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1

Zavatarelli, M., and N. Pinardi. "The Adriatic Sea modelling system: a nested approach." Annales Geophysicae 21, no. 1 (January 31, 2003): 345–64. http://dx.doi.org/10.5194/angeo-21-345-2003.

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Abstract. A modelling system for the Adriatic Sea has been built within the framework of the Mediterranean Forecasting System Pilot Project. The modelling system consists of a hierarchy of three numerical models (whole Mediterranean Sea, whole Adriatic Sea, Northern Adriatic Basin) coupled among each other by simple one-way, off-line nesting techniques, to downscale the larger scale flow field to highly resolved coastal scale fields. Numerical simulations have been carried out under climatological surface forcing. Simulations were aimed to assess the effectiveness of the nesting techniques and the skill of the system to reproduce known features of the Adriatic Sea circulation phenomenology (main circulation features, dense water formation,flow at the Otranto Strait and coastal circulation characteristics over the northern Adriatic shelf), in view of the pre-operational use of the modelling system. This paper describes the modelling system setup, and discusses the simulation results for the whole Adriatic Sea and its northern basin, comparing the simulations with the observed climatological circulation characteristics. Results obtained with the northern Adriatic model are also compared with the corresponding simulations obtained with the coarser resolution Adriatic model. Key words. Oceanography: general (continental shelf processes; numerical modelling) – Oceanography: physical (general circulation)
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2

Del Negro, Paola, Paola Ramani, Elizabeth Braun, Sergio Predonzani, and Vincenzo Zuccarello. "Dynamics of picocyanobacteria in the Northern Adriatic Sea." Algological Studies/Archiv für Hydrobiologie, Supplement Volumes 83 (December 19, 1996): 447–54. http://dx.doi.org/10.1127/algol_stud/83/1996/447.

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3

Papetti, Chiara, Antonio Di Franco, Lorenzo Zane, Paolo Guidetti, Valeria De Simone, Marianna Spizzotin, Barbara Zorica, Vanja Čikeš Keč, and Carlotta Mazzoldi. "Single population and common natal origin for Adriatic Scomber scombrus stocks: evidence from an integrated approach." ICES Journal of Marine Science 70, no. 2 (January 15, 2013): 387–98. http://dx.doi.org/10.1093/icesjms/fss201.

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Abstract Papetti, C., Di Franco, A., Zane, L., Guidetti, P., De Simone, V., Spizzotin, M., Zorica, B., Čikeš Keč, V. and Mazzoldi, C. 2013. Single population and common natal origin for Adriatic Scomber scombrus stocks: evidence from an integrated approach – ICES Journal of Marine Science, 70: 387–398. In order to implement proper fishery management strategies aimed at avoiding stock declines, information about connectivity among stocks and populations is critically required. In this perspective, the present study investigated population structure of the Atlantic mackerel Scomber scombrus in the northern–central Adriatic Sea by integrating multiple approaches (analysis of fisheries data, population genetics, and otolith chemistry). Monthly data of fishery landings indicate a latitudinal trend along the western Adriatic coast, with Atlantic mackerel disappearing from the northern waters in winter, corresponding to the reproductive season. Population genetic analyses by genotyping of eight microsatellites clearly point to the presence of a single panmictic population in the northern–central Adriatic Sea. Otolith cores of samples from the northern–central Adriatic were chemically homogeneous, suggesting a common spawning ground. These results strongly suggest that Atlantic mackerel perform an autumn–winter migration in the northern–central Adriatic Sea, from the northern to the central sector, to reach a single spawning ground, and that a single population is present in this area. Considering that S. scombrus has shown a marked decline in the last 40 years in the Adriatic, this study highlights a potential high vulnerability to collapse by overfishing for the Atlantic mackerel stocks in this geographic area.
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4

Mikac, Barbara, Adriana Giangrande, and Margherita Licciano. "Sabellidae and Fabriciidae (Polychaeta) of the Adriatic Sea with particular retrospect to the Northern Adriatic and the description of two new species." Journal of the Marine Biological Association of the United Kingdom 93, no. 6 (March 19, 2013): 1511–24. http://dx.doi.org/10.1017/s0025315412001993.

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Sabellidae is the second most diverse polychaete family in the Adriatic Sea, after Syllidae. Herein we report the updated list of the Sabellidae and Fabriciidae families in the Adriatic Sea deriving both from literature data and presently conducted researches in the northern Adriatic. During these researches polychaetes were sampled from three offshore soft-bottom and three coastal rocky shore stations. Among the analysed material three Sabellidae species are new records for the Adriatic fauna, while four Sabellidae and one Fabriciidae species were recorded for the first time in the northern part. Two new species were found and described: Amphicorina rovignensis spec. nov. and Megalomma pseudogesae spec. nov. These findings increase the number of Sabellidae taxa recorded in the northern Adriatic from 29 to 38. Our results point out the lack of the recent taxonomic studies in the area, but might also indicate the widening of the species areal. Taking into consideration that studies on only six stations raised the number of known sabellid taxa from the area by 31%, our results support the need for the regular taxonomic updating of the polychaete fauna in the northern Adriatic.
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5

Kraus, R., N. Supić, and R. Precali. "Factors favouring phytoplankton blooms in the northern Adriatic: towards the northern Adriatic empirical ecological model." Ocean Science 12, no. 1 (January 15, 2016): 19–37. http://dx.doi.org/10.5194/os-12-19-2016.

