WASHINGTON NAVY YARD – The Navy officer who took a manned submersible to the deepest part of the ocean in 1960 said it would have been impossible without the steady financial support by the Office of Naval Research for oceanographic research. Read More
Proceedings, January 2013
Marine Protected Areas (MPAs) are designated sites found throughout the World Ocean that are set aside for special protection and management. They conserve and protect sensitive ecosystems as well as cultural history. Governments ranging from the national to the local levels have established MPAs in almost every coastal nation in the world.
The United Nations Law of the Sea Treaty (UNCLOS) gives signatory coastal states a 200-mile wide Exclusive Economic Zone (EEZ). This includes a 12-mile-wide territorial sea where those countries have full sovereign rights. Beyond that point, states have quasi-sovereign rights to regulate almost all activities out to their 200-mile boundary. Thus coastal states have clear authority to establish MPAs within their EEZs. However, at present most are located within territorial waters. Read More
Proceedings, November 2012
Both are Navy-owned deep submersibles. One was retired in 1963, while the other is still active. But their histories are related.
The bathyscaph Trieste joined the U.S. Navy in 1958. Based at the Naval Electronics Laboratory (NEL) in San Diego, she was deployed to Guam for a series of deep dives in 1959–60 that included one to the deepest place in the ocean.
Proceedings, Sept. 2012
Carbon dioxide . . . it’s what makes our soft drinks zesty and champagne . . . well, champagne. It is also a major greenhouse gas. Absorbed into the sea it is an essential component for growth of plankton, the first stage of marine life. By contrast, excessive amounts can make some organisms sick and possibly extinct.
The beneficial role of CO2 is in the photosynthetic process that feeds phytoplankton, the microscopic plants of the sea. Carbon dioxide, solar energy and the chlorophyll pigment combine to make food for these organisms that are the first level of life in the sea. A critical byproduct of this chemistry is the respiration of oxygen by these tiny plants. The vast surface area of the World Ocean supplies 50–80 percent of Earth’s oxygen. Indeed, it is the lungs of our planet.
The sea has an enormous capacity to absorb CO2. Since the Industrial Revolution began about 1750, man’s activities have loaded the atmosphere with great quantities of it. However the oceans have been able to absorb about 50 percent of this anthropogenic CO2. Remarkably, this percentage has remained fairly constant over the past 250 years even as increasing amounts are injected into the Earth’s atmosphere. But this “carbon sequestration” comes at a price. When atmospheric CO2 dissolves in seawater there is a chemical reaction that forms carbonic acid, a very weak acid.
Scientists use the pH numerical scale to define the relative acidity or alkalinity of a solution using a range of 0–14. Distilled water is neutral at a value of 7.0. Numbers lower than this are acidic and those above are alkaline. At present the average pH for the oceans is 8.1, so it is slightly alkaline—but this number is decreasing steadily. To be clear, it is unlikely that the oceans’ pH will ever drop below 7.0, so the term “acidification” refers to relative acidity as seawater becomes less alkaline. The accompanying graph shows the relationship between dissolved CO2 and increasing acidity in the sea from the years 1850–2100 (estimated).