Wyniki wyszukiwania - Biblioteka Nauki

1

Sedimentary structure of the storm surge washover fan on the lake Bukowo spit

100%

Rudowski S. , Wróblewski R.

Oceanological Studies

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2000

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tom Vol. 29, No. 3

101-107

EN

A storm surge washover fan on the Lake Bukowo spit (kilometre 287.3 of the Polish Baltic coast) is described in detail. The in-depth examination of the fan relief and sedimentary facies allowed to identify two subfacies represented by the fan channel and the fan core. The importance of washover fan facies for the structure and development of sandy barriers as well as for shore sediment budget and shore protection is stressed.

2

Regularities in the transformation of coastal and accumulative forms of sea bottom relief, with application for water management

100%

Kapochkin B. , Kucherenko N. , Kapochkina M.

Meteorology Hydrology and Water Management. Research and Operational Applications

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2014

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tom Vol. 2, Iss. 2

43--48

EN

Investigate the processes of formation of accumulative forms of sea bottom relief and coast. The coincidence of the linear parts of the accumulative sea bottom relief with the direction of tectonic faults. Provides examples exploring the coast of the Atlantic Ocean, the Baltic, Black and Azov Seas. Consider the problem of continuing in the sea geological structures on dry land. On the example of the Azov Sea it was shown that the horst on land in the coastal zone is shown a linear zone of eroded beaches. Sustainable shore erosion are confined to the gorst. Graben on land continues at sea accumulative forms of type foreland. The accumulation zone of sediment are confined to grabens. Shown that different direction storms form accumulative relief in accordance with clear rules. Random exogenous factors are controlled regularities endogenous processes. Endogenous formation of sea bottom relief happens resulting impact endogenous processes on the speed currents. In those locations where currents slows down the sand falls to the bottom. Decrease in speed currents occurs lengthwise tectonic faults. Faults is the migration path lithospheric fluids. To elucidate the reasons for the formation of specific conditions sediment load was carried out mathematical modeling of currents over a linear zone submarine groundwater discharge. Hydrodynamic software decides system of Navier-Stokes equations. Made mathematical modeling the interaction currents and the water flowing from a tectonic fault.

3

An Essay on Paradigms of Socioglobalistic at Sea and Coast

86%

Woźniak R. B.

Roczniki Socjologii Morskiej

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2013

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tom 22

69-77

EN

Socioglobalistic at sea and coast deals with understanding and explaining the global problems of the modern world connected with maritime and around maritime matters. The social reality is presented in terms of objective and subjective determinants of individual and collective social relations at sea and connected with sea. The aim of the article is to present a broad scale of paradigms for new maritime sociology.

4

Native and alien malacostracan Crustacea along the Polish Baltic Sea coast in the twentieth century

86%

Jazdzewski K. , Konopacka A. , Grabowski M.

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tom 34

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nr Suppl.1

5

Bioaccumulation and translocation efficacy of heavy metals by Rhizophora mucronata from tropical mangrove ecosystem, Southeast coast of India

72%

Ganeshkumar A. , Arun G. , Vinothkumar S. , Rajaram R.

International Journal of Ecohydrology and Hydrobiology

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2019

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tom 19

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nr 1

6

Distribution and characterization of Lessepsian migrant fishes along the coast of Libya

72%

Shakman E. A. , Kinzelbach R.

Acta Ichthyologica et Piscatoria

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2007

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tom 37

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nr 1

7-15

EN

Background. The Lessepsian migrant ichthyofauna along the approximately 2000 km of the Libyan coastline has been poorly known. A comprehensive study, addressing this issue, was needed and therefore the presently reported research project is intended to close the gap, through identifying the fish species and assessing their distribution. Materials and Methods. The catches of commercial fisheries vessels were monitored and examined in a standardized procedure between January 2005 and March 2006. The project covered a total of 4273 specimens, comprising 1901 specimens of Siganus luridus, 1885 specimens of Siganus rivulatus, and 487 specimens of fourteen other Lessepsian fish species. Results. Sixteen Lessepsian fish species, representing 14 families, were recently found along the Libyan coast, two of which are considered to be first records for Libya: Herklotsichthys punctatus (Rüppell, 1837) and Liza carinata (Valenciennes, 1836). Approximately 50% of the immigrants were found along the entire stretch of the Libyan coast, 12.5% in the east and central regions, and 37.5% were restricted to the eastern part of the Libyan coast. All were found in the coastal area (1-50 m depth), 12.5% on the vegetation, 31.25% on sandy bottoms, 12.5% on rocks, while the majority of them (43.75%) were pelagic. Regarding the size, 75% were medium, 18.75% large, and 6.25% were categorized as small. Conclusion. The north African coast (west of the Nile delta)-compared with the Levantine- and Anatolian coast of the Mediterranean Sea-was considered to be settled by immigrants from the Red Sea with some delay, due to sea currents. If so, this situation has changed meanwhile at least for fishes. More than 37% of the recorded Lessepsian fish species are of commercial value, especially rabbitfish (Siganus spp.). The future research should be focussed on monitoring the stocks, especially of the commercially valuable species, regarding the biology and ecology of the Lessepsian migrants. Also, possible further additions to the fish fauna, by new invaders, should be recorded.

