Saturday, April 13, 2013

‘Lost’ sailing pioneer photo archive uncovered after 4 decades

'Circa 22nd April 1969: Robin Knox-Johnston with champagne aboard his 32ft yacht SUHAILI off Falmouth, England after becoming the first man to sail solo non-stop around the globe. Knox-Johnston was the sole finisher in the Sunday Times Golden Globe solo round the world race, having set out from Falmouth, England on 14th June 1968'    Bill Rowntree - PPL ©

From PPLmedia

A 3,000-strong archive of pictures, taken during Sir Robin Knox-Johnston’s pioneering solo non-stop round the world voyage in 1968/9, has been discovered and saved for posterity by specialist photo library PPL.
The story is published for the first time in the May issue of Classic Boat magazine.

The pictures cover Knox-Johnston’s entry in the Sunday Times Golden Globe Race in1968/9 when Robin was one of nine starters attempting to become the first to sail alone non stop around the world. The event was billed as one of the last great challenges left to man.
For the other eight, it was a challenge too far, for Robin was the only finisher, completing the 27,000 mile circumnavigation aboard his self-built 32ft ketch Suhaili in 312 days.



The valuable archive had been gathering dust in the library of the Sunday Mirror newspaper which had published Robin's stories during the voyage.
The negatives were about to be dumped in a skip when the London newspaper moved from Fleet Street to Canary Wharf, but by pure chance, Bill Rowntree, the Mirror photographer who had covered Knox-Johnston’s departure and return to Falmouth, happened to be in the newspaper the day of the big clear out.

Robin Knox-Johnston celebrates aboard

Bill, now 73, recalls, “The picture library manager poked his head round the door and asked if I had any use for them.”
Rowntree put the box under his arm and took it back to his home at Tunbridge Wells, Kent, and there the negatives may have lain, had it not been for a particular picture request from Henri-Lloyd, the clothing manufacturer that had supplied Knox-Johnston’s original oilskins, to mark their 60th anniversary celebrations this year.

 a TV helicopter hovers overhead as Robin Knox-Johnston sails his 32ft yacht SUHAILI off Falmouth

Many of the colour pictures in Knox-Johnston’s bestselling book A World of My Own, were lost after publication, but PPL Photo Agency holds what was left of the Knox-Johnston archive within its Pictures of Yesteryear Library.
This also contains the archives of other famous sailing pioneers including Sir Francis Chichester, Sir Chay Blyth, and photographer Eileen Ramsay, who captured many of these great events between 1949 and 1970.
It was Barry Pickthall’s call to Rowntree to see if he still had the negative that Henri-Lloyd needed, that prompted the question "What should we do with the other 3,000 pictures I have here?”

 Robin Knox-Johnston regailing friends with stories of his solo circumnavigation, in the bar of the Royal Cornwall Yacht Club

Sir Robin Knox-Johnston, who is now inspiring hundreds of amateur sailors to follow in his adventurous wake aboard a 12-strong fleet of yachts in the Clipper Round the World Race starting from the UK in August, says of the find, "I thought these pictures were lost, so it was a wonderful surprise to discover that this unique record of my return to Falmouth in 1969 still exists."


Dan Houston, the Editor of Classic Boat Magazine, says:

"There is something quite awe-inspiring when you look at these photographs. They capture a moment in sailing history when Sir Robin, then a young man, almost unwittingly stepped into the history books. His boat Suhaili was not the fastest – he never expected to win, but as the other competitors were beaten by the elements and gear failure, it was Robin and his seaworthy little ketch that won the day. Sir Robin went on to become Britain's most endearing and enduring sailing hero – and gave his £5,000 prize money from the race to the family of Donald Crowhurst who committed suicide during the race.


These photographs show the man as much as the hero: his parents tense faces as he reassures them saying goodbye; life aboard in his untidy cabin; his first unsteady steps as he gets ashore; his first beer ashore. It is all such a contrast with how things are done today – and it makes his feat of seamanship all the more remarkable."


Links :

Friday, April 12, 2013

Liquid Robotics unveils Wave Glider SV3 ocean robot which brings the Cloud to the waves

Liquid Robotics debuted Monday the Wave Glider SV3, the world's first hybrid wave and solar propelled unmanned ocean robot, and with it, the technology to explore portions of the world previously too challenging or costly. (Photo : Liquid Robotics)

From CNN

 Where data is concerned -- that is, where usable, potentially profitable data -- the world's oceans are somewhat akin to black holes: We know they are out there, but beyond what we can see at the horizon, we really have no idea what's happening in any one place from one moment to the next.
The amount of useful information streaming back to shore from the world's oceans, home to critical food stocks, abundant energy reserves, vital shipping lanes, and the engine driving global climate, is so thin as to be meaningless for all but the most academic purposes.

