Готові списки джерел за темами / Strait of Otranto

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Добірка наукової літератури з теми "Strait of Otranto"

Автор: Grafiati

Опубліковано: 11 березня 2023

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Статті в журналах з теми "Strait of Otranto"

Viličić, D., N. Leder, Z. Gržetić, and N. Jasprica. "Microphytoplankton in the Strait of Otranto (eastern Mediterranean)." Marine Biology 123, no. 3 (September 1995): 619–30. http://dx.doi.org/10.1007/bf00349240.

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Civitarese, G., M. Gačić, A. Vetrano, A. Boldrin, D. Bregant, S. Rabitti, and E. Souvermezoglou. "Biogeochemical fluxes through the Strait of Otranto (Eastern Mediterranean)." Continental Shelf Research 18, no. 7 (June 1998): 773–89. http://dx.doi.org/10.1016/s0278-4343(98)00016-8.

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Ursella, L., V. Kovačević, and M. Gačić. "Tidal variability of the motion in the Strait of Otranto." Ocean Science 10, no. 1 (February 13, 2014): 49–67. http://dx.doi.org/10.5194/os-10-49-2014.

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Abstract. Various current data, collected in the Strait of Otranto during the period 1994–2007, have been analysed with the aim of describing the characteristics of the tidal motions and their contribution to the total flow variance. The principal tidal constituents in the area were the semi-diurnal (M2) and the diurnal (K1), with the latter one predominant. The total flow was, in general, more energetic along the flanks than in the middle of the strait. Specifically, it was most energetic over the western shelf and in the upper layer along the eastern flank. In spite of the generally low velocities (a few cm s−1) of the principal tidal constituents, the tidal variance has a pattern similar to that of the total flow variance, that is, it was large over the western shelf and low in the middle. The proportion of non-tidal (comprising the inertial and sub-inertial low-frequency bands) to tidal flow variances was quite variable in both time and space. The low-frequency motions dominated over the tidal and inertial ones in the eastern portion of the strait during the major part of the year, particularly in the upper and intermediate layers. In the deep, near-bottom layer the variance was evenly distributed between the low frequency, diurnal and semi-diurnal bands. An exception was observed near the western shelf break during the summer season when the contribution of the tidal signal to the total variance reached 77%. This high contribution was mainly due to the intensification of the diurnal signal at that location at both upper and bottom current records (velocities of about 10 cm s−1). Local wind and sea level data were analysed and compared with the flow to find the possible origin of this diurnal intensification. Having excluded the sea-breeze impact on the intensification of the diurnal tidal signal, the most likely cause remains the generation of the topographically trapped internal waves and the diurnal resonance in the tidal response. These waves were sometimes generated by the barotropic tidal signal in the presence of summer stratification and the strong bottom slope. This phenomenon may stimulate diapycnal mixing during the stratified season and enhance ventilation of the near-bottom layers.

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Ursella, L., V. Kovačević, and M. Gačić. "Tidal variability of the motion in the Strait of Otranto." Ocean Science Discussions 10, no. 2 (March 5, 2013): 435–72. http://dx.doi.org/10.5194/osd-10-435-2013.

