Sentences with phrase «study sheet by»
Students can begin to learn about President Barack Obama with this vocabulary study sheet by reading each of the terms related to the president and its corresponding description.
https://www.thoughtco.com/ Not exact matches
It uses step - by - step how - to, sidebars, examples, case studies, expert interviews, and tip sheets to show you how, from setup to strategy, you can use Pinterest for your promotional, branding, and marketing objectives.
«I almost always start my analysis of a company by studying its balance sheet.
«The widespread loss of Antarctic ice shelves, driven by a warming ocean or warming atmosphere, could spell disaster for our coastlines — and there is sound geological evidence that supports what the models are telling us,» said Robert M. DeConto of the University of Massachusetts Amherst, a co-author of the study and one of the developers of the ice - sheet model used.
Scientists may also become able to distinguish between different scenarios sooner by studying the physics of local ice - sheet changes and refining reconstructions of changes during warm periods in geological history.
A recent study (pdf format) found that the West Antarctic ice sheet would probably collapse if sea temperatures rose by more than 5 °C.
Recent modelling by researchers from the Potsdam Institute for Climate Impact Research in Germany, as well as studies of past climate, suggest that the planet will soon have warmed enough to melt Greenland's ice sheet entirely — if it hasn't already become warm enough.
Providing women who take a powerful acne drug with a fact sheet about contraception while visiting the dermatologist can significantly improve their awareness of the most effective birth control options and may prevent unintended pregnancies and birth defects that can be caused by the drug, according to a University of Pittsburgh School of Medicine study published Feb. 4 in the journal JAMA Dermatology.
Using NASA and European Space Agency satellites, the 2015 study had measured the changing height of the ice sheet and determined that East Antarctica was ballooning upward by roughly 1.59 centimeters a year (at least from 1992 to 2001 and from 2003 to 2008).
Another alternative has been suggested by glaciologist Slawek Tulaczyk of the University of California, Santa Cruz, who studies west Antarctica's Whillans Ice Sheet, among other glaciers.
A recent study by Robert Kopp at Princeton University (Nature, DOI: 10.1038 / nature08686) suggests sea levels were 8 to 9 metres higher than now during the last interglacial, in part due to the west Antarctic ice sheet melting.
The paper also describes an atmosphere - ocean modeling study of feedback loops caused by ice sheet melting under 2 °C conditions.
In one recent study, they obtained good results by incorporating ruthenium ions into a sheet - like nanostructure composed of carbon nitride.
A new study by David Sugden at the University of Edinburgh, UK, and colleagues suggests the ice sheet may be more stable than we thought.
Studies by glaciologist Eric Rignot of the University of California, Irvine and others suggest that ice sheets could melt faster than scientists initially thought.
The other study in Nature — led by Joerg Schaefer of Lamont - Doherty Earth Observatory and Columbia University, and colleagues — looked at a small sample of bedrock from one location beneath the middle of the existing ice sheet and came to what appears to be a different conclusion: Greenland was nearly ice - free for at least 280,000 years during the middle Pleistocene — about 1.1 million years ago.
«The strong impact of ocean onto Antarctic ice sheet dynamics, or the knowledge that we have about it, is reinforced by our study,» said lead study author Hannes Konrad of the University of Leeds in an interview with E&E News.
Antarctica's great ice sheet is losing ground as it is eroded by warm ocean water circulating beneath its floating edge, a new study has found.
However, a new study from a team of researchers led by University of Wisconsin - Madison Space Science and Engineering Center scientist, Claire Pettersen, describes a unique method involving cloud characteristics that could help answer some big questions about the Greenland Ice Sheet and its snowfall.
In more recent studies the universe appears as a collection of giant bubble - like voids separated by sheets and filaments of galaxies, with the superclusters appearing as occasional relatively dense nodes.
David Ullman, a postdoctoral researcher at Oregon State University and lead author on the study, said there are two mechanisms through which ice sheets diminish — dynamically, from the jettisoning of icebergs at the fringes, or by a negative «surface mass balance,» which compares the amount of snow accumulation relative to melting.
A new study led by the University of Texas Institute for Geophysics has found that wind over the ocean off the coast of East Antarctica causes warm, deep waters to upwell, circulate under Totten Ice Shelf, and melt the fringes of the East Antarctic ice sheet from below.
By combining satellite images of the ice sheet and wind stress data from observations and computer modeling, Greene and his collaborators were able to study the chain of events that brings the warm water to Totten.
The sediment cores used in this study cover a period when the planet went through many climate cycles driven by variations in Earth's orbit, from extreme glacial periods such as the Last Glacial Maximum about 20,000 years ago, when massive ice sheets covered the northern parts of Europe and North America, to relatively warm interglacial periods with climates more like today's.
The international research initiative IceGeoHeat led by the GFZ German Research Centre for Geosciences establishes in the current online issue of Nature Geoscience that this effect can not be neglected when modeling the ice sheet as part of a climate study.
Researchers at Umeå University, together with researchers at Uppsala University and Stockholm University, show in a new study how nitrogen doped graphene can be rolled into perfect Archimedean nano scrolls by adhering magnetic iron oxide nanoparticles on the surface of the graphene sheets.
The team in today's study were able to determine that the ice sheet had partially melted during this «stable» period by analysing the chemical content of mud in sediments.
Altogether, the new study suggests that the ice sheet has the potential to raise global sea levels by about 24.3 feet, should it melt entirely.
A new study by scientists at NASA's Jet Propulsion Laboratory (JPL) in Pasadena, California, and the University of California, Irvine, shows that while ice sheets and glaciers continue to melt, changes in weather and climate over the past decade have caused Earth's continents to soak up and store an extra 3.2 trillion tons of water in soils, lakes and underground aquifers, temporarily slowing the rate of sea level rise by about 20 percent.
