4345–4364,
J. Halder, S. Terzer, L. I. Wassenaar, L. J. Araguás-Araguás, and P. K. Aggarwal
Hydrol. Earth Syst. Sci., 19, 3419–3431,Short summary
We introduce a new online global database of riverine water stable isotopes (Global Network of Isotopes in Rivers) and evaluate its longer-term data holdings. A regionalized, cluster-based precipitation isotope model was used to compare measured to predicted isotope compositions of riverine catchments. The study demonstrated that the seasonal isotopic composition and variation of river water can be predicted, which will improve the application of water stable isotopes in rivers.
L. Schulte, J. C. Peña, F. Carvalho, T. Schmidt, R. Julià, J. Llorca, and H. Veit
Hydrol. Earth Syst. Sci., 19, 3047–3072,Short summary
A 2600-year long composite palaeoflood record is reconstructed from high-resolution delta plain sediments of the Hasli-Aare floodplain on the northern slope of the Swiss Alps. Natural proxies compiled from sedimentary, geochemical and geomorphological data were calibrated by textual and factual sources and instrumental data. Geomorphological, historical and instrumental data provide evidence for flood damage intensities and discharge estimations of severe and catastrophic historical floods.
C. J. Gleason, L. C. Smith, D. C. Finnegan, A. L. LeWinter, L. H Pitcher, and V. W. Chu
Hydrol. Earth Syst. Sci., 19, 2963–2969,Short summary
Here, we give a semi-automated processing workflow to extract hydraulic parameters from over 10,000 time-lapse images of the remote Isortoq River in Greenland. This workflow allows efficient and accurate (mean accuracy 79.6%) classification of images following an automated similarity filtering process. We also give an effective width hydrograph (a proxy for discharge) for the Isortoq using this workflow, showing the potential of this workflow for enhancing understanding of remote rivers.
I. Kogelbauer and W. Loiskandl
Hydrol. Earth Syst. Sci., 19, 1427–1438,
M. Schirmer, J. Luster, N. Linde, P. Perona, E. A. D. Mitchell, D. A. Barry, J. Hollender, O. A. Cirpka, P. Schneider, T. Vogt, D. Radny, and E. Durisch-Kaiser
Hydrol. Earth Syst. Sci., 18, 2449–2462,
A. Parvathi, X. Zhong, A. S. Pradeep Ram, and S. Jacquet
Hydrol. Earth Syst. Sci., 18, 1073–1087,
B. Fournier, C. Guenat, G. Bullinger-Weber, and E. A. D. Mitchell
Hydrol. Earth Syst. Sci., 17, 4031–4042,
Hydrol. Earth Syst. Sci., 17, 1951–1962,
A. T. Rezende Filho, S. Furian, R. L. Victoria, C. Mascré, V. Valles, and L. Barbiero
Hydrol. Earth Syst. Sci., 16, 2723–2737,
Y. Schindler Wildhaber, C. Michel, P. Burkhardt-Holm, D. Bänninger, and C. Alewell
Hydrol. Earth Syst. Sci., 16, 1501–1515,
K. P. Hilgersom and W. M. J. Luxemburg
Hydrol. Earth Syst. Sci., 16, 345–356,
H. Hidayat, B. Vermeulen, M. G. Sassi, P. J. J. F. Torfs, and A. J. F. Hoitink
Hydrol. Earth Syst. Sci., 15, 2717–2728,
R. Bhamjee and J. B. Lindsay
Hydrol. Earth Syst. Sci., 15, 1009–1021,
C. von Rohden, B. Boehrer, and J. Ilmberger
Hydrol. Earth Syst. Sci., 14, 667–674,
Adams, J.: Active tilting of the United States midcontinent – Geodetic and geomorphic evidence, Geology, 8, 442–446, https://doi.org/10.1130/0091-7613(1980)8<442:ATOTUS>2.0.CO, 1980.
Anthony, E. J. and Blivi, A. B.: Morphosedimentary evolution of a delta-sourced, drift-aligned sand barrier-lagoon complex, western Bight of Benin, Mar. Geol., 158, 161–176, https://doi.org/10.1016/s0025-3227(98)00170-4, 1999.
Appleby, P. G.: Three decades of dating recent sediments by fallout radionuclides: a review, Holocene, 18, 83–93, https://doi.org/10.1177/0959683607085598, 2008.
Armas, I., Nistoran, D. E. G., Osaci-Costache, G., and Brasoveanu, L.: Morpho-dynamic evolution patterns of Subcarpathian Prahova River (Romania), Catena, 100, 83–99, https://doi.org/10.1016/j.catena.2012.07.007, 2013.
