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CU students reach big carbon neutrality goal
Feb 16th
FACILITIES REACH CARBON NEUTRALITY
The University of Colorado Student Government has reduced the net emissions of greenhouse gases, or GHGs, from its student-run facilities to zero after committing in 2007 to reach carbon neutrality.
CUSG operates three large CU-Boulder facilities including the University Memorial Center, Student Recreation Center and Wardenburg Health Center.
“We are very proud of this accomplishment,” said CUSG Vice President Carly Robinson. “It’s a reflection of our sustainability-minded campus community and the impressive resources we have on hand to be more environmentally friendly, and even save money, by implementing green strategies.”
CU-Boulder students will gather for a “Getting to Carbon Neutrality” forum on Friday, Feb. 17, from 10 a.m. to 2 p.m. in the Aspen Room of the University Memorial Center. They will discuss the campus’s carbon neutrality achievements and remaining challenges with input from a panel of CU staff. The event is open to CU students but requires pre-registration at http://ecenter.colorado.edu/carbonneutrality.
More than 9,000 metric tons of GHG emissions attributed to operating the student-run buildings have been eliminated through renewable energy generation, energy conservation measures and carbon-offset strategies implemented by CUSG. Carbon neutrality was reached even as square footage and usage of the facilities increased in recent years.
CUSG partnered with Facilities Management to install additional solar panels on CU facilities that contribute roughly 72,000 kilowatt-hours of energy per month to the electricity grid — enough to power about 80 houses. This renewable energy generation replaces a portion of the energy generated by traditional systems that emit GHGs.
CUSG buildings also have been renovated with better insulation and sealing technologies, more efficient lighting and windows. These upgrades reduced the buildings’ total energy consumption by nearly 15 percent over the last five years.
CUSG also has worked with Colorado communities on carbon reduction projects as a way to offset GHG emissions from CUSG buildings. The projects provide educational, economic development and social equity benefits for the state.
One of the projects includes solar thermal system installations, used to heat water, for low-income housing in Loveland, Colo.
Two years ago, the CUSG helped support the installation of a system that converts methane gas from the Larimer County Landfill in Fort Collins, Colo., into energy. Methane gas is a potent GHG emission.
Recently, CUSG contracted with Native Energy — a carbon offsets program provider — to support a novel kiln system used by Commercial Brick Corp., an Oklahoma brick manufacturer. The kiln system is powered by methane gas captured from a nearby landfill. It prevents methane emissions and replaces fossil fuel use. The company, which will participate in the Feb. 17 forum, provides 200 jobs and produces 144 million bricks per year sold in 15 states.
The CU Environmental Center coordinated the carbon neutrality effort. The center administers grants and loan programs within CUSG facilities that have helped fund energy conservation projects, delivering over $1.6 million in energy cost savings for CUSG over the last five years while driving down GHG emissions.
CU Boulder prof gets MAJOR cred
Feb 9th
National Academy of Engineering
Diane McKnight, professor of civil, environmental and architectural engineering and a fellow of the Institute of Arctic and Alpine Research at the University of Colorado Boulder, has been elected to the National Academy of Engineering.
McKnight is among 66 new members and 10 foreign associates of the academy announced today. She joins 16 other faculty from the campus who have been elected since the academy’s formation in 1962.
Election to the National Academy of Engineering is among the highest professional distinctions accorded an engineer. Academy membership honors those who have made outstanding contributions to “engineering research, practice or education” and to the “pioneering of new and developing fields of technology, making major advancements in traditional fields of engineering, or developing/implementing innovative approaches to engineering education.”
McKnight was recognized for making clear the interrelationship between natural organic matter and heavy metals in streams and lakes.
Her research expertise is in the interactions between freshwater biota, trace metals, and natural organic material in diverse freshwater environments, including lakes and streams in the Colorado Rocky Mountains and in the McMurdo Dry Valleys in Antarctica.
