bookmark_borderBounty of the Sea: More Plastic Than Fish?

The Ellen MacArthur Foundation and the World Economic Forum, in a report called The New Plastics Economy  (which looks at the amount of plastic that ends up in the sea) claims there will be more plastic than fish in the sea by 2050. “If we continue dumping plastic in the sea at the present rate, measured by weight, there will be more plastic than fish by 2050.”

The study examines just one area – San Francisco Bay. “If that’s not representative of the rest of the globe then you can see the potential for large deviations in this calculation,” says Prof Callum Roberts from the University of York.

Plastic Vs. Fish in the Ocean
Plastic Vs. Fish in the Ocean

The Human Induced Climate Change Experiment

bookmark_borderSea Serpents Washing Ashore

Oarfish / Sea Serpent
Oarfish / Sea Serpent

CALIFORNIA — Two rare oarfish have washed up on California beaches. A dead 18-foot-long oarfish was found off Catalina Island on October. 13. A 14-foot-long oarfish carcass was found on Oct. 18 in Oceanside, CA.

Oarfish can grow to more than 50 feet in length and are considered the longest fish. Their appearance has led to many theories of sea serpents.

Japanese folklore believes the beaching of oarfish predicts earthquakes — “a notion that some scientists have speculated could be supported by the bottom-dwelling fish being more sensitive to seismic shifts.”

“It’s probably just a coincidence,” said Rick Feeney of the Natural History Museum of Los Angeles County. “We think that they come inshore to die actually because they’re in distress for some reason, but we don’t know what the reason is,” said Feeney, adding that the fish could have been starving or disoriented.

However, the one found off Catalina Island has been dissected and found to be healthy. “It looks good enough to eat – if you have a 13ft pan,” biologist Ruff Zetter said.

 

Oarfish Found In California
Oarfish Found In California

bookmark_borderWhy Doesn’t Global Warming Feel Warmer?

The Intergovernmental Panel on Climate Change (IPCC) has released its Fifth Assessment Report (AR5). The report states that “warming of the climate system is unequivocal.”

Then, why doesn’t it feel that much hotter? Because most of the rise in temperature is in the water:

Ocean warming dominates the increase in energy stored in the climate system, accounting for more than 90% of the energy accumulated between 1971 and 2010 (high confidence). It is virtually certain that the upper ocean (0?700 m) warmed from 1971 to 2010, and it likely warmed between the 1870s and 1971.

• On a global scale, the ocean warming is largest near the surface, and the upper 75 m warmed by 0.11 [0.09 to 0.13] °C per decade over the period 1971–2010. Since AR4, instrumental biases in upper-ocean temperature records have been identified and reduced, enhancing confidence in the assessment of change.
• It is likely that the ocean warmed between 700 and 2000 m from 1957 to 2009. Sufficient observations are available for the period 1992 to 2005 for a global assessment of temperature change below 2000 m. There were likely no significant observed temperature trends between 2000 and 3000 m for this period. It is likely that the ocean warmed from 3000 m to the bottom for this period, with the largest warming observed in the Southern Ocean.
• More than 60% of the net energy increase in the climate system is stored in the upper ocean (0–700 m) during the relatively well-sampled 40-year period from 1971 to 2010, and about 30% is stored in the ocean below 700 m. The increase in upper ocean heat content during this time period estimated from a linear trend is likely.
• It is about as likely as not that ocean heat content from 0–700 m increased more slowly during 2003–2010 than during 1993–2002. Ocean heat uptake from 700–2000m, where interannual variability is smaller, likely continued unabated from 1993 to 2009.
• It is very likely that regions of high salinity where evaporation dominates have become more saline, while regions of low salinity where precipitation dominates have become fresher since the 1950s. These regional trends in ocean salinity provide indirect evidence that evaporationand precipitation over the oceans have changed (medium confidence).
• There is no observational evidence of a trend in the Atlantic Meridional Overturning Circulation (AMOC), based on the decade-long record of the complete AMOC and longer records of individual AMOC components.

bookmark_borderClimate Change Pearls of Wisdom

Learn more about global warming.

World Oceans Month Brings Mixed News for Oysters
by the National Science Foundation

Ocean acidification inhibits shell formation, but interventions at hatcheries may offset some effects, scientists find

In World Oceans Month, there’s mixed news for the Pacific Northwest oyster industry.

For the past several years, it has struggled with significant losses due to ocean acidification. Oyster larvae have had mortality rates high enough to render production no longer economically feasible.

Now a new study documents why oysters appear so sensitive to increasing acidity, but also offers some hope for the future.

It isn’t necessarily a case of acidic water dissolving the oysters’ shells, scientists say. It’s water high in carbon dioxide altering shell formation rates, energy usage and, ultimately, the growth and survival of young oysters.

“The failure of oyster seed production in Northwest Pacific coastal waters is one of the most graphic examples of ocean acidification effects on important commercial shellfish,” said Dave Garrison, program director in the National Science Foundation’s (NSF) Division of Ocean Sciences.