Aston, M.: Interpreting the landscape – Landscape archaeology and local history, Taylor and Francis, London and New York, 1–165, 1985.
Baker, V.: Palaeofloods and extended discharge records, in: Palaeohydrology, Understanding global change, edited by: Gregory, K. J. and Benito, G., Wiley, Chichester, 2003.
Bartos-Elekes, Z.: Digital analyses concerning Honter's map, Acta Geoda. Geophys. Hu., 45, 3–8, https://doi.org/10.1556/AGeod.45.2010.1.2, 2010.
Bendefy, L.: Szintezési munkálatok Magyarországon 1820–1920, Akadémiai Kiadó, Budapest, 736 pp., 1958.
Bendefy, L.: Geokinetic and crustal structure conditions of Hungary as recorded by repeated precision levelings, Acta Geol. Hu., 8, 395–411, 1964.
Bendefy, L. and Nagy, I.: A Balaton évszázados partvonalváltozásai, 1 ed., M\Huszaki Könyvkiadó, Budapest, 215 pp., 1969.
Bendefy, L.: Krieger Sámuel, Hidrológiai Tájékoztató, 11, 3–7, 1972.
Bondesan, A. and Furlanetto, P.: Artificial fluvial diversions in the mainland of the Lagoon of Venice during the 16th and 17th centuries inferred by historical cartography analysis, Geomorphologie, 2, 175–199, 2012.
Braga, G. and Gervasoni, S.: Evolution of the Po River, Italy – an example of the application of historic maps, in: Historical changes of large alluvial rivers: Western Europe, edited by: Petts, G., Moeller, H., and Roux, A. L., Wiley, Chichester, 113–126, 1989.
Bravard, J.-P., Amoros, C., and Pautou, G.: Impact of civil engineering works on the successions of communities in a fluvial system – a methodological and predictive approach applied to a section of the upper Rhone river, France, Oikos, 47, 92–111, https://doi.org/10.2307/3565924, 1986.
Bravard, J.-P.: Cartography of rivers in France, in: Historical change of large alluvial rivers, Western Europe, edited by: Petts, G., Moeller, H., and Roux, A. L., Wiley, Chichester, 95–111, 1989.
Bravard, J.-P.: Discontinuities in braided patterns: The River Rhone from Geneva to the Camargue delta before river training, Geomorphology, 117, 219–233, https://doi.org/10.1016/j.geomorph.2009.01.020, 2010.
Brown, A. G.: Global environmental change and the Palaeohydrology of Western Europe: a review, in: Palaeohydrology: Understanding global change, edited by: Gregory, K. J. and Benito, G., Wiley, Chichester, 2003.
Bruna, V., Krovakova, K., and Nedbal, V.: Historical landscape structure in the spring area of the Blanice river, Southern Bohemia – An example of the importance of old maps, Acta Geod. Geophys. Hu., 45, 48–55, https://doi.org/10.1556/AGeod.45.2010.1.8, 2010.
Cholnoky, J.: A Balaton hidrográfiája, in: A Balaton tudományos tanulmányozásának eredményei, edited by: Lóczy, L., Franklin Társulat, Budapest, 1–318, 1918.
Comiti, F., Da Canal, M., Surian, N., Mao, L., Picco, L., and Lenzi, M. A.: Channel adjustments and vegetation cover dynamics in a large gravel bed river over the last 200 years, Geomorphology, 125, 147–159, https://doi.org/10.1016/j.geomorph.2010.09.011, 2011.
Coops, H., Beklioglu, M., and Crisman, T. L.: The role of water-level fluctuations in shallow lake ecosystems – workshop conclusions, Hydrobiologia, 506, 23–27, https://doi.org/10.1023/b:hydr.0000008595.14393.77, 2003.
Craciunescu, V., Flueraru, C., and Stancalie, G.: The usage of the historical cartographic datasets and the remote sensing data for the better understanding and mapping of the 2006 Danube floods in Romania, Acta Geod. Geophys. Hu., 45, 112–119, https://doi.org/10.1556/AGeod.45.2010.1.16, 2010.
Cserny, T. and Nagy-Bodor, E.: Limnogeology of Lake Balaton, Hungary, in: Lake basins through space and time, edited by: Gierlowski-Kordesch, E. H., and Kelts, K. R., AAPG Stud. Geol., 46, 605–618, 2000.
Day, R. H., Holz, R. K., and Day, J. W.: An inventory of wetland impoundments in the coastal zone of Louisiana, USA – Historical trends, Environ. Manag., 14, 229–240, 1990.
