Tuesday, March 19, 2013

Brazil DHN update in the Marine GeoGarage


6 charts have been updated since the last update :
(DHN update March 7, 2013 / February 28, 2013)

  • 1501      BAÍA DE GUANABARA
  • 1511      BARRA DO RIO DE JANEIRO
  • 1512      PORTO DO RIO DE JANEIRO
  • 1513      TERMINAIS DA BAÍA DE GUANABARA
  • 1515      BAÍA DE GUANABARA - ILHA DO MOCANGUÊ E PROXIMIDADES
  • 1701      PORTO DE SANTOS
Today 309 charts (355 including sub-charts) from DHN are displayed in the Marine GeoGarage
Don't forget to visit the NtM Notices to Mariners (Avisos aos Navegantes)

The Bermuda triangle of space: the high-energy South Atlantic anomaly threatens satellites


From DefenseNews

Much fanfare accompanied the Sept. 25, 2010, launch of the Air Force’s Space Based Space Surveillance satellite.
The $833 million craft was finally going up to do its job: monitor orbiting items from space itself, free of the time constraints and atmospheric interference that hamper its earthbound counterpart, the Space Fence.
Its 30-centimeter telescope, mounted on a two-axis gimbal, would help keep tabs on satellites as far away as geosynchronous orbit as well as thousands of bits of space junk closer in.
The builders said SBSS would be on the job within 60 days, and forecast a working life of at least 5½ years.

Shortly after launch, the satellite passed over the South Atlantic, and things went awry.
The satellite was hit by radiation that sent the sensors reeling and knocked out an electronics board payload.
Suddenly, the expensive, specially-designed satellite could no longer do what it was built for.


The effects of radiation are part of the price of doing business in space.
There are solar flares, random magnetic distortions and what some NASA scientists call euphemistically the “killer electrons” of the Van Allen radiation belts.
The place where spacecraft are most vulnerable, though, is an area slightly larger than the United States, centered 300 kilometers off the coast of Brazil, where the trapped charged particles of the doughnut-shaped Van Allen radiation belts and cosmic rays from sun storms combine and bottom out at about 200 kilometers above the planet.
Its formal name is the South Atlantic Anomaly, but some call it the Bermuda Triangle of space.


These two nearly identical spacecraft launched in August 2012 and with only six months in operation, they may well be rewriting science textbooks. The probes study the Van Allen belts, gigantic radiation belts surrounding Earth, which can swell dramatically in response to incoming energy from the sun, engulfing satellites and spacecraft and creating potential threats to manned space flight.
James Van Allen discovered the radiation belts during the 1958 launch of the first successful U.S. satellite. Subsequent missions have observed parts of the belts, but what causes the dynamic variation in the region has remained something of a mystery.

It’s directly in the path of satellites in low Earth orbit, which fly through it regularly — in some cases, multiple times a day.
“The South Atlantic Anomaly is the rocky road of radiation storms,” said Vic Scuderi, manager of satellite electronics at BAE Systems in Manassas, Va.

NASA scientists believe that there is a cloud of protons, followed by a cloud of electrons, followed by a cloud of protons, etc., where the inner Van Allen radiation belt dips down in the anomaly.
“A lot of theoretical people have tried to justify it,” said Old Dominion University professor Francis Badavi.
“The typical spacecraft engineer hasn’t been able to come up with a reason” for it.

All they know is that radiation in the South Atlantic Anomaly is intense, that spacecraft have to be designed to deal with it and that, even then, there is potential for peril.

Killer electrons

Scientists have a working theory that the Earth’s magnetic field is caused by its molten iron center.
Because that core rotates at a slightly different pace than the planet’s surface, the field generates magnetic North and South poles slightly away from the geographic poles that form the Earth’s rotational axis.


That’s the explanation for something even every hiker knows: that the magnetic north shown on a compass is not true north.
That offset also is believed to be the reason that the Earth’s magnetic field is weakest in the area off Brazil.
Less hindered, the inner Van Allen radiation belt dips closest to Earth there.

