Tuesday, December 17, 2019

Waters off California acidifying faster than rest of oceans, study shows

The microscopic shell of foraminifera, a single-celled organism, magnified 650 times its size by a scanning electron microscope.
Scientists studying sediment samples containing the tiny shells were able to determine the rate the oceans are acidifying.
Credit : NOAA

From The NYTimes by Kendra Pierre-Louis

California’s coastal waters are acidifying twice as fast as the rest of the oceans, a study published Monday shows.
And some of California’s most important seafood — including the spiny lobster, the market squid and the Dungeness crab — are becoming increasingly vulnerable.

Why are the oceans becoming more acidic and how does that threaten biodiversity?
Human activities produce excessive carbon dioxide and much of it is absorbed by the oceans, where it is converted to an acid.

The carbon dioxide emissions that contribute to the planet’s rapidly warming climate are also changing the chemistry of the world’s oceans, which have absorbed roughly 27 percent of the carbon dioxide emitted worldwide.

Ocean water is ordinarily slightly basic, or alkaline, but is becoming more acidic as it absorbs carbon dioxide.
This can harm marine life, especially shellfish, because they struggle to make their shells in acidic waters.

Emily Osborne, a scientist in the National Oceanic and Atmospheric Administration’s ocean acidification program, with her colleagues studied the fossil record of planktonic foraminifera — tiny simple organisms which, like shellfish, build their shells from calcium carbonate.
They have been around for millions of years, but each individual organism only lives for roughly a month.
“They are creating this super tight snapshot of what the ocean looks like for a month period of time,” said Dr. Osborne, a lead researcher on the study, published in Nature Geosciences.

California’s fisheries account for slightly more than 10 percent of the nation’s seafood production.

An earlier study compared the impact of carbon dioxide emissions on immature shellfish in waters with carbon dioxide at preindustrial levels versus water with carbon dioxide at levels with concentrations expected by 2100.
It found that the latter had shells that were “malformed and eroded.”

There are a few reasons shellfish struggle in a more acidic ocean.
The first involves calcium, which, in the form of calcium carbonate, is a building block that helps create their protective shells.
But in order to make calcium carbonate, shellfish need access to a kind of carbon known as carbonate ion.
As the oceans absorb more carbon dioxide, there is more carbon than ever — but more of it is bicarbonate, not carbonate ion.

“It’s a shift in what is usable by the organisms,” Dr. Osborne said.
“So that they have fewer of those building blocks that they can actually utilize.”

Another reason is that “it could also be that they make a shell that’s weaker or that can be more easily corroded by the ocean chemistry or even weaker so it can be more easily drilled or crushed by a predator,” said Gretchen Hofmann, a marine biologist at the University of California, Santa Barbara, who was not involved in this study.

By analyzing the shell weights of almost 2,000 fossil shells from over the past century the researchers found a 20 percent reduction in calcification among surface-dwelling foraminifera.

Foraminifera shells viewed under a microscope.
Credit...NOAA

“I could just watch the shells literally getting thinner as I moved up through the record and got closer to the present day,” Dr. Osborne said.

The ocean currents off California tend to recirculate colder, more acidic water from deeper in the ocean to the surface, a process known as upwelling.
As a result, California’s waters were already more acidic than many other areas of the oceans.
Climate change is exacerbating the effect, raising the question of how marine life will fare over the long term.

“We know that evolution works and every creature has some degree of plasticity in them,” Dr.
Hofmann said.
But, she added, “the environment is changing so fast that we’re probably outstripping the role that it can play.”

Links :

Monday, December 16, 2019

Norway (NHS) layer update in the GeoGarage platform

219 nautical raster charts updated & 2 new insets added

Anak Krakatau: Giant blocks of rock litter ocean floor

There are about 40 volcanoes worldwide thought capable of doing what Anak Krakatau (centre island) did
image : Copenicus data 2019

From BBC by Jonathan Amos

Shattered remnants from the volcano that generated a devastating tsunami in Indonesia a year ago have been pictured on the seafloor for the first time.

Scientists used sonar equipment to image the giant chunks of rock that slid into the ocean when one side of Anak Krakatau collapsed.
Some of these blocks are 70-90m high.
Their plunge into the water produced tall waves that tore across the shorelines of Java and Sumatra on 22 December 2018.


Over 400 people around the Sunda Strait died in the nighttime disaster, and thousands more were injured and/or displaced.

Dave Tappin recalls the event and describes the blocks of rock on the seabed

Researchers have been trying to reconstruct what happened ever since. But all their studies to date have been based on what can be seen above the water.

Prof Dave Tappin and colleagues realised they had to investigate the island volcano's missing mass - now under the ocean's surface - or they would never truly get a full description of Anak Krakatau's failure.
A multibeam echosounder was brought in to map the seabed.
Updated: This simulation shows how the volcano's flank slipped into the water

"Early models of the collapse were based on satellite imagery that only looked at the subaerial parts of the volcano," the British Geological Survey scientist told BBC News.
"Our bathymetry is imaging at 200m water depths and we are seeing triangular-shaped blocks, which are basically coherent and they formed, before the collapse, the southwestern flank of Anak Krakatau."

