Zeitschriftenartikel: „Maggiore, Lago, in literature“

1

Steinecke, Hilke. „Frank Erdnüss: Blütenpracht am Lago Maggiore“. Der Palmengarten 74, Nr. 2 (14.06.2018): 160. http://dx.doi.org/10.21248/palmengarten.416.

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Kotzias, Dimitrios, und Elke Anklam. „Gemeinsam für Europa am Lago Maggiore“. Nachrichten aus der Chemie 55, Nr. 10 (Oktober 2007): 991–94. http://dx.doi.org/10.1002/nadc.200748084.

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3

Erdnüß, Frank. „Exoten am Lago Maggiore. Die Exkursion“. Biologie in unserer Zeit 41, Nr. 1 (Februar 2011): 61–68. http://dx.doi.org/10.1002/biuz.201110443.

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4

Falla, Nicole Mélanie, Sonia Demasi, Matteo Caser und Valentina Scariot. „Phytochemical Profile and Antioxidant Properties of Italian Green Tea, a New High Quality Niche Product“. Horticulturae 7, Nr. 5 (27.04.2021): 91. http://dx.doi.org/10.3390/horticulturae7050091.

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The hot beverage commonly known as tea results from the infusion of dried leaves of the plant Camellia sinensis (L.) O. Kuntze. Ranking second only to water for its consumption worldwide, it has always been appreciated since antiquity for its aroma, taste characteristics, and beneficial effects on human health. There are many different processed tea types, including green tea, a non-fermented tea which, due to oxidation prevention maintains the structure of the bioactive compounds, especially polyphenols; these bioactive compounds show a number of benefits for the human health. The main producers of tea are China and India, followed by Kenya, Sri Lanka, Turkey, and Vietnam, however recently new countries are entering the market, with quality niche productions, among which also Italy. The present research aimed to assess the bioactive compounds (polyphenols) and the antioxidant activity of two green teas (the “Camellia d’Oro” tea—TCO, and the “Compagnia del Lago” tea—TCL) produced in Italy, in the Lake Maggiore district, where nurserymen have recently started to cultivate C. sinensis. In this area the cultivation of acidophilic plants as ornamentals has been known since around 1820. Due to the crisis of the floricultural sector, producers have been trying to diversify their product in order to increase their competitiveness, starting to cultivate Italian tea. Their antioxidant activity was assessed, finding a similar or higher antioxidant capacity than in other green teas, as reported in literature. TCO showed a higher antioxidant activity (42,758.86 mmol Fe2+ kg−1; 532.37 µmol TE g−1 DW; 881.08 µmol TE g−1 DW) and phenolic content (14,918.91 mg GAE 100 g−1 DW) than TCL (25,796.61 mmol Fe2+ kg−1; 302.35 µmol TE g−1 DW; 623.44 µmol TE g−1 DW; 8540.42 mg GAE 100 g−1 DW). Through HPLC, a total of thirteen phenolic compounds were identified quantitatively, including catechins, benzoic acids, cinnamic acids, and flavonols, in TCO while only 9 in TCL, and mainly in lower amounts. Albeit with differences, both teas were found to be of quality proving that Italy could have the possibility to grow profitably C. sinensis.

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Stucki, Peter, Moritz Bandhauer, Ulla Heikkilä, Ole Rössler, Massimiliano Zappa, Lucas Pfister, Melanie Salvisberg et al. „Reconstruction and simulation of an extreme flood event in the Lago Maggiore catchment in 1868“. Natural Hazards and Earth System Sciences 18, Nr. 10 (23.10.2018): 2717–39. http://dx.doi.org/10.5194/nhess-18-2717-2018.

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Abstract. Heavy precipitation on the south side of the central Alps produced a catastrophic flood in October 1868. We assess the damage and societal impacts, as well as the atmospheric and hydrological drivers using documentary evidence, observations and novel numerical weather and runoff simulations. The greatest damage was concentrated close to the Alpine divide and Lago Maggiore. An atmospheric reanalysis emphasizes the repeated occurrence of streamers of high potential vorticity as precursors of heavy precipitation. Dynamical downscaling indicates high freezing levels (4000 m a.s.l.), extreme precipitation rates (max. 270 mm 24 h−1) and weather dynamics that agree well with observed precipitation and damage, and with existing concepts of forced low-level convergence, mid-level uplift and iterative northeastward propagation of convective cells. Simulated and observed peak levels of Lago Maggiore differ by 2 m, possibly because the exact cross section of the lake outflow is unknown. The extreme response of Lago Maggiore cannot be attributed to low forest cover. Nevertheless, such a paradigm was adopted by policy makers following the 1868 flood, and used to implement nationwide afforestation policies and hydraulic structures. These findings illustrate the potential of high-resolution, hydrometeorological models – strongly supported by historical methods – to shed new light on weather events and their socio-economic implications in the 19th century.