In the Rocky Mountains, she has focused on the impact of metal contamination in acid mine drainage streams and the influence of climate change and nitrogen deposition on alpine lakes and wetlands. McKnight has interacted with many state and local groups involved in mine drainage and watershed issues in the Rocky Mountains.
“Diane is a worldwide leader in the interactive effect of metals in our water system with natural organic matter,” said Professor Ross Corotis, who was dean of the College of Engineering and Applied Science when McKnight joined the faculty and the Institute of Arctic and Alpine Research in 1996. “In addition to her advanced research for protecting environments from the Antarctic to the Rocky Mountains, she is a leader in developing books for children to help them learn about the water cycle.”
McKnight has been working in Antarctica since 1987, and is a leading investigator studying extreme life at the McMurdo Dry Valleys Long Term Ecological Research site funded by the National Science Foundation. In the harsh polar environment, stream channels flow only a few weeks out of the year and the only life forms inhabiting the area are microorganisms, mosses, lichens and a few groups of invertebrates.
She wrote and published a children’s book, “The Lost Seal,” in 2006, that tells the true story of a wayward seal discovered near the research camp in 1990 and its eventual rescue. The story gives children an understanding of Antarctica’s extreme environment and the work of scientists there.
She earned three degrees from the Massachusetts Institute of Technology, including a bachelor’s degree in mechanical engineering in 1975, a master’s degree in civil engineering in 1978 and a doctorate in environmental engineering in 1979.
She was a research hydrologist with the U.S. Geological Survey’s National Research Program for 17 years before she came to CU-Boulder. She was named a fellow of the American Geophysical Union in 2004 and of the American Association for the Advancement of Science in 2009.
She is a former member of the National Research Council’s Water Science and Technology Board and Polar Research Board, and she received a Meritorious Service Award from the U.S. Geological Survey in 1995.
Other CU-Boulder faculty who have been elected to the National Academy of Engineering, and their years of election, are: Bernard Amadei, 2008; George Born and Kaspar Willam, 2004; Ross Corotis and Fred Glover, 2002; Frank Barnes, 2001; Delores Etter, 2000; Martin Mikulas, 1999; Valerian Tatarskii, elected a foreign associate in 1994; Earl Gossard, 1990; Don Hearth and Richard Strauch, 1989; Jacques Pankove, 1986; Richard Seebass (deceased), 1985; Klaus Timmerhaus (deceased), 1975; and Max Peters (deceased), 1969.
CU study: Glacial ice disappearing at record clip
Feb 8th
caps shedding billions of tons of mass annually
Earth’s glaciers and ice caps outside of the regions of Greenland and Antarctica are shedding roughly 150 billion tons of ice annually, according to a new study led by the University of Colorado Boulder.
The research effort is the first comprehensive satellite study of the contribution of the world’s melting glaciers and ice caps to global sea level rise and indicates they are adding roughly 0.4 millimeters annually, said CU-Boulder physics Professor John Wahr, who helped lead the study. The measurements are important because the melting of the world’s glaciers and ice caps, along with Greenland and Antarctica, pose the greatest threat to sea level increases in the future, Wahr said.
The researchers used satellite measurements taken with the Gravity Recovery and Climate Experiment, or GRACE, a joint effort of NASA and Germany, to calculate that the world’s glaciers and ice caps had lost about 148 billion tons, or about 39 cubic miles of ice annually from 2003 to 2010. The total does not count the mass from individual glacier and ice caps on the fringes of the Greenland and Antarctic ice sheets — roughly an additional 80 billion tons.
“This is the first time anyone has looked at all of the mass loss from all of Earth’s glaciers and ice caps with GRACE,” said Wahr. “The Earth is losing an incredible amount of ice to the oceans annually, and these new results will help us answer important questions in terms of both sea rise and how the planet’s cold regions are responding to global change.”
A paper on the subject is being published in the Feb. 9 online edition of the journal Nature. The first author, Thomas Jacob, did his research at CU-Boulder and is now at the Bureau de Recherches Géologiques et Minières, in Orléans, France. Other paper co-authors include Professor Tad Pfeffer of CU-Boulder’s Institute of Arctic and Alpine Research and Sean Swenson, a former CU-Boulder physics doctoral student who is now a researcher at the National Center for Atmospheric Research in Boulder.