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Abstract. Influenced by one of the largest Mediterranean rivers, Po, the northern Adriatic (NA) production is highly variable seasonally and interannually. The changes are especially pronounced between winters and seemingly reflect on total Adriatic bioproduction of certain species (anchovy). We analysed the long-term changes in the phytoplankton production in the region, as derived from monthly oceanographic cruises, in relation to concomitant geostrophic currents distribution in the area and to Po River discharge rates in days preceding the cruises. In winter and early spring the phytoplankton abundances depended on existing circulation fields, in summer and autumn they were related to Po River discharge rates 1–15 days earlier and on concomitant circulation fields, while in late spring phytoplankton abundances increased 1–3 days after high Po River discharge rates regardless of the circulation fields. During the entire year the phytoplankton abundances were dependent on forcing of the previous 1–12 months of surface fluxes and/or Po River rates. The role of wind was uncertain but that was partly due to unmatched sampling time frames between meteorological and sea data. Low evaporation rates in November reflected significantly on the next February circulation pattern and, although with somewhat lower significance, on large phytoplankton blooms in the same month. We showed that the role of wind in evaporative flux enhancements is not straightforward as evaporative fluxes are highly dependent on other factors, e.g. air–sea temperature difference. Wind-induced vertical mixing was only sporadically related to phytoplankton abundances. From 1990 to 2004 a shift towards large winter bioproduction induced by circulation changes appeared. The investigations performed represent the preliminary actions in the construction of an empirical ecological model of the NA which can be used in the sustainable economy of the region, as well as for validation of the numerical ecological model of the region, which is currently being developed.
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6

Horvath, Kristian, Stjepan Ivatek-Šahdan, Branka Ivančan-Picek, and Vanda Grubišić. "Evolution and Structure of Two Severe Cyclonic Bora Events: Contrast between the Northern and Southern Adriatic." Weather and Forecasting 24, no. 4 (August 1, 2009): 946–64. http://dx.doi.org/10.1175/2009waf2222174.1.

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Abstract While statistical analyses and observations show that severe bora with maximum gusts exceeding 40 m s−1 can occur in all parts of the Adriatic, the bora research to date has been mainly focused on the dynamics and structure of severe bora in the northern Adriatic. Examined to a significantly lesser degree is a less predictable counterpart in the southern Adriatic, where the Dinaric Alps are higher, broader, and steeper, and where the upwind bora layer is generally less well defined. Identification of the main differences in the sequence of mesoscale and macroscale events leading to the onset of bora in the northern and southern parts of the eastern Adriatic is of fundamental importance for its forecasting. To this end, presented here is a comparative analysis of the evolution and structure of two typical severe cyclonic bora events—one “northern” (7–8 November 1999) and one “southern” (6–7 May 2005) event. The analysis utilizes airborne, radiosonde, and ground-based observations, as well as the hydrostatic Aire Limitée Adaptation Dynamique Developement International (ALADIN/HR) mesoscale model simulations. It is shown that the development of a severe bora in both the northern and southern Adriatic is critically dependent on the synoptic setting to create an optimal set of environmental conditions. For severe bora in the northern Adriatic, these conditions include a strong forcing of the northeasterly low-level jet and pronounced discontinuities in the upstreamflow structure that promote layering, such as lower- to midtropospheric inversions and environmental critical levels. The development of severe bora in the southern Adriatic is crucially dependent on the establishment of a considerably deeper upstream layer that is able to overcome the strong blocking potential of the southern Dinaric Alps. While the upstream layering is less pronounced, it is closely tied to the presence of a cyclone in the southern Adriatic or over the southern Balkan peninsula. The upstream atmospheric layering is shown to strongly modulate bora behavior, and different phases of severe bora, related to the presence or absence of upstream layering, are shown to occur within a single bora episode. Furthermore, the presence of a mountain-parallel upper-level jet aloft appears to impede severe bora development in both the northern and southern Adriatic.
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7

Manzi, D., and L. Mazzucchelli. "Analysis of Northern adriatic sea surges." Water Science and Technology 32, no. 7 (October 1, 1995): 71–78. http://dx.doi.org/10.2166/wst.1995.0204.

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A decision support system for Coastal Resource Management (from now on called CRM) has been developed in the PC-Windows graphic environment. CRM includes the following modules: a 2-D and a 3-D time dependent barotropic numerical model, a two-layer baroclinic model, a diffusion equation solver. Analytic tests have been done both for the 2-D and the 3-D model; in the paper a validation and calibration of the 2-D model is presented using data collected in Northern Adriatic sea (Trieste and Venice).
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8

Supić, Nastjenjka, Romina Kraus, Milivoj Kuzmić, Elio Paschini, Robert Precali, Aniello Russo, and Ivica Vilibić. "Predictability of northern Adriatic winter conditions." Journal of Marine Systems 90, no. 1 (February 2012): 42–57. http://dx.doi.org/10.1016/j.jmarsys.2011.08.008.

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9

Prasnikar, Janez, Vesna Zabkar, and Tanja Rajkovic. "Should Italians, Croats and Slovenes Work Together in Developing a Northern Adriatic Tourist Destination?" South East European Journal of Economics and Business 2, no. 2 (November 1, 2007): 57–68. http://dx.doi.org/10.2478/v10033-007-0006-0.

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Should Italians, Croats and Slovenes Work Together in Developing a Northern Adriatic Tourist Destination?The article assesses opportunities for creating a macro-tourist destination in the region of the Northern Adriatic. Research was based on a survey of more than 1700 summer tourists in three different sea towns, namely Grado in Italy, Opatija in Croatia and Portorož in Slovenia in 2004. The three countries share a common past under the Austro-Hungarian monarchy and are headed for a common future within the European Union. Survey results of tourists' motivations and destination quality perceptions support the notion that the Northern Adriatic is considered by many central Europeans as the "sea closest to home". Thus, EU efforts under the framework of the Cohesion Policy of EU regions could also be adopted in the area of joint destination management of the Northern Adriatic. A Destination Management Organization for the three regions should be established as the main agent of change in the destination management of the region.
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10

Kraus, R., N. Supić, and R. Precali. "Factors favouring large organic production in the northern Adriatic: towards the northern Adriatic empirical ecological model." Ocean Science Discussions 12, no. 3 (June 25, 2015): 1219–62. http://dx.doi.org/10.5194/osd-12-1219-2015.