Di Baldassarre, G., Viglione, A., Carr, G., Kuil, L., Salinas, J. L., and Blöschl, G.: Socio-hydrology: conceptualising human-flood interactions, Hydrol. Earth Syst. Sci., 17, 3295–3303, https://doi.org/10.5194/hess-17-3295-2013, 2013.
Dobai, A.: Somogy Megye az Első katonai Felmérés (1782–1785) idején, Somogy megyei levéltár múltjából, 14, edited by: József, K., Somogy Megyei Levéltár, Kaposvár, 72 pp., 1983.
Dömötörfy, Z., Reeder, D., and Pomogyi, P.: Changes in the macro-vegetation of the Kis-Balaton Wetlands over the last two centuries: a GIS perspective, Hydrobiologia, 506, 671–679, 2003.
Dullinger, S., Essl, F., Rabitsch, W., Erb, K.-H., Gingrich, S., Haberl, H., Hulber, K., Jarosik, V., Krausmann, F., Kuhn, I., Pergl, J., Pysek, P., and Hulme, P. E.: Europe's other debt crisis caused by the long legacy of future extinctions, P. Natl. Acad. Sci. USA, 110, 7342–7347, https://doi.org/10.1073/pnas.1216303110, 2013.
Dumont, S. and Debarbat, S.: The academician astronomers travelling in the 18th century, Comptes Rendus De L'Academie Des Sciences Serie II., Fascicule B-Mecanique Physique Astronomie, 327, 415–429, 1999.
Endreny, T.: A global initiative for Hydro-Socio-Ecological watershed research, Water Resources Impact, 3, 20–25, 2001.
Feier, I. and Rădoane, M.: Dinamica în plan orizontal a Albiei Minore a râului Someşu Mic, înainte de lucrările hidrotehnice majore (1870–1968), Analele Universităţii "Ştefan cel Mare" Suceava, Secţiunea Geografie, 16, 5–22, 2007.
Fodor, L., Bada, G., Csillag, G., Horváth, E., Ruszkiczay-Rüdiger, Z., Palotás, K., Síhegyi, F., Timár, G., Cloetingh, S., and Horvath, F.: An outline of neotectonic structures and morphotectonics of the western and central Pannonian Basin, Tectonophysics, 410, 15–41, 2005.
Fouache, E., Gruda, G., Mucaj, S., and Nikolli, P.: Recent geomorphological evolution of the deltas of the rivers Seman and Vjosa, Albania, Earth Surf. Proc. Land., 26, 793–802, https://doi.org/10.1002/esp.222, 2001.
Gercsák, G.: The first printed isobath map, Acta Geod. Geophys. Hu., 44, 17–26, https://doi.org/10.1556/AGeod.44.2009.1.3, 2009.
Gerten, D.: A vital link: water and vegetation in the Anthropocene, Hydrol. Earth Syst. Sci., 17, 3841–3852, https://doi.org/10.5194/hess-17-3841-2013, 2013.
Gilvear, D. J.: Fluvial geomorphology and river engineering: future roles utilizing a fluvial hydrosystems framework, Geomorphology, 31, 229–245, https://doi.org/10.1016/s0169-555x(99)00086-0, 1999.
Gimmi, U., Lachat, T., and Buergi, M.: Reconstructing the collapse of wetland networks in the Swiss lowlands 1850–2000, Landscape Ecol., 26, 1071–1083, https://doi.org/10.1007/s10980-011-9633-z, 2011.
Gober, P. and Wheater, H. S.: Socio-hydrology and the science-policy interface: a case study of the Saskatchewan River Basin, Hydrol. Earth Syst. Sci. Discuss., 10, 6669–6693, https://doi.org/10.5194/hessd-10-6669-2013, 2013.
Gráczer, Z., Czifra, T., Kiszely, M., Mónus, P., and Zsíros, T.: Hungarian National Seismological Bulletin, Kövesligethy Radó Seismological Observatory, Budapest, 359 pp., 2012.
Gregory, K. J. and Benito, G.: Potential of palaeohydrology in relation to global change, in: Palaeohydrology: Understanding global change, edited by: Gregory, K. J., and Benito, G., Wiley, Chichester, 3–15, 2003a.
Gregory, K. J. and Benito, G.: Concluding perspective, in: Palaeohydrology: Understanding global change, edited by: Gregory, K. J., and Benito, G., Wiley, Chichester, 382–385, 2003b.
Gregory, K. J.: The human role in changing river channels, Geomorphology, 79, 172–191, https://doi.org/10.1016/j.geomorph.2006.06.018, 2006.
