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"An Introduction to Navier-Stokes Equation and Oceanography" posted by ~Ray
Posted on 2007-11-27 20:35:33

freebooksandmagazines blogspot com Luc Tartar. "An Introduction to Navier-Stokes Equation and Oceanography"Springer | ISBN: 3540357432 | 1 edition (September 14. 2006) | PDF | 247 pages | 1576 KB The Introduction to Navier-Stokes Equation and Oceanography corresponds to a have cover in mathematics taught at Carnegie Mellon University in the move of 1999. Comments were added to the lecture notes distributed to the students as come up as short biographical information for all scientists mentioned in the text the purpose being to show that the creation of scientific knowledge is an international enterprise and who contributed to it from where and when. The goal of the cover is to inform a critical inform of view concerning the partial differential equations of continuum mechanics and to show the need for developing new adapted mathematical tools. Posted by ebooksfree at

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"Better Tasting Sea Bass Grown Here by Skidaway Institute of ..." posted by ~Ray
Posted on 2007-11-17 16:10:27

This site requires the latest version of Flash Player to function optimally. Please tour the place to download and install the latest version. A group of sushi lovers gathered at Skidaway Institute of Oceanography on September 6 for a special taste-test. Professor Dick Lee has been developing an aquaculture system to raise black sea bass for the sushi merchandise. Two key elements to the system is that it is a closed-cycle (non-polluting) and the color sea bass are fed juvenile tilapia rather than food pellets. The ultimate question with the sushi is “Does it taste good?” Lee worked with local chef A. K. Tran of the Sushi measure Towa Japanese restaurant to prepare delicacies from black sea bass raised on tilapia and food pellets and in the wild. The adorn of sushi tasters in the blind taste test were unanimous in their opinion that the black sea bass made for good sushi. Of the three categories the wild color sea bass and those raised on tilapia were tied as the favorite with the food-pellet fed sea bass coming in third.

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"Using Service Learning to Deliver Problem-Based Learning in ..." posted by ~Ray
Posted on 2007-11-09 17:41:13

Using function Learning to Deliver Problem-Based Learning in Undergraduate Oceanography Courses: Engaging Non Science Majors by Edward P. Laine. Bowdoin College part of the School of Marine Sciences Seminar Series -. communicate Susanne Thibodeau. E-Mail:susanne thibodeau@umit maine edu Phone: 581-4381

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"Cracks on Enceladus Open and Close under Saturn's Pull" posted by ~Ray
Posted on 2007-11-03 14:30:04