7

Mathematical modelling of rainfall runoff from small catchments of the northwest coast of the Black Sea

72%

Moniushko M. , Daus M. , Zakharova M.

Meteorology Hydrology and Water Management. Research and Operational Applications

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2015

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tom 03

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nr 1

EN

This article is devoted to the use of a mathematical model of a flood runoff for calculating rainfall runoff hydrographs from small catchments of the northwest coast of the Black Sea. The described model was tested and applied for the following catchments located in various geographical conditions, with various amounts of initial data: experimental catchments in Zacarpathian, the northwest of the Black Sea region – Ukraine and the Republic of Moldova, small catchments of the northern part of Vietnam, etc. This work was carried out on the basis of Moldavian Water-Balance Station databases. The development of a complex approach to a mathematical simulation of the formation of the processes of rain floods from small catchments is also given further investigation in this article. A brief description of the structure of a flood runoff spatial model from small catchments then provided. As well as this, the advantages of using radiolocation measurement of rainfall in the mathematical modeling of the formation of a flood runoff are shown. The results of construction runoff hydrographs confirm the possibility of applying this spatial model with the use of radar information. The optimization of model parameters was made with the data of 123 floods. The values of the quality criterion S/σ turned out not to exceed the value 0.8 in 81% of the considered cases of floods.

8

Distribution and the role of Mytilus edulis (Linne) in the coastal zone of the Pomeranian Bay

72%

Piesik Z. , Wawrzyniak-Wydrowska B.

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline

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1997

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tom 01

9

The relief of the Western coast of Admiralty Bay, King George Island, South Shetlands

72%

Kostrzewski A. , Rachlewicz G. , Zwolinski Z.

Quaestiones Geographicae

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2003

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tom 22

10

Wstępne wyniki badań nad roślinnością dróg w borach strefy przymorskiej

72%

Herbich J. , Herbichowa M.

Zeszyty Naukowe Wydziału Biologii, Geografii i Oceanologii. Uniwersytet Gdański. Biologia

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1987

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nr 08

11

Seasonal variability of precipitation on the Polish Baltic Sea coast

72%

Swiatek M.

Acta Agrophysica. Rozprawy i Monografie

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2010

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nr 4[183]

12

First record of oilfish, Ruvettus pretiosus [Actinopterygii, Gempylidae], off the coast of Benghazi, Libya [southern Mediterranean]

72%

Elbaraasi H. , Elmariami M. , Elmeghrabi M. , Omar S.

Acta Ichthyologica et Piscatoria

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2007

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tom 37

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nr 1

67-69

XX

The first record of oilfish, Ruvettus pretiosus Cocco, 1829, (Gempylidae) from the depth of 65 m, caught off the coast of Benghazi, Libya (Southern Mediterranean), is reported herewith. The present finding appears to be an evidence of the extension in the latitude of its geographical distribution.

13

Analiza rzeźby brzegu na podstawie numerycznego modelu terenu

72%

Terefenko P. , Furmańczyk K. , Łapiński M.

