Latest Chemical oceanography Stories
Since the beginning of the Industrial Revolution, the concentration of carbon dioxide in the atmosphere has been rising due to the burning of fossil fuels.
Tiny seawater algae could hold the key to crops as a source of fuel and plants that can adapt to changing climates.
The Gulf of Mexicoâ€™s â€œdead zoneâ€ is predicted to be the largest ever recorded due to extreme flooding of the Mississippi River this spring.
The rate of release of carbon into the atmosphere today is nearly 10 times as fast as during the Paleocene-Eocene Thermal Maximum (PETM), 55.9 million years ago, the best analog we have for current global warming.
According to new findings, seas off Papua New Guinea suggest that acidifying oceans will severely hit coral reefs by the end of the century.
A new set of buoys in Alaska waters will help scientists understand how climate change may be affecting the pH level of northern seas.
Salinity â€“ the concentration of salt â€“ on the ocean surface is a key missing puzzle piece in satellite studies of Earth that will improve our understanding of how the ocean and atmosphere are coupled and work in tandem to affect our climate.
HARRISBURG, Pa., May 10, 2011 /PRNewswire-USNewswire/ -- The state departments of Environmental Protection and Agriculture, in collaboration with American Farmland Trust (AFT), plan to celebrate the partnership that has led to nutrient reductions for the Chesapeake Bay watershed. AFT will host an event to donate to DEP and the Department of Agriculture 4,023 nitrogen credits earned by five farmers from Lancaster, Clinton and Northumberland counties who participated in AFT's Best Management...
The acidification of the worldâ€™s oceans could have major consequences for the marine environment.
Last fall, EARTH caught up with geochemistry grad student Jeremy Jacquot as he was about to embark on the first U.S.-led GEOTRACES cruise across the Atlantic, where he and 32 researchers were hoping to measure and track concentrations of various trace elements and isotopes.
Ocean acidification is the name that was given to the ongoing decrease in the pH of Earth’s oceans, a cause of the uptake of anthropogenic carbon dioxide from the atmosphere. About 30 to 40 percent of the carbon dioxide that is released by humans into the atmosphere dissolves into the lakes, oceans, and rivers. To maintain the chemical equilibrium, some of it reacts with the water to create carbonic acid. Some of these extra carbonic acid molecules react with a water molecule to provide a...
- A transitional zone between two communities containing the characteristic species of each.