Sep 01

SPIE Commercial + Scientific Sensing & Imaging 2016

ThermoSense CFP: Thermal Infrared Applications XXXVIII Online  —  The Thermosense conference promotes worldwide exchange of information about research, uses and applications of infrared (IR) imaging technology. This includes infrared thermography and thermal infrared sensing (MWIR/LWIR), as well as NIR, SWIR … Continue reading

Sep 01

Still need Windows 98?

Legacy Hardware Support with Windows 98 Online — Is your production line still running on Windows 98? Are you still using ISA expansion cards? What will you do if there is a failure? DuroPC has the solution! DuroPC’s SHB299-98 will keep your legacy equipment running with brand-new, never refurbished, components. The Micro box chassis is small [11″ (280.2 mm) x 16.37″ (415.8 mm) x 7.77″ (197.3 mm)] and light. The unit can be mounted on a wall or on the side of an enclosure. This unit is filtered to help combat dust buildup. These units use a single board computer(SBC) … Continue reading

Aug 31

ChilliBlock Controls Cooling of Biological Samples

Asynt ChilliBlock System Isleham, UK  —  The ChilliBlock from Asynt is a new modular system purpose designed for precise, controlled cooling and heating of biological samples in microplates, vials and Eppendorf tubes. Traditionally methods of cooling biological samples often rely upon … Continue reading

Aug 30

Developing Component-Scale Hierarchical Composites Using Nanocarbons

Ammanford, UK  —  At the recent 20th International Conference on Composite Materials (ICCM), researchers from Cardiff University**, UK in conjunction with Haydale Ltd. presented the results from an in-depth study entitled ‘Developing Component-Scale Hierarchical Composites Using Nanocarbons’. The phenomenal properties … Continue reading

Aug 30

Thermal Infrared Sensors for Traffic Apps

FLIR ITS is revolutionizing how traffic flows Online  —   While video cameras are traditionally used for traffic video analysis, they need additional algorithms to overcome their inherent vulnerability to low visible light* conditions (nighttime), too much light (sun glare), … Continue reading

Aug 29

UK National Conference on Applied Radiation Metrology

10-12 November 2015 | National Physical Laboratory (NPL) Teddington, UK — The UK nuclear industry faces the challenge of decommissioning legacy nuclear sites at the same time as the construction of new plants looks increasingly likely. The science of radiation … Continue reading

Aug 29

Wireless Building Monitoring & HVAC Performance Solutions

Paragon Robotics Products Monitor Temp, RH & More CHESTERLAND OH, USA  —  Paragon Robotics data loggers utilize wireless sensors which can locally or remotely access office building information from HVAC systems, allow you to view gas/water/energy usage, or lighting and occupancy to track … Continue reading

Aug 28

NASA Science Zeros in on Ocean Rise:

How Much? How Soon?


This video describes the causes of sea level rise and how sea level has changed over the last two decades as observed by the Jason series of satellite missions.
Credits: NASA/JPL

NASA HQ  —  Seas around the world have risen an average of nearly 3 inches (76 mm) since 1992, with some locations rising more than 9 inches (229 mm) due to natural variation, according to the latest satellite measurements from NASA and its partners.

An intensive research effort now underway, aided by NASA observations and analysis, points to an unavoidable rise of several feet in the future.

Members of NASA’s new interdisciplinary Sea Level Change Team discussed recent findings and new agency research efforts during a media teleconference Tuesday at 12:30 p.m. EDT. NASA streamed the teleconference live online.

The question scientists are grappling with is how quickly will seas rise?

“Given what we know now about how the ocean expands as it warms and how ice sheets and glaciers are adding water to the seas, it’s pretty certain we are locked into at least 3 feet of sea level rise, and probably more,” said Steve Nerem of the University of Colorado, Boulder, and lead of the Sea Level Change Team.

“But we don’t know whether it will happen within a century or somewhat longer.”

Team scientists will discuss a new visualization based on 23 years of sea level data – the entire record of available satellite data — which reveals changes are anything but uniform around the globe.

The record is based on data from three consecutive satellite missions, the first a collaboration between NASA and the French space agency, Centre National d’Études Spatiales, launched in 1992.

The next in the series is Jason-3, led by the National Oceanic and Atmospheric Administration (NOAA) with participation by NASA, CNES and the European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT).