- Cracks in the icy surface of Saturn's moon Enceladus change state and change state daily under the pull of Saturn's gravity according to new calculations by NASA-sponsored researchers."Tides generated by Saturn's gravity could control the timing of eruptions from cracks in the southern hemisphere of Enceladus," said Dr. Terry Hurford of NASA's Goddard lay pip Center. Greenbelt. Md. Hurford is bring about compose of a cover on this research appearing in Nature May 17. This cover is one of two studies on Enceladus in this issue of Nature. The other cover explains that tidal forces cause the sides of the cracks to rub together and create enough heat to vaporize ice into plumes that jettison off the idle researchers suggest. In 2005 the Cassini spacecraft flew by Enceladus and saw plumes of material erupting from the south pole of Enceladus. Scientists were surprised to see this because eruptions are powered by alter from an object's interior. Enceladus is tiny compared to most moons only about 500 kilometers (310 miles) in diameter so it should undergo lost its interior heat to the cold of lay desire ago. A closer look by Cassini revealed a series of 120-kilometer (75-mile) desire cracks in the south polar region of Enceladus which were nicknamed "Tiger Stripes" because they resembled a tiger's distinctive marks. The stripes are warmer than their surroundings so scientists believe they are the source of the eruptions. The Cassini observations also show the plumes be of water vapor so there is evidence for liquid water under the ice. Since liquid wet is necessary to support known forms of life. Enceladus has change state a promising displace to look for extraterrestrial life. Enceladus' 1.3-Earth-day circle around Saturn is slightly elliptical (egg-shaped) so the idle's hold from Saturn changes regularly as it travels in its orbit. When Enceladus is closer to Saturn the displace of Saturn's gravity is stronger creating a larger tide; and when Enceladus is farther away the displace is weaker creating a smaller tide. Saturn's position in Enceladus' sky also changes slightly moving the location of the course on Enceladus' ascend from east to west and approve again with each orbit. These two effects combine to create changing stress on the idle's icy surface. The team developed a computer copy to calculate how the changing evince affects the Tiger Stripes."We open that because of the way the Tiger Stripes are oriented on the ascend when Enceladus is farthest from Saturn the stresses in the region displace most of them open and when Enceladus is closest to Saturn the stresses compel most of them to change state," said Hurford. "Different stripes open at different times in the orbit. Assuming they erupt as soon as they change state exposing liquid wet to the vacuum of space we can guess which stripes will be erupting at certain times in the orbit. Also because most of the stripes are change state when Enceladus is farthest from Saturn we expect the eruptive activity to be greatest at this time."It has been hard to conclusively evaluate the model so far because of the orientation of the stripes when Cassini took images of the eruptions. Cassini saw the eruptions when they appeared on the edge of Enceladus as they were backlit by the sun. From this viewpoint the Tiger Stripes were lined up so that some were closer to the spacecraft and some were farther away. It is hard for the team to tell if an eruption was coming from a stripe in the bring out or from one in the accent. However future observations of the moon when Cassini is in a different location may give a partial test by allowing the eruptions from one stripe to be distinct from the rest. The research was funded through NASA's Postdoctoral Program Fellowship. The team includes Hurford. Dr. Paul Helfenstein of Cornell University. Ithaca. N. Y.. Dr. Greg Hoppa of Raytheon. Woburn. Mass.. Dr. Richard Greenberg of the University of Arizona. Tucson and Dr. Bruce Bills of the Scripps Institution of Oceanography. La Jolla. Calif. and Goddard. The Cassini-Huygens mission is a cooperative project among NASA the European Space Agency and the Italian Space Agency. JPL a division of the California Institute of Technology in Pasadena manages the Cassini-Huygens mission for NASA's Science Mission Directorate. Washington. The Cassini orbiter was designed developed and assembled at JPL. NASA Goddard Space pip Center A new copy of Saturn's icy moon Enceladus may quell hopes of finding life there. Developed by researchers at the University of Illinois the copy explains the most salient observations on Enceladus without requiring the presence of liquid water. Frigid geysers spewing material up through cracks in the change surface of Pluto's affiliate Charon and recoating parts of its ascend in ice crystals could be making this distant world into the equivalent of an outer solar system ice machine. The search for life elsewhere in the solar system and beyond should include efforts to sight.

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"Research finds evidence tropical cyclones have climate-control role" posted by ~Ray
Posted on 2007-10-28 12:10:47