 Liquid Robotics's Wave Glider are the first unmanned autonomous marine robots that use the ocean's waves for energy.

"Do you realize that in the ocean today there is often one sensor for an area the size of California?" says Liquid Robotics CEO Bill Vass.
He likens this to standing in Death Valley and trying to determine the local temperature via a thermometer that is hundreds of miles away.
"It may not feel like 58 degrees to you," he says, capping off the analogy.
"But that's what your sensor says because your sensor is in San Francisco."

This dearth of data places Liquid Robotics in a truly unique position.
Its seaworthy, sensor-laden, surfboard-shaped Wave Glider robots use a novel propulsion system to convert the rolling motion of ocean waves into energy for forward thrust, creating a self-contained system that requires no refueling and very little maintenance as long as the ocean continues to move. 

The company proved this last December when one of its Wave Gliders -- launched from San Francisco a year prior -- arrived in Brisbane, Australia after autonomously completing a 9,000-mile trans-Pacific crossing.
It proved its durability again when one of the NOAA's Wave Gliders traveled right through the center of Hurricane Sandy in October.
But with the release of its latest iteration of Wave Glider this week at the Navy's Sea-Air-Space expo near Washington, D.C., Liquid Robotics has more or less completed a transition from robot manufacturer to one of the world's more interesting big data companies.

Why?
Because the Wave Glider's trip across the Pacific was little more than a warm-up lap.
Liquid Robotics has previously sold and leased its robotic sensing platforms to the U.S. Navy and the National Oceanic and Atmospheric Administration, but for most applications -- oil and gas exploration, tropical storm tracking and prediction, fisheries management, maritime threat interdiction -- data, rather than a robot, is what the customer really wants.

Wave Glider can provide data by the terabyte.
But the brand new Wave Glider SV3 processes data by the terabyte and networks with other Wave Gliders in its vicinity, basically creating an information-rich cloud stretching across the high seas.


 Roger Hine, co-founder and CTO of Liquid Robotics talks about the process of developing the Wave Glider SV3, the next generation of Wave Glider, autonomous ocean surface vehicle

Key to this is a proprietary cloud-based operating system called Regulus (designed for Liquid Robotics by Java creator James Gosling) that allows the SV3 to exhibit a fairly dazzling degree of autonomy while also maintaining an open source component that allows for rapid deployment of new sensor payloads and software packages as well as rapidly swappable software and hardware to run them.
Sensor payloads can include virtually anything that fits in the SV3's seven modular payload units: atmospheric and oceanographic sensors applicable to ocean and climate science, video cameras and acoustic sensors useful for national security and marine environment protection purposes, or instruments for mapping and evaluating geography on the seafloor and below.
And thanks to the cloud-based software architecture, some SV3s could carry all of these sensors and more while offloading some of the data processing to another nearby Wave Glider serving as a central data hub.

In other words, Liquid Robotics can deploy something like a floating server farm to process the data collected by other Wave Gliders in the area, then supply customers on shore with only the refined, processed data that they want -- something oil and gas exploration companies in particular have been quick to embrace.
(Alongside the NOAA and U.S. Navy, Liquid Robotics' client list includes names like Schlumberger (SLB) and BP (BP).)

"If you look at an ocean-rated crew vessel that can do this, it costs about $150,000 a day in a commercial environment," Vass says.
"An ocean-rated research vessel is about $40,000 a day. We do the same kind of data collection -- usually denser data collection actually, because we move more slowly -- at about a tenth of that cost, and we don't pollute or put people at risk when we do it."

 SV3 & SV2 side by side

Currently Liquid Robotics is operating 200 Wave Gliders at sea in every ocean on Earth, Vass says, a number that is growing 60% year over year.
The company has provided data to about 100 customers thus far, and when its current fleet of SV2s -- which largely stream raw data back to shore for processing -- are replaced and upgraded with the SV3's onboard processing capability (the new SV3 begins shipping in Q3, though most of its upgrades are retrofittable to existing SV2s) Liquid Robotics' ability to provide companies with dense but highly refined data sets will likely grow exponentially.