The anomaly was discovered in 1958 as part of a study of space radiation belts by University of Iowa physicist James Van Allen, whose suspicion was aroused by the Soviet Union’s Sputnik satellites. Soviet scientists believed the primitive data-recording device on board Sputnik I was faulty because it told of radiation levels well beyond anything they believed possible.

But Van Allen postulated that the device was fine and that the inexplicable radiation did indeed exist. Four months after Sputnik went up, the U.S. launched its first satellite, Explorer I, and Van Allen began to investigate the radiation belts that today bear his name.

In the 1960s and early ’70s, the Air Force and NASA flew a covey of 22 satellites to map the Van Allen radiation belts between altitudes of 200 and 36,000 kilometers.
The flights generated databases that are still in use today.

On Aug. 30, NASA launched its Radiation Belt Storm Probes (later renamed Van Allen Probes), twin satellites on a two-year mission to do more mapping and to update those databases.
Shielded by quarter-inch aluminum, the sensors are flying into the radiation belts for long periods, trying to solve a puzzle.
Sometimes, when solar storms hit the belts, they fill with energetic particles, the so-called “killer electrons.”
At other times, the belts lose particles.
And sometimes nothing at all happens.

“The problem is, there is no unified idea of what phenomena are most important inside the belts,” said mission scientist David Sibeck.
“If there are 100 people at a [scientific] meeting, there will be 100 answers for every question: ‘How are ‘killer electrons’ energized?’ “

Quick and not-so-quick fixes

The Space Based Space Surveillance satellite that was bashed so badly in 2010 was eventually brought back to life.
A software patch was developed and tested over the course of more than a year, and the SBSS was declared operationally capable 23 months after launch.
SBSS builders Boeing and Ball Aerospace referred questions to the Air Force, which did not respond by press time.
The satellites’ fate illustrates the problems the South Atlantic Anomaly can cause even to the most well-planned ISR missions.

Tom Logsdon, a former Rockwell Collins engineer, now retired, explained that the radiation can confound the very heart of the software on a satellite.
“One of the things that happens is, you can get logic upsets,” Logsdon said.
“You get a charged particle coming through the satellite, and it can flip some of the binary ones to binary zeros, and vice versa.
“Someone would have to upload the memory again or command it to reset, and it would start all over.”

Not every satellite damaged by the Anomaly takes so long to fix.
In October, the SpaceX Dragon, part of a $1 billion contract with NASA to supply the International Space Station, suffered a single-event upset en route to docking with the ISS.
A remote electronic unit became inoperable as the craft passed through the South Atlantic Anomaly.
A quick power cycle and re-synching remedied the issue.

Other programs work around the Anomaly.
To avoid exposing astronauts to intense radiation, spacewalks are not scheduled on the International Space Station when it’s passing through the Anomaly — which happens two to five times a day.

As a precaution, NASA engineers simply shut down the Hubble Telescope as it is going through the SAA, to protect its equipment.
Smaller commercial and military satellites carry radiation detection devices — themselves vulnerable to radiation — that trigger shutdowns and power-ups of sensors and computers.

Satellites carry radiation-hardened electronics of varying degrees to deal with the energy that accumulates.
“Commercial and defense-contracted satellites are typically on a 15-year mission timeframe, and they have to withstand hammering the whole time,” BAE’s Scuderi said.
“The electronics that we put on board the satellites can accumulate up to 500,000 rads” or radiation absorbed doses.

“A human being can only absorb about 400 rads in a lifetime,” he said, by way of comparison.
That accumulative effect is called a “total ionizing dose,” and it’s largely predictable, in part because orbital trips through the SAA are predictable.
As the ions pile up, the satellite can become impaired.
“Solar arrays become less efficient,” Logsdon said. “Silicon solar cells get damaged, so they generate less electricity.”

