The Atlantic hurricane season begins June 1, and forecasts suggest an above average year. And as we all know, Atlantic hurricanes are deadliest when they get into the warm Gulf of Mexico. It is almost like a hurricane jumping on a trampoline. They can go from Category 1 to Category 5 in 24 hours in such a favorable environment. But this year, as we also know, there is something different about the Gulf. It is full of oil. What are the implications of this fact for hurricanes? And conversely, what might a powerful hurricane do to the oil spill if it were to run across it? This is a topic I've been thinking about, and I don't have definitive answers yet. I'd like to do more research and interview some experts--but for now, let's take a rough and dirty approach to the issue, based on what is already out there. And let's tackle the first question first: What would an oil slick do to a hurricane? According to storm ace Jeff Masters, the answer is not very much. Here's what Masters is thinking. It's certainly true that oil on the surface of the ocean could inhibit a hurricane's access to its fuel source--the warm seawater ...
Monthly Archives: May 2010
Youtube Videos
Earlier we used to copy URLs and download videos from youtube. Recently youtube has removed the URLs from it pages. Any other option to download our favourite programs? anyother similar website from where we can download good educational videos?
Regards,
PG
Need copy of IS 2309
does anybody have soft copy of IS 2309?
Regards,
consult electric
Control Room Air Conditioning
What are the major specification of control room air condition?
Is that true that the ordinary split unites does not provide the necessary positive pressure in the control so we must use central air condition ?
Using orifice plate for minimum flow protection
Why / what would be the reason for you to use an orifice plate for minimum flow protection for a pump? Since the discharge side always has a higher pressure, the discharge fluid will keep on flowing through the orifice plate until the delta P is zero (meaning a big increase in suction head), basical
LVDT Design
I am doing a project regarding the design of an LVDT, I need help in this regard.
Calculate heat loss in stainless steel piping
People,
I have a request please. Does anyone have any experience in calulating heat loss in stainless steel water pipes? I have looked at Newtons law of cooling and Fouriers law but I don't think they apply to my situation. I know that forced convection heat loss applies due to the pump.
P
EN8 and SLD Mechanical Properties?
I need a mechanical properties of en8 and sld materials
Back flow in a compressor / pump
If the purpose of a compressor or a pump is to increase the pressure at the discharge, then since the pressure at discharge > suction, why doesn't the flow at discharge flow backward towards the suction?
Chickens are like people | Gene Expression
In that their demographic history is complicated. The Origin and Genetic Variation of Domestic Chickens with Special Reference to Junglefowls Gallus g. gallus and G. varius:
… domestic chickens diverged from red junglefowl 58,000±16,000 years ago, well before the archeological dating of domestication, and that their common ancestor in turn diverged from green junglefowl 3.6 million years ago. Several shared haplotypes nonetheless found between green junglefowl and chickens are attributed to recent unidirectional introgression of chickens into green junglefowl. Shared haplotypes are more frequently found between red junglefowl and chickens, which are attributed to both introgression and ancestral polymorphisms. Within each chicken breed, there is an excess of homozygosity, but there is no significant reduction in the nucleotide diversity. Phenotypic modifications of chicken breeds as a result of artificial selection appear to stem from ancestral polymorphisms at a limited number of genetic loci.
I wonder if domesticates in particular exhibit these more complex reticulated patterns in their phylogenies because they spread along human trade routes.
Problem with throttle response after few miles of driving- carburettor model car
One of my friends has a 90s model Maruti 800... After driving the car for sometime... roughly for about 25 Km, the vehicle shows a hesitation to pull... the throttle response gets poor... What are the possible reasons for this???... Pls help!
What causes soot to flow inside lance tube?
i have got a problem with long retractable type soot blowers. the soot blower lance tubes contain alot of soot though the design pressure of sealing air that is 600 mm of h2o is maintained the furnace pressure is 300 mm of h20. the scavenging air is also provided from the same header. inside the sea
Root Three in Three Phase Calculation
Hiiiii.. i am just keeping my first step in electrical engineering and i would like to know how root three comes in various three phase calculation. A small help will boost my understanding.......Thanks
How to post products on your site?
hello,I am a new member, i just want to how to post new products!is it free or charge?
thanks!
Short time current withstand calculation for busbars
is K2S2 = I2t (K square S square = I square t) a correct formula for calculating the busbar cross section using short time current value?for example i have 40kA overcurrent for duration of 3 sec for a copper busbar and i want to have the cross section.
if it is a correct formula,what is K??
New Study Finds Ocean Warmed Significantly Since 1993

The upper layer of Earth's ocean has warmed since 1993, indicating a strong climate change signal, according to a new international study co-authored by oceanographer Josh Willis of NASA's Jet Propulsion Laboratory, Pasadena, Calif. The energy stored is enough to power nearly 500 100-watt light bulbs for each of the roughly 6.7 billion people on the planet.
"We are seeing the global ocean store more heat than it gives off," said John Lyman, an oceanographer at the National Oceanic and Atmospheric Administration's Joint Institute for Marine and Atmospheric Research, who led the study that analyzed nine different estimates of heat content in the upper ocean from 1993 to 2008.