Gyucha, A., Duffy, P. R., and Frolking, T. A.: The Körös Basin from the Neolithic to the Habsburgs: Linking Settlement Distributions with Pre-Regulation Hydrology Through Multiple Data Set Overlay, Geoarchaeology, 26, 392–419, https://doi.org/10.1002/gea.20350, 2011.
Harman, C. and Troch, P. A.: Darwinian hydrology: can the methodology Charles Darwin pioneered help hydrologic science?, Hydrol. Earth Syst. Sci. Discuss., 10, 6407–6444, https://doi.org/10.5194/hessd-10-6407-2013, 2013.
HELP Task Force: The design and implementation strategy of the HELP initiative, Technical documents in Hydrology, UNESCO, Paris, 62 pp., 2001.
Herget, J.: Holocene development of the River Lippe Valley, Germany: A case study of anthropogenic influence, Earth Surf. Proc. Land., 25, 293–305, https://doi.org/10.1002/(SICI)1096-9837(200003)25:3<293::AID-ESP63>3.0.CO;2-F, 2000.
Herget, J., Bremer, E., Coch, T., Dix, A., Eggenstein, G., and Ewald, K.: Engineering impact on river channels in the river Rhine catchment, Erdkunde, 59, 294–320, 2005.
Hobo, N., Makaske, B., Middelkoop, H., and Wallinga, J.: Reconstruction of floodplain sedimentation rates: a combination of methods to optimize estimates, Earth Surf. Proc. Land., 35, 1499–1515, https://doi.org/10.1002/esp.1986, 2010.
Hoffmann, T., Thorndycraft, V. R., Brown, A. G., Coulthard, T. J., Damnati, B., Kale, V. S., Middelkoop, H., Notebaert, B., and Walling, D. E.: Human impact on fluvial regimes and sediment flux during the Holocene: Review and future research agenda, Global Planet. Change, 72, 87–98, https://doi.org/10.1016/j.gloplacha.2010.04.008, 2010.
Hofstätter, E.: Beiträge zur Geschichte der österreichischen Landesaufnahmen, I. Teil, Bundesamt für Eich- und Vermessungswesen, Wien, 196 pp., 1989.
Hooke, J. M. and Redmond, C. E.: Use of cartographic sources for analysing river channel change with examples from Britain, U.K., in: Historical change of large alluvial rivers: Western Europe, edited by: Petts, G. E., Moeller, H., and Roux, A. L., Wiley, Chichester, 79–94, 1989.
Iványi, K., Kása, I., and Guti, G.: 3th IAD Conference – Living Danube – Proceedings, 3th IAD Conference – Living Danube, Szentendre, Hungary, 279–283, 2012.
Jabaloy-Sanchez, A., Jose Lobo, F., Azor, A., Barcenas, P., Miguel Fernandez-Salas, L., Diaz del Rio, V., and Vicente Perez-Pena, J.: Human-driven coastline changes in the Adra River deltaic system, southeast Spain, Geomorphology, 119, 9–22, https://doi.org/10.1016/j.geomorph.2010.02.004, 2010.
James, A.: Time and the persistence of alluvium: River engineering, fluvial geomorphology, and mining sediment in California, Geomorphology, 31, 265–290, https://doi.org/10.1016/s0169-555x(99)00084-7, 1999.
Jankó, A.: Magyarország topográfiai felmérései 1763-1950, 1 ed., A Hadtörténeti Intézet és Múzeum Könyvtára, Argumentum Kiadó, Budapest, 2007.
Joó, I.: Recent vertical surface movements in the Carpathian Basin, Tectonophysics, 202, 129–134, 1992.
Kern, Z., Morgós, A., and Grynaeus, A.: Reconstructed precipitation for Southern Bakony Mountains (Transdanubia, Hungary) back to AD 1467 based on ring widths of oak trees, Időjárás, 113, 299–314, 2009.
Kiss, T., Fiala, K., and Sipos, G.: Alterations of channel parameters in response to river regulation works since 1840 on the Lower Tisza River (Hungary), Geomorphology, 98, 96–110, https://doi.org/10.1016/j.geomorph.2007.02.027, 2008.
Klimek, K. and Trafas, K.: Young-Holocene changes in the course of the Dunajec river in the Beskid Sadecki Mts. (Western Carpathians), Studia Geomorphologica Carpatho-Balcanica, 6, 85–90, 1972.
Kovács, G.: The advantages of using the second military survey maps in fluvial studies, Acta Geod. Geophys. Hu., 45, 64–70, https://doi.org/10.1556/AGeod.45.2010.1.10, 2010.
Krejci, J. and Cajthaml, J.: Müller's maps of the Czech lands and their analysis, Acta Geod. Geophys. Hu., 44, 27–38, https://doi.org/10.1556/AGeod.44.2009.1.4, 2009.