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Анотація:
Abstract. Influenced by one of the largest Mediterranean rivers, Po, the northern Adriatic production is highly variable seasonally and interannually. The changes are especially pronounced between winters and seemingly reflect on total Adriatic bioproduction of certain species (anchovy). We analysed the long-term changes in the phytoplankton production at the transect in the region, as derived from monthly oceanographic cruises, in relation to concomitant geostrophic currents distribution in the area and in the Po River discharge rates in days preceding the cruises. In winter and early spring the phyto-abundances depended on existing circulation fields, in summer and autumn they were related to 1–15 days earlier Po River discharge rates and on concomitant circulation fields, while in late spring phyto-abundances increased 1–3 days after high Po River discharge rates regardless of circulation fields. During the entire year the phyto-abundances were dependant on forcing of the previous 1–12 months of surface fluxes and/or Po River rates. Large February blooms are, as well as February circulation patterns, precondited by low evaporation rates in previous November. From 1990 to 2004 a shift towards large winter bioproduction induced by circulation changes appeared. Performed investigations represent the preliminary actions in building of an empirical ecological model of the northern Adriatic which can be used in the sustainable economy of the region, however also in validation of the numerical ecological model of the region, which is currently being developed.
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11

Plavšić, Marta, Senka Terzic, Marijan Ahel, and C. M. G. van den Berg. "Folic acid in coastal waters of the Adriatic Sea." Marine and Freshwater Research 53, no. 8 (2002): 1245. http://dx.doi.org/10.1071/mf02044.

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The concentration of folic acid (FA), an important constituent of the vitamin B group, was determined over a period of 2 years in the water column of a small meromictic saline lake on the eastern Adriatic coast (Rogoznica Lake), as well as in the western part of the northern Adriatic Sea. The FA concentration was over the range of 0.1–13.5 nM in the oxic part of Rogoznica Lake, and 0.1–22 nM in the northern Adriatic, with a maximum of 22 nM in the upper layer of the water column, possibly caused by the impact of Po River freshets on the FA concentrations. A weak but statistically significant correlation was established between photosynthetic pigment zeaxanthin, a characteristic biomarker of cyanobacteria, and FA in the oxic layer of the Rogoznica Lake (r2 = 0.3967; n = 29; P < 0.01), indicating cyanobacteria as a possible source of FA in this ecosystem. A statistically significant correlation (r2 = 0.36; n = 18; P < 0.01) between the two parameters was also found for the surface layer of the northern Adriatic (0 m). However, a low contribution of cyanobacteria to the total photosynthetic biomass in the northern Adriatic, and a lack of correlation between FA and zeaxanthin in the deeper layers of the water column, suggested that cyanobacteria were probably not the main source of FA in these waters. A stronger relationship (r2�= 0.46; n = 16; P < 0.01) between FA and chlorophyll b was found for the top 10 m of the northern Adriatic, indicating green algae as one of the possible sources of FA.
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12

Dulčić, Jakov, Bojan Marčeta, Valter Žiža, Armin Pallaoro, and Lovrenc Lipej. "Northern extension of the range of the vadigo Campogramma glaycos (Pisces: Carangidae) from the Adriatic Sea." Journal of the Marine Biological Association of the United Kingdom 83, no. 4 (August 2003): 877–78. http://dx.doi.org/10.1017/s0025315403007951h.

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One juvenile specimen of the vadigo Campogramma glaycos was caught on 5 December 2000 in Piran Bay (northern Adriatic). This represents a northernmost extension in the known range of this species in the Adriatic Sea (and Mediterranean), and first record of a juvenile specimen in the Adriatic Sea.
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13

Bettoso, Nicola, and Jakov Dulicié. "First record of the oilfish Ruvettus pretiosus (Pisces: Gempylidae) in the northern Adriatic Sea." Journal of the Marine Biological Association of the United Kingdom 79, no. 6 (December 1999): 1145–46. http://dx.doi.org/10.1017/s0025315499001496.

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14

Wolf, Marion A., Katia Sciuto, Christine A. Maggs, Antonella Petrocelli, Ester Cecere, Alessandro Buosi, and Adriano Sfriso. "Merging the cryptic genera Radicilingua and Calonitophyllum (Delesseriaceae, Rhodophyta): molecular phylogeny and taxonomic revision." Algae 36, no. 3 (September 15, 2021): 165–74. http://dx.doi.org/10.4490/algae.2021.36.7.18.

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Radicilingua Papenfuss and Calonitophyllum Aregood are two small genera of the family Delesseriaceae that consist of only three and one taxonomically accepted species, respectively. The type species of these genera, Radicilingua thysanorhizans from England and Calonitophyllum medium from the Americas, are morphologically very similar, with the only recognized differences being vein size and procarp development. To date, only other two species were recognized inside the genus Radicilingua: R. adriatica and R. reptans. In this study, we analysed specimens of Radicilingua collected in the Adriatic and Ionian Sea (Mediterranean), including a syntype locality of R. adriatica (Trieste, northern Adriatic Sea), alongside material from near the type locality of R. thysanorhizans (Torpoint, Cornwall, UK). The sequences of the rbcL-5P gene fragment here produced represent the first molecular data available for the genus Radicilingua. Phylogenetic reconstruction showed that the specimens from the Adriatic and Ionian Seas were genetically distinct from the Atlantic R. thysanorhizans, even if morphologically overlapping with this species. A detailed morphological description of the Mediterranean specimens, together with an accurate literature search, suggested that they were distinct also from R. adriatica and R. reptans. For these reasons, a new species was here described to encompass the Mediterranean specimens investigated in this study: R. mediterranea Wolf, Sciuto & Sfriso. Moreover, in the rbcL-5P tree, sequences of the genera Radicilingua and Calonitophyllum grouped in a well-supported clade, distinct from the other genera of the subfamily Nitophylloideae, leading us to propose that Calonitophyllum medium should be transferred to Radicilingua.
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15

Gereš, D., J. Rubinič, and N. Ožanić. "Ecological incidents in Northern Adriatic Karst (Croatia)." Water Science and Technology 42, no. 1-2 (July 1, 2000): 281–85. http://dx.doi.org/10.2166/wst.2000.0326.

