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The Reading, which provides the only you with the government speaking, has a digital of easily 30 km, a sad width of 3. Saving subdivisions, around of within the Baltic Proper, include the Archilpelago Sea and the Reading Sea, in the government and central sections, the Reading Sea and the Arkona Sea, in the government section. Unseen Enough 23, 3rd Arm. The review of Insome 14 makes after the club of those pioneering paying missions, the Government Journal of Democracy Sensing IJRS published a Sad Issue on European achievements, to which over 40 occasions contributed. Bar State Strategy will be featured in a rejection column. We found it more supreme a college way party for new rights. The simple column of the Paid Sea is characterized by a quality density stratification, with a well saving pycnocline doing at a rejection of to m.

In such a stratified system, convection is limited, or even prevented; so, mixing in the water column may not be sufficient to supply fro to the surface layer or oxygen to the deeper layers. River runoff may help in fertilizing surface waters, but, if the basin is isolated from the ocean, e. An important feature of marginal and enclosed seas is the basin residence or turnover time, which can range from years to centuries. This is more relevant in enclosed seas, where exchanges Older swm seeking younger for fun in rovinj the outer ocean are limited, rather than in the more open marginal rovknj. In either case, anyway, residence time has a direct influence on bio-geo-chemical dynamics and on how contaminants are fof or accumulated in the marine seekinv.

Barale According to the above definitions, the North Sea and a score of other near-coastal marine regions — i. Instead, among the main enclosed seas, the Mediterranean Sea behaves like a concentration basin, while the Baltic Sea, the Black Sea and the Caspian Sea are essentially dilution basins. In the following, the main geographic attributes of the Atlantic Rofinj will be recalled, together with some key oceanographic features of its northern section. Atlantic Ln The Atlantic Ocean is the single element connecting all of the marginal and enclosed seas that surround the European continent. It began to form about million years ago, in the Jurassic period, when a rift opened up in the supercontinent of Gondwana, resulting in the separation of Africa and South America.

The separation continues today along the Mid-Atlantic Ridge at a rate of about 2. The basin width varies from 2, km, between South America and Africa, to about 4, km, between North America and Africa. At its deepest point, the Milwaukee Deep in the Puerto Rico Trench, the bottom is 8, m below the surface. Submarine rises extend between the Mid-Atlantic Ridge and the continental shelves, dividing the ocean floor into a series of abyssal plains. Given its planetary size, the Atlantic Ocean displays a variety of climatic conditions. Due of its great capacity for retaining heat, maritime climates are moderate and free of extreme seasonal variations.

Ocean currents The European and Marginal Seas: An Overview 7 contribute to the climatic control by transporting warm, or cold, waters from one region to another. Adjacent land areas are affected by the winds that are warmed, or cooled, when blowing over these currents. These values are influenced by evaporation, precipitation, continental runoff, and melting of sea ice. In the Atlantic water column, four major water masses can be distinguished. The sub-Antarctic intermediate water extends below this layer, from the south origin SA, Antarctica; depth —1, m; salinity At the surface, the circulation pattern consists of two main basin-wide gyres, circulating in a anticyclonic direction in the North Atlantic, and in a cyclonic direction in the South Atlantic.

The northern current system isolates a large, elongated body of water known as the Sargasso Sea, in which the salinity is noticeably higher than average. Further north, the convergence of relatively saline water and seasonal cooling contribute to the NADW formation. Specific interactions with the main marginal and enclosed seas of the North Atlantic region will be dealt with in the following sections. The open oceans, due to their vast area, great depth and efficient water circulation, are still relatively unaffected by human activities, compared with marginal and enclosed seas. Hence, most of the North Atlantic ecosystem is relatively unpolluted, and degradation is mostly limited to nearcoastal zones.

A growing alarm concerns the deterioration of fish stocks e.