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Abstract. Various current data, collected in the Strait of Otranto during the period 1994–2007, have been analysed with the aim of describing the characteristics of the tidal motions and their contribution to the total flow variance. The principal tidal constituents in the area were the semi-diurnal (M2) and the diurnal (K1), with the latter one predominant. The total flow was, in general, more energetic along the flanks than in the middle of the Strait. Specifically, it was most energetic over the western shelf and in the upper layer along the eastern flank. In spite of the generally low velocities (a few cm s−1) of the principal tidal constituents, the tidal variance has a pattern similar to that of the total flow variance, that is, it was large over the western shelf and low in the middle. The proportion of non-tidal (comprising the inertial and sub-inertial low-frequency bands) to tidal flow variances was quite variable in both time and space. The contribution of the low-frequency motions predominated over the tidal and inertial ones in the eastern portion of the strait during the major part of the year, particularly in the upper and intermediate layers. In the deep, near-bottom, layer the variance was evenly distributed between the low frequency, diurnal and semi-diurnal bands. A prominent exception was observed near the western shelf break during the summer season when the contribution of the tidal signal alone to the total variance reached 77%. This high contribution was mainly due to the intensification of the diurnal signal at that location in the proximity of both the surface and bottom layers (velocities of about 10 cm s−1). Local wind and sea level data were analysed and compared with the flow to find the possible origin of this diurnal intensification. Having excluded the sea-breeze impact on the intensification of the diurnal tidal signal, the most likely cause remains the generation of the topographically trapped internal waves and the diurnal resonance in the tidal response. These waves were sometimes generated by the barotropic tidal signal in the presence of summer stratification. The effect was seen only in the presence of the topographic slope change. This phenomenon may stimulate the diapycnal mixing during the stratified season and enhance ventilation of the near-bottom layers.

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MANCINI, FRANCESCO, ANTONIO OSCAR LILLO, ROBERTA BARDELLI, SALVATRICE VIZZINI, and GIORGIO MANCINELLI. "Variation in the stable isotope trophic position of the bluefish Pomatomus saltatrix (Linnaeus, 1766) from two Mediterranean sites: insights from a global meta-analysis." Mediterranean Marine Science 23, no. 4 (October 13, 2022): 850–63. http://dx.doi.org/10.12681/mms.29325.

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A direct consequence of sea warming is the shift in the distribution range of thermo-tolerant species that have the potential to determine novel inter-specific interactions, ultimately altering food web structures and ecosystem processes. In this study, we investigated the trophic position of the bluefish Pomatomus saltatrix (Linnaeus, 1766), a pelagic predator that has recently expanded its distribution in the Mediterranean basin and for which scant information is available on its functional role in recently-colonised areas. Nitrogen and carbon stable isotopes were determined in muscle tissues of bluefish specimens collected in south-east Italy in the Gulf of Taranto (NW Ionian Sea) and in the Strait of Otranto (SW Adriatic Sea) at two coastal sites showing contrasting oceanographic conditions. The bluefish trophic position (TP) was estimated using locally abundant forage fish species as isotopic baselines. The results indicated for bluefish from the Strait of Otranto a TP value of 5.1, significantly higher than that determined in the Gulf of Taranto (4.2), and exceeding stomach content-based estimations reported by the online database FishBase and by literature sources. A synthesis of 30 publications reporting isotopic data for the bluefish and its potential prey at a global scale indicated that the species’ trophic position varied considerably between 2.7 and 5.2. The observed variability depended on locationand on the baseline species used in the estimations. Yet, a significant difference in trophic position was observed for bluefish from transitional and inshore environments as compared with offshore areas, mirroring the results obtained from the Gulf of Taranto and the Strait of Otranto. The findings of the study highlight the high trophic plasticity characterizing the bluefish in recently colonized areas, suggesting that it may play a key role in facilitating the expansion of its distribution range. However, additional investigations are essential to provide an advanced resolution of the bluefish functional role in Mediterranean coastal food webs.

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De Lazzari, Amelia, Alfredo Boldrin, Sandro Rabitti, and Margherita M. Turchetto. "Variability and downward fluxes of particulate matter in the Otranto Strait area." Journal of Marine Systems 20, no. 1-4 (April 1999): 399–413. http://dx.doi.org/10.1016/s0924-7963(98)00076-1.

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Krasakopoulou, Evangelia, Ekaterini Souvermezoglou, and Catherine Goyet. "Anthropogenic CO2 fluxes in the Otranto Strait (E. Mediterranean) in February 1995." Deep Sea Research Part I: Oceanographic Research Papers 58, no. 11 (November 2011): 1103–14. http://dx.doi.org/10.1016/j.dsr.2011.08.008.

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Ursella, Laura, Miroslav Gačić, Vedrana Kovačević, and Davide Deponte. "Low-frequency flow in the bottom layer of the Strait of Otranto." Continental Shelf Research 44 (August 2012): 5–19. http://dx.doi.org/10.1016/j.csr.2011.04.014.