Space radiation affects satellites

No escape from radiation

On March 8, 2012, a flurry of eruptions on the sun began sending enough energy into the Earth’s upper atmosphere to power every home in New York City for two years.
Over three days, 26 billion kilowatt-hours pounded the thermosphere, which begins about 53 miles up.
Infrared radiation from the thermosphere’s carbon dioxide and nitrous oxide re-radiated about 95 percent of that energy back into space.
Some satellites orbiting Earth were hit going and coming by radiation that, NASA assessed, would cut their lives short.
And there are more storms ahead because, this year, the planet reaches the apex of an 11-year solar event cycle.

Around the world, a satellite is launched about every four days with varying radiation mitigation capability, generally dictated by its budget.
While the day-to-day radiation in the South Atlantic Anomaly and throughout the Van Allen radiation belts can be anticipated, the inability to predict solar storms makes the jobs of designers and operators more difficult.
With more notice, operators could do things like shut down equipment to lessen vulnerability.

But they understand the problem.
“We can’t produce an accurate forecast for rain here on Earth more than three days ahead,” Scuderi said.
“The number of variables in space is probably 10 to 100 times more than on Earth.”

Still, NASA and NOAA try, albeit with diminishing funding and satellites that are wearing out.
The Radiation Belt Storm Probes twin-satellite mission is another in a long line of research efforts.
“We’ve spent a lot of resources trying to predict solar activity, but we’re still not there,” Badavi said.

A former DoD intelligence official said the South Atlantic Anomaly is just part of the ISR challenge.
“We’re just lucky,” he said, “there’s not a lot of demand for satellite imagery over the South Atlantic.”

Monday, March 18, 2013

How Arctic ice may have influenced superstorm Sandy

A striking image of Verrazano Bridge in Brooklyn as Hurricane Sandy approaches on Oct. 29, 2012.
CREDIT: Carlos Ayala

From OurAmazingPlanet

The sea ice covering the Arctic Ocean may not seem to be connected to a hurricane like Superstorm Sandy, but a group of scientists is suggesting the record lack of ice last summer could have set up the atmospheric pattern that sent Sandy barreling into the Northeast.

The potential link is just one of many ways that human activities can, and in some cases already seem to be affecting Earth's weather and driving it toward extremes, be they droughts, megafloods or superstorms like Sandy.

"Extreme weather of all sorts has been increasing around the Northern Hemisphere.
When Sandy hit such a high-impact and vulnerable part of the East Coast, many reporters and local people have asked us whether climate change played a role," said Jennifer Francis of Rutgers University in New Jersey, one of the scientists who looked at the link. "It's the question on everyone's mind."

Sandy's start

Sandy began its life as a "classic late-season hurricane" over the Caribbean in mid-October, as the National Hurricane Center put it in its summary of the storm.
It tore across Haiti, Jamaica, Cuba and the Bahamas, killing at least 67 people and causing enormous damage.

While Sandy weakened over the Bahamas, it also ballooned in size, giving its wind field an enormous footprint; then, like many storms that form when and where it did, it curved northward, paralleling the U.S. East Coast, driven by the prevailing currents in the atmosphere.
As it skirted the coast, moving over the warm waters of the Gulf Stream, it also regained strength. [On the Ground: Hurricane Sandy in Images]

The storm weakened again as it moved farther north over colder waters, but never lost its extreme size. And as it continued on its path, a mass of high-pressure air sitting over Greenland kept it from simply curving out to sea.
Not only that, noted Francis and her colleagues in their article, but it also caused the storm to do "something never observed before in records going back to 1851 — it took a sharp turn to the west and toward the most populated area along the eastern seaboard."

That's where the Arctic sea ice comes in.


Sea ice and Sandy

The extent of sea ice covering the Arctic waxes and wanes with the seasons, reaching its high point near the end of the Northern Hemisphere winter, and its low point near the end of summer.
But as Earth's average temperature has risen with global warming, the Arctic has been warming at two to three times the rate of the rest of the globe, Francis explained.
This accelerated Arctic warming has fueled ice melt beyond normal summertime levels, which reinforces the warming because open ocean waters absorb the sun's rays, while ice reflects it.