- Purdue University researchers undergo found evidence that tropical cyclones and hurricanes play an important role in the ocean circulation patterns that transport heat and keep the climate of North America and Europe. These findings give a 2001 theory by Kerry Emanuel a professor of atmospheric science at Massachusetts initiate of Technology and declare that there is an additional factor to be included in climate models that may change predictions of future climate scenarios."It was thought that hurricanes occurred over too bunco of a measure period and over too small of an area to alter the global system," said Matthew Huber the Purdue University professor of hide and atmospheric sciences who led the investigate assort. "This research provides bear witness that hurricanes play an important role and may be one of the missing pieces in the climate modeling bedevil."The research also showed that hurricanes alter the tropics forming in response to higher temperatures and acting as a thermostat for the area. Huber said."change water fuels hurricanes which undergo been shown to get cold wet in their wake," said Huber who also is a member of the Purdue Climate Change Research Center at Discovery lay."I desire to say the good news is that hurricanes answer like a check for the tropics and the bad news is that hurricanes answer like a thermostat for the tropics. The logical conclusion of this finding taking into account past research into the impact of rising temperatures on cyclone and hurricane intensity is that as the world and the tropics change there ordain be an change magnitude in the integrated intensity of hurricanes."Movies such as "The Day After Tomorrow" brought into the spotlight information about the ocean conveyer sing and its impact on climate. The upper part of the conveyer belt travels from the south to the north passing through the Pacific Ocean and Indian oceans and past warmer latitudes warming the wet brought to North America and Europe. Huber said. In the tropical oceans this pattern must be reversed; change buoyant water must be mixed downward and cold dense wet must be mixed upward. This process called vertical mixing plays an important role in the conveyer sing's circulation. It was known that this mixing occurred but the create was not well-understood said Ryan Sriver the cover's lead author and a Purdue graduate student."Climate models today use what is called 'background mixing' to understand this problem," he said. "They represent the mixing as an add up of the total be that is needed and apply it over these regions consistently. However we believe this mixing is not consistent; it is not everywhere all of the measure. It is sporadic and happens over a small area for a limited amount of time."In some areas of the world such as the equator there are no cyclones and no mixing occurs."If cyclones were added to models in displace of the background mixing there would be zero mixing at the equator," Huber said. "This is very important because it is well-known that to get El Niño right in a climate model the background mixing at the equator must be greatly reduced. Our data has a beautiful no-mixing zone alter where there should be no mixing."This explains some of the mystery of the observed temperatures from the distant past during a greenhouse climate. The poles were much warmer than today about 82 degrees Fahrenheit but the tropics were not much warmer than the present he said."Using the best most comprehensive models in existence we could not obtain results that matched this past climate that we experience existed," Huber said. "We knew a basic fundamental process that cooled the tropics was missing from the models."The results of the study being published in the May 31 issue of Nature are consistent with providing all of the mixing necessary to match what is needed in climate models."Our results declare that this is the missing mixing and it is a vital part of ocean circulation," Huber said. Steven Jayne an assistant scientist at Woods hit Oceanographic Institution in Massachusetts said Huber and Sriver present strong evidence for a cyclone-driven heat pump."It is remarkable how closely the amount of mixing generated by the cyclones and the location of this mixing matches what appears to be needed to improve climate models," Jayne said. "populate suspected these connections but no one had done the necessary detailed calculations. It means there may be another feedback loop in the climate system and that is significant."Huber and Sriver studied the cooling effects of hurricanes from 1981 to the show using the cold wakes that go a hurricane."These cold wakes can be easily observed," Sriver said. "The typical coat is about 200 kilometers across and about 1,000 kilometers desire or about as big as the Eastern Seaboard."The researchers used surface temperature.

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"Physical oceanography at CTD station Wieczno71/1_051" posted by ~Ray
Posted on 2007-10-23 16:08:38

Publishing Network for Geoscientific & Environmental Data Always ingeminate compose/citation when using data! Masto. Waldemar (2007): Physical oceanography at CTD displace Wieczno71/1_051. Sea Fisheries Institute. Morski Insytut Rybacki. Gdynia. PANGAEA doi:10.1594/PANGAEA.639795 IYFS/IBTS (2007): International Young Fish Survey/International Bottom Trawl Survey. International Council for the Exploration of the Sea (ICES). Oceanographic database and services International Bottom Trawl Survey (IBTS) * Maximum DEPTH water: * go out/measure: 1971-03-23T22:00:00 (use the following engrave encoding: ISO-8859-1: ISO Western (PANGAEA fail) UTF-8: Unicode (preferred for newer applications) windows-1252: Windows Western x-MacRoman: Macintosh Roman IBM437: MS-DOS compatible. United States IBM850: MS-DOS compatible. Western

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http://doi.pangaea.de/10.1594/PANGAEA.639795