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Bertoni, Roberto. „Size distribution of particulate organic carbon in Lago Maggiore“. SIL Proceedings, 1922-2010 27, Nr. 5 (Dezember 2000): 2836–39. http://dx.doi.org/10.1080/03680770.1998.11898185.

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7

de Bernardi, R., G. Giussani, M. Manca und D. Ruggiu. „Trophic status and the pelagic system in Lago Maggiore“. Hydrobiologia 191, Nr. 1 (Februar 1990): 1–8. http://dx.doi.org/10.1007/bf00026032.

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8

Morabito, Giuseppe, Alessandro Oggioni, Emanuele Caravati und Pierisa Panzani. „Seasonal morphological plasticity of phytoplankton in Lago Maggiore (N. Italy)“. Hydrobiologia 578, Nr. 1 (März 2007): 47–57. http://dx.doi.org/10.1007/s10750-006-0432-5.

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9

Bernardi, Riccardo de, und Sven E. Jorgensen. „Exergy content in the pelagic food chain of Lago Maggiore“. Lakes and Reservoirs: Research and Management 3, Nr. 2 (Juni 1998): 135–38. http://dx.doi.org/10.1111/j.1440-1770.1998.tb00040.x.

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10

Putyrskaya, V., E. Klemt, S. Röllin, J. A. Corcho-Alvarado und H. Sahli. „Dating of recent sediments from Lago Maggiore and Lago di Lugano (Switzerland/Italy) using 137Cs and 210Pb“. Journal of Environmental Radioactivity 212 (Februar 2020): 106135. http://dx.doi.org/10.1016/j.jenvrad.2019.106135.

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11

Ambrosetti, Walter, Luigi Barbanti und Angelo Rolla. „THE CLIMATE OF LAGO MAGGIORE AREA DURING THE LAST FIFTY YEARS“. Journal of Limnology 65, Nr. 1s (01.09.2006): 1. http://dx.doi.org/10.4081/jlimnol.2006.s1.1.

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12

de Bernardi, R., G. Giussani, M. Manca und D. Ruggiu. „Long-term dynamics of plankton communities in Lago Maggiore (N. Italy)“. SIL Proceedings, 1922-2010 23, Nr. 2 (August 1988): 729–33. http://dx.doi.org/10.1080/03680770.1987.11899700.

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AMBROSETTI, Walter, Luigi BARBANTI und Elisabetta A. CARRARA. „Mechanisms of hypolimnion erosion in a deep lake (Lago Maggiore, N. Italy)“. Journal of Limnology 69, Nr. 1 (01.02.2010): 3. http://dx.doi.org/10.4081/jlimnol.2010.3.

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VISCONTI, Anna, und Marina MANCA. „The invasive appearance of Eudiaptomus gracilis (G.O. Sars 1863) in Lago Maggiore“. Journal of Limnology 69, Nr. 2 (01.08.2010): 353. http://dx.doi.org/10.4081/jlimnol.2010.353.

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15

Lodari, Renata. „Villa San Remigio a Verbania nel paesaggio dei giardini del Lago Maggiore“. Italies, Nr. 8 (01.11.2004): 39–50. http://dx.doi.org/10.4000/italies.2013.

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16

Morabito, Giuseppe, Alessandro Oggioni und Emanuele Caravati. „Decadal trends of pelagic algal biomass capacities in Lago Maggiore (N. Italy)“. SIL Proceedings, 1922-2010 29, Nr. 1 (März 2005): 231–34. http://dx.doi.org/10.1080/03680770.2005.11902003.

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Callieri, C. „Grazing by ciliates and heterotrophic nanoflagellates on picocyanobacteria in Lago Maggiore, Italy“. Journal of Plankton Research 24, Nr. 8 (01.08.2002): 785–96. http://dx.doi.org/10.1093/plankt/24.8.785.

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18

BARBIERI, Alberto, Mauro VERONESI, Marco SIMONA, Stefano MALUSARDI und Viera STRAŠKRABOVÁ. „Limnological survey in eight high mountain lakes located in Lago Maggiore watershed (Switzerland)“. Journal of Limnology 58, Nr. 2 (01.08.1999): 179. http://dx.doi.org/10.4081/jlimnol.1999.179.

