«Our study is the first example of
how atmospheric measurements can help to check on fossil fuel CO2 emissions over an area large enough to encompass nations, provinces or states.»
Not exact matches
New
measurements of
atmospheric loss by NASA's MAVEN probe should help scientists determine
how a planet with rushing water and a temperate climate a few billion years ago transformed into a cold, dry desert.
New
measurements by NASA's Goddard Institute for Space Studies indicate that 2012 was the ninth warmest year since 1880, and that the past decade or so has seen some of the warmest years in the last 132 years.One way to illustrate changes in global
atmospheric temperatures is by looking at
how far temperatures stray from «normal», or a baseline.
Results: When it comes to understanding
how atmospheric particles affect climate, one
measurement can't tell the whole story, especially in areas that haven't been studied.
Find out
how researchers are using data from U.S. Department of Energy's
Atmospheric Radiation
Measurement (ARM) Climate Research Facility — the world's most comprehensive outdoor laboratory and data archive for research related to
atmospheric processes that affect Earth's climate — to improving regional and global climate models.
Find out
how researchers are using data from the U.S. Department of Energy's
Atmospheric Radiation
Measurement (ARM) Climate Research Facility — the world's most comprehensive outdoor laboratory and data archive for research related to
atmospheric processes that affect Earth's climate — to improve earth system models.
As NOAA's Mauna Loa
measurement of
atmospheric methane concentrations are only currently increasing at a rate of approximately 0.25 % per year (or 12.5 % change in 50 - years);
how could anyone be concerned that the change in
atmospheric methane burden in 50 - years could be 300 % (as per Isaken et al (2011) case 4XCH4; which would require an additional 0.80 GtCH4 / yr of methane emissions on top of the current rate of methane emissions of 0.54 GtCH4 / yr)?
Mike's work, like that of previous award winners, is diverse, and includes pioneering and highly cited work in time series analysis (an elegant use of Thomson's multitaper spectral analysis approach to detect spatiotemporal oscillations in the climate record and methods for smoothing temporal data), decadal climate variability (the term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth of GFDL showing evidence in both climate model simulations and observational data for a 50 - 70 year oscillation in the climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing
how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in
atmospheric chemistry (an analysis of beryllium - 7
measurements).
The standard logbook entries made at the time contain no information about
how the
measurements were taken, so the cause was overlooked, says David Thompson, first author on the paper and an
atmospheric scientist at Colorado State University in Fort Collins.
Historical temperature time series and series of
atmospheric carbon dioxide
measurements show clearly
how climate has changed over the past 100 years.
Even if we could discriminate between human - originated CO2 and natural CO2 isotopically with reliability I don't see
how carbon isotope
measurements could prove we have increased
atmospheric CO2 by 40 % anyway (or 110ppm) because, problematically, CO2 has a very short
atmospheric residence time.
Also, given the
atmospheric CO2
measurements at South Pole range between 246.59ppm - 521.48 ppm I don't see
how the trapped CO2 in the ice - core bubbles could accurately represent the back - ground level.
It's early days, but this first real - world
measurement of a slowdown in the ocean's ability to dissolve carbon could have worrying implications for those currently thinking about
how to stabilize
atmospheric greenhouse levels.
Also, while we have good
atmospheric measurements of other key greenhouse gases such as carbon dioxide and methane, we have poor
measurements of global water vapor, so it is not certain by
how much
atmospheric concentrations have risen in recent decades or centuries, though satellite
measurements, combined with balloon data and some in - situ ground
measurements indicate generally positive trends in global water vapor.»
When we analysed the
atmospheric water concentration
measurements for the balloons, we found that the different slopes in Region 3 depended on
how humid the air in the region was, and whether or not the balloon was travelling through any clouds or rain.
Carrying out
atmospheric measurements often entails having to consider
how representative
measurements taken in a single location are, and whether local conditions, such as landforms, affect observations.
It is now contributing to
atmospheric (carbon dioxide) concentration,» he said.Using a one million sq. km stretch of forest in Manitoba, Gower and his colleagues coupled their
measurements of
how carbon moved between the atmosphere and the trees with past records and computer models to examine
how the forest's ability to store carbon dioxide has changed since mid-century.
Moreover, since DLR varies widely according to
atmospheric conditions, it is very important to achieve enough coverage to be sure that we understand
how the localized
measurements can be generalized to the global scale.
The standard logbook entries made at the time contain no information about
how the
measurements were taken, so the cause was overlooked, says David Thompson, first author on the paper and an
atmospheric scientist at the State University of Colorado in Boulder.
Currently, many observing systems capture elements of
how climate is changing, such as direct
measurements of
atmospheric and ocean temperature.