Tuesday, March 14, 2017

The world’s oceans are storing up staggering amounts of heat — and it’s even more than we thought

 Eighty to 90 percent of the heat from global warming is going into Earth's oceans.

From Washington Post by Chelsea Harvey

The world is getting warmer every year, thanks to climate change — but where exactly most of that heat is going may be a surprise.

As a stunning early spring blooms across the United States, just weeks after scientists declared 2016 the hottest year on record, it’s easy to forget that all the extra warmth in the air accounts for only a fraction of the heat produced by greenhouse gas emissions.
In fact, more than 90 percent of it gets stored in the ocean.
And now, scientists think they’ve calculated just how much the ocean has warmed in the past few decades.


A new study, out Friday in the journal Science Advances, suggests that since 1960, a staggering 337 zetajoules of energy — that’s 337 followed by 21 zeros — has been added to the ocean in the form of heat.
And most of it has occurred since 1980.
“The ocean is the memory of all of the past climate change,” said study co-author Kevin Trenberth, a senior scientist at the National Center for Atmospheric Research.
The new value is a number that significantly exceeds previous estimates, Trenberth noted.
Compared with ocean warming estimates produced by the Intergovernmental Panel on Climate Change, the new values are about 13 percent greater.
This is the result of a new methodology for estimating ocean warming, involving a series of steps “that really make this paper different than previous ones,” Trenberth told The Washington Post.

This visualization shows the locations of the ARGO buoy array over time.
When the buoys are above water, the lines are brighter; when the buoys are under water, the lines are fainter.
The ARGO buoys measure ocean salinity, column temperature, and current velocities.
This version of the visualization uses a slow camera move.
Credit: NASA/Goddard Space Flight Center Scientific Visualization Studio

In previous decades, there have been a lot of challenges associated with monitoring temperature changes in the ocean.
Before the year 2000 or so, most monitoring instruments had to be deployed from ships.
This mean that scientists only had the most reliable data for parts of the world that lie along major shipping routes.
In the past 15 years, though, scientists have developed the “Argo” network, a system of free-drifting devices that are designed to periodically adjust their buoyancy, so they can sink several thousand meters into the sea, collect measurements, and then rise back up to the surface.
There are now about 3,500 of these devices deployed throughout the world’s oceans, leading to a much better dispersal of observations.


Argo is the largest ocean research project in the world and aims to report the climatic status of the world oceans in real-time every 10 days and report the data for use by anyone, anywhere on the planet.
The global array is now in place and is reporting as planned.
Accomplishing this required the cooperation of 24 nations deploying ocean-going robots in support of the global array.
Today the Argo array is gathering more data each year from the Southern Ocean than has been acquired by the sum of all previous research in that ocean.
The data are being used for seasonal climate forecasting, ocean exploration, fisheries management and innumerable other purposes.
It can be accessed in real time by anyone who has a connection to the internet.

The new study, which was led by Lijing Cheng of the Chinese Academy of Sciences and included other scientists from that institution, from the National Center for Atmospheric Research, and from the National Oceanic and Atmospheric Administration, employs a new methodology for using both the recent Argo measurements and past observations from ships to produce a continuous series of estimates from 1960 to 2015.
The scientists incorporated an updated database of pre-Argo measurements that have been corrected for certain biases, as well as information from climate models, and extended existing observations of ocean conditions taken at specific locations to larger areas of the sea.
They then conducted a comparison of recent Argo data with measurements created using their new methodology and found that the method produces true-to-life results.

 Earth scientist Alex Gardner reveals a world of rapid change as seen through the eyes of a NASA glaciologist.
Glaciers and ice sheets hold massive amounts of freshwater locked up as ice.
These stores of freshwater feed water supplies that support millions of people around the world, raise global sea levels, and can even change the rate of Earth’s rotation.
It is now nearly certain that as Earth’s atmosphere and oceans warm over the coming centuries, glaciers and ice sheets will continue to retreat and sea levels will continue to rise.
The big question now is at what rate and by how much?

