The Oceans
Oceanography is another application of Earth Science and it consists in
the study of the oceans and seas. These disciplines are subdivided into four
branches: physical oceanography (related with the physical properties of oceans
and seas), chemical oceanography (studies chemical properties), biological
oceanography (studies the biological and ecological features of these water
bodies) and geological oceanography (studies the geological nature of oceans).
This multidiscipline science uses other sciences to investigate and understand
the natural processes of oceans to know and predict their behavior. For this
reason, oceanography studies everything related with these water bodies
including their formation, natural processes, their origins, the life there and
the interaction of humans with oceans, seas and also gulfs. Therefore,
understanding the oceans is important to understand the relationship with other
terrestrial phenomena.
Separating the ocean and sea term is important to have a clear picture
of who they are. Oceans are very large salt water bodies with particular
features that differentiate from continents, and seas are saltwater bodies much
smaller than the oceans and usually they are delimited by land or islands. Earth
oceans are Pacific (the bigger), Atlantic (an ocean with a S form and extending
toward both poles), Indian (with a triangular form), Artic (located in the North
Pole) and Antarctic (located in the South Pole), the last two are the smallest.
Some of the most important seas of Earth are Mediterranean Sea, Red Sea, Dead
Sea, Black Sea, Caribbean Sea, among many others. Gulfs, bays, narrows and
inlets are also part of the oceans. Oceans, seas, and ocean ice compose the
97.957% of total volume of water that exists on Earth. In general terms, the greater
amount of water of oceans was originated from the melting of the rocks and the
impacts of meteors, these and other events cause that the water trapped in the
rocks escapes to the atmosphere in form of water vapor and becoming liquid
precipitate as rain. The salt in the oceans is the result of physic and
chemical weathering of igneous rock of the Earth crust. The relief, depth, composition
and slope of the oceans are also studied by oceanographers.
In the oceans many processes occur, all working and contributing to
these water bodies at same time. The Hydrologic Cycle is very important to the
oceans because it removes and deposits water from and to the oceans, also
involving lands. An important process of the oceans is the salinity that is the
quantity of dissolved solids in the ocean water. Chlorine and sodium are the
major components of ocean water, although there are others components like
sulfate, calcium, potassium, bicarbonate, acids and other substances. In areas
of high rainfall on land and in the mouth of large rivers the salinity is lower
due to discharge of fresh water from runoff. On the other hand, the sea waters
near desserts and enclosed seas are high in salinity. The oceanic circulations
are another process of these, for example the thermohaline circulation is the movement
of depth water generated by the salinity and temperatures, these circulations
distributes the water of the Atlantic Ocean to the rest of the oceans and brings
oxygen from surface to depth areas. Surface circulation is the most important
and is driven by the winds. These circulations influence the atmosphere and
therefore affect the weather, generating most of the atmospheric phenomena. Tides
and waves are natural processes of oceans and seas; the tides are the
horizontal and vertical movements of the water caused by the gravitational
forces of the Moon and Sun, every day and depending on the position of the Moon
in regard to respect the Earth there are high and low tides. The waves are
energy or a periodic disturbance that moves from one part to another over the
surface of water, these are generated offshore and arrive to the coast
generating breaking waves.
Oceanographic biology is an important part of this discipline. This
studies all the life and ecosystems that exists in these water bodies. The
marine environment is dominated by some factors like temperatures, depth,
salinity, nutrients, acidification, underwater currents, etc. The terrestrial
environment, influences the sea and oceans ecosystems, for example, all the
nutrients that arrive from lands through rivers are deposited in seas, these
nutrients are used by sea plants and other organisms. The atmosphere also influence in the life of
oceans because it provides the majority of gases including oxygen and carbon
dioxide. The oceans harbor life of all
kinds and size, from microscopic plants to microscopic animals, also there are
the bigger animals of Earth. Into the ocean and seas we have different
ecosystems like rocky coasts, the beaches, estuaries, mangroves, marine
lagoons, sea grasses, coral reefs, polar zones and also there is life in the
deepest areas of the oceans. The majority of these ecosystems have a direct
relation with land and therefore with the organisms and humans that live here. In
geological terms the oceans plays a very important role, the majority part of
sand is originated in the seas, also part of the rocky coast is formed due to
the energetic action of waves and these rocks are composed of death sea
organisms.
References:
Information:
Alonso J., Serie
Naturales. (1998). Descubrimiento 9 Ciencia Integrada.
Puerto Rico: Ediciones Santillana,
Inc.
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