EARLY last year a professor of physics at James Cook University was sacked – after a successful career spanning some forty years. Peter Ridd had won many university awards, including the inaugural ‘Supervisor of the Year’, presumably nominated by one or more of his thirty-something PhD students. He published over 100 scientific papers and earned […]
The post Fake Photographs at Heart of Peter Ridd’s Sacking appeared first on Jennifer Marohasy.
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March 24, 2019 at 06:00AM
Marlo Lewis, Jr. • March 19, 2019 Yesterday I submitted comments on behalf of the Competitive Enterprise Institute supporting the Environmental Protection Agency’s proposal to dramatically scale back the agency’s 2015 rule establishing “carbon pollution” standards for new coal power plants. This post provides some quick background on EPA’s proposal and then summarizes the key…
via Watts Up With That?
March 24, 2019 at 04:04AM
The ability to recognize patterns in Earth’s behaviour by sifting through masses of geological data could be programmed into machines.
Scientists seeking to understand Earth’s inner clockwork have deployed armies of sensors listening for signs of slips, rumbles, exhales and other disturbances emanating from the planet’s deepest faults to its tallest volcanoes.
“We measure the motion of the ground continuously, typically collecting 100 samples per second at hundreds to thousands of instruments,” said Stanford geophysicist Gregory Beroza. “It’s just a huge flux of data.”
Yet scientists’ ability to extract meaning from this information has not kept pace, reports Phys.org.
The solid Earth, the oceans and the atmosphere together form a geosystem in which physical, biological and chemical processes interact on scales ranging from milliseconds to billions of years, and from the size of a single atom to that of an entire planet.
“All these things are coupled at some level,” explained Beroza, the Wayne Loel Professor in the School of Earth, Energy & Environmental Sciences (Stanford Earth). “We don’t understand the individual systems, and we don’t understand their relationships with one another.”
Now, as Beroza and co-authors outline in a paper published March 21 in the journal Science, machine-learning algorithms trained to explore the structure of ever expanding geologic data streams, build upon observations as they go and make sense of increasingly complex, sprawling simulations are helping scientists answer persistent questions about how the Earth works.
“When I started collaborating with geoscientists five years ago, there was interest and curiosity around machine learning and data science,” recalled Karianne Bergen, lead author on the paper and a researcher at the Harvard Data Science Initiative who earned her doctorate in computational and mathematical engineering from Stanford. “But the community of researchers using machine learning for geoscience applications was relatively small.”
That’s changing rapidly. The most straightforward applications of machine learning in Earth science automate repetitive tasks like categorizing volcanic ash particles and identifying the spike in a set of seismic wiggles that indicates the start of an earthquake.
This type of machine learning is similar to applications in other fields that might train an algorithm to detect cancer in medical images based on a set of examples labeled by a physician.
More advanced algorithms unlocking new discoveries in Earth science and beyond can begin to recognize patterns without working from known examples.
“Suppose we develop an earthquake detector based on known earthquakes. It’s going to find earthquakes that look like known earthquakes,” Beroza explained. “It would be much more exciting to find earthquakes that don’t look like known earthquakes.”
Beroza and colleagues at Stanford have been able to do just that by using an algorithm that flags any repeating signature in the sets of wiggles picked up by seismographs – the instruments that record shaking from earthquakes – rather than hunting for only the patterns created by earthquakes that scientists have previously catalogued.
Both types of algorithms – those with explicit labeling in the training data and those without – can be structured as deep neural networks, which act like a many-layered system in which the results of some transformation of data in one layer serves as the input for a new computation in the next layer.
Among other efforts noted in the paper, these types of networks have allowed geoscientists to quickly compute the speed of seismic waves – a critical calculation for estimating earthquake arrival times – and to distinguish between shaking caused by Earth’s natural motion as opposed to explosions.
Full article here.
via Tallbloke’s Talkshop
March 24, 2019 at 04:00AM
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March 24, 2019 at 02:30AM
Iowa Climate Science Education 