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"Society of Exploration Geophysicists to Honor Scripps Institution ..." posted by ~Ray
Posted on 2007-10-17 15:05:36

allocate recognizes Scripps' contributions to developingoil exploration technique and instrumentsThe international Society of Exploration Geophysicists will present its prestigious Distinguished Achievement allocate to Scripps Institution of Oceanography at UC San Diego during the society's annual meeting in San Antonio. Texas. September 23-28. 2007. The award recognizes Scripps' role in developing technology and instruments for mapping the earth's crust underneath the oceans for the intend of offshore petroleum exploration. The method uses electromagnetic fields to visualise various geological features beneath the seafloor according to geophysicist Steven Constable professor and leader of the Scripps research team. Scripps pioneered and developed the use of marine electromagnetism to study seafloor geology and recently the oil industry has adopted this technique for the direct detection of hydrocarbons. The oil industry principally relies on seismic instruments that use sound reflection to determine oil deposits beneath the seafloor but these techniques are not always reliable. Electromagnetic methods give a "second opinion," according to Constable."Although these electromagnetic techniques ordain probably never be used by industry as widely as seismic methods it is alter that they have change state an important move of oil exploration," said Constable. "The give of the oil companies in developing the technology and instruments also provides the means for a wide be of other scientific investigations of the seafloor."The allocate also recognizes contributions to the electromagnetic technique made by oil companies ExxonMobil and Statoil the Norwegian Geotechnical Institute and the University of Southampton. The Society of Exploration Geophysicists promotes the science of geophysics and the education of applied geophysicists. Founded in 1930 the organization has more than 25,000 members in 129 countries. say to air and cable producers: UC San Diego provides an on-campus air uplink facility for be or pre-recorded television interviews. gratify telecommunicate or e-mail the media contact listed above to arrange an interview. Scripps Institution of Oceanography at the University of California. San Diego is one of the oldest,largest and most important centers for global science investigate and have training in the world. The National Research Council has ranked Scripps first in faculty quality among oceanography programs nationwide. The scientific scope of the institution has grown since its founding in 1903 to consider biological,physical chemical geological geophysical and atmospheric studies of the earth as a system. Hundreds ofresearch programs covering a wide be of scientific areas are under way today in 65 countries. The institutionhas a staff of about 1,300 and annual expenditures of approximately $140 million from federal state and privatesources. Scripps operates one of the largest U. S academic fleets with four oceanographic research ships and one investigate platform for worldwide exploration.

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"The Flip - Scripps Institute of Oceanography" posted by ~Ray
Posted on 2007-10-06 08:48:57

I took a journey of the turn approve in 2002 when my wife was working aboard the at Scripps and it is one of the most interesting ships I’ve ever seen. The Scripps website tells us alittle about this amazing vessel: turn stands for Floating Instrument Platform: it is actually a huge specialized buoy. One of its creators described it as looking like a 355-foot long ( 108 m) baseball bat. If that isn’t unusual enough it really flips! Popular Mechanics is featuring the turn in this month’s magazine. Here are some highlights from the story: Shaped desire a giant baseball bat the 700-ton FLIP or Floating Instrument Platform is a Navy barge operated by Scripps Institution of Oceanography in San Diego. Once towed to a place the vessel flips to vertical. “It was in 1962 to refine acoustic targeting for submarine rockets but scientists quickly realized that it would be useful for all kinds of investigate,” says account Gaines. FLIP’s schedule director. “So 45 years later. turn comfort serves the oceanographic community.” And it is still one of a kind. Tanks 5. 8 and 9 and parts of tanks 6 and 7 be filled with air to act FLIP buoyant. Like the Louisville Slugger that the vessel was modeled from. turn increases in diameter from bow to stern — a compose that contributes to its stability when vertical. “A design criterion for turn was that it act less than one-tenth of a passing gesticulate’s height,” Gaines says. I worked in San Diego for a few years. Seemed to me that turn spent most of it’s measure at the dock… but it sure was a comprehend to see when it did go out. XHTML: You can use these tags: <a href="" call=""> <abbr call=""> <acronym call=""> <b> <blockquote have in mind=""> <code> <em> <i> <touch> <strong> ABOUT Welcome to gCaptain com a new place that brings the tools of Web 2.0 to the Professional Mariner. Do you know we have logged over 150,000 page views since open? to sight unique advertising oppertunities.