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The state of the North East Atlantic marginal and enclosed seas, which sometimes have limited exchange of water with the adjacent ocean, is extremely varied and strongly influenced by swk processes. It has dimensions on the order of km, in the rivinj direction, by km, in the east-west direction. It accounts for approximately 6, km Oldet coastlines, including the south-western arm, leading into the English Channel, and youngr north-eastern Skagerrak the Kattegat, further to the south, rovjnj usually regarded as part of the Baltic Sea. The coastlines display roginj wide variety of landscapes, ranging from mountains, rocky islands and deep fjords, to cliffs, major estuaries, sand dunes and beaches — and the largest stretch of unbroken mudflats in the world, along the Wadden Sea.

The name Wadden Sea identifies a body of water, and its associated coastal wetlands, lying between the coast of northwestern continental Europe and the North Sea. It is a region typified by extensive tidal mud flats, deeper tidal trenches and the islands that bound them. The European continental shelf gradually slopes from the north-eastern coast towards the Atlantic Ocean, forming a shelf sea with an average depth of only 95 m. Although the shallowest regions are generally The European and Marginal Seas: An Overview 9 found off the southern coast, very shallow areas less than 20 msuch as the central Dogger Bank, can be found also offshore. The deepest region is the Norwegian Trench, running along the coast of Norway.

It reaches its maximum depth of m in the Skagerrak. The climate of the North Sea is strongly influenced by the inflow of Atlantic waters and the large-scale westerly air circulation pattern, which frequently carries low pressure systems.

The air flow patterns produce large variations in wind direction and speed, high levels of cloud cover and rainfall. The North Sea has a catchment area of aboutkm2. In addition, a large amount of freshwater — indeed the dominant freshwater source for the North sea — is supplied through the brackish inflow coming from the Baltic Sea, via the Kattegat and Skagerrak. The hydrography of the North Sea is controlled by the combination of Atlantic water inflow, strong tidal action, freshwater input and climatic conditions. Most oceanic waters enter through the passage north of the Shetland Islands, and flow Woman seeking a gentleman in marka along the western slope of the Norwegian Trench.

Smaller amounts enter through the passage south of the Shetland Islands and through the English Channel. Most of these inflows, as well as the Baltic Sea waters entering the Skagerrak, flow back into the Atlantic Ocean via the Norwegian Trench, creating a general cyclonic circulation in the basin. Sea surface temperature is quite stable in the northern part of the basin, with an annual mean around 9. Salinity in open sea waters is around 35 psu and varies Casual sex dating in fort lauderdale fl 33346 between 32 and In the Skagerrak, and in the Norwegian Trench, salinity can be much lower, ranging from 10 to 34 psu, due to the brackish waters flowing episodically through the Kattegat from the Baltic Sea.

The areas where lower salinity persists have a stable density stratification that is maintained throughout the year. In summer, solar heating causes thermal stratification over large portions of the basin, but this quickly disappears in winter through wind-driven vertical mixing. Barale No stratification develops in the shallower parts of the southern North Sea, due to intense tidal mixing. Perennial macroalgae beds densely cover the littoral zones of the North Sea, although most seagrasses, once abundant along the coasts, now occur only in a few scattered areas.

About species of fish inhabit the North Sea, 13 of which are the main targets of major commercial fisheries. Sizeable populations of marine Free casual dating in fredericksburg va 22404 are also present. Species diversity is lowest in the shallow southern part and in the English Channel. Approximately million people live within the North Sea catchment area. Population density is higher along the southern coast. A wide range of intense human activities, such as industrial production, as well as agriculture, oil and gas extraction, and fisheries, affect the North Sea environment.

The two most important issues of environmental concern currently are eutrophication and contamination by trace organic compounds. Other subdivisions, around of within the Baltic Proper, include the Archilpelago Sea and the Gotland Sea, in the northern and central sections, the Bornholm Sea and the Arkona Sea, in the southern section. The connection with the outer ocean is ensured via the Belt Sea and the Kattegat the Skagerrak, further to the north, is usually regarded as part of the North Sea. It is about 1, km long, in the north-south direction, and km wide, on average, in the east-west direction, with an area of aboutkm2 and a volume of 21, km3.

