River Inflow

Clastic material

Aeolian (windblown) dust

Dissolved Components

Clay Minerals etc.

Organic material

Skeletal Material

Biological aggregation (packaging)

Sinking Particles

Clay, calcium carbonate, silica and organic material

Photosynthesis

Respiration

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Oceanography


My Blogs (olelog) are mainly based on my daily reading of earth science news.

Here on whatonearth.olehnielsen.dk I try to weave some of the pieces together to a greater whole with added background info.

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Particle Formation in Oceans

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Ocean Circulation

Ocean circulation is driven by energy from the sun and the rotation of the Earth.

(Solar) Energy

causes circulation of the atmosphere = winds

and variations in temperature and salinity of seawater -> temperature and salinity controls the water's density.

Earth rotation and the Coriolus Force

Due to the rotation of the earth, currents are deflected to the right in the northern hemisphere and to the left in the southern hemisphere. This effect is known as the "Coriolis force."

In the Northern Hemisphere currents curve to the right (clockwise).

In the Southern Hemisphere currents curve to the left (counter-clockwise)

Dust Busters

How do essential nutrients like iron and other minerals get into vast watery stretches of the open ocean?

According to one theory, large swirling currents, called eddies, pump nutrients from the depths up toward the sunlit surface, giving phytoplankton (microscopic marine plants) the ingredients they need to flourish. But a larger source of iron may be dust storms, which blow huge quantities of mineral-rich soil particles (called Aeolian dust) out to sea, particularly from desert regions in Africa and Asia.

A team calling themselves the “Dust Busters” have designed a device, mounted on a buoy that collects wind-blown particles in the open ocean, to investigate the theory. Their first findings will be published in the journal Deep-Sea Research.
NSF will fund further research.

News from Oceanus


The image shows Saharan dust swept off the west coast of Africa, then turned northwards on March 8, 2006. http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=17207
NASA image courtesy Jeff Schmaltz, MODIS Land Rapid Response Team at NASA GSFC

The pelagic zone (also known as the open-ocean zone) is further divided into parts, creating a number of sub-zones, based on their different ecological characteristics (which is roughly a function of depth):
* Epipelagic (from the surface down to around 200 m) - the illuminated surface zone where there is enough light for photosynthesis. Due to this, plants and animals are largely concentrated in this zone. Here one will typically encounter fish such as tuna and many sharks.
* Mesopelagic (from 200 m down to around 1000 m) - the twilight zone. Although some light penetrates this deep, it is insufficient for photosynthesis. The name stems from Greek ?????, middle.
* Bathypelagic (from 1000 m down to around 4000 m) - by this depth the ocean is almost entirely dark (with only the occasional bioluminescent organism). There are no living plants, and most animals survive by consuming the snow of detritus falling from the zones above, or (like the marine hatchetfish) by preying upon others. Giant squid live at this depth, and here they are hunted by deep-diving sperm whales. From Greek ????? (bathys), deep.
* Abyssopelagic (from 4000 m down to above the ocean floor) - no light whatsoever penetrates to this depth, and most creatures are blind and colourless. The name is derived from the Greek ??????? (ábyssos), abyss, meaning bottomless (a holdover from the times when the deep ocean was believed to be bottomless).
* Hadopelagic (the deep water in ocean trenches) - the name is derived from Hades, the classical Greek underworld. This zone is 90% unknown and very few species are known to live here (in the open areas). However, many organisms live in hydrothermal vents in this and other zones.


Oceanography treated in Olelog

Oceans as Carbon Sinks

Wednesday, 15 February 2006, 17:11:48
It was generally thought that organic particles sink vertically to the ocean floor relatively rapidly. New studies show that particles are transported to the deep ocean over thousands of years before being deposited on the seabed. This may change our views of how the carbon cycle works (with relevance for global climate) and how oil deposits form.

EurekAlert of 15 February 2006 at http://www.eurekalert.org/pub_releases/2006-02/uonu-toa021506.php


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