Archiwum Fotogrametrii, Kartografii i Teledetekcji

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2008

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tom Vol. 18b

581--588

PL

Strefa brzegowa morza to bardzo ważny gospodarczo i społecznie obszar wzajemnej interakcji pomiędzy trzema żywiołami: lądem, morzem i atmosferą a obecnością i działalnością ludzką. Od wieków człowiek obserwuje i bada wybrzeże w celu przewidzenia jego zmiennej natury i ujarzmienia jej. Ochrona brzegu morskiego zmierza przede wszystkim do powstrzymania i usuwania skutków niszczącej działalności morza. Aby działania takie mogły przynieść pożądany skutek niezbędna jest wiedza o miejscu występowania najbardziej wrażliwych i narażonych części brzegu. W tym celu przeprowadzono analizę rzeźby dla pasa technicznego Urzędu Morskiego w Szczecinie z wykorzystaniem numerycznego modelu terenu. Numeryczny model terenu z uwagi na duże możliwości jakie daje informatyka stał się istotnym elementem w modelowaniu różnorodnych zjawisk przestrzennych w systemach GIS. W niniejszym opracowaniu model utworzony na podstawie mapy zasadniczej z roku 2002 w skali 1:2000 był podstawą do przeprowadzenia analiz i w rezultacie pozwolił na stworzenie klasyfikacji morfologicznej badanego terenu i jego ocenę pod kątem zagrożeń od strony morza. Niniejsze badania mogą służyć jako podstawa do bardziej złożonych analiz zmian rzeźby brzegu morskiego z uwzględnieniem dodatkowych parametrów takich jak tempo erozji i akumulacji oraz wzrost poziomu morza.

EN

The coastal zone of the sea is an economically and socially important area of interaction between three basic elements: the land, the sea and the atmosphere; it is also affected by human activities. Coastal processes have been for ages investigated to forecast, restrain, and tame their nature. Coastal defence systems are mostly designated to stop or mitigate destructive effects of the sea. Such activities can succeed only if there is sufficient knowledge on the most sensitive and fragile parts of the coast. To identify such areas, a coast strip managed by the Szczecin Maritime Office was analysed with a digital terrain model. Due to its large technical potential, the digital terrain model (DTM) has become a very important tool in modelling of a variety of spatial phenomenon within GIS systems. In this work, a TIN model developed from a 1:2000 map of a technical strip belt for 2002 was used to analyse the morphology of the Polish coast. The analysis allowed to distinguish several morphological classes; in addition, coastal safety classes were identified. The results should be analysed in a wider context taking into account additional variables such as erosion and accumulation rates or the mean sea level rise.

14

Variations in weather on the East and West coasts of South Spitsbergen, Svarbald

72%

Maciejowski W. , Michniewski A.

Polish Polar Research

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2007

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tom 28

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nr 2

EN

This paper describes the weather conditions on the NE coast of Sørkappland (South Spitsbergen) during August 2005, and considers them in the context of the general synoptic situation over the North Atlantic. A comparison of local climates features for the East and West coast of southern Spitsbergen shows that the general atmospheric circulation and direct solar radiation in summer are the decisive factors affecting weather on the East coast. Foehn effects were observed during the study period. In the East, these were triggered by the westerly cyclonic situation and, in the West, by the easterly. The differences in the intensity of foehn effects may be explained by a specific relief of the Sørkappland peninsula.

15

Longidorus balticus sp.nov. [Nematoda: Longidoridae] from coastal sand dunes in Northeast Poland

72%

Brzeski M. W. , Peneva V. , Brown D. J. F.

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nr 3

EN

A description is provided of Longidorus balticus sp. nov., a bisexual species recovered from the rhizosphere of Elymns arenarias L. growing in coastal sand dunes in northeast Poland. The species is characterized by having a long (L=6.7-9.2 mm) and slender (a= 119-175) body; expanded labial region, flattened anteriorly; assymetrically bilobed amphids; anteriorly situated guide ring (23-29 µm); odontostyle of medium length (91-105 µm); and a short, rounded tail. Males having spicules of medium size (58-69 µm), and a row of 9-15 supplements. Longidorus baltieus sp. nov. has four juvenile developmental stages. Longidorus balticus sp. nov. resembles L. vineacola, L. belloi, L. lusitaniens, L. moesicus, L. profundorum and L. apulus.

16

The biochemical composition of Enteromorpha spp. from the Gulf of Gdańsk coast on the southern Baltic Sea

72%

Haroon A. M. , Szaniawska A. , Normant M. , Janas U.

Oceanologia

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2000

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tom 42

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nr 1

EN

Variations in lipid, protein and carbohydrate contents of Enteromorpha spp. were examined over a seven-month period from April to October 1993. The samples were collected from seven sampling stations along the Gulf of Gdańsk coast. The lipid content was low and varied slightly from 3.47±1.76% of DW at Puck to 4.36±2.17% of DW at Rewa and Chałupy. The protein content varied from 9.42±4.62% of DW at Puck to 20.60±5.00% of DW at Jurata. At the remaining stations the values vary over a narrow range. The maximum protein contents were recorded at the beginning and end of the growing season. The level of carbohydrate was very high compared to that of lipid and protein and varied from 29.09±6.44% of DW at Osłonino to 39.81±11.15% of DW at Puck. Seasonal carbohydrate changes were noted at all sampling stations, the minimum occurring in spring and autumn and the maximum in summer.