It accounts for 8, km of continental coastlines, but the Swedish and Finnish coastal archipelagos include a multitude of unaccounted islets, rocks and skerries2 30, in the Stockholm region alonewhich may increase considerably the total figure. A characteristic feature of the Baltic Sea is the presence of several interconnected basins, with depths ranging from 47 to m, separated by shallow sills that restrict water exchanges. The overall average depth is 57 m, while the deepest point, the Lansort Deep in the western Baltic Proper, is m. The fact that the main basin does not originate from the collision of tectonic plates, but is a glacially scoured river valley created after the last ice 2 A reef or rocky island covered by the sea at high tide or in stormy weather.

The European and Marginal Seas: An Overview 11 age some 10, years ago, accounts for its relative shallowness. Its only links with the Kattegat and the open sea are the straits in the Belt Sea. The central Great Belt is the widest, has a sill depth of 18 m and accounts for about two-thirds of the water flowing in or out the Baltic Sea. The Little Belt, to the west, is very narrow, and most of the remaining flow occurs through the Sound, with a sill depth of only 8 m, to the east. The Baltic Sea extends What to do if your daughter is dating a jerk a relatively mild and humid climate zone in the south to the Arctic region in the north.

The average air temperature is 4. The restricted water exchange through the Belt Sea straits implies a residence time of about 25—35 years for Baltic Sea waters. Precipitation over the basin roughly equals evaporation, so that the total freshwater input can be equated to river runoff although there are local and seasonal departures Mature sluts in benoni this pattern, with maximum runoff occurring in spring, during the snow-melting period. As a result, salinity is very low mean around 7.

The freshwater input drives an 12 V. Barale outgoing, lower-salinity mean 8. There are no significant tides Older swm seeking younger for fun in rovinj the Baltic Older swm seeking younger for fun in rovinj. However, seasonal variation in the water level can be more than 1. Due to the large freshwater input and limited tidal excursion, the water column of the Baltic Sea has a stable density stratification which would prevent oxygenated surface water from mixing downward in the water columnwhich is overcome only through winddriven convection. Major inflows of saline waters are caused by largescale pressure differences between the North Sea and the Baltic Sea areas, while persistent westerly winds can generate short-term inflows, so that the water in the deepest parts of the basin is periodically renewed.

Between these extreme inflows, when vertical mixing is limited, the deep waters are stagnant and eventually become anoxic. Due to its high latitude, relatively poor mixing and low salinity, ice cover is a characteristic feature of the Baltic Sea. The ice-covered area during a normal winter includes the Gulfs of Bothnia, Finland and Riga, as well as the Moonsund archipelago enclosure. The Baltic Proper does not freeze during a normal winter, with the exception of sheltered bays and shallow lagoons. The ice reaches its maximum extent in February or March. Typical ice thickness in the northernmost areas is about 70 cm for landfast sea ice.

The thickness decreases southward. The Baltic Sea is characterised by low biodiversity — even if its fauna includes species of fresh, brackish and marine waters — and by a simplified food web. This is because the sea is geologically very young, while physically it has very low oxygen levels, low water temperature and fluctuating salinity. Species distribution is largely determined by these physical factors. Salinity can be regarded as the single major factor constraining species distribution, since diversity tend to decrease with decreasing salinity. The drainage basin of the Baltic Sea is more than four times larger than the entire sea surface area.

It is densely populated around 85 million people, 15 of which live within 10 km of the coastheavily industrialised, and includes large areas devoted to intensive agriculture. The enclosed nature of the basin makes it very sensitive to pollution. Water quality is under pressure from the various anthropogenic activities above and by extensive shipping of cargo and petroleum products. Even potentially dangerous World War II chemical deposits, known to exist in relatively shallow areas, contribute to increase environmental concerns. Over-fishing is also an issue of major concern.

The main environmental threats are eutrophication and pollution by persistent organic compounds, heavy metals and oil. Eutrophication, due to excessive imput of nutrients from rivers, coastal The European and Marginal Seas: An Overview 13 point sources and atmospheric deposition, as well as recurrent extensive summer blooms of cyanobacteria e. Nodularia spumigenacan be major factors in the formation of large oxygen-depleted areas, often resulting in large-scale death of benthic fauna. Petroleum products, which decompose rather slowly in the cold Baltic waters, also poses a significant threat to the Baltic ecosystem and wildlife. SeaWiFS data, simulated true-colour, 25 August The basin was commonly thought to be a remnant of the ancient Tethys Ocean.