The results suggest that the ocean has been sucking up more heat than previous research has indicated.
In fact, according to Trenberth, the new estimates help explain observations of global sea-level rise that scientists have had difficulty accounting for until now.
A certain percentage of sea-level rise can be attributed to the expansion of ocean water, caused by rising water temperatures, while the rest comes from melting glaciers.
Scientists have good estimates of how much melting ice is going into the ocean, but they’ve come up a bit short in the past in trying to reconcile the rest of the planet’s observed sea-level rise with their estimates of how much the ocean has warmed in recent decades.
“This actually fills in the gap,” Trenberth said.
The study also suggests that the extra heat is not being stored evenly throughout the oceans.
The Atlantic and Southern oceans, in particular, are the biggest new heat reservoirs, the results indicate, storing about 59 percent of the heat despite accounting for less than half of all the ocean area in the world.

How can we better prepare for tropic storms or drought?
Jochem Marotzke investigates the oscillations of the atlantic currents, responsible for these extreme climatic conditions.
He can precisely predict them within a few years.

The researchers think the reason has to do with a major ocean current system known as “overturning circulation.”
This system is kind of like a giant ocean conveyor belt that runs warm water from the equator toward the poles, where it cools, sinks to the bottom of the oceans and flows back in the other direction.
The system helps transport both heat around the world, and the overturning process is pronounced in both the Atlantic and Southern ocean waters.
While the paper’s staggering new results reaffirm the importance of the ocean as a climate change buffer — without it, much of that heat would remain in the atmosphere or the earth’s land masses — it’s certainly not without consequences.
Rising ocean temperatures are believed to be a major cause of the mass coral bleaching that’s occurred all over the world over the past several years, in conjunction with an unusually strong El NiƱo beginning in 2015.

It’s still unclear how other organisms might be affected, but many marine animals thrive best within specific temperature ranges.
Many marine biologists believe that continued warming, along with other climate-related changes such as ocean acidification, may force certain species to migrate to cooler or deeper areas in the future.
Trenberth added that increasing heat moving into the surface of the ocean could also lead to “dead spots” in the ocean — places where layers of warm water get stuck on top of layers of cooler water.
When this stratification happens, it can become more difficult for the waters to mix and churn as they normally would, a process that helps stir up nutrients and oxygen that are vital to marine organisms.

All this is to say that climate change affects far more than just our air temperature — and the new study documents its clear progression in places thousands of meters below the surface of the sea.
The results also come at a sensitive point for ocean and climate research, just a week after The Washington Post revealed a proposal from the Trump administration that calls for significant budget cuts for the National Oceanic and Atmospheric Administration, including a 26 percent cut for its Office of Oceanic and Atmospheric Research.
It’s the primary research arm of NOAA, Trenberth pointed out, and such drastic cuts to the program could mean even basic observations programs like Argo may no longer continue.
“As a result, the information will not even be there,” Trenberth said “That would be tragic.”

Links :

Monday, March 13, 2017

From flight 370 hunt, new insight into Indian Ocean’s unknown depths

A 3-D image of the Diamantina Escarpment on the seafloor of the Indian Ocean.The search for Malaysia Airlines Flight 370 has helped create maps revealing the ocean floor’s topological complexity. 
Credit Kim Picard and Jonah Sullivan

From NYTimes by Nicholas St Fleur

On March 8, 2014, Malaysia Airlines Flight 370 vanished with 239 passengers and crew aboard as it crossed the Indian Ocean, triggering a large-scale search for its remains that lasted nearly three years.

 South West of Australia with the GeoGarage (AHS chart)

 As a byproduct of the tragedy, scientists have gained access to more than 100,000 square miles of seafloor mapped at a level of detail that provides a rare look at the ocean’s geological processes.
“It’s an incredible trove of data,” said Millard F. Coffin, a marine geophysicist from the Institute for Marine and Antarctic Studies at the University of Tasmania in Australia. 
“I’ve been working in this part of the Indian Ocean for 30-plus years and over many voyages in the eastern Indian Ocean I’ve never seen this level of resolution.”
Dr. Coffin worked with a group of about 10 scientists from Geoscience Australia, the national geosciences agency in Australia, to analyze data from the search. 
They were given access to high-resolution sonar information collected on ships, and data obtained by remotely operated vehicles and autonomous underwater drones. 
The information was provided by the Australian Transport Safety Bureau, which led the search.
“When we look at these data, we’re constantly keeping in mind that we wouldn’t have this data if it weren’t for a terrible tragedy,” Dr. Coffin said.
 He and his colleagues published a summary of their findings on Wednesday in the journal EOS.