17

First report on Noctiluca scintillans blooms in the Red Sea off the coasts of Saudi Arabia: consequences of eutrophication

72%

Mohamed Z. A. , Mesaad I.

Oceanologia

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2007

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tom 49

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nr 3

EN

Blooms of Noctiluca scintillans are reported for the first time in the Red Sea off the south-western coasts of Saudi Arabia. During the present study, surface water samples were collected weekly on the coasts of the Al Shuqayq region from February to April 2004–2006. The abundance of N. scintillans correlated negatively with most nutrients, as well as the cell densities of diatoms and dinoflagellate species. Microscopic examination of live cells from Noctiluca blooms showed the presence of some species of diatoms and dinoflagellates within the Noctiluca body – confirmation of its grazing on these microalgae. The presence of a Noctiluca bloom in the coastal waters off south-western Saudi Arabia could be linked indirectly to water eutrophication by an increase in prey abundance. The physico-chemical properties of Red Sea coastal waters should therefore be monitored regularly in order to minimize the formation of harmful algal blooms, which may affect all food web levels, including the human level.

18

Density, biomass, and distribution of benthic invertebrates in the mid-lake zone of the coastal Lake Gardno

72%

Dobrowolski Z.

Oceanological Studies

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2001

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tom 30

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nr 1-2

19

Light minerals of beach sediments from Southern Tamilnadu, South East coast of India

72%

Cherian A. , Chandrasekar N. , Rajamanickam V.

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nr 2

EN

A brief investigation of light minerals along the beaches between Valinokkam and Tuticorin has been carried out for the first time along the Southern Tamilnadu coast in order to discover the provenance of the sediments. The study spotlights a wide variation in light mineralogy along the three zones of the investigated area (Valinokkam, Vaippar and Tuticorin). A higher percentage of quartz is reported from the Valinokkam (48.34 to 68.63%) and Tuticorin zones (55.66 to 73.05%) than from the Vaippar zone (40.24 to 60.77%). The trend with regard to the maturity index is similar, with appreciably higher values in Valinokkam (1.15 to 1.89) and Tuticorin (1.61 to 1.94) than Vaippar (0.79 to 1.39). Morphological analysis of quartz grains shows a higher order of sphericity and roundness values in Valinokkam and Tuticorin as compared to Vaippar. Moreover, the surface texture of quartz grains observed with the aid of scanning electron microscope (SEM) photographs reveals the presence of different depositional environments and the multiple origin of beach sediments in the study area. From the present study of the light mineralogy of beach sediments, it is inferred that the source of the sediments is a mixed type: igneous and metamorphic crystalline rocks, together with palaeosediments.

20

Appraisal of tsunami inundation and run-up along the coast of Kanyakumari District, India - GIS analysis

72%

Chandrasekar N. , Immanuel J. L. , Sahayam J. D. , Rajamanickam M. , Saravanan S.

Oceanologia

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2007

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tom 49

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nr 3

EN

On 26D ecember 2004, a tsunami severely affected almost all the coastal villages of Kanyakumari District, India. It was one of the worst affected coastal sectors of South India. An attempt has been made here to assess the impact of the tsunami hazard on coastal landforms and the level of inundation using GIS techniques. The areas of inundation were surveyed and mapped by fixing regular transects along the coastal regions. The percentage of inundated area in the total area was estimated. It was found that inundation was higher on low-lying coasts and relatively less on elevated coasts. In some cases, the extent of inundation was a few kilometres in relation to other coasts, but the percentage of inundated area in the total coastal area was high. The extent of inundation along the study area varied from 50 m to 450 m. Inundation was minimal in coastal villages like Kanyakumari, Agastheeswaram, Madhysoodhanapuram and Dharmapuram, but extensive at Colachel. The percentage of inundated area in the total area ranges from 8% (Dharmapuram) to 39% (Colachel). The degree of inundation was controlled by coastal geomorphological features such as sand dunes, cliffs, coastal vegetation, nature and configuration of the beach, not to mention the angle and velocity of the invading tsunami surge.