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Yari, Sadegh, Vedrana Kovačević, Vanessa Cardin, Miroslav Gačić, and Harry L. Bryden. "Direct estimate of water, heat, and salt transport through the Strait of Otranto." Journal of Geophysical Research: Oceans 117, no. C9 (September 2012): n/a. http://dx.doi.org/10.1029/2012jc007936.

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Poulain, P. M., M. Gačcić, and A. Vetrano. "Current measurements in the Strait of Otranto reveal unforeseen aspects of its hydrodynamics." Eos, Transactions American Geophysical Union 77, no. 36 (1996): 345. http://dx.doi.org/10.1029/96eo00236.

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Дисертації з теми "Strait of Otranto"

Yari, Sadegh. "Heat and salt transport across the strait of Otranto." Doctoral thesis, Università degli studi di Trieste, 2009. http://hdl.handle.net/10077/3213.

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2007/2008
The water transport and advected heat through the Strait of Otranto are computed applying a new methodology to the historical data set. According to the previous oceanographic studies, the Adriatic Sea annually loses heat through the air-sea interface. This heat loss should be balanced by the heat advected across the Strait of Otranto. Direct current measurements for almost one year (from December 94 through November 95), and five seasonal oceanographic campaigns are used in this study. The current data are measured at sixteen locations at different depths; near surface, intermediate depths and near bottom. The measured current data are detided and low pass filtered in order to remove tidal and inertial oscillations. A variational inverse method based on a variational principle and a finite element solver is used to reconstruct the current field across the Strait section from sparse measurements. The mean water flow across the strait consists of an inflow on the eastern side and an outflow on the western side, while there is a two layer structure in the central part. The latter has an inflow in the surface layer and an outflow in the bottom layer. The mean monthly, seasonally and yearly water transports and corresponding errors are calculated. The mean annual inflow and outflow water transport rates are estimated as 0.90±0.04 Sv and -0.94±0.31 (error) Sv and the net transport is equal to -0.04±0.32 (error) Sv. Thus, on a yearly time interval, the inflow and the outflow are practically compensated. These estimations of water transport are in agreement with previous studies. The seasonal heat flux is estimated by using the data collected during the hydrographic surveys conducted in December 1994, February, May, August and November 1995. The results show a net heat advection into the Adriatic Sea on a yearly basis. The estimated values of advected heat applying two different methods are 2.93±0.35 TW and 2.5±0.35 TW, which are equivalent to heat gain of 21.3±2.5 (error) Wm-2 and 17±2.5 Wm-2 for the whole basin which are compared to the calculated heat loss of -36±152 (std) Wm-2 over the Adriatic Sea. Salt transported salt is calculated by using salinity and current data. The average annual salt transport is estimated as an inflow of salt equal to 0.05106 Kgs-1. This is in agreement with the fact that the Adriatic Sea is a dilution basin. The average annual fresh water budget is estimated as -0.002 Sv which is equivalent to fresh water gain of 0.45 m/year for the entire Adriatic Sea.
XXI Ciclo
1972

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Книги з теми "Strait of Otranto"

Gasparovich, László. Csata az Adrián: Megregényesített dokumentumok. [Budapest]: Gemini Budapest, 1998.

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Halpern, Paul G. The battle of the Otranto Straits: Controlling the gateway to the Adriatic in World War I. Bloomington: Indiana University Press, 2004.

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Halpern, Paul G. Battle of the Otranto Straits: Controlling the Gateway to the Adriatic in World War I. Indiana University Press, 2004.

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Тези доповідей конференцій з теми "Strait of Otranto"

Salusti, Ettore, and Roberta Serravall. "Barotropic and baroclinic currents in the Strait of Otranto (southern Adriatic Sea)." In International Symposium on Remote Sensing, edited by Charles R. Bostater, Jr. and Rosalia Santoleri. SPIE, 2002. http://dx.doi.org/10.1117/12.452756.

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