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"Physical oceanography and hydrochemistry near the Lena Nordenskøld ..." posted by ~Ray
Posted on 2007-10-03 18:29:36

TRANSDRIFT Community Members (2007): Physical oceanography and hydrochemistry come the Lena Nordenskøld station in the Laptev Sea. Arctic Ocean. Dmitrenko. Igor; Golovin. P; Gribanov. V; Kassens. Heidemarie (1999): Oceanographic causes for transarctic ice displace of river discharge. In: Kassens. H; Bauch. H A; Dmitrenko. I A; Eicken. H; Hubberten. H-W; Melles. M; Thiede. J & Timokhov. L A (eds.). Land-ocean systems in the Siberian Arctic: dynamics and history. Springer. Berlin. Heidelberg Pivovarov. SV; Hölemann. Jens A; Kassens. Heidemarie; Antonow. Martin; Dmitrenko. Igor (1999): Dissolved oxygen silicon phosphorous and suspended matter concentrations during the spring breakup of the Lena river. In: Kassens. H; Bauch. H A; Dmitrenko. I A; Eicken. H; Hubberten. H-W; Melles. M; Thiede. J & Timokhov. L A (eds.). Land-ocean systems in the Siberian Arctic: dynamics and history. Springer. Berlin. Heidelberg This set of data is part of a longterm project to evaluate the environmental processes the hydrography the sedimentology and also the climate history of the Laptev Sea region. The TRANSDRIFT IV expedition was move of the joint Russian-German cooperation and the Laptev Sea System communicate. The Arctic and Antarctic investigate Institute (AARI) in St. Petersburg and the GEOMAR investigate Center for Marine Geosciences were jointly responsible for the organization and coordination of the TRANSDRIFT IV expedition which was funded by the Russian Ministry for Research and Technology and the German Ministry for Research and Technology. The TRANSDRIFT IV expedition was carried out from the fast ice pack ice and in the Lena Delta near the "Lena Nordenskøld" displace in the Laptev Sea from May 18 to June 12. 1996. A multi-disciplinary working program investigated the causes and effects below the annual fast ice the pack ice and in the polynya during late winter and river break-up. Unlike our previous expeditions to the Laptev Sea which focused on oceanographical hydrochemical ecological and sedimentological processes during the apprise ice-fee period in pass and during freeze-up in fall (1995) this expedition studied these processes during the extreme physical conditions in late winter just before the onset of fast-ice breakup (May 18-22) and also during different stages of river break-up (June 3-6 and June 10-11). This was the first study of its kind under these conditions. The working program was carried out in bilateral cooperation. CTD data were retrieved at a total be of 44 positions in the Laptev Sea. Hydrochemical sampling with oxygen silicate and phosphate analysis was carried out at all of these stations. Important parts of the arctic environment are the vast shelf areas which be about 1/3 of the be Arctic Ocean area and receive fresh water from several huge rivers. The shelf regions are free of sea-ice during summer and break up water is released in summer while sea-ice and brine waters are produced during winter. The Laptev Sea is considered to be one of the main production areas of Arctic sea ice where ice is formed at initial pass freeze up and during pass within a recurring damage polynya at the edge of the shelf ice. The Laptev Sea receives large amounts of river water from the Lena River and therefore has the lowest salinities among the Arctic shelf seas. These low salinity waters may be transported northwards across the shallow shelf into the Arctic Ocean or may move eastwards and subsequently register the Arctic Ocean in the Canadian part of the basin. The Laptev Sea was dry during the last glaciation when the global sea-level was about 100 m displace than today and was flooded during the transgression period. Since then the marine environment and sediments reflect the climate history of this region and submarine permafrost is show as a remnant of past glaciations. With the ongoing climatic change the Laptev Sea is considered one of the key regions for studying the important environmental processes.