Kremer, K.: Giant Lake Geneva tsunami in AD 563, Nat. Geosci., 5, 840–840, https://doi.org/10.1038/ngeo1656, 2012.
Kretschmer, I., Dörflinger, J., and Wawrik, F.: Österreichische Kartografie, Wiener Schriften zur Geographie und Regionalforschung, Institut für Geographie und Regionalforschung der Universität Wien, Wien, 318 pp., 2004.
Kunszt, G., Kovács, O.: www.muemlekem.hu, (last access: 14.06.2013), 2012.
Large, A. R. G.: Historical channel-floodplain dynamics along the River Trent, Appl. Geogr., 16, 191–209, 1996.
Lazarus (Secretarius): Tabula Hungariae ad quatuor latera. Eine kurze unnd warhafftige beschreibung des Ungerlands, Johannes Cuspinian, Ingostadt, 1528.
Leys, K. F. and Werritty, A.: River channel planform change: software for historical analysis, Geomorphology, 29, 107–120, https://doi.org/10.1016/s0169-555x(99)00009-4, 1999.
Lóczy, L.: A Balaton környékének geológiai képződményei és ezeknek vidékek szerinti telepedése, in: A Balaton tudományos tanulmányozásának eredményei, edited by: Lóczy, L., Franklin Társulat, Budapest, 1913.
Longhitano, S. and Colella, A.: Geomorphology, sedimentology and recent evolution of the anthropogenically modified Simeto River delta system (eastern Sicily, Italy), Sediment. Geol., 194, 195–221, https://doi.org/10.1016/j.sedgeo.2006.06.004, 2007.
Lotz, G.: A Balaton vízszintje a XIX. század első felében, Vízügyi Közlemények, 3, 337–341, 1973.
Manville, V., Hodgson, K. A., and Nairn, I. A.: A review of break-out floods from volcanogenic lakes in New Zealand, New Zeal. J. Geol. Geop., 50, 131–150, 2007.
Márton, M. and Gede, M.: Virtual Globes Museum: http://terkeptar.elte.hu/vgm/pubs.php?lang=en, (last access: 08.05.2013), 2009.
Mather, P. M.: Computer processing of remotely sensed images, John Wiley and Sons Ltd, Chichester, 324 pp., 2006.
Meissner, D. M.: Die Regulirung des Plattensees, Allgemeine Bauzeitung Wien, 27, 257–284, 1867.
Mészáros, J.: The georeferencing method of the 1:5000 scale Danube maps, e-Perimetron, 7, 45–49, 2012.
Molnár, G. and Timár, G.: Mosaicking of the 1:75 000 sheets of the Third Military Survey of the Habsburg Empire, Acta Geod. Geophys. Hu., 44, 115–120, https://doi.org/10.1556/AGeod.44.2009.1.11, 2009.
Molnár, G.: Making a georeferenced mosaic of historical map series using constrained polynomial fit, Acta Geod. Geophys. Hu., 45, 24–30, https://doi.org/10.1556/AGeod.45.2010.1.5, 2010.
Molnár, G. and Kutics, K.: Foreseen hydrological changes drive efforts to formulate water balance improvement measures as part of the management options of adaptation at Lake Balaton, Hungary, EGU General Assembly, Vienna, Austria, EGU2013-12296, 2013.
Mossa, J. and McLean, M.: Channel planform and land cover changes on a mined river floodplain, Appl. Geogr., 17, 43–54, 1997.
Nováky, B.: A Balaton vízpótlása és az éghajlat, Vízügyi Közlemények, 87, 105–123, 2005.
Ostendorp, W.: Dieback of reeds in Europe – a critical review of literature, Aquat. Bot., 35, 5–26, 1989.
Padisák, J.: Általános Limnológia, 1 ed., ELTE Eötvös Kiadó, Budapest, 1, 310 pp., 2005.
Passmore, D. G. and Macklin, M. G.: Late Holocene channel and floodplain development in a wandering gravel-bed river: The River South Tyne at Lambley, northern England, Earth Surface Processes and Landforms, 25, 1237–1256, https://doi.org/10.1002/1096-9837(200010)25:11<1237::AID-ESP134>3.0.CO;2-S, 2000.
Pasternack, G. B., Brush, G. S., and Hilgartner, W. B.: Impact of historic land-use change on sediment delivery to a Chesapeake Bay subestuarine delta, Earth Surf. Proc. Land., 26, 409–427, https://doi.org/10.1002/esp.189, 2001.