Vass and his colleagues envision a globe swimming with Wave Gliders, creating a mesh network that spans the 70% of the Earth that is, as yet, largely unwired.
"Our customer is anyone who moves over the ocean or extracts value from it," Vass says.
"Or anyone who deals with weather," he adds, more or less tying up what the company sees as its real value proposition.
Not every company needs high-resolution data streaming in from far out at sea, but the data Liquid Robotics provides could have impacts far beyond its client base (think anyone who relies on NOAA or the National Weather Service to make decisions).
And those entities that directly need this kind of data -- whether oil and gas outfits, national security agencies, or wildlife management, oceanographic researchers, or international shipping concerns -- have never been able to access it before.
At least not like this.
"Ten years ago this company would've been science fiction," Vass says.
" Bringing all of this technology together is really going to change the world."

Links :

Thursday, April 11, 2013

Probing the reasons behind the changing pace of warming


From YaleEnvironment360

A consensus is emerging among scientists that the rate of global warming has slowed over the last decade.
While they are still examining why, many researchers believe this phenomenon is linked to the heat being absorbed by the world’s oceans.

Whatever happened to global warming? Right now, that question is a good way of starting a heated argument. Some say it is steaming ahead.
But others say it has stalled, gone into reverse, or never happened at all — and they don’t all run oil companies or vote Republican.

So what is going on?

First, talk of global cooling is palpable nonsense.
This claim relies on the fact that no year has yet been hotter than 1998, an exceptional year with a huge planet-warming El Nino in the Pacific Ocean.
Naysayers pretend that 1998 was typical, when it was anything but, and that temperatures have been declining since, which is statistical sleight of hand.

Meanwhile consider this.
According to the National Oceanic and Atmospheric Administration (NOAA), all 12 years of the new century rank among the 14 warmest since worldwide record-keeping began in 1880. The second-warmest year on record, after 1998, was 2010.
This is not evidence of cooling.

But there is a growing consensus among temperature watchers that the pace of warming in the atmosphere, which began in earnest in the 1970s and seemed to accelerate in the 1990s, has slackened, or stalled, or paused, or whatever word you choose.
It may turn out to be a short blip; but it is real.
“Although the first decade of the 21st century was the warmest on record, warming has not been as rapid since 2000,” says Pete Stott, head of climate monitoring and attribution at the UK’s Met Office, one of the leading keepers of the global temperature.
He calls it a “hiatus” in warming.

In a blog last week, James Hansen, the retiring head of NASA’s Goddard Institute for Space Studies (GISS), agreed that “the rate of global warming seems to be less this decade than it has been during the prior quarter century”

Something is going on.
With heat-trapping greenhouse gases accumulating in the atmosphere ever faster, we might expect accelerated warming.
So it needs explaining.

There are a number of theories.
Hansen suggested that extra emissions of particles in Asian smogs could be shading the Earth and camouflaging the greenhouse effect.
In a February post on RealClimate, his Goddard Institute colleague Gavin Schmidt instead pointed to fewer warming El Ninos and more cooling La Ninas.
He suggested that adjusting for their influence produced an unbroken pattern of warming.


Schmidt’s analysis certainly hints at a role for the oceans in all this.
And most researchers on the case argue that, one way or another, the most likely explanation for the heating hiatus is that a greater proportion of the greenhouse warming has been diverted from the atmosphere into heating the oceans.
A new study from Kevin Trenberth of the National Center for Atmospheric Research in Boulder, Colorado, published online in Geophysical Research Letters, found that ocean warming has been accelerating over the last 15 years.

Richard Allan of the University of Reading in England says simply: “Warming over the last decade has been hidden below the ocean surface.”
If you take the oceans into account, he says, “global warming has actually not slowed down.”

This should not come as a surprise, notes Chris Rapley of University College London.
The oceans are the planet’s main heat sinks.
More than 90 percent of the extra heat trapped in the atmosphere by greenhouse gases ends up there.
But, while climate models are good at calculating atmospheric processes, they are poorer at plumbing the ocean-atmosphere interactions that determine how fast and how regularly this happens.

That makes those interactions a big source of uncertainty about atmospheric global warming, especially over the short term.
If oceans grab a bit more heat one year, they can shut down that year’s warming. Equally, if they release a bit more they can accelerate atmospheric warming.
This matters. “The way the ocean distributes the extra energy trapped by rising greenhouse gases is critical... [to] global surface temperatures,” says Allan.
For forecasters trying to figure out the next decade or so, oceans could screw it all up.