NSF funded the study through its Ocean Acidification Program, part of NSF’s Science, Engineering and Education for Sustainability programs.

“This research is among the first to identify the links among organism physiology, ocean carbonate chemistry and oyster seed mortality,” said Garrison.

Results of the study are online in the journal Geophysical Research Letters, published by the American Geophysical Union.

“From the time eggs are fertilized, Pacific oyster larvae precipitate roughly 90 percent of their body weight as a calcium carbonate shell within 48 hours,” said George Waldbusser, an Oregon State University marine ecologist and lead author of the paper.

“Young oysters rely solely on the energy they derive from the egg because they have not yet developed feeding organs.”

During exposure to increasing carbon dioxide in acidified water, however, it becomes more energetically expensive for organisms like oysters to build shells.

Adult oysters and other bivalves may grow more slowly when exposed to rising carbon dioxide levels. But larvae in the first two days of life do not have the luxury of delayed growth.

“They must build their first shell quickly on a limited amount of energy–and along with the shell comes the organ to capture external food,” said Waldbusser.

“It becomes a death race of sorts. Can the oyster build its shell quickly enough to allow its feeding mechanism to develop before it runs out of energy from the egg?”

The results are important, marine scientists say, because they document for the first time the links among shell formation rate, available energy, and sensitivity to acidification.

The researchers say that the faster the rate of shell formation, the more energy is needed. Oyster embryos building their first shells need “to make a lot of shell on short order,” said Waldbusser.

“As the carbon dioxide in seawater increases, but before waters become corrosive, calcium carbonate precipitation requires more energy to maintain higher rates of shell formation during this early stage.”

The researchers worked with Whiskey Creek Shellfish Hatchery in Netarts Bay, Ore. They found that on the second day of life, 100 percent of the larval tissue growth was from egg-derived carbon.

“The oyster larvae were still relying on egg-derived energy until they were 11 days old,” said Elizabeth Brunner of Oregon State University and a co-author of the paper.

The earliest shell material in the larvae contained the greatest amount of carbon from the surrounding waters.

Increasing amounts of carbon from respiration were incorporated into shells after the first 48 hours, indicating an ability to isolate and control the shell surfaces where calcium carbonate is being deposited.

Waldbusser notes that adult bivalves are well-adapted to growing shell in conditions that are more acidified, and have evolved several mechanisms to do so.

These include use of organic molecules to organize and facilitate the formation of calcium carbonate, pumps that remove acid from the calcifying fluids, and outer shell coatings that protect minerals to some degree from surrounding waters.

Waldbusser said that the results help explain previous findings at the Whiskey Creek Hatchery of larval sensitivity to waters that are high in carbon dioxide but not corrosive to calcium carbonate.

They also explain carryover effects later in larval life of exposure to high carbon dioxide, similar to human neonatal nutrition effects.

The discovery may be good news, scientists say, because there are interventions that can be done at hatcheries that may offset some of the effects of ocean acidification.

Some hatcheries have begun “buffering” water for larvae–essentially adding antacids to incoming waters–including the Whiskey Creek Hatchery and the Taylor Shellfish Farms in Washington.

The study provides a scientific foundation for the target level of buffering.

“You can make sure that eggs have more energy before they enter the larval stage,” said Waldbusser, “so a well-balanced adult diet may help larval oysters cope better with the stress of acidified water.”

-NSF-

bookmark_borderEarth

Special Picture Of Earth
Special Picture Of Earth

Information:

Go here to view an image that explains how composite images like these are created: www.flickr.com/photos/gsfc/6803619953

Responding to public demand, NASA scientists created a companion image to the wildly popular ‘Blue Marble’ released last week (January 25, 2012). www.flickr.com/photos/gsfc/6760135001

The new image is a composite of six separate orbits taken on January 23, 2012 by the Suomi National Polar-orbiting Partnership satellite. Both of these new ‘Blue Marble’ images are images taken by a new instrument flying aboard Suomi NPP, the Visible Infrared Imaging Radiometer Suite (VIIRS).

Compiled by NASA Goddard scientist Norman Kuring, this image has the perspective of a viewer looking down from 7,918 miles (about 12,742 kilometers) above the Earth’s surface from a viewpoint of 10 degrees South by 45 degrees East. The four vertical lines of ‘haze’ visible in this image shows the reflection of sunlight off the ocean, or ‘glint,’ that VIIRS captured as it orbited the globe. Suomi NPP is the result of a partnership between NASA, NOAA and the Department of Defense.

Credit: NASA/NOAA

For more information about Suomi NPP go to: www.nasa.gov/npp

NASA image use policy.

NASA Goddard Space Flight Center enables NASA’s mission through four scientific endeavors: Earth Science, Heliophysics, Solar System Exploration, and Astrophysics. Goddard plays a leading role in NASA’s accomplishments by contributing compelling scientific knowledge to advance the Agency’s mission.