Petrovszki, J. and Mészáros, J.: The Great Hungarian Plain in the sheets of the Habsburg Military Surveys and some historical maps – A case study of the Körös/Cris drainage basin, Acta Geoda. Geophys. Hu., 45, 56–63, https://doi.org/10.1556/AGeod.45.2010.1.9, 2010.
Petrovszki, J. and Timár, G.: Channel sinuosity of the Körös River system, Hungary/Romania, as possible indicator of the neotectonic activity, Geomorphology, 122, 223–230, https://doi.org/10.1016/j.geomorph.2009.11.009, 2010.
Petrovszki, J., Székely, B., and Timár, G.: A systematic overview of the coincidences of river sinuosity changes and tectonically active structures in the Pannonian Basin, Global Planet. Change, 98, 109–121, https://doi.org/10.1016/j.gloplacha.2012.08.005, 2012.
Pettersen, B. R.: The first astro-geodetic reference frame in Norway 1779-1815, Acta Geod. Geophys. Hu., 44, 67–78, https://doi.org/10.1556/AGeod.44.2009.1.7, 2009.
Petts, G.: Historical analysis of fluvial hydrosystems, in: Historical changes of large alluvial rivers: Western Europe, edited by: Petts, G. E., Moeller, H., and Roux, A. L., Wiley, Chichester, 1–18, 1989.
Pišút, P.: Channel evolution of the pre-channelized Danube River in Bratislava, Slovakia (1712–1886), Earth Surf. Proc. Land., 27, 369–390, https://doi.org/10.1002/esp.333, 2002.
Pišút, P.: Evolution of the meandering Lower Morava River (West Slovakia) during the first half of the 20th century, Geomorphologica Slovaca, 6, 55–68, 2006.
Podobnikar, T.: Georeferencing and quality assessment of Josephine Survey maps for the mountainous region in the Triglav National Park, Acta Geod. Geophys. Hu., 44, 49–66, https://doi.org/10.1556/AGeod.44.2009.1.6, 2009.
Popov, D., Markovic, S. B., and Štrbac, D.: Generations of meanders in Serbian part of Tisa valley, Geographical Institute "Jovan Cvijic" Sasa collection of papers, 58, 29–42, 2008.
Raczky, P. and Anders, A.: Régészeti kutatások egy késő neolitikus településen – Polgár-Bosnyákdomb (Előzetes jelentés), Archaeológiai \`Ertesítő, 134, 5–21, 2009.
Rice, S. P., Lancaster, J., and Kemp, P.: Experimentation at the interface of fluvial geomorphology, stream ecology and hydraulic engineering and the development of an effective, interdisciplinary river science, Earth Surf. Proc. Land., 35, 64–77, https://doi.org/10.1002/esp.1838, 2010.
Rumsey, D. and Williams, M.: Historical maps in GIS, in: Past Time, Past Place - GIS for History, 1 Edn., edited by: Knowles, A. K., ESRI Press, Redlands, CA, USA, 1–19, 2002.
Rychtář, J.:Moll's map collection: http://mapy.mzk.cz/en/, (last access: 08.05.2013), 2012.
Sabatier, F., Samat, O., Ullmann, A., and Suanez, S.: Connecting large-scale coastal behaviour with coastal management of the Rhone delta, Geomorphology, 107, 79–89, https://doi.org/10.1016/j.geomorph.2006.09.026, 2009.
Sági, K.: A Balaton vízállástendenciái 1863-ig a történeti és kartográfiai adatok tükrében, A Veszprém megyei múzeumok közleményei, 7, 441–468, 1968.
Sear, D. A. and Arnell, N. W.: The application of palaeohydrology in river management, Catena, 66, 169–183, https://doi.org/10.1016/j.catena.2005.11.009, 2006.
Síkhegyi, F.: Active structural evolution of the western and central parts of the Pannonian basin: a geomorphological approach, EGU Stephan Mueller Special Publication Series, 3, 203–216, 2002.
Sivapalan, M., Savenije, H. H. G., and Bloeschl, G.: Socio-hydrology: A new science of people and water, Hydrol. Process., 26, 1270–1276, https://doi.org/10.1002/hyp.8426, 2012.
Srinivasan, V., Lambin, E. F., Gorelick, S. M., Thompson, B. H., and Rozelle, S.: The nature and causes of the global water crisis: Syndromes from a meta-analysis of coupled human-water studies, Water Resour. Res., 48, 1–15, https://doi.org/10.1029/2011wr011087, 2012.
Srinivasan, V.: Socio-hydrology: patterns, feedbacks, goals and trajectories in coupled human-water systems, Catchment Science Symposium, Vienna, Austria, 13 April 2013, 2013.
