Sentences with phrase «in atmospheric response»
Screen J. A., C. Deser, D. M. Smith, X. Zhang, R. Blackport, P. J. Kushner, T. Oudar, K. E. McCusker and L. Sun (February 2018): Consistency and discrepancy in the atmospheric response to Arctic sea - ice loss across climate models.
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Consistency and discrepancy in the atmospheric response to Arctic sea - ice loss across climate models.
Not exact matches
Using information on how atmospheric rivers have previously behaved in response to these oscillations, they found that the quasi-biennial oscillation matters — a lot.
The researchers believe the greening is a response to higher atmospheric carbon dioxide inducing decreases in plant stomatal conductance — the measure of the rate of passage of carbon dioxide entering, or water vapor exiting, through the stomata of a leaf — and increases in soil water, thus enhancing vegetation growth.
A substantial portion of the planet is greening in response to increasing atmospheric carbon dioxide, nitrogen deposition, global warming and land use change.
E. coli cells will be genetically engineered to change color in response to conditions under study: carbon dioxide levels, atmospheric pollutants and pathogens, for example.
Paul Dirmeyer, a professor in the department of atmospheric, oceanic and earth sciences at George Mason University who was not involved in the study, notes: «Green et al. put forward an intriguing and exciting new idea, expanding our measures of land - atmospheric feedbacks from mainly a phenomenon of the water and energy cycles to include the biosphere, both as a response to climate forcing and a forcing to climate response.»
He and Abordo, a mathematics major at the time, jumped at the chance to study how plants adjust their stomata in response to different atmospheric conditions.
Consequently the global climate in these models becomes less sensitive in its response to atmospheric carbon dioxide.
«1C rise in atmospheric temperature causes rapid changes to world's largest High Arctic lake: An interdisciplinary team of scientists explores Lake Hazen's response to climate change.»
Kevin Trenberth, an atmospheric scientist at the National Center for Atmospheric Research in Colorado, gets asked the question so often about the connection between big rain events and climate change that he had this response via email: «Here we go again.»
Earth's climate may warm considerably more than expected in response to a doubling of atmospheric carbon dioxide, a new study hints.
Their results showed that changes in key water - stress variables are strongly modified by vegetation physiological effects in response to increased CO2 at the leaf level, illustrating how deeply the physiological effects due to increasing atmospheric CO2 impact the water cycle.
«Our finding that vegetation plays a key role future in terrestrial hydrologic response and water stress is of utmost importance to properly predict future dryness and water resources,» says Gentine, whose research focuses on the relationship between hydrology and atmospheric science, land / atmosphere interaction, and its impact on climate change.
«These results suggest that continuing increases in atmospheric CO2 associated with global climate change will increase both the level of Alternaria exposure and antigenicity [the ability to produce an immune response] of spores that come in contact with the airways.»
The CO2 physiological response has a dominant role in evapotranspiration and has a major effect on long - term runoff and soil moisture compared to radiative or precipitation changes due to increased atmospheric CO2.
ARM atmospheric observatories operate continuously but the facility is always changing in response to new science and user needs, and available technology.
Your statement that «Thus it is natural to look at the real world and see whether there is evidence that it behaves in the same way (and it appears to, since model hindcasts of past changes match observations very well)» seems to indicate that you think there will be no changes in ocean circulation or land use trends, nor any subsequent changes in cloud responses thereto or other atmospheric circulation.
The role of ocean — atmosphere coupling in the zonal - mean atmospheric response to Arctic sea ice loss.
Chen, K., Gawarkiewicz, G. G., Lentz, S. J. & Bane, J. M. Diagnosing the warming of the Northeastern US Coastal Ocean in 2012: a linkage between the atmospheric jet stream variability and ocean response.
The climate sensitivity classically defined is the response of global mean temperature to a forcing once all the «fast feedbacks» have occurred (atmospheric temperatures, clouds, water vapour, winds, snow, sea ice etc.), but before any of the «slow» feedbacks have kicked in (ice sheets, vegetation, carbon cycle etc.).
The atmospheric circulation response seems to be sensitive to the magnitude and geographic pattern of sea - ice loss and, in some cases, to the background climate state.
Blackport, R. & Kushner, P. J. Isolating the atmospheric circulation response to Arctic sea ice loss in the coupled climate system.
The seasonal atmospheric response to projected sea ice loss in the late twenty - first century.
Seasonal atmospheric responses to reduced Arctic sea ice in an ensemble of coupled model simulations.
Predictions of the climate's development in response to elevated atmospheric CO2 levels started in earnest over 25 years ago.
[Response: You may also be interested in the article by Richard Feely and colleagues, Impact of Anthropogenic CO2 on the CaCO3 System in the Oceans arguing that quite apart from any climate impact from atmospheric CO2, there is a much more direct impact from the dissolution of CO2 in the world's oceans.
Here, we analyze a 28 - year record of tropical flower phenology in response to anthropogenic climate and atmospheric change.