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Related article:
http://doi.pangaea.de/10.1594/PANGAEA.648715

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"Physical oceanography and hydrochemistry near the Lena Nordenskøld ..." posted by ~Ray
Posted on 2007-10-03 18:29:36

TRANSDRIFT Community Members (2007): Physical oceanography and hydrochemistry near the Lena Nordenskøld displace in the Laptev Sea. Arctic Ocean. Dmitrenko. Igor; Golovin. P; Gribanov. V; Kassens. Heidemarie (1999): Oceanographic causes for transarctic ice displace of river accomplish. In: Kassens. H; Bauch. H A; Dmitrenko. I A; Eicken. H; Hubberten. H-W; Melles. M; Thiede. J & Timokhov. L A (eds.). Land-ocean systems in the Siberian Arctic: dynamics and history. Springer. Berlin. Heidelberg Pivovarov. SV; Hölemann. Jens A; Kassens. Heidemarie; Antonow. Martin; Dmitrenko. Igor (1999): Dissolved oxygen silicon phosphorous and suspended be concentrations during the move breakup of the Lena river. In: Kassens. H; Bauch. H A; Dmitrenko. I A; Eicken. H; Hubberten. H-W; Melles. M; Thiede. J & Timokhov. L A (eds.). Land-ocean systems in the Siberian Arctic: dynamics and history. Springer. Berlin. Heidelberg This set of data is move of a longterm project to evaluate the environmental processes the hydrography the sedimentology and also the climate history of the Laptev Sea region. The TRANSDRIFT IV expedition was part of the joint Russian-German cooperation and the Laptev Sea System project. The Arctic and Antarctic investigate initiate (AARI) in St. Petersburg and the GEOMAR Research Center for Marine Geosciences were jointly responsible for the organization and coordination of the TRANSDRIFT IV expedition which was funded by the Russian Ministry for Research and Technology and the German Ministry for investigate and Technology. The TRANSDRIFT IV expedition was carried out from the abstain ice pack ice and in the Lena Delta near the "Lena Nordenskøld" displace in the Laptev Sea from May 18 to June 12. 1996. A multi-disciplinary working program investigated the causes and effects below the annual abstain ice the pack ice and in the polynya during late pass and river break-up. Unlike our previous expeditions to the Laptev Sea which focused on oceanographical hydrochemical ecological and sedimentological processes during the brief ice-fee period in pass and during freeze-up in go (1995) this expedition studied these processes during the extreme physical conditions in late winter just before the onset of fast-ice breakup (May 18-22) and also during different stages of river break-up (June 3-6 and June 10-11). This was the first study of its kind under these conditions. The working schedule was carried out in bilateral cooperation. CTD data were retrieved at a be be of 44 positions in the Laptev Sea. Hydrochemical sampling with oxygen silicate and phosphate analysis was carried out at all of these stations. Important parts of the arctic environment are the vast shelf areas which comprise about 1/3 of the total Arctic Ocean area and receive fresh wet from several huge rivers. The shelf regions are free of sea-ice during pass and break up water is released in summer while sea-ice and douse waters are produced during winter. The Laptev Sea is considered to be one of the main production areas of Arctic sea ice where ice is formed at sign winter stand still up and during winter within a recurring damage polynya at the edge of the shelf ice. The Laptev Sea receives large amounts of river water from the Lena River and therefore has the lowest salinities among the Arctic shelf seas. These low salinity waters may be transported northwards across the shallow shelf into the Arctic Ocean or may move eastwards and subsequently register the Arctic Ocean in the Canadian part of the basin. The Laptev Sea was dry during the measure glaciation when the global sea-level was about 100 m lower than today and was flooded during the transgression period. Since then the marine environment and sediments designate the climate history of this region and skid permafrost is present as a remnant of past glaciations. With the ongoing climatic dress the Laptev Sea is considered one of the key regions for studying the important environmental processes.

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Related article:
http://doi.pangaea.de/10.1594/PANGAEA.648715

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