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19

CALLIERI, C., und R. PISCIA. „Photosynthetic efficiency and seasonality of autotrophic picoplankton in Lago Maggiore after its recovery“. Freshwater Biology 47, Nr. 5 (25.04.2002): 941–56. http://dx.doi.org/10.1046/j.1365-2427.2002.00821.x.

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20

Menziani, M., S. Pugnaghi, L. Pilan, R. Santangelo und S. Vincenzi. „TDR soil moisture measurements at the Lago Maggiore MAP target area: preliminary results“. Physics and Chemistry of the Earth, Part B: Hydrology, Oceans and Atmosphere 26, Nr. 5-6 (2001): 431–36. http://dx.doi.org/10.1016/s1464-1909(01)00031-4.

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21

Manca, Marina, und Anna Galli Tognota. „Seasonal changes in morphology and size of Daphnia hyalina Leydig in Lago Maggiore“. Hydrobiologia 264, Nr. 3 (Juli 1993): 159–67. http://dx.doi.org/10.1007/bf00007286.

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22

GALASSI, Silvana, Pietro VOLTA, Alcide CALDERONI und Licia GUZZELLA. „Cycling pp'DDT and pp'DDE at a watershed scale: the case of Lago Maggiore (Italy)“. Journal of Limnology 65, Nr. 2 (01.08.2006): 100. http://dx.doi.org/10.4081/jlimnol.2006.100.

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23

de Bernardi, R., G. Giussani und M. Manca. „Seasonal evolution of Cladocera in Lago Maggiore (N. Italy) as influenced by environmental parameters“. SIL Proceedings, 1922-2010 23, Nr. 1 (Januar 1988): 530–34. http://dx.doi.org/10.1080/03680770.1987.11897975.

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24

VISCONTI, Anna, und Marina MANCA. „Seasonal changes in the δ13C and δ15N signatures of the Lago Maggiore pelagic food web“. Journal of Limnology 70, Nr. 2 (01.08.2011): 263. http://dx.doi.org/10.4081/jlimnol.2011.263.

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25

MANCA, Marina. „Invasions and re-emergences: an analysis of the success of Bythotrephes in Lago Maggiore (Italy)“. Journal of Limnology 70, Nr. 1 (01.02.2011): 76. http://dx.doi.org/10.4081/jlimnol.2011.76.

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26

Panziera, L., C. N. James und U. Germann. „Mesoscale organization and structure of orographic precipitation producing flash floods in the Lago Maggiore region“. Quarterly Journal of the Royal Meteorological Society 141, Nr. 686 (03.04.2014): 224–48. http://dx.doi.org/10.1002/qj.2351.

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27

Bravničar, Jernej, Anja Palandačić, Simona Sušnik Bajec und Aleš Snoj. „Neotype designation for Thymallus aeliani Valenciennes, 1848 from a museum topotype specimen and its affiliation with Adriatic grayling on the basis of mitochondrial DNA“. ZooKeys 999 (30.11.2020): 165–78. http://dx.doi.org/10.3897/zookeys.999.56636.

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In 1848, the grayling Thymallus aeliani (Valenciennes) was described from Lake Maggiore, Italy, in the north Adriatic basin. Genetic analyses of the mitochondrial control region showed a unique evolutionary history of grayling inhabiting the rivers of northern Adriatic basin, from the upper reaches of the Po River and its left tributaries in the west to the Soča River in the east, which resulted in the designation of this phylogenetic lineage as Adriatic grayling. Consequently, the name T. aeliani was connected to the Adriatic lineage, re-establishing the validity of this taxon. However, the mitochondrial haplotypes belonging to Adriatic grayling were never compared with the type specimens of T. aeliani, as their whereabouts were unknown. In this study, a neotype for T. aeliani was designated using topotypical specimens stored at the Natural History Museum in Vienna. The neotype (NMW 68027:2 labelled as “Lago Maggiore, Bellotti, 1880”) was designated pursuant to the conditions stipulated in Article 75.3 of the International Code of Zoological Nomenclature. Furthermore, the mitochondrial control region of the neotype was compared to haplotypes of the Adriatic lineage and showed high genetic similarity, which therefore connects the species name T. aeliani to the Adriatic grayling. This crucial step in fixing nomenclatural status of this species is very important for its protection and management.

