Monday, October 30, 2017

New science suggests the ocean could rise more — and faster — than we thought

Shot just off the coast of Ilulissat , the best western Greenland has to offer, covering vast glaciers, icebergs and Icefjords melting away.
Rising air and sea temperatures is causing the massive Greenland ice sheet to shed 300 gigatons of ice a year into the ocean, the single largest source of sea level rise from melting ice!

From Washington Post by Chris Mooney


Climate change could lead to sea level rises that are larger, and happen more rapidly, than previously thought, according to a trio of new studies that reflect mounting concerns about the stability of polar ice.

In one case, the research suggests that previous high end projections for sea level rise by the year 2100 — a little over three feet — could be too low, substituting numbers as high as six feet at the extreme if the world continues to burn large volumes of fossil fuels throughout the century.

“We have the potential to have much more sea level rise under high emissions scenarios,” said Alexander Nauels, a researcher at the University of Melbourne in Australia who led one of the three studies.
His work, co-authored with researchers at institutions in Austria, Switzerland, and Germany, was published Thursday in Environmental Research Letters.

The results comprise both novel scientific observations — based on high resolution seafloor imaging techniques that give a new window on past sea level events — and new modeling techniques based on a better understanding of Antarctic ice.

The observational results, from Texas and Antarctica, examine a similar time period — the close of the last Ice Age a little over 10,000 years ago, when seas are believed to have risen very rapidly at times, as northern hemisphere ice sheets collapsed.

Off the Texas coast, this would have inundated ancient coral reefs. Usually, these reefs can grow upward to keep pace with sea level rise, but there’s a limit — one observed by a team of scientists aboard a vessel called the Falcor in 200 foot deep waters off the coast of Corpus Christi.

These so-called drowned reefs showed features that the researchers called “terraces,” an indicator of how the corals would have tried to respond to fast rising sea levels.
Because the organisms must maintain access to a certain amount of sunlight, they would have tried to grow higher to keep up with fast rising seas — but they wouldn’t have been able to do so over a very large area.
And so their growth became concentrated in progressively smaller, stepped regions:

A 3-D representation of Dream Bank, a long-dead reef offshore South Texas.
The vertical scale of the image has been increased to clearly illustrate the terrace structures that form due to rising sea levels via a process known as backstepping.
(Image courtesy of P. Khanna/Rice University)

“The reef under stress often has a tendency to kind of shrink to this higher elevated area,” said AndrĂ© Droxler, one of the authors of the study in Nature Communications and a researcher at Rice University.
“It creates this pyramid-like system.” (Droxler completed the research with colleagues from Rice and Texas A&M University, Corpus Christi.)

The youngest drowned corals date to the end of the last ice age, around 11,500 years ago — corresponding to what scientists believe were large warming events in the northern hemisphere and so-called meltwater pulses from now melted ice sheets.
And multiple drowned reefs off Texas show a similar pattern — and terminate in similar water depths.
“Over 120 kilometers, the reefs behaved the same way. It’s difficult to find any other reason why they would do this,” Droxler said.

Droxler thinks the reef structures suggest eras when sea level was rising by tens of millimeters annually, far beyond the current, roughly 3 millimeters per year.
(A 50 millimeter annual sea level rise would produce a meter, or over 3 feet, of rise every 20 years.)
The new study therefore concludes that during the last ice age, there were multiple bursts of fast sea level rise — and implies that our future could hold something similar.
“The steady and gradual sea-level rise, observed over the past two centuries [may] not be a complete characterization of how sea level would rise in the future,” the study concludes.

Meanwhile, far away in the Southern hemisphere, a team of scientists used a very similar seafloor mapping technology to detect ancient iceberg “plough marks” etched deep into the seafloor of Pine Island Bay, an ocean body that currently sits in front of one of West Antarctica’s most worrying glaciers, Pine Island.
The results were published in the journal Nature on Wednesday by researchers at the University of Cambridge, the British Antarctic Survey, and the Bolin Center for Climate Research in Stockholm.