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In spite of growing efforts to preserve the quality of groundwater resources, accidental pollution is becoming increasingly frequent, resulting in long-lasting impact on the groundwater status. The consequences of ecological accidents are particularly expressed in karst regions, which are caused by the geological properties of the area where the groundwater aquifers are situated, as well as by hydrological circumstances which also influence the dynamic mechanisms of water flow and transportation of pollution in the karst environment. The paper stresses the hydrological component of karst aquifer function and the related role of hydrology in assessment of the hazards caused by accidental pollution and, once the accident has happened, in monitoring the situation and forecasting the possible impact on water resources. The analysis of ecological accidents in the karst has been made, based on the actual examples of accidents involving fuel substances recorded in the Northern Adriatic karst area in Croatia in the period from 1990 to 1998. The basic characteristics of the mechanism of water movement in the karst are presented from the hydrological standpoint, as well as the related risk of rapid transportation of pollutants into the parts of the aquifers used for water supply. The paper also contains proposals for possible approaches to protection of particularly valuable water resources in the karst from accidental pollution occurring in road transport.
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16

Faganeli, Jadran, Bojana Mohar, Romina Kofol, Vesna Pavlica, Tjaša Marinšek, Ajda Rozman, Nives Kovač, and Angela Šurca Vuk. "Nature and Lability of Northern Adriatic Macroaggregates." Marine Drugs 8, no. 9 (September 6, 2010): 2480–92. http://dx.doi.org/10.3390/md8092480.

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17

Zampieri, M., F. Giorgi, P. Lionello, and G. Nikulin. "Regional climate change in the Northern Adriatic." Physics and Chemistry of the Earth, Parts A/B/C 40-41 (January 2012): 32–46. http://dx.doi.org/10.1016/j.pce.2010.02.003.

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18

Vested, Hans Jacob, Per Berg, and Thomas Uhrenholdt. "Dense water formation in the Northern Adriatic." Journal of Marine Systems 18, no. 1-3 (December 1998): 135–60. http://dx.doi.org/10.1016/s0924-7963(98)00009-8.

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19

Degobbis, Danilo. "Increased eutrophication of the northern Adriatic sea." Marine Pollution Bulletin 20, no. 9 (September 1989): 452–57. http://dx.doi.org/10.1016/0025-326x(89)90066-0.

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20

Pavičić-Hamer, Dijana, Delko Barišić, Brigita Šimunac, Branko Petrinec, and Marko Štrok. "137Cs distribution in the northern Adriatic Sea." Journal of Radioanalytical and Nuclear Chemistry 309, no. 3 (February 4, 2016): 989–98. http://dx.doi.org/10.1007/s10967-016-4727-3.

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21

Malačič, Vlado, Dino Viezzoli, and Benoit Cushman-Roisin. "Tidal dynamics in the northern Adriatic Sea." Journal of Geophysical Research: Oceans 105, no. C11 (November 15, 2000): 26265–80. http://dx.doi.org/10.1029/2000jc900123.

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22

Volf, Goran, Nataša Atanasova, Boris Kompare, and Nevenka Ožanić. "Modeling nutrient loads to the northern Adriatic." Journal of Hydrology 504 (November 2013): 182–93. http://dx.doi.org/10.1016/j.jhydrol.2013.09.044.

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23

Ruggeri, Paolo, Andrea Splendiani, Sara Bonanomi, Enrico Arneri, Nando Cingolani, Alberto Santojanni, Andrea Belardinelli, Massimo Giovannotti, and Vincenzo Caputo. "Temporal genetic variation as revealed by a microsatellite analysis of European sardine (Sardina pilchardus) archived samples." Canadian Journal of Fisheries and Aquatic Sciences 69, no. 10 (October 2012): 1698–709. http://dx.doi.org/10.1139/f2012-092.

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The Adriatic stock of European sardine ( Sardina pilchardus ) has experienced large interannual demographic fluctuations over the last 30 years, with a severe decline beginning in 1991 and continuing until 1997. In the present study, six microsatellite loci were used on a time series collection of otoliths and scales from sampling locations of northern (Chioggia) and southern (Vieste) Adriatic Sea, with the aim to investigate the genetic effects of these stock biomass fluctuations. The northern samples showed significant reduction in observed heterozygosity (HO) and mean number of alleles (Na) that explain the genetic diversity variation, while the same parameters turned out to be more stable in the southern samples. In addition, we detected the presence of a genetic bottleneck and low effective population size (Ne) values in several northern samples. Even if the northern and southern Adriatic sardine samples belong to the same genetic stock, the more pronounced decrease in genetic variability recorded in the northern sample led us to speculate that a more intensive fishing pressure and a more pronounced oceanographic isolation of this area could have accentuated the effects of the genetic bottleneck.
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24

Zecchin, Massimo, Federica Donda, and Edy Forlin. "Genesis of the Northern Adriatic Sea (Northern Italy) since early Pliocene." Marine and Petroleum Geology 79 (January 2017): 108–30. http://dx.doi.org/10.1016/j.marpetgeo.2016.11.009.