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Putyrskaya, Victoria, Eckehard Klemt und Stefan Röllin. „Migration of 137Cs in tributaries, lake water and sediment of Lago Maggiore (Italy, Switzerland) – analysis and comparison with Lago di Lugano and other lakes“. Journal of Environmental Radioactivity 100, Nr. 1 (Januar 2009): 35–48. http://dx.doi.org/10.1016/j.jenvrad.2008.10.005.

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29

Ciampittiello, M., H. Saidi, C. Dresti, M. Coluccino, L. Turconi, W. W. Little und F. Luino. „Landslides along the Lago Maggiore western coast (northern Italy): intense rainfall as trigger or concomitant cause?“ Natural Hazards 107, Nr. 2 (22.02.2021): 1225–50. http://dx.doi.org/10.1007/s11069-021-04626-8.

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30

MARCHETTO, Aldo, und Simona MUSAZZI. „Comparison between sedimentary and living diatoms in Lago Maggiore (N. Italy): implications of using transfer functions“. Journal of Limnology 60, Nr. 1 (01.02.2001): 19. http://dx.doi.org/10.4081/jlimnol.2001.19.

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31

KAMENIR, Yury, und Giuseppe MORABITO. „Lago Maggiore oligotrophication as seen from the long-term evolution of its phytoplankton taxonomic size structure“. Journal of Limnology 68, Nr. 1 (01.02.2009): 146. http://dx.doi.org/10.4081/jlimnol.2009.146.

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32

Omair, M., Henry A. Vanderploeg, David J. Jude und Gary L. Fahnenstiel. „First observations of tumor-like abnormalities (exophytic lesions) on Lake Michigan zooplankton“. Canadian Journal of Fisheries and Aquatic Sciences 56, Nr. 10 (01.10.1999): 1711–15. http://dx.doi.org/10.1139/f99-146.

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Tumor-like abnormalities (exophytic lesions) were found on a variety of planktonic calanoid copepods and cladocerans (Diaptomus spp., Epischura lacustris, Limnocalanus macrurus, Polyphemus pediculus, Diaphanosoma sp., and Daphnia galeata mendotae) collected from inshore (3-m depth contour) and offshore (100- to 110-m depth contours) stations of eastern Lake Michigan. The abnormalities, which were quite large relative to animal size and variable in shape, are documented in photographs. Abnormality incidences among species ranged between 0 and 72%. Predatory species of calanoids and cladocerans had higher incidences of tumors than herbivorous species. The abnormalities on some copepods were very similar to cysts described for calanoid copepods in Lago Maggiore, Italy, which like Lake Michigan is undergoing oligotrophication. The recent appearance of the lesions in Europe and North America may indicate an emerging global phenomenon that has a common cause.

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BERTONI, Roberto, Roberta PISCIA und Cristiana CALLIERI. „Horizontal heterogeneity of seston, organic carbon and picoplankton in the photic zone of Lago Maggiore, Northern Italy“. Journal of Limnology 63, Nr. 2 (01.08.2004): 244. http://dx.doi.org/10.4081/jlimnol.2004.244.

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VOLTA, Pietro, und Niels JEPSEN. „The recent invasion of Rutilus rutilus (L.) (Pisces: Cyprinidae) in a large South- Alpine lake: Lago Maggiore“. Journal of Limnology 67, Nr. 2 (01.08.2008): 163. http://dx.doi.org/10.4081/jlimnol.2008.163.

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35

VISCONTI, Anna, Marina MANCA und Riccardo DE BERNARDI. „Eutrophication-like response to climate warming: an analysis of Lago Maggiore (N. Italy) zooplankton in contrasting years“. Journal of Limnology 67, Nr. 2 (01.08.2008): 87. http://dx.doi.org/10.4081/jlimnol.2008.87.

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36

Guilizzoni, Piero, Suzanne N. Levine, Marina Manca, Aldo Marchetto, Andrea Lami, Walter Ambrosetti, Achim Brauer et al. „Ecological effects of multiple stressors on a deep lake (Lago Maggiore, Italy) integrating neo and palaeolimnological approaches“. Journal of Limnology 71, Nr. 1 (19.01.2012): 1. http://dx.doi.org/10.4081/jlimnol.2012.e1.

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37

CASTELLANO, Leonardo, Walter AMBROSETTI, Luigi BARBANTI und Angelo ROLLA. „The residence time of the water in Lago Maggiore (N. Italy): first results from an Eulerian-Lagrangian approach“. Journal of Limnology 69, Nr. 1 (01.02.2010): 15. http://dx.doi.org/10.4081/jlimnol.2010.15.