Some bits of the puzzle have been known for a while.
For instance, during El Nino years, warm water spreads out across the equatorial Pacific and the ocean releases heat into the air, warming the air measurably.
That is what happened in 1998.

But while El Ninos come and go within a year or so, there are other cycles in heat distribution and circulation of the oceans that operate over decades.
They include the Pacific Decadal Oscillation and the Atlantic Multidecadal Oscillation (AMO), both of which have been implicated in climate fluctuations in the 20th century.
So have these or other ocean cycles been accelerating the uptake of heat by the oceans?


Virginie Guemas of the Catalan Institute of Climate Sciences in Barcelona, believes so.
In a paper published in Nature Climate Change this week, she claims to provide the first “robust” evidence linking ocean uptake of heat directly to what she calls the recent “temperature plateau” in the atmosphere.

By plugging detailed measurements of recent atmospheric and sea temperatures into EC-Earth, a European model of interactions between atmosphere, oceans, ice and land surfaces, Guemas found that about 40 percent of the take-up was in the tropical Pacific, and another 40 percent in the tropical and North Atlantic.

She told me that it seems likely the changing thermohaline ocean circulation, which starts in the North Atlantic, plus the cycles of El Nino and perhaps the AMO, may play a prominent role.
She thinks her model could have predicted the recent slowdown of atmospheric warming ahead of time.

That would be a breakthrough, but nobody has done it yet.
Meanwhile, the climate modellers are skating on thin ice when they make predictions that play out over the timescales of a decade or so on which ocean cycles seem to operate.
These forecasters can claim that, all things considered, they have done pretty well.
But the forecasts remain hostages to fortune.

If anything, the recent pause shows the model forecasts in a good light. Myles Allen, a climate modeller at Oxford University in England, reported in Nature Geoscience last month on an audit of one of his own forecasts, which he made in 1999.
He had predicted a warming of a quarter-degree Celsius between the decade that ended in 1996 and the decade that ended in 2012.
He found that, in the real world, temperatures got too warm too soon during the 1990s; but the slackening pace since had brought the forecast right back on track.

That shows the forecast is performing well so far, but Allen admitted it might not stay that way.
If temperatures flat-line out to 2016, his model’s prediction for that year will look no better than a forecast based on a series of random fluctuations.

Some in the mainstream climate community privately admit that they were caught out by the slackening pace of warming in the past decade or so.
Back in the 1990s, some suggested — or at least went along with — the idea that all the warming then was a result of greenhouse gases.
They were slow to admit that other factors might also be at work, and later failed to acknowledge the slowdown in warming. As Allen pointed out earlier this year: “A lot of people were claiming in the run-up to the Copenhagen 2009 [climate] conference that warming was accelerating. What has happened since then has demonstrated that it is foolish to extrapolate short-term climate trends.”

Not surprisingly they have been taken to task for this hubris.
Roger Pielke Jr., an environmental studies professor at the University of Colorado at Boulder, who enjoys baiting the mainstream, told me last month: ”It is good to see climate scientists catching up with the bloggers. They should ask why it took so long to acknowledge what has been apparent to most observers for some time.”

But modellers are now responding more actively to the new real-world temperature data.
For instance, the Met Office’s Stott reported last month that global temperatures were following the “lower ranges” of most model forecasts, and that higher projections were now “inconsistent” with the temperature record.

And last December, the Met Office downgraded its best guess for temperatures in the five years to 2017 from 0.54 degrees C higher than the average for the late-20th century average to 0.43 degrees higher. It said the new forecast was the first output of its latest climate model, HadGEM3, which incorporates new assessments of natural cycles.

But the problem is that these cycles are not well integrated into most climate models.
Natural cycles could switch back to warming us again at any time, admits Stott.
But he has no clear idea when.

The stakes for the climate forecasting community are high.
It may be unfair, but the brutal truth is that if the climatologists get their forecasts for the coming decade badly wrong, then a great many in the public will simply not believe what they have to say about 2050 or 2100 – even though those forecasts may well be more reliable.