Srinivasan, V., Seto, K. C., Emerson, R., and Gorelick, S. M.: The impact of urbanization on water vulnerability: A coupled human-environment system approach for Chennai, India, Global Environ. Chang., 23, 229–239, https://doi.org/10.1016/j.gloenvcha.2012.10.002, 2013.
Stegena, L.: Distortions on Lazarus maps, in: Lazarus Secretarius – The first Hungarian mapmaker and his work, edited by: Stegena, L., Akadémiai Kiadó, Budapest, 97–102, 1982.
Sümegi, P.: Early Neolithic man and riparian environment in the Carpathian Basin, in: Morgenrot der Kulturen, edited by: Jerem, E. and Raczky, P., Archaeolingua Press, Budapest, 53–60, 2003.
Sümegi, P., Gulyás, S., and Jakab, G.: Holocene paleoclimatic and paleohydrological changes in Lake Balaton as inferred from a complex quantitative environmental historical study of a lacustrine sequence of the Szigliget embayment, Documenta Praehistorica, 35, 33–43, 2008.
Szabó, M., Timár, G., and Gyǒri, H.: A Csicsói-holtág (Alsó-Csallóköz) kialakulása és fejlödése – a tájhasználat és a vizes élőhelytípusok változása, Tájökológiai Lapok, 2, 267–286, 2004.
Szanto, Z. and Medzihradszky, Z.: Holocene environmental changes in western Hungary, Radiocarbon, 46, 691–699, 2004.
Székely, B.: Rediscovering the old treasures of cartography – what an almost 500 year-old map can tell to a geoscientist, Acta Geod. Geophys. Hu., 44, 3–16, https://doi.org/10.1556/AGeod.44.2009.1.2, 2009.
Szilassi, P., Jordan, G., van Rompaey, A., and Csillag, G.: Impacts of historical land use changes on erosion and agricultural soil properties in the Kali Basin at Lake Balaton, Hungary, Catena, 68, 96–108, 2006.
Taylor, M. P. and Lewin, J.: River behaviour and Holocene alluviation: The River Severn at Welshpool, mid-Wales, UK, Earth Surf. Proc. Land., 21, 77–91, https://doi.org/10.1002/(SICI)1096-9837(199601)21:1<77::AID-ESP547>3.0.CO;2-O, 1996.
Timár, G., Sümegi, P., Geiger, J., Szántó, Z., and Bodor, E.: Story of an oxbow lake: An outlook to the Holocene tectonics and climate of the Great Hungarian Plain, in: EGS Stephan Mueller Topical Conference Series, Quantitative Neotectonics and seismic hazard assessment: New integrated approaches for environmental management, Balatonfüred, Hungary, 2001.
Timár, G.: Controls on channel sinuosity changes: a case study of the Tisza River, the Great Hungarian Plain, Quaternary Sci. Rev., 22, 2199–2207, https://doi.org/10.1016/s0277-3791(03)00145-8, 2003.
Timár, G., Lévai, P., Molnár, G., and Varga, J.: A második világháború német katonai térképeinek koordinátarendszere, Geodézia és Kartográfia, 56, 28–35, 2004.
Timár, G. and Gábris, G.: Estimation of water conductivity of the natural flood channels on the Tisza flood-plain, the Great Hungarian Plain, Geomorphology, 98, 250–261, https://doi.org/10.1016/j.geomorph.2006.12.031, 2008.
Timár, G., Molnár, G., Székely, B., and Plihál, K.: Lázár térképe és a ptolemaioszi vetület, Geodézia és Kartográfia, 60, 20–26, 2008a.
Timár, G., Székely, B., Molnár, G., Ferencz, C., Kern, A., Galambos, C., Gercsák, G., and Zentai, L.: Combination of historical maps and satellite images of the Banat region - Re-appearance of an old wetland area, Global Planet. Change, 62, 29–38, https://doi.org/10.1016/j.gloplacha.2007.11.002, 2008b.
Timár, G.: System of the 1:28800 scale sheets of the Second Military Survey in Tirol and Salzburg, Acta Geod. Geophys. Hu., 44, 95–104, https://doi.org/10.1556/AGeod.44.2009.1.9, 2009.
Timár, G., Biszak, S., Székely, B., and Molnár, G.: Digitized maps of the Habsburg military surveys: overview of the projects of Arcanum Ltd. (Hungary), in: Preservation in digital cartography, edited by: Jobst, M., Lecture Notes in Geoinformation and Cartography, Springer, Berlin-Heidelberg, 273–283, 2010a.