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38

Morabito, Giuseppe, Alessandro Oggioni und Pierisa Panzani. „Phytoplankton assemblage at equilibrium in large and deep subalpine lakes: a case study from Lago Maggiore (N. Italy)“. Hydrobiologia 502, Nr. 1-3 (Juli 2003): 37–48. http://dx.doi.org/10.1023/b:hydr.0000004268.17068.dc.

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Markey, T. L. „Early celticity in Slovenia and at rhaetic Magrè (Schio)“. Linguistica 46, Nr. 1 (01.12.2006): 145–72. http://dx.doi.org/10.4312/linguistica.46.1.145-172.

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From the area around lakes Maggiore and Como in the west clear across the northern alpine crest of the Italian peninsula to the Balkans (albeit primarily in Slovenia) in the east we find the following varieties of early Continental Celtic: Golaseccan ILepontic (with highly archaic features by virtue of dramatically early attestation, ca. 550-350 BC); Camunic (meagerly recorded, etymologically opaque, but, if anything, probably mainly Celtic) in Valcamonica north of Lago d'Iseo, also beginning about 550 BC; Rhaeto Celtic (also but fragmentarily recorded, ca. 450-40 BC) from various sites such as Vadena (Pfatten) south of Bolzano (Bozen) in the Fritzens Sanseno and Magre Horizons; Carnian (northward from Udine, evidenced chiefly by onomastics, e.g. present-day Cadore < *Catubrigum 'battle-mount') and East Celtic in southwestern Austria and the Balkans (again but fragmentarily retrievable from, for example, Magdalensberg and the onomastics retrievable from Roman necropoli such as that at lg south of the Ljubljana marshes; see Hamp [1976, 1978]).

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Caser, M., A. Berruti, R. Bizioli, V. Bianciotto, M. Devecchi und V. Scariot. „Floriculture and territory – the protection of the traditional Italian tipicity: the case of “La Camelia del Lago Maggiore (PGI)”“. Acta Horticulturae, Nr. 1191 (Februar 2018): 241–50. http://dx.doi.org/10.17660/actahortic.2018.1191.33.

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KÄMPF, LUCAS, ACHIM BRAUER, PETER DULSKI, ANDREA LAMI, ALDO MARCHETTO, STEFANO GERLI, WALTER AMBROSETTI und PIERO GUILIZZONI. „Detrital layers marking flood events in recent sediments of Lago Maggiore (N. Italy) and their comparison with instrumental data“. Freshwater Biology 57, Nr. 10 (03.05.2012): 2076–90. http://dx.doi.org/10.1111/j.1365-2427.2012.02796.x.

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Manca, M. „Exotopic protrusions and ellobiopsid infection in zooplanktonic copepods of a large, deep subalpine lake, Lago Maggiore, in northern Italy“. Journal of Plankton Research 26, Nr. 11 (16.06.2004): 1257–63. http://dx.doi.org/10.1093/plankt/fbh117.

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Manca, Marina, Claudio Ramoni und Patrizia Comoli. „The decline of Daphnia hyalina galeata in Lago Maggiore: a comparison of the population dynamics before and after oligotrophication“. Aquatic Sciences 62, Nr. 2 (August 2000): 142–53. http://dx.doi.org/10.1007/pl00001328.

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Georgis, Jean-François, Frank Roux, Michel Chong und Stephanie Pradier. „Triple-Doppler radar analysis of the heavy rain event observed in the Lago Maggiore region during MAP IOP 2b“. Quarterly Journal of the Royal Meteorological Society 129, Nr. 588 (01.01.2003): 495–522. http://dx.doi.org/10.1256/qj.02.46.

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Bugini, Roberto, und Luisa Folli. „Ubicazione delle cave di pietra da calce utilizzata come materia prima degli intonaci romani nella Lombardia occidentale“. Arqueología de la Arquitectura, Nr. 13 (17.01.2017): 049. http://dx.doi.org/10.3989/arq.arqt.2016.167.

