sábado, 7 de agosto de 2010

BBC E-mail: Timeline: BP oil spill

Trajano Paiva saw this story on the BBC News website and thought you
should see it.

** Timeline: BP oil spill **
A timeline of events since the 20 April start of the BP oil leak in the Gulf of Mexico.
< http://www.bbc.co.uk/go/em/fr/-/news/world-us-canada-10656239 >


** BBC Daily E-mail **
Choose the news and sport headlines you want - when you want them, all
in one daily e-mail
< http://www.bbc.co.uk/email >


** Disclaimer **
The BBC is not responsible for the content of this e-mail, and anything written in this e-mail does not necessarily reflect the BBC's views or opinions. Please note that neither the e-mail address nor name of the sender have been verified.

If you do not wish to receive such e-mails in the future or want to know more about the BBC's Email a Friend service, please read our frequently asked questions. http://news.bbc.co.uk/1/hi/help/4162471.stm

sexta-feira, 6 de agosto de 2010

Another Greenhouse Gas to Watch: Nitrous Oxide

Another Gas to watch !

The article below from WHOI has been sent to you by trajano@sosoceanos.com

http://www.whoi.edu/oceanus/viewArticle.do?id=53680

Another Greenhouse Gas to Watch: Nitrous Oxide
Caitlin Frame
Graduate student
MIT/WHOI Joint Program

The Mysterious Movements of Deep-Sea Larvae

About Deep Sea Life

The article below from WHOI has been sent to you by trajano@sosoceanos.org

http://www.whoi.edu/oceanus/viewArticle.do?id=65406

The Mysterious Movements of Deep-Sea Larvae

The marvelous migrations of fish and whales through the deep sea have been hard enough for us humans to follow. But what about tiny organisms—many smaller than the dot beneath this question mark? How they move from one spot to another in the depths has long remained beyond our grasp.

The enigma deepened in 1977, when scientists discovered spectacular and strange communities of animals clustered near vents on the seafloor. These so-called hydrothermal vents spew chemical-rich fluids that sustain clams, mussels, tubeworms, snails, and other species. Like shellfish in shallow waters, most of these relatively sedentary deep-sea animals reproduce by releasing eggs and sperm into the water. These develop into tiny floating larvae—the aquatic animal equivalent of seeds—that disperse, settle at vent sites, and grow.

Here’s the catch: The vents are distributed intermittently along mid-ocean ridges—the long volcanic mountain chains that bisect the seafloor throughout the globe. These vents “turn on” and “turn off,” fueled by the ebbs and flows of hot magma beneath the seafloor.

So how do the larvae, tinier than specks of dust, maintain their populations in such a patchy, transient environment? How do they get transported from one active vent site to another that might be tens of miles or more away?

These questions are keys to understanding how life has evolved on the seafloor and how it survives. Answering them requires a blend of biology, oceanographic physics, geology, and chemistry.

Clean Energy from the Ocean temperature gradient

ScienceDaily (Aug. 4, 2010) — Researchers at the University of Hawaii at Manoa say that the Leeward side of Hawaiian Islands may be ideal for future ocean-based renewable energy plants that would use seawater from the oceans' depths to drive massive heat engines and produce steady amounts of renewable energy.



The technology, referred to as Ocean Thermal Energy Conversion (OTEC), is described in the Journal of Renewable and Sustainable Energy, which is published by the American Institute of Physics (AIP).
It involves placing a heat engine between warm water collected at the ocean's surface and cold water pumped from the deep ocean. Like a ball rolling downhill, heat flows from the warm reservoir to the cool one. The greater the temperature difference, the stronger the flow of heat that can be used to do useful work such as spinning a turbine and generating electricity.
The history of OTEC dates back more than a half century. However, the technology has never taken off -- largely because of the relatively low cost of oil and other fossil fuels. But if there are any places on Earth where large OTEC facilities would be most cost competitive, it is where the ocean temperature differentials are the greatest.

http://www.sciencedaily.com/releases/2010/08/100803175019.htm