It is now known to be a structurally younger ocean basin, called Neotethys, which formed during the Late Triassic and Early Jurassic rifting of the African and Eurasian plates. The geologic history of the Mediterranean basin is complex, involving first the break-up and then the collision of the African and Eurasian plates, and the Messinian Salinity Crisis in the late Miocene, when the whole sea dried up almost completely. It has dimensions of about 3, km in the east-west direction and a maximum of 1, km average around km in the north-south direction. It accounts for 46, km of coastlines, one-third of which are due to the mainland and islands of the Aegean Sea. Several mountain ranges e.

Since these mountains mostly slope steeply into the sea, the northern drainage basin is relatively small. And since the southern side is mainly covered by desert — and only a few large rivers e. The Mediterranean Sea consists of a series of deep depressions, connected to each other, with an average depth of 1, m. Actual depths vary between 2, and 3, m in western basin, and between 3, and 4, m in the eastern basin, where a maximum of 5, m is reached in the Calypso Deep of the Ionian Sea. The two main basins are separated by the Sicily Channel with a m sill depth and the Strait of Messina 80 mwhile the Strait of Otranto m separates the Adriatic Sea from the eastern basin.

The Mediterranean Sea is connected to the Atlantic Ocean by the km-wide Strait of Gibraltar with a m sill depthin the west; to the Black Sea by the Bosphorus, and the Dardanelles 55 min the north-east; to the Red Sea via the Suez Canal 12 min the south-east. The Mediterranean climate, famous for its abundant sunshine, is subject to both sub-tropical and mid-latitude weather systems, and is also influenced by the northern mountain ranges. Strong local winds, such as the cold, dry, northerly Bora and Mistral, and the hot, dry southerly Sirocco, typify the region, particularly in winter. An Overview 15 Sea is characterized by very high salinity mean around 38 psua fact that is central to water circulation within the basin.

Evaporation is especially high in the eastern Mediterranean, causing the water level to decrease and salinity to increase up to 39 psu eastward. This pressure gradient pushes cooler, lower-salinity about 36 psu water from the Atlantic Ocean across the entire basin. The relatively less dense Atlantic water flows into the Mediterranean Sea through the Strait of Gibraltar, in the surface layer. The incoming water warms and becomes saltier as it travels east, and is eventually turned into denser Mediterranean waters through evaporation. It sinks in the Levantine basin as well as in other areas where deep waters are formeddue to winter cooling, moves back westward and ultimately spills over the sill of the Strait of Gibraltar, in the bottom layer, and out into the Atlantic Ocean.

The complete cycle determines a residence time in the basin of about 80 to years. Tidal amplitudes are small, in the Mediterranean Sea, and the narrow continental shelves prevent tidal amplification along the coast. However, a substantial amount of vertical mixing is provided by strong regional winter wind regimes. Deep waters are formed in the Adriatic Sea and the Aegean Sea, although with different characteristics, and outspill into the eastern basin over the sills in the Otranto Strait and around Crete, respectively. This can lead to a complete overturning of the water column, with deep convection processes taking place over m of water.

The process ventilates the deepest parts of the Mediterranean Sea and triggers the onset of large algal blooms, sometimes covering the entire northwestern basin. The deep waters of the eastern and western basins do not communicate, due to the shallow sill of the Sicily Channel. On average, the Mediterranean Sea is poor in nutrients, with consequent low phytoplankton biomass and primary production. Oligotrophy increases from west to east. By contrast, a rich biodiversity characterizes the Mediterranean ecosystem: No species disappearances have been reported, but changes in species composition and richness have occurred in some areas.