The team combined the estimates to assess the size and certainty of growing heat storage in the ocean. Their findings will be published in the May 20 edition of the journal Nature. The scientists are from NASA, NOAA, the Met Office Hadley Centre in the United Kingdom, the University of Hamburg in Germany and the Meteorological Research Institute in Japan.
"The ocean is the biggest reservoir for heat in the climate system," said Willis. "So as the planet warms, we're finding that 80 to 90 percent of the increased heat ends up in the ocean."
A warming ocean is a direct cause of global sea level rise, since seawater expands and takes up more space as it heats up. The scientists say that this expansion accounts for about one-third to one-half of global sea level rise.
Combining multiple estimates of heat in the upper ocean – from the surface to about 610 meters (2,000 feet) down – the team found a strong multi-year warming trend throughout the world's ocean. According to measurements by an array of autonomous free-floating ocean floats called Argo, as well as by earlier devices called expendable bathythermographs, or XBTs, that were dropped from ships to obtain temperature data, ocean heat content has increased over the last 16 years.
The team notes that there are still some uncertainties and some biases.
"The XBT data give us vital information about past changes in the ocean, but they are not as accurate as the more recent Argo data," said Gregory Johnson, an oceanographer at NOAA's Pacific Marine Environmental Laboratory. "However, our analysis of these data gives us confidence that on average, the ocean has warmed over the past decade and a half, signaling a climate imbalance."
Data from the array of Argo floats -- deployed by NOAA and other U.S. and international partners -- greatly reduce the uncertainties in estimates of ocean heat content over the past several years, the team said. There are now more than 3,200 Argo floats distributed throughout the world's ocean sending back information via satellite on temperature, salinity, currents and other ocean properties.
For more information, see http://www.noaanews.noaa.gov/stories2010/20100519_ocean.html
View my blog's last three great articles...
- Cassini Heading to Titan after Tagging Enceladus
- NASAs Mars Rovers Set Surface Longevity Record
- NASA video explains how to poop in space
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Cassini Heading to Titan after Tagging Enceladus

This raw, unprocessed image of Titan behind Saturn's rings was taken on May 18, 2010, by the Cassini spacecraft. The dark curve of Enceladus is visible at the bottom of the image.
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In other images, Enceladus put its craggy face forward, exhibiting some of the fractures and cratering that have made the Saturnian moon a favorite of both planetary scientists and outer-planet mission groupies. A view of Enceladus' terminator was taken by NASA's Cassini spacecraft on May 18 from approximately 75,000 kilometers (46,500 miles) away.
Cassini sent back numerous images May 18, 2010, as it finished the first leg of its planned double flyby. Cassini passed within about 435 kilometers (270 miles) of the Enceladus surface.
Cassini is heading toward Titan for a flyby that occurs in the late evening May 19 Pacific time, which is in the early hours of May 20 UTC. Because of a fortuitous cosmic alignment, Cassini can catch glimpses of these two contrasting worlds within less than 48 hours, with no maneuver in between.
The main scientific goal at Enceladus was to watch the sun play peek-a-boo behind the water-rich plume emanating from the moon's south polar region. Scientists using the ultraviolet imaging spectrograph will be able to use the flickering light to measure whether there is molecular nitrogen in the plume. Ammonia has already been detected in the plume, and scientists know heat can decompose ammonia into nitrogen molecules. Determining the amount of molecular nitrogen in the plume will give scientists clues about thermal processing in the moon's interior.
The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Cassini-Huygens mission for NASA's Science Mission Directorate in Washington. The Cassini orbiter was designed, developed and assembled at JPL. <!--JPLIMAGEMARKER __JPL_CAPTION_2
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More raw images from the Enceladus flyby, dubbed "E10," are available at: http://saturn.jpl.nasa.gov/photos/raw/
More information on the Titan flyby, dubbed "T68," is online at: http://saturn.jpl.nasa.gov/mission/flybys/titan20100520/
View my blog's last three great articles...
- NASAs Mars Rovers Set Surface Longevity Record
- NASA video explains how to poop in space
- Tropical Cyclone 1B (Northern Indian Ocean)
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Scratch Resistant Polycarbonate
Hello Friends and Associates ...
Somewhat of a perplexing situation that I write in hopes of finding a simple solution.
In our products we use a lot of plastic components, most often ABS and Polycarbonates, the latter primarily for "faceplates" and "display panels" ... usually small-ish (m
NASAs Mars Rovers Set Surface Longevity Record

NASA's Mars Exploration Rover Opportunity used its navigation camera for this northward view of tracks the rover left on a drive from one energy-favorable position on the northern end of a sand ripple to another.
› Larger image› Interactive: Mars Exploration Rovers
NASA's Mars Exploration Rover Project will pass a historic Martian longevity record on Thursday, May 20. The Opportunity rover will surpass the duration record set by NASA's Viking 1 Lander of six years and 116 days operating on the surface of Mars. The effects of favorable weather on the red planet could also help the rovers generate more power.