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25

MARKOVIĆ, O., M. GÖKOĞLU, S. PETOVIĆ, and M. MANDIĆ. "First record of the Northern brown shrimp, Farfantepenaeus aztecus (Ives, 1891) (Crustacea: Decapoda: Penaeidae) in the South Adriatic Sea, Montenegro." Mediterranean Marine Science 15, no. 1 (December 17, 2013): 165. http://dx.doi.org/10.12681/mms.673.

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A single adult female specimen of the Northern brown shrimp, Farfantepenaeus aztecus, a species native to the western Atlantic coasts, was caught in Boka kotorska bay (southern Adriatic Sea) on 19 September 2013. This is the first record of this alien species in the Adriatic Sea.
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26

Oblak, Renato, Svjetlana Hess, and Alen Jugović. "Inland Container Terminals in the Function of the Northern Adriatic Ports Enhanced Operation." Journal of Maritime & Transportation Science 51, no. 1 (March 2016): 85–102. http://dx.doi.org/10.18048/2016.51.06.

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Continuous growth in the Northern Adriatic ports container traffic has caused a high utilization rate of the existing loading/unloading and storage capacities. In order to relieve pressure in ports and avoid traffic congestion and overcrowding which are already occurring, a possible solution is imposed by the construction of a new inland container terminal in their catchment background. This would meet the need for additional storage areas, speed up the flow of containers and ensure sustainable development of the Northern Adriatic container ports. In this paper, a proposition is presented for development of an inland container terminal in Kotoriba as a transit logistics centre for the ports of Rijeka, Trieste and Koper. Using the concept of their transport interlinkage and business policy pursuing their common appearance on the market, unlimited possibilities will be provided for the development of the Northern Adriatic supply chain toward the markets of the Central and Eastern Europe
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27

Bonacci, Ognjen, and Adrijana Vrsalović. "Differences in Air and Sea Surface Temperatures in the Northern and Southern Part of the Adriatic Sea." Atmosphere 13, no. 7 (July 21, 2022): 1158. http://dx.doi.org/10.3390/atmos13071158.

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The paper compares air and sea surface temperatures in recent years on two islands in the Adriatic Sea. The data measured at the climatological station Krk on the island of Krk and the main meteorological station Lastovo on the island of Lastovo are used. The island of Krk is located in the north of the Adriatic Sea and Lastovo in the south. Since a significant increase in air and sea surface temperatures has been observed over the last thirty years, the goal is to establish how they reflect at these two stations, 313 km apart. The goal of the analysis is to monitor the changes in these two islands to reduce the negative impacts they may cause. The analysis of sea temperatures showed that global warming has a greater impact in the northern Adriatic than in the southern Adriatic. Air and sea surface temperatures have a faster upward trend on Krk than on Lastovo. Similar to the Mediterranean Sea, a positive trend was observed in the Adriatic Sea for both sea surface temperature and air temperature.
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28

Korbar, Tvrtko, Dražen Navratil, Cléa Denamiel, Branko Kordić, Sara Biolchi, Ivica Vilibić, and Stefano Furlani. "Coarse-Clast Storm Deposit and Solitary Boulders on the Island of Mana (NP Kornati, Central Adriatic, Croatia)." Geosciences 12, no. 10 (September 22, 2022): 355. http://dx.doi.org/10.3390/geosciences12100355.

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There is growing evidence that many large coastal boulder deposits found on the exposed rocky ocean shores were deposited by extreme storm waves rather than by catastrophic tsunamis, as previously thought. In addition, before the first discovery in the northern Adriatic a few years ago, such deposits were not expected in relatively shallow semi-enclosed inland basins. Here we report on a large coastal coarse-clast deposit on the central Adriatic island of Mana, which also contains numerous large storm boulders that weigh up to several tons. Large solitary boulders are also located outside of the deposit, closer to the partly submerged sea cliff and the wave impact. The erosion of the cliff top and displacement of the carbonate bedrock fragments began when the extreme waves inundated the lowermost part of the cliff edge, probably during the late Holocene sea-level rise. The UAS photogrammetry-based fragmentation analysis of the storm deposit and the calculated fractal dimension value indicate that the material was fragmented by multiple high-energy events. A comparison of the available photographs indicates that displacements of the most exposed solitary boulders probably occurred during Vaia, the last extreme storm that hit the Adriatic on the 29th of October 2018. However, the modeled maximum wave height south of Mana during the peak of the storm would be insufficient to move these boulders. Yet local geomorphology probably further influenced the increase in wave height that, in combination with specific geological features, caused displacements of the boulders. There is a shorter fetch affecting Mana Island with respect to the northern Adriatic boulder field in southern Istria. Thus, such an active local erosion of the generally stable eastern Adriatic karstic coast depends on the extreme storms that have a weaker impact in the central than in the northern Adriatic.
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29

Santini, Stefano, Stefano Mazzoli, Antonella Megna, and Stefania Candela. "Thermal Structure of the Outer Northern Apennines along the CROP-03 Profile." Journal of Geography and Geology 8, no. 4 (November 18, 2016): 1. http://dx.doi.org/10.5539/jgg.v8n4p1.