As the Arctic warms, the temperature difference between the poles and lower latitudes is reduced, which influences flow patterns in the atmosphere, because "that temperature difference is what drives the jet stream," Francis said.

 Atmospheric conditions during Hurricane Sandy’s transit along the eastern seaboard of the United States, including the invasion of cold Arctic air into the middle latitudes of North America and the high-pressure blocking pattern in the northwest Atlantic.

The jet stream is what moves weather systems from west to east across the midlatitudes.
When the temperature difference decreases, the jet stream slows down, and the kinks, or waves, in it hang around longer, as do the weather systems associated with them.

In the case of Superstorm Sandy, a large northward excursion of the jet stream hung around over Greenland, giving Sandy nowhere to go but west.
(As it did so, it converged with another low-pressure system, becoming a hybrid extratropical cyclone-nor'easter, which fueled its destructiveness.)

  After the convergence of tropical and extra-tropical storm systems, the hybrid Superstorm Sandy made landfall in New Jersey and New York, bringing strong winds, storm surge, and flooding to areas near the coast and blizzard conditions to Appalachia.

"Our research suggests that these northward swings in the jet stream are happening more frequently now, especially in the North Atlantic, just like the situation that was in place when Sandy came along," Francis told OurAmazingPlanet in an email.

In particular last year, the sea-ice extent (or area covered) in the Arctic reached a record low in September, just over a month before Sandy made its ominous turn toward the coast.

What's expected in a warming world

Right now, as with other individual weather events and climate change, a direct link can't be made between that record sea-ice low and Sandy's path.

"We can't say that the record sea-ice loss last summer definitely created or enhanced the block that affected Sandy, but it's the kind of situation we'd expect to see more of as greenhouse gases continue to build up in the atmosphere and sea ice continues to dwindle," Francis said.

Francis added that it is possible to investigate the statistical likelihood that this record low played a part in Sandy's story.

"Numerical weather prediction computer models can be used to assess this question," she said.
"They can be run with and without the various factors related to climate change to see how the storm would have developed in an environment before climate change really got going."

While Francis doesn't have funding ("yet," she said) to study Sandy, she expects many other scientists to delve into the conditions that led to the superstorm.

"I'm sure there will be a flurry of studies coming out over the next couple of years," she said.

Links :
  • ThinkProgress : How Arctic Ice Loss Amplified Superstorm Sandy — Oceanography Journal

Sunday, March 17, 2013

NOAA satellite captures "The Storm of the Century"



From NOAA

What started out as an area of low pressure off the coast of Texas on March 12, 1993 quickly developed into what many people refer to as "The Storm of the Century".
The evolution of this winter superstorm can be seen in this imagery from the GOES-7 satellite, using both visible and colorized infrared data.
As the storm developed in the Deep South, it spawned 11 tornadoes in Florida and dumped from 8 to 33 inches of snow from Alabama to the Carolinas.
As the storm moved north and intensified, conditions became even worse.
With a central pressure of 960 millibars, usually found only in Category 2 hurricanes, whiteout conditions were common.
Snowfall exceeded 3.5 feet in some locations.

When the storm passed, 208 people were dead and $6.6 billion dollars in damage were sustained.
The National Climatic Data Center still ranks the 1993 as the most impactful winter storm to hit the Northeast.
Though the 1978 and 1996 blizzards may have brought more intense localized conditions, the scale of the 1996 storm has not been equaled in recent history.

Links :
  • NOAA : storm archive description of the 1993 Storm of the Century

Saturday, March 16, 2013

Sea urchins - Planktonic origins


Barely visible to the naked eye, sea urchin larvae grow and transform into bottom-dwelling urchins.
Plankton Chronicles Project by Christian Sardet, CNRS / Noe Sardet and Sharif Mirshak, Parafilms


See complementary videos on Marine food web and Reproduction in the Ocean