Forecasters badly need a way to forecast the ocean fluctuations, and it could just be that Guemas’s new study will help them do that.
She claims that her findings open the way to the future delivery of “operational decadal climate predictions.”
For now she is cautious about making firm predictions, but told me she believes that “the heat that has been absorbed recently by the ocean might very well be released back to the atmosphere soon. This would be the scenario of highest probability. It would mean an increased rate of [atmospheric] warming in the next decade.”

It would indeed.
If natural cycles start pushing towards strong warming, they will add to the continued inexorable upward push from rising concentrations of heat-trapping greenhouse gases.
In that case, we would see climate change returning to the rapid pace of the 1990s.
Whatever happened to global warming?
The odds may be that by 2020 it will have come roaring back.

Links :
  • DiscoveryNews : Think the Planet Isn't Warming? Check the Ocean

Wednesday, April 10, 2013

France SHOM update in the Marine GeoGarage

26 charts have been withdrawn since the last update :

  • 1619    Mouillages de Tarifa   
  • 3357    De la Pte Banda à la Riv. Coanza   
  • 3462    Baie de Ba (Baie Le Bris)   
  • 3519    Delta du Tonkin   
  • 3865    De l'île Hon Tseu au Cap Lay   
  • 4697    Baie de Diego-Suarez   
  • 5414    Baie d'Halong   
  • 5427    Baie de Cam-Ranh   
  • 5509    Du Cap Padaran à la Baie de Cam-Ranh   
  • 5549    De la Baie d'Halong à Pak-Ha-Mun   
  • 5559    Chenaux entre Quang-Yen et la Baie d'Halong   
  • 5563    Baie de Nhatrang   
  • 5571    Cambodge et Cochinchine Mékong  
  • 5652    Grande Baie des Faï Tsi Long   
  • 5676    Abords de Poulo Condore et embouchure du Bassac   
  • 5691    Annam et Cochinchine   
  • 5809    Du Cap Varella à l'île Nuoc   
  • 5892    De la Pointe Samit à Tian-Moi (Ile à l'Eau) Koh Prins, Koh Tang, Poulo Wai  
  • 5899    De Hon-Tseu à Hon-Matt   
  • 6150    Mouillage et Passes de Tamatave   
  • 6238    Iles Anjouan et Mohéli   
  • 6239    Grande Comore   
  • 6290    Abords de Sihanoukville (Kompong Som)   
  • 6527    Port de Tamatave   
  • 6666    De l'estuaire du Gabon à l'estuaire du Congo   
  • 7520    INT 7115 Abords de Djibouti    

and 6 charts have been added

  • 7547    Abords de Djibouti
  • 7678    ÃŽles Anjouan et Mohéli
  • 7679    ÃŽles Grande Comore et Mohéli
  • 7681    Baie d'Antsiranana (Diégo-Suarez)
  • 7683    Port et Passes de Toamasina (Tamatave)
  • 7791    De Gamba à Luanda 

so 600 charts from SHOM are displayed in the Marine GeoGarage




















































Sharper view of the Southern Ocean: New chart shows the entire topography of the Antarctic seafloor in detail for the first time


 The new IBCSO map of Antarctica (Alfred-Wegener-Institut)

From AWI

Reliable information on the depth and floor structure of the Southern Ocean has so far been available for only few coastal regions of the Antarctic.
An international team of scientists under the leadership of the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, has for the first time succeeded in creating a digital map of the entire Antarctic seafloor.
The International Bathymetric Chart of the Southern Ocean (IBCSO) for the first time shows the detailed topography of the seafloor for the entire area south of 60°S.
An article presented to the scientific world by IBCSO has now appeared online in the scientific journal Geophysical Research Letters.
The IBCSO data grid and the corresponding Antarctic chart will soon be freely available in the internet and are intended to help scientists amongst others to better understand and predict sea currents, geological processes or the behaviour of marine life.

 Multibeam bathymetric survey techniques provide a rapid means of determining the morphology and nature of the seafloor.
The recent Hydrosweep DS-2 System onboard R/V Polarstern provides 59 individual soundings of the water depth and echo strength for each ping.
Moreover sidescan information (2048 echos per ping) is retrieved.
The system can be operated with 90 or 120 degrees fan angle and is designed for deep sea observations.

The new bathymetric chart of the Southern Ocean is an excellent example of what scientists can achieve if researchers from around the world work across borders.
“For our IBCSO data grid, scientists from 15 countries and over 30 research institutions brought together their bathymetric data from nautical expeditions. We were ultimately able to work with a data set comprising some 4.2 billion individual values”, explains IBCSO editor Jan Erik Arndt, bathymetric expert at the Alfred Wegener Institute in Bremerhaven.

