Sunday, September 26, 2010

Articles


Global Cycle of Mercury


Mercury cycles in the environment as a result of natural and human  activities.  Most of the mercury in the atmosphere is elemental mercury vapor, which circulates in the atmosphere for up to a year, and can be widely dispersed and transported thousands of miles from likely sources of emission. Most of the mercury in water, soil, sediments, or plants and animals is in the form of inorganic mercury salts and organic forms of mercury (e.g., methylmercury). The inorganic form of mercury, when either bound to airborne particles or in a gaseous form, is readily removed from the atmosphere by precipitation and is also dry deposited. Wet deposition is the primary mechanism for transporting mercury from the atmosphere to surface waters and land. Even after it deposits, mercury commonly is emitted back to the atmosphere either as a gas or associated with particles, to be re-deposited elsewhere. As it cycles between the atmosphere, land, and water, mercury undergoes a series of complex chemical and physical transformations, many of which are not completely understood.  Because it is very toxic and accumulates in organisms, particularly fish, merucry is an important pollutant and one of the most studied.

http://www.jstor.org/pss/221718


Red Tides and Dead Zones

The intensification of agriculture, waste disposal, coastal development, and fossil fuel use has increased the discharge of nitrogen, phosphorus, and other nutrients into the environment.  The nutrients are moved by streams, rivers, groundwater, sewage outfalls, and the atmosphere toward the sea.  Once they reach the ocean, nutrients stimulate the growth of timy marine plants called phytoplankton or algae.  When these species occur in high concentrations, they can color the water and produce what are popularly referred to as “red tides” or “brown tides.”  Scientist prefer to call these outbreaks harmful algal blooms of HABs.


Andrew R Solow.  (2004). Red Tides and Dead Zones. Oceanus, 43(1), 43-45.  Retrieved September 26, 2010, from Research Library. (Document ID: 978253011).


 http://proquest.umi.com/pqdweb?index=2&did=978253011&SrchMode=1&sid=1&Fmt=4&VInst=PROD&VType=PQD&RQT=309&VName=PQD&TS=1285545203&clientId=30360



Precursors to the El Nino/La Nina onset and their Interrelationship

This article was rather technical and extremely boring.  The jest of the article was about the equatorial sea level, western Pacific zonal wind, and high-frequency wind variability as precursors of the onset of El Nino and La Nina. 



Sunday, September 12, 2010

Bathymetric Maps and Hypsographic curves

The term bathymetry is defined as the depth of water relative to sea level. Thus bathymetric measurements can determine the topography of the ocean floor, and have shown that the sea floor is varied, complex, and ever-changing, containing plains, canyons, active and extinct volcanoes, mountain ranges, and hot springs. Some features, such as mid-ocean ridges (where oceanic crust is constantly produced) and subduction zones, also called deep-sea trenches (where it is constantly destroyed), are unique to the ocean floor.   Bathymetric maps also depict the contours of lakes.  From these maps you can create a hypsographic curve, which we did for class.  To figure out the total volume of the lake, just add up all the volumes of the different contours.

These are my hypsographic charts:
also for more info on bathymetric maps and hypsographic curves, check out:
http://www.waterencyclopedia.com/Oc-Po/Ocean-Floor-Bathymetry.html
http://lakewatch.ifas.ufl.edu/circpdffolder/Morph2ndEdPt2.pdf

Thursday, September 9, 2010

The Marianas Trench

The Marianas Trench:
It's the deepest spot in any ocean of the world. It is located in the Pacific Ocean, just east of the Phillippines.
Nearby is the island of Guam, a U.S. Territory inhabited by natives identified as Chamorros.  I lived there for four years attending middle school and high school.  It was such a fun place to live.

The Marianas trench is sometimes called the 'Challenger Deep' because it was located and named after His Majesty's Ship 'Challenger' of the British Royal Navy in the 19th century.

The Marianas Trench's depth is about 10,924 m, or almost 11 km (7 miles). This is a height greater than any mountain on the surface of the earth!

Creatures of the deep

Guam