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In this study, we elaborated a 2D model that reproduces the thermal structure of the central-northern Adriatic offshore and adjacent onshore area of the Italian peninsula. Based on the crustal structure along the trace of the CROP-03 deep section, the geotherms offshore Gabicce (northern Marche region) were obtained by an analytical procedure taking into account the role of thrusting within the sedimentary cover. Basement involvement at depth beneath the neighbouring Mondaino area to the SW, where a crustal thrust ramp dips towards the hinterland, required the use of a different analytical procedure. The results obtained in this study allowed us to define a satisfactory description of the thermal state of the northern Marche coastal area and adjacent Adriatic offshore. These results, integrated with those obtained by previous studies, confirm that the isotherms of 250°C and 400°C are placed in the stable Adriatic lithosphere at depths of about 11 km and 22 km, respectively. Furthermore, the 400°C isotherm is deeper in the onshore area, reaching a depth of about 30 km in the zone comprised between Gabicce and Mondaino, whereas the 250°C isotherm deepens towards the SW along the Adriatic Sea sector, to reach a maximum depth of 13 km in coastal area, rising again at a depth of 11 km in the innermost sector of the studied section.
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30

Twrdy, Elen, and Milan Batista. "COMPETITION BETWEEN CONTAINER PORTS IN THE NORTHERN ADRIATIC." INTERNATIONAL JOURNAL FOR TRAFFIC AND TRANSPORT ENGINEERING 4, no. 4 (December 2014): 363–71. http://dx.doi.org/10.7708/ijtte.2014.4(4).01.

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31

Berthon, Jean-François, and Giuseppe Zibordi. "Bio-optical relationships for the northern Adriatic Sea." International Journal of Remote Sensing 25, no. 7-8 (April 2004): 1527–32. http://dx.doi.org/10.1080/01431160310001592544.

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32

FRASCARI, F., M. FRIGNANI, S. GUERZONI, and M. RAVAIOLI. "Sediments and Pollution in the Northern Adriatic Sea." Annals of the New York Academy of Sciences 534, no. 1 Living in a C (June 1988): 1000–1020. http://dx.doi.org/10.1111/j.1749-6632.1988.tb30191.x.

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33

Ciminiello, Patrizia, Ernesto Fattorusso, Martino Forino, Silvana Magno, Roberto Poletti, Masayuki Satake, Romano Viviani, and Takeshi Yasumoto. "Yessotoxin in mussels of the northern Adriatic Sea." Toxicon 35, no. 2 (February 1997): 177–83. http://dx.doi.org/10.1016/s0041-0101(96)00130-4.

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34

Justić, D. "Long-term eutrophication of the Northern Adriatic Sea." Marine Pollution Bulletin 18, no. 6 (June 1987): 281–84. http://dx.doi.org/10.1016/0025-326x(87)90505-4.

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35

Bolaños, Rodolfo, Jacob V. Tornfeldt Sørensen, Alvise Benetazzo, Sandro Carniel, and Mauro Sclavo. "Modelling ocean currents in the northern Adriatic Sea." Continental Shelf Research 87 (September 2014): 54–72. http://dx.doi.org/10.1016/j.csr.2014.03.009.

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36

Cavaleri, L., L. Bergamasco, L. Bertotti, L. Bianco, M. Drago, L. Iovenitti, A. Lavagnini, et al. "Wind and waves in the Northern Adriatic Sea." Il Nuovo Cimento C 19, no. 1 (January 1996): 1–36. http://dx.doi.org/10.1007/bf02511831.

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37

Brunetti, Riccardo. "Ascidians of the northern adriatic sea. aplousobranchia I." Bolletino di zoologia 61, no. 1 (January 1994): 89–96. http://dx.doi.org/10.1080/11250009409355864.

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38

Ciminiello, Patrizia, and Ernesto Fattorusso. "Shellfish Toxins− Chemical Studies on Northern Adriatic Mussels." European Journal of Organic Chemistry 2004, no. 12 (June 2004): 2533–51. http://dx.doi.org/10.1002/ejoc.200300769.

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39

Cuffaro, Marco, Federica Riguzzi, Davide Scrocca, Fabrizio Antonioli, Eugenio Carminati, Michele Livani, and Carlo Doglioni. "On the geodynamics of the northern Adriatic plate." RENDICONTI LINCEI 21, S1 (October 22, 2010): 253–79. http://dx.doi.org/10.1007/s12210-010-0098-9.

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40

Capano, Fabio. "The evolution of nationhood in twentieth century Europe: Lessons from the Northern Adriatic borderlands." Nationalities Papers 46, no. 6 (November 2018): 955–57. http://dx.doi.org/10.1080/00905992.2018.1501670.

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This article is a short introduction for a special edition on Italian nationhood. The articles that comprise the special edition are the following: From a cosmopolitan to a fascist land: Adriatic irredentism in motion; Erecting fascism: nation, identity, and space in Trieste in the first half of the twentieth century; Building Italianità in northern Adriatic: The case of population from Pola.
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41

SVIBEN, SONJA, DOMEN TRKOV, BORUT MAVRIČ, PETAR KRUŽIĆ, and LOVRENC LIPEJ. "Observations on the diet of the Starry skate, Raja asterias Delaroche, 1809 (Elasmobranchii: Rajidae) in the Adriatic Sea." Mediterranean Marine Science 20, no. 3 (October 18, 2019): 577. http://dx.doi.org/10.12681/mms.19338.

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Diet of im­mature specimens of the Starry skate (Raja asterias) was investigated in three different parts of the northern Adriatic Sea. Decapod crabs were found to be the skate’s primary food source, followed by teleost fish and cephalopods. An ontogenetic shift in the diet towards teleost fish was observed. No significant differences were noted comparing the diet of 22 females and 63 males, 81 juveniles and 4 adults and different size groups. The prey species preferences were different for the specimens feeding on the Italian side of the northern Adriatic, but nonetheless decapods remained the preferred food source.
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42

Casellato, Sandra, Luciano Masiero, Elena Sichirollo, and Stefano Soresi. "Hidden secrets of the Northern Adriatic: “Tegnúe”, peculiar reefs." Open Life Sciences 2, no. 1 (March 1, 2007): 122–36. http://dx.doi.org/10.2478/s11535-007-0004-3.