The seafloor grooves, the researchers believe, were made during a similar era to the Texas coral steppes (the close of the last ice age), and signal a very rapid retreat of Pine Island over roughly a thousand years.

Here’s what they looked like in the seafloor imagery the study produced:


Linear-curvilinear iceberg-keel ploughmarks on the surface of a large grounding-zone wedge located in the mid-shelf Pine Island Trough, West Antarctica. (Martin Jakobsson)

What’s critical about the markings, explains lead study author Matthew Wise of the University of Cambridge, is their maximum depth — 848 meters, or around 2,800 feet.
Because ice floats with 10 percent of its mass above the surface and the remaining 90 percent below it, this suggests that when the ice broke from the glacier, close to 100 meters (over 3oo feet) of it was extending above the water surface.

That’s a key number, because scientists are converging on the belief that ice cliffs of about this height above the water level are no longer sustainable and collapse under their own weight — meaning that when you get a glacier this tall up against the ocean, it tends to crumble and crumble, leading to fast retreat and potentially fast sea level rise.
“If we think about how thick these icebergs would have needed to be considering these float with 90 percent of their mass and thickness beneath the sea,” Wise said, “we think of an ice cliff that was at the maximum thickness implied by the physics of the ice.”

 NASA

The problem is that if it happened then, well, it could happen again.
Both Pine Island glacier and its next door neighbor, Thwaites, are known to get thicker as one travels inland away from the sea, which means they are capable of once again generating ice cliffs taller than the critical size detected by the current study.
“If a cliff even higher than the ~100 m subaerial/900 m submarine cliffs were to form, as might occur with retreat of Thwaites Glacier in West Antarctica, it might break repeatedly with much shorter pauses than now observed, causing very fast grounding line retreat and sea level rise,” explained Richard Alley, a glaciologist at Penn State University, by email after reviewing the current study for the Post.

The final study, released Thursday morning in Environmental Research Letters, takes a different approach but provides perhaps the most sweeping verdict.

The study used five “shared socioeconomic pathways” that analyze possible futures for global society and its energy system, and resulting climate change, over the course of this century.
These scenarios will feed into the next report of the United Nations Intergovernmental Panel on Climate Change, the most influential scientific body that assesses climate change, according to the University of Melbourne’s Alexander Nauels, the lead author of the current study

The research combined these scenarios with tools to project future sea level rise in light of recent science suggesting that Antarctic ice in key regions could collapse relatively rapidly.
That includes possible fast retreat at Pine Island and Thwaites glaciers due, in part, to the problem of ice cliff instability.

The result was that in one scenario assuming high fossil fuel use and strong economic growth during the century, the study predicted that seas could rise by as much as 4.33 feet on average — with a high end possibility of as much as 6.2 feet — by 2100.
That includes possibly rapid sea level rise as high as 19 millimeters per year by the end of the century.

These numbers are considerably higher than high end projections released in 2013 by the Intergovernmental Panel on Climate Change.
(It is important to emphasize that the highest sea level numbers presented in the new study would result from human choices to pursue large fossil fuel exploitation and economic growth with little attempt to slow climate change. It is far from clear that this is the path the world will actually take.)

On the other hand, if the world limits global warming to the Paris climate agreement emissions target, the study finds that sea level rise might be held as low as 1.7 feet by 2100, on average.
Here’s an image illustrating the results:

21st century global mean sea level rise projections with median and shaded 66 percent model ranges under a baseline high warming scenario and low warming scenario.
The dashed lines represent scenarios consistent with the United Nations’ Intergovernmental Panel on Climate Change’s (IPCC) findings in 2013, while the solid lines present revised sea level rise modeling results based on Antarctic ice sheet contributions suggested by DeConto and Pollard (2016).
The IPCC consistent sea level rise likely ranges are based on Nauels et al. (2017).
Global mean sea level rise is provided in centimeters relative to the 1986-2005 mean.
(Nauels et al.)