Alexander, M.A., et al., 2004: The atmospheric response to realistic Arctic sea ice anomalies in an AGCM during winter.
«We know rather little about how much methane comes from different sources and how these have been changing in response to industrial and agricultural activities or because of climate events like droughts,» says Hinrich Schaefer, an atmospheric scientist at the National Institute of Water and Atmospheric Research (NIWA) in New Zealand, who collaborates with Petrenko.
Hu, A.X., G.A. Meehl, W.M. Washington, and A. Dai, 2004: Response of the Atlantic thermohaline circulation to increased atmospheric CO2 in a coupled model.
Wood, R.A., A.B. Keen, J.F.B. Mitchell, and J.M. Gregory, 1999: Changing spatial structure of the thermohaline circulation in response to atmospheric CO2 forcing in a climate model.
Stouffer, R.J., and S. Manabe, 2003: Equilibrium response of thermohaline circulation to large changes in atmospheric CO2 concentration.
Webb will reveal the interplay of chemistry and atmospheric dynamics in response to the shift of Titan's seasons.
Gregory, J.M., et al., 2005: A model intercomparison of changes in the Atlantic thermohaline circulation in response to increasing atmospheric CO2 concentration.
«We find this fingerprint both in a high - resolution climate model in response to increasing atmospheric carbon dioxide concentrations, and in the temperature trends observed since the late nineteenth century.»
[Response: I agree that there are serious problems with the representation of atmospheric feedbacks in the model, but the lack of a fourth - power dependence in infrared emission vs T is not the key one them.
In the tropical Pacific, the distance from Indonesia to South America and the way tropical winds push warm water west combine to allow special waves to travel along the equator and are amplified by the atmospheric wind response to produce large fluctuations in temperatures (up to 3 degrees Celsius) in the Eastern Pacific that last for monthIn the tropical Pacific, the distance from Indonesia to South America and the way tropical winds push warm water west combine to allow special waves to travel along the equator and are amplified by the atmospheric wind response to produce large fluctuations in temperatures (up to 3 degrees Celsius) in the Eastern Pacific that last for monthin temperatures (up to 3 degrees Celsius) in the Eastern Pacific that last for monthin the Eastern Pacific that last for months.
In response to the board's decision, three plaintiffs — a retired high - school math teacher, a professor of atmospheric science at the University of Washington, and a mother of a high - school student — filed suit, calling the Discovering series deficient and dumbed down.
This page outlines a map of assessment through the unit, including skill based questions, short writing responses and extended writing responses including essays.The atmospheric system, including the natural greenhouse effect and energy balance (incoming shortwave radiation and outgoing long wave radiation) Changes in the global energy balance, and the role of feedback loops, resulting from: Glossary - Student should make...
It feels nothing short of rabid in a straight line, with the kind of throttle response that only ever comes from a big, atmospheric engine that revs high and hits hard, everywhere.
Constant upstream air pressure, atmospheric for naturally aspirated and higher for turbocharged engines, together with the extremely fast air mass control, cylinder - by - cylinder and stroke - by - stroke, result in a superior dynamic engine response.
Lisa Grossman's oil paintings of the wide open rural eastern Kansas, painted en plein air (or on location), are a meditation on open spaces, exploring the emotional responses to atmospheric shifts in light, color, and the vast distance of land and sky.
[Response: The ratio is not constant in time, because aerosols have a much shorter perturbation time on atmospheric composition than CO2.
The climate sensitivity classically defined is the response of global mean temperature to a forcing once all the «fast feedbacks» have occurred (atmospheric temperatures, clouds, water vapour, winds, snow, sea ice etc.), but before any of the «slow» feedbacks have kicked in (ice sheets, vegetation, carbon cycle etc.).
[Response: You may also be interested in the article by Richard Feely and colleagues, Impact of Anthropogenic CO2 on the CaCO3 System in the Oceans arguing that quite apart from any climate impact from atmospheric CO2, there is a much more direct impact from the dissolution of CO2 in the world's oceans.
Since the climate response to the North Atlantic SST anomalies is primarily forced at the low latitudes and the AWP is in the path of or a birthplace for Atlantic tropical cyclones, the influence of the AMO on Atlantic tropical cyclone activity may operate through the mechanism of the AWP - induced atmospheric changes.
Presumably the water vapour feedback in models is dealt with by determining / estimating / calculating the radiative forcing from water vapour and then making some assumption about the water vapour response to atmospheric warming (e.g. assuming constant relative humidity).
The other challenge we readily acknowledge is that Arctic amplification has only emerged from the noise of natural variability within the last decade or so (strongest in fall and winter, weakest in summer), thus finding a statistically robust atmospheric response in the real world is not easy.
For example, they describe the unexpectedly high amounts of beetle herbivory in soybeans in response to elevated atmospheric carbon dioxide, as evidenced by FACE experiments.