The debris field runs out to 2,000m from the volcano.
A seismic survey also conducted by the team shows how this material is layered on top of older deposits.
Crucially, the underwater imaging has allowed Prof Tappin's team to revise its estimate for the volume of rock involved in the flank failure.
And it's smaller than previously thought.
Calculations based on above-water measurements of what was left of the once 335m-high volcano had suggested a figure of 0.27 cubic km.
The new assessment now points to 0.19 cubic km sliding into the ocean, almost 200 million cubic metres.

Stephan Grilli: New simulations reproduce the damage observed on nearby islands

This smaller volume might have presented something of a problem for tsunami modellers.
Their original simulations of how the waves generated in the collapse moved across the Sunda Strait had already proved a good match for what had been observed at tide gauges and from what was known of the extent of damage along nearby coasts.

Now, the models are having to be re-run but with a smaller input.
The simulations still work, however - and with good reason.
Prof Tappin's team has also discovered that the failure plane on the volcano - the angle of slope along which the rock mass slid - was shallower than earlier assumptions.

Whereas it was once thought the failure plane cut down steeply into the basin created when the old volcano on the site blew its top in 1883, it's now obvious the collapse slope entered the water much nearer the surface.

This simulation, based on the new data, shows how the tsunami moved outwards

"We've already redone the near-field modelling with a finer resolution based on the new bathymetry and the results are about the same, despite having a smaller volume of rock," explained tsunami expert Prof Stephan Grilli from the University of Rhode Island.

"The shallower slide occurs almost like a ski jump, maintaining the collapse material closer to the surface and making it more tsunamigenic than a steeper failure, which would have brought the sediment down deeper, much quicker."

Profs Tappin and Grilli were speaking here in San Francisco at the American Geophysical Union's annual Fall Meeting.
This is the first chance they've had to present their findings to the wider scientific community.

Also speaking was Prof Hermann Fritz from the Georgia Institute of Technology.
He reviewed the damage on nearby shores, describing from on-the-ground studies how high the tsunami waves must have been and how far inland they reached.

On the islands in the immediate vicinity of Anak Krakatau, trees up to 80m above the normal sea surface were torn from their roots.

Ujung Kulon National Park is due southwest of Anak Krakatau, some 50km away

Much of the wave energy took a path away from the volcano in the same direction of the collapse - to the southwest. This resulted in 10m-high waves laying waste to a corner of Ujung Kulon National Park on Panaitan Island - a distance of 50km from Anak Krakatau.

"Local residents were very fortunate that the collapse was in the southwest direction, in the direction where few people were living - towards the national park," said Prof Fritz.

"Had the collapse direction been different, the outcome could have been very different as well in terms of tsunami heights on populated areas."

Lessons learned from Anak Krakatau are being used to assess the hazards at other volcanoes. There are about 40 other locations around the world where flank collapse into surrounding water is considered a danger.

Anak Krakatau the child of Krakatau, will grow into an island by 1930 with the GeoGarage platform (NGA nautical raster chart)

The map shows the area covered by the bathymetric survey, to the southwest and northeast of Anak Krakatau

Links :

Sunday, December 15, 2019

Icebreaker crowd (1900s)

Opening shots from the award-winning Finnish film director and academic Kari Peter Conrad von Bagh (1943 –2014) documentary "Helsinki, ikuisesti" ("Helsinki Forever" 2008) show a crowd admiring (and soon being chased by) the icebreaker Tarmo in Helsinki, Finland.
Apparently filmed in the 1920s.
The film draws a portrait of Helsinki and also acts as an essay on Finnish culture in a wider sense.
The voiceover quoting Eino Leino towards the end is not related to this footage in particular.
It translates roughly as: "We do not live only in the present. The past – with all its memories, events and experiences – lives in us And often it just might so happen that the past is stronger than the present"

Russia's nuclear-powered icebreaker Arktika, said to be the world's biggest and most powerful, has returned to St. Petersburg after a two-day test run
Arktika, ordered by state nuclear company Rosatom and meant to transport liquefied natural gas from the Arctic, is 173 meters long and 15 meters high. 
The run tested the vessel's functioning and maneuverability, said Mustafa Kashka, general director of Atomflot, the company which runs Russia's icebreaking fleet. 
However, the nuclear-propelled ship, which can supposedly break through almost 3 meters of ice, was fueled by diesel oil on its maiden voyage. 
Inaugurated in 2016, Arktika is the first vessel in a project aimed at allowing year-round navigation in the Northeast Passage -- a sea route connecting the Atlantic and Pacific oceans traversing the Arctic following Russia's coast. 
The Arctic holds huge oil and natural-gas reserves that are being eyed by Russia and other countries, including the United States, Canada, and Norway. 
 The plan will also make it easier for Russia to deliver hydrocarbons to Southeast Asia. 
The final tests for Arktika are scheduled for March and April and it is set to start operating in May. Two other similar vessels -- the Ural and the Sibir -- are under construction. 

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Saturday, December 14, 2019