In the study, researchers analyzed a series of transient Coupled General Circulation Model simulations forced by changes in greenhouse gases, orbital forcing, meltwater discharge and the ice - sheet history throughout the past 21,000 years.
Looking to solve this problem on its manned and unmanned aircraft, the U.S. Air Force will by the end of the year to kick off an 18 - month study of the use of carbon nanotube sheets to create a shielding layer on the surfaces of lightweight composites.
Gerhard Kuhn, co-author of the study, said, «Our results provide evidence that in the past, [West Antarctic Ice Sheet -RCB- retreat was also predominantly caused by melting through warm ocean water.»
The study, co-authored by Dr Thomas Stevens, from the Department of Geography at Royal Holloway, University of London, found a previously unknown mechanism by which the joining of North and South America changed the salinity of the Pacific Ocean and caused major ice sheet growth across the Northern Hemisphere.
«Based on the likely location of ice deposits during this period of Mars» history, and the amount of meltwater that could have been produced by Lyot ejecta landing on an ice sheet, we think this is the most plausible scenario for the formation of these valleys» said David Weiss, a recent Ph.D. graduate from Brown and the study's lead author.
Even if we could freeze - frame the atmosphere as it is today, sea levels would still rise by 25 metres, says the latest study into the effects of climate change on melting ice sheets.
A new study combines the latest observations with an ice sheet model to estimate that melting ice on the Antarctic ice sheet is likely to add 10 cm to global sea levels by 2100, but it could be as much as 30 cm.
While some earlier studies, using different approaches, have posited that Antarctic ice sheets could add as much as a metre to sea levels by 2100, this new evidence suggests ice loss on this scale is «implausible», the paper says.
A 2008 study led by James Hansen found that climate sensitivity to «fast feedback processes» is 3 °C, but when accounting for longer - term feedbacks (such as ice sheet disintegration, vegetation migration, and greenhouse gas release from soils, tundra or ocean), if atmospheric CO2 remains at the doubled level, the sensitivity increases to 6 °C based on paleoclimatic (historical climate) data.
This study links a framework for global and local sea - level rise projections with simulations of two major mechanisms by which climate change can affect the vast Antarctic ice sheet.
It is important to regard the LGM studies as just one set of points in the cloud yielded by other climate sensitivity estimates, but the LGM has been a frequent target because it was a period for which there is a lot of data from varied sources, climate was significantly different from today, and we have considerable information about the important drivers — like CO2, CH4, ice sheet extent, vegetation changes etc..
One recent modeling study focused on this mode of instability estimated that the Antarctic ice sheet has a 1 - in - 20 chance of contributing about 30 centimeters (1.0 feet) to global average sea - level rise over the course of this century and 72 centimeters (2.4 feet) by the end of the next century.
However, in the new study, when the researchers looked at Sup35 surrounded by other cellular proteins, they found that the intrinsically disordered region actually does take on a regular structure, which they believe to be beta sheets.
The long timescales (even ignoring the «Earth system» responses like ice sheets and vegetation) are not easy to get at in the instrumental record or by studying «abrupt forcing» events like volcanic eruptions.
Model studies for climate change between the Holocene and the Pliocene, when Earth was about 3 °C warmer, find that slow feedbacks due to changes of ice sheets and vegetation cover amplified the fast feedback climate response by 30 — 50 % [216].
October 26, 2015 Sheet music for creating the artificial sense of touch A new study led by neuroscientists from the University of Chicago brings us one step closer to building prosthetic limbs for humans that re-create a sense of touch through a direct interface with the brain.
A new study shows clouds are playing a larger role in heating the Greenland Ice Sheet than scientists previously believed, raising its temperature by 2 to 3 degrees compared to cloudless skies.
The study, which was carried out by dating site EliteSingles, looked at anonymous user data to see how much New Zealand singles value time spent between the sheets.
The study, which was carried out by dating site EliteSingles, aimed to discover how much value Canadian singles assign to time spent between the sheets.
After studying this chapter, you will be able to: Explain the basic nature of a joint stock company as a form of business organisation and the various kinds of companies based on liability of their members Describe the types of shares issued by a company Explain the accounting treatment of shares issued at par, at premium and at discount including oversubsription Outline the accounting for forfeiture of shares and reissue of forfeited shares under varying situations Workout the amounts to be transferred to capital reserve when forfeited shares are reissued; and prepare share forfeited account State the meaning of debenture and explain the difference between debentures and shares Describe various types of debentures; Record the journal entries for the issue of debentures at par, at a discount and at premium Explain the concept of debentures issued for consideration other than cash and the accounting thereof Explain the concept of issue of debentures as a collateral security and the accounting thereof Show the items relating to issue of debentures in company's balance sheet Describe the methods of writing - off discount / loss on issue of debentures Explain the methods of redemption of debentures and the accounting thereof Explain the concept of sinking fund, its use for redemption of debentures and the accounting thereof Topic List Features of a Company Kinds of Companies Share Capital of a Company Nature and Classes of Shares Issue of Shares Accounting Treatment Forfeiture of Shares Meaning of Debentures Types of Debentures Issue of Debentures Over Subscription Terms of Issue of Debentures Interest on Debentures Writing - off Discount / Loss on Issue of Debentures Redemption of Debentures Redemption by Payment in Lump Sum Sinking Fund Method
Relevant for Exams in Religious Studies till June 2017 Colleagues can cover the syllabus through revision using this knowledge organiser This is condensed so can save on printing by printing two pages per sheet and can also be used as a desk help sheet These Knowledge organisers have been used and I have received positive feedback from colleagues and pupils.