When the IPCC undertakes a similar analysis, Nauels said, it could produce results like these.
“I think the numbers will go up,” he said of the body’s report, which is expected in 2021.

So in sum — new research is affirming that seas have risen quite rapidly in the planet’s past, and that major glaciers have retreated quickly because their enormous size makes them potentially unstable.
Meanwhile, additional modeling projects these kinds of observations forward and suggests that the century in which we are now living could — could — see similar changes, at least in more severe global warming scenarios in which the world continues to burn high volumes of fossil fuels.

But unlike those submerged corals off the coast of Texas, the difference is that we know this could be coming — which gives us a chance to stop it.

Links :


Sunday, October 29, 2017

Home

Home from Frost Films
A Cinematic Short Film celebrating the life of a man called Bob.
Throughout his entire life he's always put the ocean first,
which has lead to him being homeless and living in a van.
But he loves the ocean and his life as much as ever, and of course, still surfs every day.
"Your happiness comes within yourself"

Links :

Saturday, October 28, 2017

How did early sailors navigate the Oceans ?

Do you know how the early sailors navigate the oceans?
The technology today makes it real easy to navigate the oceans.
But it's very interesting to know how the early sailors managed to navigate without it.
There's a lot of history on it.
I tried my best to compile some important and interesting parts of it into this video.

How did Polynesian wayfinders navigate the Pacific Ocean ?
by Alan Tamayose and Shantell De Silva

Friday, October 27, 2017

US NOAA layer update in the GeoGarage platform

7 nautical raster charts updated

A spacecraft graveyard exists in the middle of the ocean — here's what's down there


Point Nemo on Google Earth

From Business Insider by Dave Mosher

  • Large satellites, space stations, and other objects can pose a threat when they fall to the ground.
  • As a result, many nations de-orbit old spacecraft over the most remote place on Earth, called Point Nemo.
  • This "spacecraft cemetery" is about 1,450 miles away from any piece of land and home to hundreds of dead satellites.
  • Space agencies and companies are concerned about space junk and working on ways to prevent its formation and clean it up.

The most remote location on Earth has many names:
It's called Point Nemo (Latin for "no one") and the Oceanic Pole of Inaccessibility.
Most precisely, its exact coordinates are 48 degrees 52.6 minutes south latitude and 123 degrees 23.6 minutes west longitude.

The spot is about 1,450 nautical miles from any spot of land — and the perfect place to dump dead or dying spacecraft, which is why its home to what NASA calls its "spacecraft cemetery."
"It's in the Pacific Ocean and is pretty much the farthest place from any human civilization you can find," NASA said.
Bill Ailor, an aerospace engineer and atmospheric reentry specialist, put it another way: "It's a great place you can put things down without hitting anything," he said.

To "bury" something in the cemetery, space agencies have to time a crash over that spot.
Smaller satellites don't generally end up at Point Nemo, since, as NASA explains, "the heat from the friction of the air burns up the satellite as it falls toward Earth at thousands of miles per hour. Ta-da! No more satellite."

The problem is larger objects, like Tiangong-1: the first Chinese space station, which launched in September 2011 and weighs about 8.5 tons.

A scale model of China's Tiangong-1 space station.
Jason Lee/Reuters

China lost control of the 34-foot-long orbital laboratory in March 2016, and it is now doomed to crash by early 2018.

Where, exactly?
No one yet knows.
Ailor, who works for the nonprofit Aerospace Corporation, said his company likely won't generate a forecast until five days before the space station is expected to break apart in Earth's atmosphere.

When it does, hundreds of pounds of the spacecraft — like titanium scaffolding and glass-fiber-wrapped fuel tanks — could be falling at more than 180 miles per hour just before slamming into the ground (and thousands of miles per hour faster in the upper atmosphere).

