Oceanography Term Papers

Reports on the topic of oceanography are preferred to be written in APA style.

These are the folowing Branches of Oceanography:

Marine biology
Chemical oceanography
Marine geology
Meteorologic oceanography
Physical oceanography

Oceanographers:

Dr. Robert Duane Ballard
Roger Revelle (1909-1991)
VADM W. W. Behrens, Jr.
Svante Arrhenius (1859-1927)
Henry Bryant Bigelow
John Martin (1935-1993)
RADM Richard E. Byrd

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Oceanography Term:

Science of the ocean, as well as the lessons of current, tides, current of air, geology of the seafloor, living organisms, and the ocean-atmosphere interactions.

It is the study of oceans and seas. Oceanography is the science of studying the sea. But why do humans who live on the land want to spend their time investigating the oceans? Because oceans play a big part in how we live our lives on land.

For instance, the oceans affect the weather. They also provide us with an abundance of food and with many different sources of energy, In fact, without the oceans, we could not exist! Many scientists have devoted their lives to discovering the mysteries of aquatic life.

Oceans cover nearly 71 percent of the earth's surface! That is a lot of ground to cover for the oceanographers, or scientists involved in the study of the sea.

The science of oceanography is rapidly growing, becoming progressively complex as comprehensive hypothetical studies of different oceanic facts are carried out and as more observations become available to check and direct them.

Over two-thirds of the Earth's surface is covered by oceans and play a vital part in life on Earth, pretty separate from their own basic concern.

THE oceans form one of the fundamental divisions of the Earth's surface and their volume is considerably greater than that of the land above sealevel. Indeed, if all the inequalities of the Earth were leveled off there would be enough water in the oceans to cover the whole surface of the Earth to a depth of about 8,600 ft. Most of the land lies fairly close to sea-level, the mean height of the continents being 2,300 ft. above sealevel, while the oceans, on the other hand, have their greatest area between 12,000 and 18,000 ft. below sea-level. In fact, 41 per cent of the whole surface of the Earth lies between the last two depths. It is worth noting that in terms of the diameter of the globe, which is nearly 8,000 miles, the relief features of the continents and oceans are relatively insignificant. The highest mountains and greatest deeps are only just over 65,000 ft. apart vertically; this is about 12.3 miles or ⅓30 of the radius. Nevertheless there are very important differences between the structure and relief of the ocean basins and the continental areas.

Of all the major units of the Earth's surface the Pacific Ocean is the greatest, covering about half of the whole globe. It also contains the largest single unit of truly oceanic structure, although this is considerably smaller than the aerial extent of the whole of the Pacific. Recent work has given a much clearer picture of the nature and extent of the major structural types within the oceans.

The circulation of the oceans is an important aspect of oceanography from the geographical point of view; it helps to distribute heat received in low latitudes to certain areas in higher ones, with all this implies with regard to climatic modifications.

Conclusion
The subject of oceanography is so wide that it has not been possible to do more than indicate some of the very interesting fields which are now being actively explored. A few of the ways in which the oceans influence and play their part in human life on Earth have been briefly mentioned, but the interaction of the oceans and the land are so intricately interwoven that it is impossible to unravel all the threads. They play a part on the Earth which is much greater than the attention normally given to them would suggest, and exert an influence either direct or indirect over the surface of the globe. Within them are still hidden many secrets, but elaborate and detailed research work is gradually revealing the unknown and fascinating processes operating in the oceans, on their surface, at their edge, where they meet the land, and on their floor.

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