Not exact matches
It is entirely likely that causes such
as fluctuations in the sun's intensity and volcanic eruptions may have contributed to a
change in the global
atmospheric temperature.
Also, Ice core samples that go back
as far
as 800,000 years have
atmospheric gasses trapped within, so give a source to determine the make - up of the air, showing consistant level of carbon... directly refuting the AiG site that claimns the air has
changed.
There is also growing understanding of the links between
atmospheric problems such
as local air pollution, acid rain, global climate
change and stratospheric ozone depletion.
Combined with a decrease in
atmospheric water vapor and a weaker sun due to the most recent solar cycle, the aerosol finding may explain why climate
change has not been accelerating
as fast
as it did in the 1990s.
The new study covers the entire U.S. West, from the High Plains states to the Pacific coast, and provides the first detailed look at how groundwater recharge may
change as the climate
changes, said senior author Thomas Meixner, UA professor and associate department head of hydrology and
atmospheric sciences.
The indirect effects of rising
atmospheric carbon dioxide (CO2) levels, such
as changes in soil moisture and plant structure, can have a bigger impact on ecosystems than previously thought.
Countless additional forces — melting ice sheets, shifts in precipitation,
changes in
atmospheric and oceanic circulation, to name a few — will influence the process
as well.
That would cover seasonal
changes in climate, lakes and
atmospheric circulation vital to understanding Titan
as a whole.
Black carbon aerosols — particles of carbon that rise into the atmosphere when biomass, agricultural waste, and fossil fuels are burned in an incomplete way — are important for understanding climate
change,
as they absorb sunlight, leading to higher
atmospheric temperatures, and can also coat Arctic snow with a darker layer, reducing its reflectivity and leading to increased melting.
As the shock wave travels away from the blast, it
changes the
atmospheric pressure and creates a low - pressure trough in its wake.
Beyond basic subjects such
as climate and weather, this site from the U.K. Department of Environment, Food & Rural Affairs covers a wide range of pressing
atmospheric science issues including acid rain, air quality, climate
change, global warming and ozone depletion.
Using sophisticated
atmospheric and climate models, the researchers estimated the levels of PM2.5 directly attributable to wildfires during a recent six - year period, 2004 to 2009,
as well
as under projected future climate
change conditions (2046 - 2051).
As atmospheric CO2 levels rise, those in the oceans do too,
changing the chemistry of the seawater.
But in the case of
atmospheric pressure low - density plasma, due to the influences of
changes in the
atmospheric pressure in a plasma
as well
as around the plasma, it was difficult to accurately measure electron density.
«
As remarkable as it is that climate can change that quickly naturally, what is even more remarkable is that some of the rates of change we're experiencing today — increases in atmospheric carbon dioxide for example — are faster than anything we've been able to find in the past several million years of geologic histor
As remarkable
as it is that climate can change that quickly naturally, what is even more remarkable is that some of the rates of change we're experiencing today — increases in atmospheric carbon dioxide for example — are faster than anything we've been able to find in the past several million years of geologic histor
as it is that climate can
change that quickly naturally, what is even more remarkable is that some of the rates of
change we're experiencing today — increases in
atmospheric carbon dioxide for example — are faster than anything we've been able to find in the past several million years of geologic history.
World weather patterns will also start to
change,
as a frigid Antarctic continent and the icy ocean currents that surround it play an important role in global
atmospheric and oceanic circulation.
Gentine and his team are now exploring ways to model how biosphere - atmosphere interactions may
change with a shifting climate,
as well
as learning more about the drivers of photosynthesis, in order to better understand
atmospheric variability.
According to the study, winter flooding in the UK is set to get more severe and more frequent under the influence of climate
change as a result of a
change in the characteristics of
atmospheric rivers (ARs).
As the balloon rises in altitude, the
change in
atmospheric pressure on the balloon also
changes, and the pressure waves are larger than infrasound waves.
«When we look at this critical assembly protein, CGL71, it's
as if we are looking back in time to the era when photosynthetic apparatus had to gradually adjust to the
changing atmospheric conditions of our planet,» Grossman said.
«
As a result, some atmospheric circulations systems can not be resolved by these models, and this clearly impacts the accuracy of climate change predictions as shown in our study.&raqu
As a result, some
atmospheric circulations systems can not be resolved by these models, and this clearly impacts the accuracy of climate
change predictions
as shown in our study.&raqu
as shown in our study.»
Non-polar glacial ice holds a wealth of information about past
changes in climate, the environment and especially
atmospheric composition, such
as variations in temperature,
atmospheric concentrations of greenhouse gases and emissions of natural aerosols or human - made pollutants... The glaciers therefore hold the memory of former climates and help to predict future environmental
changes.
But it is a complicated picture: the effect that extra
atmospheric CO2 has in these kind of experimental setups might not reflect its effects in the real world, where other factors — such
as elevated heat, or
changes in precipitation — come into play.
In the North Atlantic, more heat has been retained at deep levels
as a result of
changes to both the ocean and
atmospheric circulations, which have led to the winter atmosphere extracting less heat from the ocean.
When it comes to climate
change science, researchers typically use
atmospheric carbon dioxide levels from the late 19th century
as a guideline, because that's when instrumentation was developed to accurately measure temperatures.