Timár, G., Csillag, G., Székely, B., Molnár, G., Galambos, C., and Czanik, C.: A Balaton legnagyobb kiterjedésének rekonstrukciója a függőleges kéregmozgások figyelembevételével, Földtani Közlöny, 140, 455–462, 2010b.
Timár, G., Molnár, G., Székely, B., and Plihál, K.: Orientation of the map of Lazarus (1528) of Hungary – result of the Ptolemian projection?, in: Cartography in Central and Eastern Europe, edited by: Gartner, G., and Ortag, F., Lecture Notes in Geoinformatics and Cartography, Springer, Berlin-Heidelberg, 487–496, 2010c.
Timár, G. and Mugnier, C. J.: Rectification of the Romanian 1 : 75 000 map series, prior to World War I, Acta Geod. Geophys. Hu., 45, 89–96, https://doi.org/10.1556/AGeod.45.2010.1.13, 2010.
Tiron, L.: Delta du Danube – Bras de St. George/Mobilité morphologique et dynamique hydro-sedimentaire depuis 150 ans, Geo-Eco-Marina Publications, 4, 1–280, 2010.
Toth, A. J.: River archaeology – a new tool for historical hydrology, 24th Conference of The Danubian Countries on The Hydrological Forecasting and Hydrological Bases of Water Management, Bled, Slovenia, 1–8, 2008.
Virág, Á.: A Balaton Múltja és Jelene, 1 Edn., Egri nyomda, Eger, 904 pp., 1998.
Virág, Á.: A Sió és a Balaton közös története, 1 Edn., Közlekedési Dokumentációs Kft., Budapest, 437 pp., 2005.
Wallinga, J.: Optically stimulated luminescence dating of fluvial deposits: a review, Boreas, 31, 303–322, 2002.
Wetzel, R., G: Limnology, 3 Edn., Academic Press, London, 1066 pp., 2001.
Widlok, T., Aufgebauer, A., Bradtmoeller, M., Dikau, R., Hoffmann, T., Kretschmer, I., Panagiotopoulos, K., Pastoors, A., Peters, R., Schaebitz, F., Schlummer, M., Solich, M., Wagner, B., Weniger, G.-C., and Zimmermann, A.: Towards a theoretical framework for analyzing integrated socio-environmental systems, Quatern. Int., 274, 259–272, https://doi.org/10.1016/j.quaint.2012.01.020, 2012.
Yaeger, M. A., Sivapalan, M., McIsaac, G. F., and Cai, X.: Comparative analysis fo hydrologic signatures in two agricultural watersheds in east-central Illinois: legacies of the past to inform the future, Hydrol. Earth Sys. Sci. Discuss., 10, 6515–6558, https://doi.org/10.5194/hessd-10-6515-2013, 2013.
Zamolyi, A., Szekely, B., Draganits, E., and Timar, G.: Neotectonic control on river sinuosity at the western margin of the Little Hungarian Plain, Geomorphology, 122, 231–243, https://doi.org/10.1016/j.geomorph.2009.06.028, 2010.
Ziliani, L. and Surian, N.: Evolutionary trajectory of channel morphology and controlling factors in a large gravel-bed river, Geomorphology, 173, 104–117, https://doi.org/10.1016/j.geomorph.2012.06.001, 2012.
Zimova, R., Pestak, J., and Veverka, B.: Historical military mapping of the Czech lands – Cartographic Analysis, International Conference on Cartography and GIS, Borovets, Bulgaria, 1–7, 2006.
Zlinszky, A. and Molnár, G.: The first bathymetric maps of Lake Balaton, Hungary, European Geosciences Union General Assembly 2008, Vienna, 2008.
Zlinszky, A., Székely, B., and Clement, A.: Comparing sediment load and deposit thickness values in the eastern embayment of shallow Lake Balaton, Hungary, European Geosciences Union General Assembly 2008, Wien, Austria, 13–18 April 2008, SRef-ID: 1607-7962/gra/EGU2008-A-06101, 2008.
Zlinszky, A. and Molnár, G.: Georeferencing the first bathymetric maps of Lake Balaton, Hungary, Acta Geod. Geophys. Hu., 44, 79–94, https://doi.org/10.1556/AGeod.44.2009.1.8, 2009.
Zlinszky, A.: Measuring historic water levels of Lake Balaton and the neighbouring valleys, Acta Geod. Geophys. Hu., 45, 39–47, https://doi.org/10.1556/AGeod.45.2010.1.7, 2010.
Zólyomi, B., and Nagy, L.: A Balaton múltja a pollensztratigráfiai vizsgálatok tükrében, in: 100 éves a Balatonkutatás, XXXII. Hidrobiológus napok, Tihany, 1991, 25–32, 1992.