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Computing the transport time scales of a stratified lake on the basis of Tonolli’s model
2197PDF: 831XLS: 430HTML: 1354 -
Leaf breakdown in a natural open tropical stream
4331PDF: 1018Supplementary: 268HTML: 930 -
Synchrony in whitefish stock dynamics: disentangling the effects of local drivers and climate
2555PDF: 459Appendix A: 66Appendix B: 64Appendix C: 72Appendix D: 63HTML: 22 -
Multidecadal analysis of Lake Garda water balance
2164PDF: 772Supplementary: 55HTML: 43 -
Deep-mixing and deep-cooling events in Lake Garda: Simulation and mechanisms
1965PDF: 779Supplementary: 134HTML: 91 -
Exploiting high frequency monitoring and satellite imagery for assessing chlorophyll-a dynamics in a shallow eutrophic lake
1995PDF: 313Supplementary 1: 62Supplementary 2: 60Supplementary 3: 63HTML: 77 -
The use of the term ‘limnology’ and its scientometrics consequences for limnologists
1365PDF: 261Dataset: 0Supplementary Table 1: 297Supplementary Table 2: 92HTML: 44 -
Zooplankton biodiversity and community structure vary along spatiotemporal environmental gradients in restored peridunal ponds
4761PDF: 1059Supplementary: 296HTML: 1978 -
Effects of morphology in controlling propagation of density currents in a reservoir using uncalibrated three-dimensional hydrodynamic modeling Effects of morphology in propagation of density currents
2112PDF: 421HTML: 49 -
Behavioural responses of juvenile Daphnia magna to two organophosphorus insecticides
2483PDF: 355Supplementary: 204HTML: 155 -
Temporal changes in nutrients in a deep oligomictic lake: the role of external loads versus climate change
1905PDF: 409Supplementary: 78HTML: 61 -
Limnology for the ornithologist: effects of Lake Maggiore water level on migratory flows
1000PDF: 127Supplementary Tab. 1: 44HTML: 7 -
Fluctuations of Lake Orta water levels: preliminary analyses
3019PDF: 624HTML: 1644 -
Hydrological characteristics of extreme floods in the Klaserie River, a headwater stream in southern Africa
2014PDF: 430Supplementary: 53HTML: 50 -
Daily and seasonal variability of CO2 saturation and evasion in a free flowing and in a dammed river reach
3449PDF: 1102Supplementary: 297HTML: 950