«These findings add to mounting evidence suggesting that there are sweet spots or «windows of opportunity» within climate space where so - called boundary conditions, such
as the level of
atmospheric CO2 or the size of continental ice sheets, make abrupt
change more likely to occur.
In the field of planetary and
atmospheric sensing, linear arrays capable of simultaneously measuring height - resolved spectral features would have a major impact on issues such
as climate
change and ozone chemistry,» explains Peter de Maagt, ESA's project manager for Star Tiger.
The researchers warn, however, that the future evolution of the AMO remains uncertain, with many factors potentially affecting how it interacts with
atmospheric circulation patterns, such
as Arctic sea ice loss,
changes in solar radiation, volcanic eruptions and concentrations of greenhouse gases in the atmosphere.
Whereas the South Pole remains protected by differing geographic,
atmospheric and oceanic conditions, the North Pole is undergoing rapid
change not seen in at least 6,000 years and perhaps
as much
as 125,000 years, and which may spread to lower latitudes.
As for the paper's conclusion that removing
atmospheric carbon is necessary in order to achieve the 2 ˚C target, climate scientist Richard Moss of the Pacific Northwest National Laboratory's Joint Global
Change Research Institute in College Park, Maryland, says that's a nearly impossible goal «with what we know about today.»
The finding opens new avenues for predicting future trends in
atmospheric nitrous oxide
as well
as in identifying climate
change mitigation actions in the Arctic, a region that is particularly sensitive to climate
change.
There are strong competing effects such
as changes in the large - scale
atmospheric circulation, sea surface temperature
changes like El Niño and La Niña and the dynamics of westerly storm tracks that all interact at the mid-latitudes,» said Stanford co-author Matthew Winnick who contributed to the study with fellow doctoral student Daniel Ibarra.
The study argued that
changes in the sun's radiation output played a major role in influencing shifts in Arctic air temperatures — a view at odds with mainstream climate science, which fingered
atmospheric carbon dioxide
as a bigger player.
There is, therefore, much current interest in how coccolithophore calcification might be affected by climate
change and ocean acidification, both of which occur
as atmospheric carbon dioxide increases.
«
Changes in ocean conditions that affect fish stocks, such
as temperature and oxygen concentration, are strongly related to
atmospheric warming and carbon emissions,» said author Thomas Frölicher, principal investigator at the Nippon Foundation - Nereus Program and senior scientist at ETH Zürich.
«We came
as close
as one can to demonstrating a direct link between climate
change and a large family of extreme recent weather events,» said Michael Mann, distinguished professor of
atmospheric science and director, Earth System Science Center, Penn State.
Study lead author Michael Raupach, GCP co-chair and
atmospheric physicist at Australia's Commonwealth Scientific and Industrial Research Organization, says it will take economic, policy and social
changes to reverse the trend, such
as capturing the CO2 emitted by coal - fired power plants and increased international cooperation.
For the study, Gentine and Lemordant took Earth system models with decoupled surface (vegetation physiology) and
atmospheric (radiative) CO2 responses and used a multi-model statistical analysis from CMIP5, the most current set of coordinated climate model experiments set up
as an international cooperation project for the International Panel on Climate
Change.
A recent trend in GCMs is to extend them to become Earth system models, that include such things
as submodels for
atmospheric chemistry or a carbon cycle model to better predict
changes in carbon dioxide concentrations resulting from
changes in emissions.
Human activities emit about two times
as much sulfur dioxide into the atmosphere, according to co-author Vitali Fioletov, an
atmospheric scientist at Environment and Climate
Change Canada in Toronto, Ontario.
The Arctic is
changing rapidly under pressure from increasing temperatures and other stressors, such
as atmospheric pollution.
Scientists are reluctant to directly link climate
change with extreme weather events such
as storms and drought, saying these fluctuate according to
atmospheric conditions, but green groups link the two in their calls for action.
«I predict that due to the loss of these
atmospheric whirlpools, the average temperature on Jupiter will
change by
as much
as 10 degrees Celsius, getting warmer near the equator and cooler at the poles,» says Marcus.
For
as much
as atmospheric temperatures are rising, the amount of energy being absorbed by the planet is even more striking when one looks into the deep oceans and the
change in the global heat content (Figure 4).
However,
atmospheric change has profoundly affected the ocean,
as well.
The effects on
atmospheric carbon levels from landuse
changes are highly uncertain,
as I'm sure Ruddiman knows.
As discussed in the Climate chapter, large - scale
atmospheric circulation patterns connected to
changes in sea - surface temperatures strongly influence natural variations in precipitation and temperature (e.g., Cayan et al. 1999; Mantua and Hare 2002).
Changes in Hadley circulation affects convection and thus
atmospheric moisture content and cloud cover which may in turn affect net solar heating
as well
as the transfer of heat from Earth to space.
Overall, studies are inconclusive
as to net impacts of
changing atmospheric chemistry and climate on seedling establishment and growth.
In addition, he praised her leadership with the National Center for
Atmospheric Research in advancing the Weather Research and Forecasting model for climate research, and in projects such
as the North American Regional Climate
Change Assessment Program,
as demonstration of her prominence in the
atmospheric and climate science community.