This video shows typical use cases of a modern multibeam echosounder, like the HYDROSWEEP of the 3rd generation, on a modern research vessel, like the German research icebreaker POLARSTERN.

Collecting bathymetric data, as with the German research vessel Polarstern with its multibeam echo sounding system, was nowhere near enough, however, to develop a useful, three-dimensional model of the seafloor:
“The ocean south of the 60th parallel extends over an area of some 21 million square kilometres and is therefore around 60 times as large as the Federal Republic of Germany. Reliable bathymetric data have so far existed for only 17 per cent of this area. The largest data gaps, for example, are in the deep sea regions of the south Indian Ocean and the South Pacific and in areas which experience difficult sea ice conditions throughout the year in some places, such as in the Weddell Sea”, says Jan Erik Arndt.

 The IBCSO database currently consists of more than 4200 million data points contributed by more than 30 institutions from 15 countries.
In total 177 Multibeam cruises were available building the nuclei of the database.
Single beam echo sounding data, digitized soundings from nautical charts and regional bathymetric compilations are rounding off the database

For this reason the mappers did not just take the trouble to digitize old Antarctic nautical charts and to convert satellite data.
They also used a mathematical trick by interpolating the data set.
“We treated every existing measurement point like a tent pole to a certain extent and arithmetically covered these poles with a tarpaulin. In this way we obtained approximate values about the height of the tarpaulin between the poles”, explains the AWI specialist for data modeling.

 Marie Byrd seamounts
Depiction of the Marie Byrd seamounts in the IBCSO grid (bottom) compared to its depiction in the older GEBCO_08 data grid (top).
The lines one can see in the IBCSO-graph are the multibeam tracklines of the research vessels.

This work was worth it: the IBCSO data grid has a resolution of 500 times 500 metres.
This means that one data point reflects the depth of a sea area of 500 times 500 metres – a feature that leads to impressive degree of detail.
Where older models only offer a glimpse of a mountain in the deep sea, IBCSO shows an elevation with sharp ridge crests and deep channels in the slopes.

 Depiction of the region around Ritscher Canyon in the IBCSO grid (bottom) compared to its depiction in the older GEBCO_08 data grid (top).

A formerly flat point at the bottom of the Riiser-Larsen Sea can now be identified as an offshoot, some 300 metres deep, of the underwater Ritscher Canyon which runs along a length of over 100 kilometres from the south west to the north.
And not far away from today’s shelf ice edge of the large Getz ice shelf the furrows are to be seen quite clearly which were ploughed into the seafloor by the ice tongue as it grew.

Depiction of the region north of Neumayer station III (Weddell sea) in the IBCSO grid (bottom) compared to its depiction in the older GEBCO_08 data grid (top).

Using this degree of detail IBCSO is primarily intended to push ahead with research: “The depth data of the Southern Ocean are of great interest to polar researchers from many disciplines. The 3D data grids of the seafloor enable oceanographers to model currents and the movement of the deep Antarctic water which is of such great importance. Geologists are able to recognise the structures of geological processes more easily. Biologists may be able to better estimate the regions in which certain biological communities may emerge or whether, for example, seals dive to the bottom of the sea in a certain area in search of food”, explains Jan Erik Arndt.

Depiction of the region around Dotson Getz trough in the IBCSO grid (bottom) compared to its depiction in the older GEBCO_08 data grid (top).

However, despite the elation about the new model and its chart, it should not be forgotten that more than 80 per cent of the area of the South Polar Sea is still unchartered.
Jan Erik Arndt: “We hope that as our data grid becomes better known in the scientific world, other scientists will be more willing to provide us with their data of current and future depth measurements in the South Polar Sea. The chances are not bad. A few new research ice breakers are currently being built around the world and every one of them will presumably be equipped with a modern multibeam echo sounder in the same way as Polarstern.”

IBCSO is a project of the General Bathymetric Chart of the Oceans (GEBCO).
It is supported by the Intergovernmental Oceanographic Commission (IOC) of UNESCO, the International Hydrographical Organisation (IHO), the Hydrographic Commission on Antarctica  (HCA) and by the Scientific Committee on Antarctic Research (SCAR).
The geodesy and bathymetry working group of the Alfred Wegener Institute coordinates the project and is responsible for the entire modelling work.

Links :