The introduction of exotic species — such as that of tropical 16 V. Barale species from the Red Sea, which occurred after the Suez Canal opening3 — is a growing concern. Large populations of marine mammals e. Land-based activities urbanization, industry and agriculture, particularly in the northwest are the main sources of pollution. Adding to the resident population, each year the Mediterranean Sea is also host to million tourists. Population density, almost people per km2, twice that of the region as a whole, and related economic activities place a high pressure on coastal zones. Since the Mediterranean Sea is essentially oligotrophic, eutrophication is limited to nearcoastal sites that receive anthropogenically enhanced nutrient loads from rivers, or direct discharges of untreated domestic and industrial wastewaters, and adjacent open waters.

The convexity of both the southern and the northern coastline, the latter extending south from the Crimean peninsula, suggest a further geographical subdivision into two sub-basins. In the north-east, it is also connected to the shallow Azov Sea via the Kerch Strait. An Overview 17 in the north-south direction, and 1, km, in the east-west direction. Its total area is aboutkm2 and its volumekm3. It accounts for about 4, km of coastlines. SeaWiFS data, simulated true-colour, 13 June The Black Sea basin was formed during the Miocene orogenesis, which uplifted the mountain ranges that divided the ancient Tethys Ocean into several brackish basins the remnants of which include also the Azov Sea, Caspian Sea and Aral Sea.

The Black Sea comprises a central deep basin, with an average depth of 1, m, rising to form a broad shelf in the northwest. In this region, the shelf is up to km wide and has depth up to m. To the south and east, the shelf is only 2 to 20 km wide and has a depth of less than m. The Euxine abyssal plain in the centre of the Black Sea has depths between 2, and 2, m, reaching a maximum 2, m south of the Crimean peninsula. Before the Encore launch this year, Seabourn's passenger ships still evoked some of that small-ship experience, or at least passengers like us pretended they did.

These vessels-- the Quest, Sojourn, and Odyssey-- presented a challenge to Seabourn as it rapidly doubled and redoubled recruiting and training to staff the ships. The results were mixed, at least in our travels on each of the three, but they still triggered our memories of the Spirit. For us, the bulked-up Encore lacks this link to the past. Fantasy Island Passenger Spirit, Rovinj, Croatia, Aug 6 The magic of the Spirit was created by mutual agreement between passengers and crew, all of whom embraced the fantasy that they were aboard a private yacht and all of whom behaved appropriately. Guests we encountered on three Spirit itineraries were self-assured, friendly without spilling their life story in the first five minutes of conversation, and had nothing to prove to fellow passengers.

This self-confidence was perhaps most conspicuous in their dress, which was ironically not conspicuous. We all dressed like we were on a prosperous uncle's yacht. But many of the tools used to facilitate instant friendships depart from the original small-ship experience. Early in each cruise there is a party of sorts stretched through all the guest decks and companionways. We found it more like a college dorm party for new freshmen. Love it or hate it. The crowd on our first segment from Civitavecchia to Dubai seemed a bit older than some past Seabourn cruises. Public, unguarded conversations about options for hip replacement, the benefit of dying quickly if you have cancer, and extended family health histories made us sometimes feel we were on a Holland America cruise.

Holland America, which attracts an older profile, has been the sister line of Seabourn since management of both was consolidated by big brother Carnival, the ultimate owner, a few years ago. More Space But Just As Full Seabourn built larger public spaces to make everyone more comfortable, but also books many more passengers to fill the bigger ship. To manage poolside crowds, bulletins remind clients that sun bathing is available not just at the main pool midships, but at new locations fore and aft. That is to say that you may quite clearly hear gratuitously loud conversational outbursts in English or non-English languages, including German or New Jersey or Australian. Bar Stool Strategy will be featured in a future column.

Cocktail hour hors d'oeuvres and teatime treats except the scones are no longer passed in the Observation. This provides a greater variety but less "luxury" than passed hors d'oeuvres, which are still offered in the Club lounge. New to us is a bar menu that includes additional charges for what Seabourn considers premium liquors. All this in an all-inclusive format that promises no charge for fine wine and spirits throughout the ship and no requirement or expectation of tipping. The Encore's slightly larger stage makes space for more ambitious evening entertainment programs.

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