In 2013, the United Nations Intergovernmental Panel on Climate Change (IPCC) issued an assessment based on a consensus of international researchers that stated global sea levels would likely rise from 1 to 3 feet (305 to 915 mm) by the end of the century.

According to Nerem, new research available since this report suggests the higher end of that range is more likely, and the question remains how that range might shift upward.

The data reveal the height of the sea surface is not rising uniformly everywhere. Regional differences in sea level rise are dominated by the effects of ocean currents and natural cycles such as the Pacific Decadal Oscillation (PDO). But, as these natural cycles wax and wane, they can have major impacts on local coastlines.

“Sea level along the west coast of the United States has actually fallen over the past 20 years because long-term natural cycles there are hiding the impact of global warming,” said Josh Willis, an oceanographer at NASA’s Jet Propulsion Laboratory (JPL) in Pasadena, California.

“However, there are signs this pattern is changing. We can expect accelerated rates of sea level rise along this coast over the next decade as the region recovers from its temporary sea level ‘deficit.’”

Scientists estimate that about one-third of sea level rise is caused by expansion of warmer ocean water, one-third is due to ice loss from the massive Greenland and Antarctic ice sheets, and the remaining third results from melting mountain glaciers. But, the fate of the polar ice sheets could change that ratio and produce more rapid increases in the coming decades.

GRACE consists of twin co-orbiting satellites that fly in a near polar orbit separated by a distance of 220 km. GRACE precisely measures the distance between the two spacecraft in order to make detailed measurements of the Earth’s gravitational field. Since its launch in 2002, GRACE has provided a continuous record of changes in the mass of the Earth’s ice sheets.
Credits: NASA Goddard’s Scientific Visualization Studio
Download this video in HD formats from NASA Goddard’s Scientific Visualization Studio

The Greenland ice sheet, covering 660,000 square miles — nearly the area of Alaska — shed an average of 303 gigatons of ice a year over the past decade, according to satellite measurements.

The Antarctic ice sheet, covering 5.4 million square miles –larger than the United States and India combined — has lost an average of 118 gigatons a year.

“We’ve seen from the paleoclimate record that sea level rise of as much as 10 feet in a century or two is possible, if the ice sheets fall apart rapidly,” said Tom Wagner, the cryosphere program scientist at NASA Headquarters in Washington.

“We’re seeing evidence that the ice sheets are waking up, but we need to understand them better before we can say we’re in a new era of rapid ice loss.”

Although Antarctica’s contribution to sea level rise currently is much smaller than that of Greenland, recent research indicates this could change in the upcoming century. In 2014, two West Antarctica studies focused on the acceleration of the glaciers in the Amundsen Sea sector showed its collapse is underway.

East Antarctica’s massive ice sheet remains the primary unknown in sea level rise projections. Though it appears to be stable, a recent study found under a major glacier two deep troughs that could draw warm ocean water to the base of the glacier, causing it to melt.

“The prevailing view among specialists has been that East Antarctica is stable, but we don’t really know,” said glaciologist Eric Rignot of the University of California Irvine and JPL.

“Some of the signs we see in the satellite data right now are red flags that these glaciers might not be as stable as we once thought. There’s always a lot of attention on the changes we see now, but as scientists our priority needs to be on what the changes could be tomorrow.”

One of the keys to understanding future rates of ice loss is determining the role ocean currents and ocean temperatures play in melting the ice sheets from below its edges. A new six-year NASA field campaign took to the waters around Greenland this summer to probe how warming ocean waters are triggering Greenland glacier degradation.

The Oceans Melting Greenland (OMG) project is taking coastal ocean temperature measurements, observing glacial thinning at the ice’s edge, and producing the first high-resolution maps of the seafloor, fjords and canyons in the continental shelf surrounding Greenland.

NASA uses the vantage point of space to increase our understanding of our home planet, improve lives, and safeguard our future. NASA develops new ways to observe and study Earth’s interconnected natural systems with long-term data records. The agency freely shares this unique knowledge and works with institutions around the world to gain new insights into how our planet is changing.

Images and video supporting the media teleconference today are available at: http://go.nasa.gov/risingseasbriefing

Learn more about NASA’s research into sea level change at: http://www.nasa.gov/risingseas

For more information on NASA’s Earth science activities, visit: http://www.nasa.gov/earth