Opportunity's twin rover, Spirit, began working on Mars three weeks before Opportunity. However, Spirit has been out of communication since March 22. If it awakens from hibernation and resumes communication, that rover will attain the Martian surface longevity record.
Spirit's hibernation was anticipated, based on energy forecasts, as the amount of sunshine hitting the robot's solar panels declined during autumn on Mars' southern hemisphere. Unfortunately, mobility problems prevented rover operators from positioning Spirit with a favorable tilt toward the north, as during the first three winters it experienced. The rovers' fourth winter solstice, the day of the Martian year with the least sunshine at their locations, was Wednesday, May 12 (May 13 Universal time).
"Opportunity, and likely Spirit, surpassing the Viking Lander 1 longevity record is truly remarkable, considering these rovers were designed for only a 90-day mission on the surface of Mars," Callas said. "Passing the solstice means we're over the hump for the cold, dark, winter season."
Unless dust interferes, which is unlikely in the coming months, the solar panels on both rovers should gradually generate more electricity. Operators hope that Spirit will recharge its batteries enough to awaken from hibernation, start communicating and resume science tasks.
Unlike recent operations, Opportunity will not have to rest to regain energy between driving days. The gradual increase in available sunshine will eventually improve the rate of Opportunity's progress across a vast plain toward its long-term destination, the Endeavour Crater.
This month, some of Opportunity's drives have been planned to end at an energy-favorable tilt on the northern face of small Martian plain surface ripples. The positioning sacrifices some distance to regain energy sooner for the next drive. Opportunity's cameras can see a portion of the rim of Endeavour on the horizon, approximately eight miles away, across the plain's ripples of windblown sand.
"The ripples look like waves on the ocean, like we're out in the middle of the ocean with land on the horizon, our destination," said Steve Squyres of Cornell University in Ithaca, N.Y. Squyres is the principal investigator for Opportunity and Spirit. "Even though we know we might never get there, Endeavour is the goal that drives our exploration."
The team chose Endeavour as a destination in mid-2008, after Opportunity finished two years examining the smaller Victoria Crater. Since then, the goal became even more alluring when orbital observations found clay minerals exposed at Endeavour. Clay minerals have been found extensively on Mars from orbit, but have not been examined on the surface.
"Those minerals form under wet conditions more neutral than the wet, acidic environment that formed the sulfates we've found with Opportunity," said Squyres. "The clay minerals at Endeavour speak to a time when the chemistry was much friendlier to life than the environments that formed the minerals Opportunity has seen so far. We want to get there to learn their context. Was there flowing water? Were there steam vents? Hot springs? We want to find out."
Launched in 1975, Project Viking consisted of two orbiters, each carrying a stationary lander. Viking Lander 1 was the first successful mission to the surface of Mars, touching down on July 20, 1976. It operated until Nov. 13, 1982, more than two years longer than its twin lander or either of the Viking orbiters.
The record for longest working lifetime by a spacecraft at Mars belongs to a later orbiter: NASA's Mars Global Surveyor operated for more than 9 years after arriving in 1997. NASA's Mars Odyssey, in orbit since in 2001, has been working at Mars longer than any other current mission and is on track to take the Mars longevity record late this year.
Science discoveries by the Mars Exploration Rover have included Opportunity finding the first mineralogical evidence that Mars had liquid water, and Spirit finding evidence for hot springs or steam vents and a past environment of explosive volcanism.
JPL manages the Mars rovers for NASA's Science Mission Directorate in Washington. For more information about the rovers, visit http://www.nasa.gov/rovers . The California Institute of Technology in Pasadena manages JPL for NASA.
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h+ Magazine on Switching Memory Back On
From h+ Magazine: "A new study [sheds] some light on how 'memory disturbances' in an aging mouse brain are associated with altered 'hippocampal chromatin plasticity' - the combination of DNA, histones, and other proteins that make up the chromosomes associated with the hippocampus. Specifically, the study describes an acetyl genetic switch that produces memory impairment in aging 16-month-old mice. Because the acetyl wasn't present in young 3-month-old mice, the study concludes that it acts as a switch for a cluster of learning and memory genes. ... when young mice are learning, an acetyl group binds to a particular point on the histone protein. The cluster of learning and memory genes on the surrounding DNA ends up close to the acetyl group. This acetyl group was missing in the older mice that had been given the same tasks. By injecting an enzyme known to encourage acetyl groups to bind to any kind of histone molecule, [researchers] flipped the acetyl genetic switch to the 'on' position in the older mice and their learning and memory performance became similar to that of 3-month-old mice. ... [Researchers hope] that the study of hippocampal chromatin plasticity and gene regulation in mice will help them to identify therapeutic strategies to encourage neuroplasticity (the formation of new neural networks in the brain), to improve learning behavior, and to recover seemingly lost long-term memories in human patients."
View the Article Under Discussion: http://www.hplusmagazine.com/articles/neuro/switch-memory
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