Sunday, October 28, 2012

Storm Surge

A bit later this trimester, when we focus our attention in oceanography class on the interactions between the atmosphere and the world ocean, we will learn about one of the key interactions that takes place.  We call them hurricanes, typhoons, tropical cyclones (even willy-willies!), depending on one's geographic location.

Just one of the potentially deadly aspects of a hurricane is its accompanying storm surge.  Hurricane Sandy is no exception.

In included in this post some pertinent information regarding Sandy its predicted surge.




Below is the latest set of storm surge predictions regarding Hurricane Sandy (courtesy of NOAA, via Weatherundground.com):


You can view the Google Maps Interactive Version of this map at the source website:
NOAA - NHC Storm Surge Model

Click on the next link for an excellent short video from NOAA about storm surge.
NOAA Storm Surge Video

Thursday, October 25, 2012

Shifting Phytoplankton Patters


Warmer Future Oceans Could Cause Phytoplankton to Thrive Near Poles, Shrink in Tropics

ScienceDaily (Oct. 25, 2012) — In the future, warmer waters could significantly change ocean distribution of populations of phytoplankton, tiny organisms that could have a major effect on climate change.
Reporting in this week's online journal Science Express, researchers show that by the end of the 21st century, warmer oceans will cause populations of these marine microorganisms to thrive near the poles and shrink in equatorial waters.
"In the tropical oceans, we are predicting a 40 percent drop in potential diversity, the number of strains of phytoplankton," says Mridul Thomas, a biologist at Michigan State University (MSU) and co-author of the journal paper.
"If the oceans continue to warm as predicted," says Thomas, "there will be a sharp decline in the diversity of phytoplankton in tropical waters and a poleward shift in species' thermal niches--if they don't adapt."
Thomas co-authored the paper with scientists Colin Kremer, Elena Litchman and Christopher Klausmeier, all of MSU.
"The research is an important contribution to predicting plankton productivity and community structure in the oceans of the future," says David Garrison, program director in the National Science Foundation's (NSF) Division of Ocean Sciences, which funded the research along with NSF's Division of Environmental Biology.
"The work addresses how phytoplankton species are affected by a changing environment," says Garrison, "and the really difficult question of whether adaptation to these changes is possible."
The MSU scientists say that since phytoplankton play a key role in regulating atmospheric carbon dioxide levels, and therefore global climate, the shift could in turn cause further climate change.
Phytoplankton and Earth's climate are inextricably intertwined.
"These results will allow scientists to make predictions about how global warming will shift phytoplankton species distribution and diversity in the oceans," says Alan Tessier, program director in NSF's Division of Environmental Biology.
"They illustrate the value of combining ecology and evolution in predicting species' responses."
The microorganisms use light, carbon dioxide and nutrients to grow. Although phytoplankton are small, they flourish in every ocean, consuming about half of the carbon dioxide emitted into the atmosphere.
When they die, some sink to the ocean bottom, depositing their carbon in the sediment, where it can be trapped for long periods of time.
Water temperatures strongly influence their growth rates.
Phytoplankton in warmer equatorial waters grow much faster than their cold-water cousins.
With worldwide temperatures predicted to increase over the next century, it's important to gauge the reactions of phytoplankton species, say the scientists.
They were able to show that phytoplankton have adapted to local temperatures.
Based on projections of ocean temperatures in the future, however, many phytoplankton may not adapt quickly enough.
Since they can't regulate their temperatures or migrate, if they don't adapt, they could be hard hit, Kremer says.
"We've shown that a critical group of the world's organisms has evolved to do well under the temperatures to which they're accustomed," he says.
But warming oceans may significantly limit their growth and diversity, with far-reaching implications for the global carbon cycle.
"Future models that incorporate genetic variability within species will allow us to determine whether particular species can adapt," says Klausmeier, "or whether they will face extinction."
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The above story is reprinted from materials provided byNational Science Foundation.
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Journal Reference:
  1. Mridul K. Thomas, Colin T. Kremer, Christopher A. Klausmeier, and Elena Litchman. A Global Pattern of Thermal Adaptation in Marine PhytoplanktonScience, 2012; DOI: 10.1126/science.1224836
 APA

 MLA
National Science Foundation (2012, October 25). Warmer future oceans could cause phytoplankton to thrive near poles, shrink in tropics. ScienceDaily. Retrieved October 25, 2012, from http://www.sciencedaily.com­/releases/2012/10/121025161747.htm
Note: If no author is given, the source is cited instead.
Disclaimer: Views expressed in this article do not necessarily reflect those of ScienceDaily or its staff.

Tuesday, October 23, 2012

Two Fascinating Volcanoes

Sorry to post the same article as earth science again, but it is a timely topic.  Given our recent discussions of seafloor geology, including hot spots and nemataths, I thought this was appropriate...


Geologists recently concluded a study attempting to figure out whether Mauna Loa and Kilauea are connected.  There has long been speculation that they are connected due to their close proximity.

Read on for some more...