Since China doesn't have control of Tiangong-1, it can't assure the space station will disintegrate over Point Nemo.


Footage courtesy of NASA
The dead-spacecraft dumping zone

Astronauts living aboard the International Space Station actually live closer to the graveyard of spacecraft than anyone else.
This is because the ISS orbits about 250 miles above Earth — and Point Nemo, when the orbital laboratory flies overhead. (The nearest island, meanwhile, is much farther away.)

Between 1971 and mid-2016, space agencies all over the world dumped at least 260 spacecraft into the region, according to Popular Science.
That tally has risen significantly since the year 2015, when the total was just 161, per Gizmodo.

Buried under more than two miles of water is the Soviet-era MIR space station, more than 140 Russian resupply vehicles, several of the European Space Agency's cargo ships (like the Jules Verne ATV), and even a SpaceX rocket, according to Smithsonian.com.

These dead spacecraft aren't neatly tucked together, though.

Ailor said a large object like Tiangong-1 can break apart into an oval-shaped footprint of debris that extends 1,000 miles long and dozens of miles wide.
Meanwhile, the land-free zone around Point Nemo stretches more than 6.6 million square miles — so paying your respects to a specific item isn't easy.

While not all spacecraft wind up in the cemetery, the chances are extremely slim that anyone would get hit by debris regardless of where the spacecraft break up on Earth, Ailor said.

"It's not impossible, but since the beginning of the space age .... a woman who was brushed on the shoulder in Oklahoma is the only one we're aware of who's been touched by a piece of space debris," he said.

A bigger risk is leaving dead spacecraft in orbit.

An illustration of space junk. Satellites and debris are not to scale.
ESA

The pernicious threat of space junk

Some 4,000 satellites currently orbit Earth at various altitudes.
There's space for more — even the 4,425 new internet-providing satellites that Elon Musk and SpaceX wish to launch in the near future.

But it's getting crowded up there when considering the threat of space junk.

In addition to all those satellites, there are thousands of uncontrolled rocket bodies orbiting earth, along with more than 12,000 artificial objects larger than a fist, according to Space-Track.org.
That's not to mention countless screws, bolts, flecks of paint, and bits of metal.

"Countries have learned over the years that when they create debris, it presents a risk to their own systems just as it does for everybody else," Ailor said.

The worst kind of risk, according to the European Space Agency, is when a piece of space junk accidentally hits another piece, especially if the objects are large.

Such satellite collisions are rare but do happen; one occurred in 1996, another in 2009, and two in 2013.
These accidents — along with the intentional destruction of space satellites — have generated countless pieces of space debris that can threaten satellites in nearby orbits years later, leading to a kind of runaway effect.

"We've figured out that this debris can stay up there for hundreds of years," Ailor said, later clarifying that some objects in higher orbits, like geosynchronous satellites, can stay in orbit for thousands of years.

Getting old spacecraft out of orbit is a key to preventing the formation of space junk, and many space agencies and corporations now build spacecraft with systems to de-orbit them (and land them in the spacecraft cemetery).

But Ailor and others are pushing for the development of new technologies and methods that can lasso, bag, tug, and otherwise remove the old, uncontrolled stuff that's already up there and continues to pose a threat.
"I've proposed something like an XPRIZE or a Grand Challenge, where would you identify three spacecraft and give a prize to an entity to remove those things," he said.

The most important hurdle to clear, though, may be politics on Earth.
"It's not just a technical issue. This idea of ownership gets to be a real player here," Ailor said.
"No other nation has permission to touch a US satellite, for instance. And if we went after a satellite ... it could even be deemed an act of war."

Ailor said someone needs to get nations together to agree on a treaty that spells out laws-of-the-sea-like salvage rights to dead or uncontrollable objects in space.
"There needs to be something where nations and commercial [companies] have some authority to go after something," he said.

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