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AbstractResearch carried out over the last 40 years has underlined the scientific importance of the rocky outcrops scattered on the Northern Adriatic Sea bed sometimes referred to as “tegnúe”. The zoobenthic biocenoses developing over these peculiar geological formations are as extraordinary as they are unique. A study carried out for an entire year in two sampling stations, at different distances from the coast, revealed a very high number of zoobenthic species, including those which have now become rare and are therefore protected in Italian seas. The water turbidity of the northern Adriatic Sea greatly reduces the quantity of light reaching these outcrops, limiting the activity of autotrophic organisms only to sciaphilous genera. Thus, the most represented trophic categories of zoobenthos are suspension, especially filter feeders. Biodiversity values calculated for the communities of these particular reefs are far higher than normally found in the soft seabed in nearby areas, but even higher than in other coralligenous outcrops in other marine ecosystem in the world. The ecological role played by the tegnúe in the Northern Adriatic is extraordinary because as well as being true oases of biodiversity, they are areas naturally protected against bottom trawl-fishing. Thus, they offer shelter and reproduction sites for a number of fish and invertebrate species, including some under stress due to severe fishing pressure.
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43

Lipej, Lovrenc, Domen Trkov, Danijel Ivajnšič, Daša Donša, Nicola Bettoso, Tomaso Fortibuoni, and Borut Mavrič. "Pojava volonje Hexanchus griseus (Bonnaterre, 1788.) u Tršćanskom zaljevu (sjeverni Jadran) s posebnim osvrtom na povijesne i nove zapise u Jadranskom moru." Acta Adriatica 63, no. 1 (August 8, 2022): 93–108. http://dx.doi.org/10.32582/aa.63.1.10.

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A specimen of a sixgill bluntnose shark, Hexanchus griseus (Bonnaterre, 1788), was caught 1.5 NM north of Cape Ronek (Izola, Slovenia) in a fishing net for large-sized flatfish (such as turbot) on 28 January 2018. Three other older cases of catch of sixgill bluntnose sharks were recorded in Slovenia and the Gulf of Trieste. Among these, the finding of the specimen in the Lagoon of Marano and Grado is unusual although there are reported cases of sixgill bluntnose sharks in rivers. An analysis of the available data on the bluntnose sixgill shark in the Adriatic Sea, obtained from different published papers, social media and other sources, was done to understand whether the occurrence of H. griseus in the northern Adriatic differs from other parts. A generalised linear model (GLM) approach revealed that larger specimens are more frequently sighted across the Adriatic Sea, while in the Northern Adriatic part, significantly smaller specimens (juveniles) were recorded in comparison to the Central and Southern parts. It seems that the bluntnose sixgill shark is not in conjunction with a common large shark decreasing trend across the whole Mediterranean Sea.
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44

Zorica, B., V. Čikeš Keč, A. Pešić, S. Gvozdenović, J. Kolitari, and M. Mandić. "Spatiotemporal distribution of anchovy early life stages in the eastern part of the Adriatic Sea in relation to some oceanographic features." Journal of the Marine Biological Association of the United Kingdom 99, no. 5 (December 27, 2018): 1205–11. http://dx.doi.org/10.1017/s0025315418001145.

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AbstractDuring the summer of 2013 two scientific surveys (northern, at the beginning of July and southern, at the end of July) were carried out along the eastern Adriatic Sea. In these surveys, ichthyoplankton samples of anchovy (Engraulis encrasicolus, Linnaeus 1758) eggs and larvae were collected. In the whole investigated area, egg and larvae abundance varied from 2.61 to 1040.24 eggs m−2 (geometric mean ± CL: 25.43 ± 1.48 eggs m−2) and 2.73 larvae m−2 to 611.14 larvae m−2 (geometric mean ± CL: 17.07 ± 1.41 larvae m−2), respectively. Higher abundance of anchovy early life stages was noted in the northern part of the investigated area. The length of the collected specimens lay within the range of 2.39–3.68 mm and those individuals were less than 12 h old. Analysis of spatial and temporal distribution of collected anchovy early life stages indicated their higher abundance in areas of upwelling (four areas were distinguished on the eastern Adriatic side). Larger and older specimens were collected at the beginning of July in the northern part of Adriatic indicating that the anchovy population in the Adriatic tends to shift among its spawning centres in this area. In general, anchovy eggs were accompanied by its larvae (r = 0.453, P < 0.05), while statistically significant negative correlation was obtained between egg abundance and temperature (r = −0.380, P < 0.05) as well as sea depth (r = −0.321, P < 0.05).
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45

CUESTA, J. A., N. BETTOSO, G. COMISSO, C. FROGLIA, G. MAZZA, A. RINALDI, A. RODRIGUEZ, and T. SCOVACRICCHI. "Record of an established population of Palaemon macrodactylus Rathbun, 1902 (Decapoda, Palaemonidae) in the Mediterranean Sea: confirming a prediction." Mediterranean Marine Science 15, no. 3 (September 18, 2014): 569. http://dx.doi.org/10.12681/mms.712.

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The capture of larvae of Palaemon macrodactylus off Mallorca (Balearic Islands) has been recently reported as evidence of a potential presence of a population of this species in the Mediterranean Sea. Photos of this species, taken during dives in the Sacca di Goro (northern Adriatic) were published in the same year, but no specimen could be collected at that time. Herein we report the capture in 2013 of numerous individuals of the oriental shrimp, including ovigerous females, both in the Sacca di Goro and in the Lagoon of Marano and Grado (northern Adriatic Sea, Italy), confirming the existence of a well-established population of this species in the Mediterranean Sea.
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46

Kowalewski, Michał, Jacalyn M. Wittmer, Troy A. Dexter, Alessandro Amorosi, and Daniele Scarponi. "Differential responses of marine communities to natural and anthropogenic changes." Proceedings of the Royal Society B: Biological Sciences 282, no. 1803 (March 22, 2015): 20142990. http://dx.doi.org/10.1098/rspb.2014.2990.