Connection Between Hawaii's Dueling Volcanoes Explained

ScienceDaily (Oct. 23, 2012) — A new Rice University-led study finds that a deep connection about 50 miles underground can explain the enigmatic behavior of two of Earth's most notable volcanoes, Hawaii's Mauna Loa and Kilauea. The study, the first to model paired volcano interactions, explains how a link in Earth's upper mantle could account for Kilauea and Mauna Loa's competition for the same deep magma supply and their simultaneous "inflation," or bulging upward, during the past decade.
The study appears in the November issue of Nature Geoscience.
The research offers the first plausible model that can explain both the opposing long-term eruptive patterns at Mauna Loa and Kilauea -- when one is active the other is quiet -- as well as the episode in 2003-2007 when GPS records showed that each bulged notably due to the pressure of rising magma. The study was conducted by scientists at Rice University, the University of Hawaii, the U.S. Geological Survey (USGS) and the Carnegie Institution of Washington.
"We know both volcanoes are fed by the same hot spot, and over the past decade we've observed simultaneous inflation, which we interpret to be the consequence of increased pressure of the magma source that feeds them," said lead author Helge Gonnermann, assistant professor of Earth science at Rice University. "We also know there are subtle chemical differences in the lava that each erupts, which means each has its own plumbing that draws magma from different locations of this deep source.
"In the GPS records, we first see inflation at Kilauea and then about a half a year later at Mauna Loa," he said. "Our hypothesis is that the pressure is transmitted slowly through a partially molten and thereby porous region of the asthenosphere, which would account for the simultaneous inflation and the lag time in inflation. Because changes in pore pressure are transmitted between both volcanoes at a faster rate than the rate of magma flow within the porous region, this can also explain how both volcanoes are dynamically coupled, while being supplied by different parts of the same source region."
Gonnermann said the transmission of pressure through the permeable rock in the asthenosphere is akin to the processes that cause water and oil to flow through permeable layers of rock in shallower regions of Earth's crust.
"When we fitted the deformation, which tells us how much a volcano inflates and deflates, and the lava eruption rate at Kilauea, we found that our model could simultaneously match the deformation signal recorded over on Mauna Loa," said James Foster, co-author and assistant researcher at the University of Hawaii School of Ocean and Earth Science and Technology. "The model also required an increase in the magma supply rate to the deep system that matched very nicely with our interpretations and the increased magma supply suggested by the jump in CO2 emissions that occurred in late 2003."
Mauna Loa and Kilauea, Earth's largest and most active volcanoes, respectively, are located about 22 miles apart in the Hawaii Volcanoes National Park on the island of Hawaii. They are among the planet's most-studied and best-instrumented volcanoes and have been actively monitored by scientists at USGS's Hawaiian Volcano Observatory (HVO) since 1912. Kilauea has erupted 48 times on HVO's watch, with a nearly continuous flank eruption since 1983. Mauna Loa has erupted 12 times in the same period, most recently in 1984.
"To continue this research, we submitted a proposal to the National Science Foundation (NSF) earlier this summer to extend our study back in time to cover the last 50 years," Foster said. "We plan to refine the model to include further details of the magma transport within each volcano and also explore how some known prehistoric events and some hypothetical events at one volcano might impact the other. This work should help improve our understanding of volcanic activity of each volcano."
Gonnermann said there has been disagreement among Earth scientists about the potential links between adjacent volcanoes, and he is hopeful the new model could be useful in studying other volcanoes like those in Iceland or the Galapagos Islands.
"At this point it is unclear whether Hawaii is unique or whether similar volcano coupling may exist at other locations," Gonnermann said. "Given time and ongoing advances in volcano monitoring, we can test if similar coupling between adjacent volcanoes exists elsewhere."
Study co-authors include Michael Poland and Asta Miklius, both of HVO; Benjamin Brooks of the University of Hawaii; and Cecily Wolfe of the University of Hawaii and the Carnegie Institution of Washington.
The research was supported by the USGS and the NSF. The Kilauea and Mauna Loa GPS networks are supported by grants from the USGS, NSF and NASA and operated in collaboration by the USGS, Stanford University and the Pacific GPS Facility at the University of Hawaii.
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Story Source:
The above story is reprinted from materials provided byRice University. The original article was written by Jade Boyd.
Note: Materials may be edited for content and length. For further information, please contact the source cited above.

Journal Reference:
  1. Helge M. Gonnermann, James H. Foster, Michael Poland, Cecily J. Wolfe, Benjamin A. Brooks, Asta Miklius.Coupling at Mauna Loa and KÄ«lauea by stress transfer in an asthenospheric melt layerNature Geoscience, 2012; DOI: 10.1038/ngeo1612
 APA

 MLA
Rice University (2012, October 23). Connection between Hawaii's dueling volcanoes explained.ScienceDaily. Retrieved October 23, 2012, from http://www.sciencedaily.com­/releases/2012/10/121023134810.htm
Note: If no author is given, the source is cited instead.
Disclaimer: Views expressed in this article do not necessarily reflect those of ScienceDaily or its staff.