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Healthy & Resilient Ocean

To describe how the "North Sea Machinery” works takes more than a few maps and very quickly we found ourself overwhelmed with the amount of information that lies in the sea. We Interpreted the task by showing you how the whole sea is connected. To do so we decided to chose some themes to dig down in to. These themes is built on a wish of understanding the different mechanics the ocean needs to be healthy and resilient.

 

Water                        Seabed                          Flora                          Fauna    

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Flora map til blog.jpg
Light map 1_4000000.jpg
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Water Mass.png
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Salinity.png
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Temperature.png
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Water Current + Quantity.png
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Seabed

Substrates

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​​​The benthic substrate of the Greater North Sea is predominantly characterized by soft sediments (from muds to gravel beds). Sediments from mobile muds to coarse sands are present throughout the region. Gravel beds are mainly distributed in the English Channel and the southern North Sea. The North Sea contains limited biogenic and geogenic reefs, except for patches of Sabellaria spinulosa reefs and scattered boulder fields. The shores consist mainly of mobile sediment types, i.e. mud, sand, and boulder beaches, while rocky shores are mostly found in the northern North Sea and the English Channel. The North Sea benthic habitats are impacted by bottom trawling, sand and gravel extraction, and recently also the growing introduction of offshore renewable energy structures such as wind farms, leading to pressures of abrasion, smothering, habitat loss, and selective extraction of non-living resources. Artificial hard substrates, such as hydrocarbon production platforms, wind turbines, and ship wrecks may act as new hard substrate habitat types that increase local biodiversity.

Light reaching the seabed

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Vegetation relies on photosynthesis for energy; sunlight can't penetrate the ocean depths, so plants can't grow in deeper waters. 

In the map of «Light reaching the seabed» We can see a lighter grey zone and a very dark one. The light one is the zone where light breaks the surface of the ocean and travels all the way down to the seabed floor. Most of the southern area of the North sea is only 20 - 40 meters deep. If you look North, the seabed goes deeper, almost reaching 200 meters before drastically going of the cliff and down to 500-1000 meters. 

 

Life exsist both in the dark and in the light. But Photosynthesis only takes place in Euphotic zone (0-200m). If you go further down this proses do not take place, beacuse lack of sunlight.

 

Different plants have their own depth limit. Some plant can live far down in the sea, without much light, meanwhile others need a lot of it and therfor needs to be close to the surface.

 

- 40m Kelp

- 42m Poseidonia

- 58m Seagrasses

- 200m Seaweed

Research

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Water

Water Mass 

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According to the the report by Arthur J. Lee at 1980, he divided different water region in the north sea. This division most likely a conclusion of how water input, temperature circulation and salinity stratification influence the north sea. The water mass map at the left side contains following information:


A1: Water input give lower surface salinity seasonally.

A2: English Coastal Water, vertically mixed

A3: Water being saline 35.0% and relatively warm in winter

A4: Water flowing from the Dover Strait with low salinity and a large annual temperature range.

A5: Salinity increase and shows stratification in summer and break down in August

A6: a mixture of types

A1-A4
B: High salinity (>35.2%) water with small annual temperature range.

C: Low salinity and high annual temperature range.

D: A transition between B and C with strong near surface salinity gradients.

Surface Annual Salinity

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Salinity

Combine the information from water mass map, this north sea surface annual salinity map indicates the influence by fresh water input and also Atlantic water input through the northern entrance.

Water Salinity is a major factor for marine creatures to survive. When the water temperatures and the salinities in the donor and recipient areas show a high degree of similarity, a transferred species is more likely to survive in this condition. The left map indicate salinity conditions in the North Sea can give high survive ability for euryhaline marine species and normal marine species. This conclusion also points a risk of species invasion.

Ballast water Risk

A report made by M. Karin de Boer and Marcel Veldhuis at 2016 mentioned Ballast Water Risk. Due to the salinity condition of north sea, cargo ship contains ballast water from other water region and discharged in the north sea brings a serious risk of marine species invasion which give a down award trend for the local species and also influence biodiversity and ecosystem functions.

Temperature

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Due to wind-induced circulation dominated the north sea, atmosphere gives a considerable influence of heat budget by heat fluxes and variability. During the summer surface sea water shows a clear heat stratification. Till to autumn wind heavily mixed water which let north sea water lose heat stratification, this nonstratification phenomenon also happens at winter by water column. In annual view, surface temperature dosen’t shows a significant difference between regions.

Circulation

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North sea is wind-induced circulation pattern which give considerable influence to the temperature and salinity. On the other hand, inflow and outflow water also play an important role to change temperature and salinity. At north entrance is influenced by Atlantic ocean and shows high salinity. While at the western of north sea shows low salinity and receive species invasion risk and eutrophication fact by fresh water input. 

Flora and Fauna

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Research

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