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[it] La calce come materiale da costruzione ebbe larga diffusione nell’architettura romana della Lombardia occidentale. La presenza di carbonato di magnesio è stata per lo più riscontrata negli intonaci dipinti provenienti dai siti romani di Milano. Il carbonato di magnesio testimonia l’impiego di dolomia per la preparazione della calce e rocce di questa composizione affiorano per esteso nelle Prealpi lombarde: dolomie e calcari dolomitici grigio chiari (Dolomia del Salvatore, Ladinico-Anisico), dolomie grigie, talvolta con ciclotemi (Dolomia principale, Norico). Non sono conservate evidenze di cave o di forni romani in quest’area prealpina: i Romani sfruttarono gli stessi affioramenti dolomitici, situati lungo la sponda orientale del lago Maggiore, affioramenti da cui si produsse calce a partire dal Medio Evo in avanti. I depositi fluvio-glaciali del medio corso del fiume Adda tra Brivio e Trezzo (massi, ciottoli di calcari marnosi, calcari e dolomie che affiorano nel bacino fluviale) furono un’altra fonte medievale e moderna di materia prima, soprattutto per produrre una calce debolmente idraulica (chiamata “calce forte”), ma questo tipo di calce è assente negli intonaci romani.

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46

Manca, Marina, Patrizia Comoli und Teresa Spagnuolo. „Length-specific carbon content of theDaphnia population in a large subalpine lake, Lago Maggiore (Northern Italy): The importance of seasonality“. Aquatic Sciences 59, Nr. 1 (März 1997): 48–56. http://dx.doi.org/10.1007/bf02522550.

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47

Bellew, R. Shelton. „Examining the apocalyptic in Roberto Saviano’s Gomorra“. Forum Italicum: A Journal of Italian Studies 52, Nr. 2 (31.01.2018): 505–22. http://dx.doi.org/10.1177/0014585818755358.

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This article examines the apocalyptic in Gomorra ( Saviano, 2006 ). Wu Ming 1 (2008) declared Saviano’s novel to be part of a new body of literature called the “New Italian Epic” based upon the narrative’s seven characteristics. Alessandro Dal Lago (2010) , on the other hand, does not think that Saviano’s work represents a new genre. For him, Ming’s sixth characteristic, the unidentified narrative object, has been the narrative technique of various historical authors such as Giovanni Verga (1978) and almost any work by Jorge Borges, just to name two. This technique is that of a composite narrator, which employs mimesis in combination with a diegetic narrative that alternates between being intradiegetic and extradiegetic according to the author’s whim. In assessing Gomorra, Dal Lago argues that there has always been literature that appears to tell an objective truth but that, in fact, represents the author’s subjective portrayal. He calls this writing style the “heroic rhetoric.” Dal Lago is correct in assessing this rhetorical style, but does not fully explain Saviano’s popular success. This article will review the apocalyptic literature to show how it applies to the narrative of Saviano’s prophetic voice in an eschatological context.

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Bacchi, Baldassare, und Roberto Ranzi. „Hydrological and meteorological aspects of floods in the Alps: an overview“. Hydrology and Earth System Sciences 7, Nr. 6 (31.12.2003): 785–98. http://dx.doi.org/10.5194/hess-7-785-2003.

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Abstract. This introductory paper presents and summarises recent research on meteorological and hydrological aspects of floods in the Alps. The research activities were part of the international research project RAPHAEL (Runoff and Atmospheric Processes for flood HAzard forEcasting and controL) together with experiments within the Special Observing Period-SOP conducted in autumn 1999 for the Mesoscale Alpine Programme —MAP. The investigations were based on both field experiments and numerical simulations, using meteorological and hydrological models, of ten major floods that occurred in the past decade in the European Alps. The two basins investigated were the Ticino (6599 km2) at the Lago Maggiore outlet on the southern side of the Alps and the Ammer catchment (709 km2) in the Bavarian Alps. These catchments and their sub-catchments cover an appropriate range of spatial scales with which to investigate and test in an operational context the potential of both mesoscale meteorological and distributed hydrological models for flood forecasting. From the data analyses and model simulations described in this Special Issue, the major sources of uncertainties for flood forecasts in mid-size mountain basins are outlined and the accuracy flood forecasts is assessed. Keywords: floods, mountain hydrology, meteorological models, Alps

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Manca, Marina, Patrizia Comoli und Teresa Spagnuolo. „Length-specific carbon content of the Daphnia population in a large subalpine lake, Lago Maggiore (Northern Italy): The importance of seasonality“. Aquatic Sciences 59, Nr. 1 (April 1997): 48–56. http://dx.doi.org/10.1007/pl00001306.

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50

Asencio, N., J. Stein, M. Chong und F. Gheusi. „Analysis and simulation of local and regional conditions for the rainfall over the Lago Maggiore Target Area during MAP IOP 2b“. Quarterly Journal of the Royal Meteorological Society 129, Nr. 588 (01.01.2003): 565–86. http://dx.doi.org/10.1256/qj.02.37.

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