 A 3-D model of the Broken Ridge along the Diamantina Escarpment. 
Credit Geoscience Australia 

Previous satellite data provided scientists with information about the Indian Ocean at a resolution of about five square kilometers, or about two square miles. 
With the instruments from the search ships, they have collected information at a resolution of meters, and in some locations they have used remote operating vehicles and underwater autonomous vehicles to gain detail on the scale of centimeters.
The search has helped create three-dimensional maps of the ocean floor that reveal its topological complexity and will allow researchers to further investigate unique features like the oceanic plateau called Broken Ridge, and its southern-flank Diamantina Escarpment
The Flight 370 search also provided information about tectonic and volcanic activity, Dr. Coffin said.
The team plans to release more detailed looks into its findings later in the year, and the full data set from the search will be made available in the middle of the year.
Walter H.F. Smith, a geophysicist with the National Oceanic and Atmospheric Administration, said the hunt for the lost jetliner highlighted how little we know about the oceans. 
In a paper that was also published Wednesday in the journal EOS, he and his colleagues explained how common unmapped areas of ocean are.

 Satellite-derived gravity field (gray) [Sandwell et al., 2014] and multibeam echo sounder (color) data were used to produce these maps of the MH370 search area in the southeast Indian Ocean.
The relief models are shown in Sun-illuminated (shaded relief) mode.
The inset map shows the MH370 search area that was mapped with multibeam echo sounding (shown in red).
This map highlights the Southeast Indian Ridge (SEIR) and the Kerguelen Plateau, and it includes estimated spreading rates of the SEIR [Argus et al., 2011], lines delineating regions of approximately equal age (isochrons [Muller et al., 2008]), and interpretations of SEIR segments (I–VII [Small et al., 1999]).
Other abbreviations are AAD, Australian-Antarctic Discordance; CIR, Central Indian Ridge; RTJ, Rodriguez Triple Junction; SWIR, Southwest Indian Ridge; WA, Western Australia.
The larger map shows details of the ocean depth mapping effort using multibeam echo sounder bathymetry data. Locations of Deep Sea Drilling Project (Leg 26) and Ocean Drilling Program (Legs 121 and 183) Sites 255, 752 to 755, 1141, and 1142 are also indicated, as are the locations of Figures 2, 3, and 4.
 Multibeam echo sounder bathymetry map of two regions of the ocean floor around the Geelvinck Fracture Zone in the Australian-Antarctic Basin south of Broken Ridge (see above for locations).
The fracture zone offsets the SEIR by about 310 kilometers. 
The right-lateral transform fault motion (a person standing on one side of the fault would see the opposite side displaced to the right) that created this fracture zone was mostly horizontal.
Note the fracture zone fault valleys, mid-ocean ridge spreading fabric, and isolated volcanoes.

“There are all kinds of things you can’t do if you don’t know the shape of the ocean bottom, or don’t know it properly,” Dr. Smith said. 
The consequences of not knowing, he said, can hinder how experts predict tsunamis, understand ocean currents, make climate forecasts, study marine life and search for missing planes.
Previous studies have suggested that only 8 percent of the world’s oceans have been mapped, meaning that a ship measured an area’s depth and recorded it in a scientific database. 
Before Flight 370’s disappearance, only 5 percent of the southeast Indian Ocean had been mapped, Dr. Smith said.
The differences in resolution between multibeam and satellite-derived bathymetry data for the northern flank of Broken Ridge are apparent here.
Numerous mass wasting features are evident, including slides and debris flows (delineated by their head scarps) that crosscut and run out as debris fans into the large semicircular depression

To figure out how often people fly over unmapped parts of the world’s oceans, 
Dr. Smith and his colleagues compared data on mapped and unmapped segments of the world’s ocean segments with a database of commercial airline routes
They found that about 60 percent of all commercial flights that cross over the ocean travel over waters with unmeasured depths.
The longest contiguous route over unmapped ocean was from Kennedy International Airport in New York to Chongqing Jiangbei International Airport in China, a journey over more than 1,200 nautical miles of unmapped ocean.
“I wanted people to realize that it’s not just Malaysia Airlines straying into the southeast Indian Ocean where it shouldn’t have been,” he said. 
“Even when your aircraft is exactly where it’s supposed to be, it might be over unknown ocean.”

Links :

New Zealand Linz layer update in the GeoGarage platform

5 nautical raster charts updated

Saturday, March 11, 2017