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Responses of ecosystems to environmental changes vary greatly across habitats, organisms and observational scales. The Quaternary fossil record of the Po Basin demonstrates that marine communities of the northern Adriatic re-emerged unchanged following the most recent glaciation, which lasted approximately 100 000 years. The Late Pleistocene and Holocene interglacial ecosystems were both dominated by the same species, species turnover rates approximated predictions of resampling models of a homogeneous system, and comparable bathymetric gradients in species composition, sample-level diversity, dominance and specimen abundance were observed in both time intervals. The interglacial Adriatic ecosystems appear to have been impervious to natural climate change either owing to their persistence during those long-term perturbations or their resilient recovery during interglacial phases of climate oscillations. By contrast, present-day communities of the northern Adriatic differ notably from their Holocene counterparts. The recent ecosystem shift stands in contrast to the long-term endurance of interglacial communities in face of climate-driven environmental changes.
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47

Froglia, Carlo, Simone D’Acunto, Sara Segati, and Sara Bonanomi. "New records of Charybdis japonica (A. Milne-Edwards, 1861) (Crustacea: Decapoda: Portunidae) in the Adriatic Sea." Acta Adriatica 63, no. 1 (August 8, 2022): 27–34. http://dx.doi.org/10.32582/aa.63.1.2.

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Fifteen years after the first capture of a specimen of Charybdis japonica in the Adriatic Sea, we report the collection of two more specimens near the port of Ravenna. This swimming crab, native from the North Western Pacific, has already proved its invasive capacity in New Zealand coastal waters. Its possible establishment in the northern Adriatic lagoons may represent a treat for the local Manila clam fishery and aquaculture activities.
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48

Vilibić, Ivica, Petra Zemunik, Jadranka Šepić, Natalija Dunić, Oussama Marzouk, Hrvoje Mihanović, Clea Denamiel, Robert Precali, and Tamara Djakovac. "Present climate trends and variability in thermohaline properties of the northern Adriatic shelf." Ocean Science 15, no. 5 (October 17, 2019): 1351–62. http://dx.doi.org/10.5194/os-15-1351-2019.

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Abstract. The paper documents seasonality, interannual-to-decadal variability, and trends in temperature, salinity, and density over a transect in the shallow northern Adriatic Sea (Mediterranean Sea) between 1979 and 2017. The amplitude of seasonality decreases with depth and is much larger in temperature and density than in salinity. Time series of temperature and salinity are correlated in the surface but not in the bottom layer. Trends in temperature are large (up to 0.6 ∘C over 10 years), significant through the area, and not sensitive to the sampling interval and time series length. In contrast, trends in salinity are largely small and insignificant and depend on the time series length. The warming of the area is more during spring and summer. Such large temperature trends and their spatial variability emphasize the importance of maintaining regular long-term observations for the proper estimation of thermohaline trends and their variability. This is particularly important in regions which are key for driving thermohaline circulation such as the northern Adriatic, with the potential to affect biogeochemical and ecological properties of the whole Adriatic Sea.
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49

Pinar Gil, Joan. "Cast bronze vessels in the northern Adriatic region (c. 600 AD)." Arheološki vestnik 73 (July 7, 2022): 313–43. http://dx.doi.org/10.3986/av.73.09.

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Although cast bronze vessels of the 6th–8th centuries are not recorded in particularly large numbers, their production and distribution provide a representative sample of the general economic trends and of the evolution of trade networks in the post-Roman Mediterranean. The geographical dissemination of these objects shows that at the turn of the 6th century, the northern Adriatic region became the main gateway of ‘eastern-style’ vessels into Central Europe and the Western Mediterranean. The region was thus replacing the Rome area as the main Western hub for redistributing this type of object. From the northern Adriatic area, several types of vessels were distributed both over land along the Po and Rhine valleys and through maritime routes connecting the Adriatic with Carthage and the Spanish Levant. The intrinsic features and the depositional contexts of the post-Roman cast bronze vessels suggest that they were manufactured according to different quality standards, which targeted different social milieus. Furthermore, mapping the distribution of the different quality standards reveals that each of them might have been distributed by different networks of merchants and unveils the impact of transportation costs on the final price of these products.
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50

Umer, Borut, and Vlado Malačič. "Biexponential decrease of PAR in coastal waters (Northern Adriatic)." Geofizika 39, no. 1 (March 31, 2022): 1–29. http://dx.doi.org/10.15233/gfz.2022.39.2.

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The attenuation coefficients of photosynthetically active radiation (PAR) were extracted from the vertical profiles of PAR in coastal waters (the Gulf of Trieste, Northern Adriatic). The vertical profiles were collected roughly twice per month from July 2011 to December 2015, and the PAR values just above the sea surface were compared with the PAR data measured on a buoy.This research supports the nonlinear fit with the biexponential expression for the dependence of PAR with depth, yielding a much better match with the data than the fit with a mono-exponential expression. However, another reasoning for biexponential attenuation is because it functions as a solution for a homogeneous differential equation of a second order. The method for estimating the water type is offered with an analysis of the attenuation coefficients of PAR. It was found that for a particular location (the Gulf of Trieste), the attenuation coefficient in a mono-exponential decrease of PAR is 0.19-0.21 m-1, while for a biexponential decrease of PAR, the coefficient of the long-range attenuation is 0.12-0.14 m-1 and that of short-range attenuation is 0.8-0.9 m-1. This leads to the conclusion that most water columns match coastal water type 1, while the surface layer is represented by coastal water types 7 or 9. From the estimate of the water types, the coefficients of downward irradiation were inferred as 0.19 m-1∓0.01 m-1 (long-range attenua-tion) and 3.0 m-1∓0.7 m-1 (short-range attenuation). These coefficients can determine the heat source inside the water column.
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