“The strength of GRACE is that it sees everything in the system,” said Wahr. “Even though we don’t have the resolution to look at individual glaciers, GRACE has proven to be an exceptional tool.” Traditional estimates of Earth’s ice caps and glaciers have been made using ground-based measurements from relatively few glaciers to infer what all of the unmonitored glaciers around the world were doing, he said. Only a few hundred of the roughly 200,000 glaciers worldwide have been monitored for a decade or more.
Launched in 2002, two GRACE satellites whip around Earth in tandem 16 times a day at an altitude of about 300 miles, sensing subtle variations in Earth’s mass and gravitational pull. Separated by roughly 135 miles, the satellites measure changes in Earth’s gravity field caused by regional changes in the planet’s mass, including ice sheets, oceans and water stored in the soil and in underground aquifers.
A positive change in gravity during a satellite approach over Greenland, for example, tugs the lead GRACE satellite away from the trailing satellite, speeding it up and increasing the distance between the two. As the satellites straddle Greenland, the front satellite slows down and the trailing satellite speeds up. A sensitive ranging system allows researchers to measure the distance of the two satellites down to as small as 1 micron — about 1/100 the width of a human hair — and to calculate ice and water amounts from particular regions of interest around the globe using their gravity fields.
For the global glaciers and ice cap measurements, the study authors created separate “mascons,” large, ice-covered regions of Earth of various ovate-type shapes. Jacob and Wahr blanketed 20 regions of Earth with 175 mascons and calculated the estimated mass balance for each mascon.
The CU-led team also used GRACE data to calculate that the ice loss from both Greenland and Antarctica, including their peripheral ice caps and glaciers, was roughly 385 billion tons of ice annually. The total mass ice loss from Greenland, Antarctica and all Earth’s glaciers and ice caps from 2003 to 2010 was about 1,000 cubic miles, about eight times the water volume of Lake Erie, said Wahr.
“The total amount of ice lost to Earth’s oceans from 2003 to 2010 would cover the entire United States in about 1 and one-half feet of water,” said Wahr, also a fellow at the CU-headquartered Cooperative Institute for Research in Environmental Sciences.
The vast majority of climate scientists agree that human activities like pumping huge amounts of greenhouse gases in the atmosphere is warming the planet, an effect that is most pronounced in the polar regions.
One unexpected study result from GRACE was that the estimated ice loss from high Asia mountains — including ranges like the Himalaya, the Pamir and the Tien Shan — was only about 4 billion tons of ice annually. Some previous ground-based estimates of ice loss in the high Asia mountains have ranged up to 50 billion tons annually, Wahr said.
“The GRACE results in this region really were a surprise,” said Wahr. “One possible explanation is that previous estimates were based on measurements taken primarily from some of the lower, more accessible glaciers in Asia and were extrapolated to infer the behavior of higher glaciers. But unlike the lower glaciers, many of the high glaciers would still be too cold to lose mass even in the presence of atmospheric warming.”
“What is still not clear is how these rates of melt may increase and how rapidly glaciers may shrink in the coming decades,” said Pfeffer, also a professor in CU-Boulder’s civil, environmental and architectural engineering department. “That makes it hard to project into the future.”
According to the GRACE data, total sea level rise from all land-based ice on Earth including Greenland and Antarctica was roughly 1.5 millimeters per year annually or about 12 millimeters, or one-half inch, from 2003 to 2010, said Wahr. The sea rise amount does include the expansion of water due to warming, which is the second key sea-rise component and is roughly equal to melt totals, he said.
“One big question is how sea level rise is going to change in this century,” said Pfeffer. “If we could understand the physics more completely and perfect numerical models to simulate all of the processes controlling sea level — especially glacier and ice sheet changes — we would have a much better means to make predictions. But we are not quite there yet.”