Sentences with phrase «changing forcing agents»

Forcings, measured in W / m2 averaged over the globe, are imposed perturbations of Earth's energy balance caused by changing forcing agents such as solar irradiance and human - made greenhouse gases (GHGs).

Not exact matches

Betty didn't believe there was any spiritual force in the universe and that the only agent of change capable of making the world a better place was the people who live here.
The Leicester City goalkeeper is said to be changing agents this week to join forces with Luca Bascherini, as reported by The Sun, with the Italian representative having strong links with Old Trafford.
Gravity is a long - range force and is the primary agent of the radical changes in a galaxy's structure when another galaxy comes close to it.
The new method provides excellent comparisons of the forcing agents for a wide range of changes.
It concludes with the following, «The Sun still appears to be the main forcing agent in global climate change».
The team increased one forcing agent (see sidebar) in a climate model, for example carbon dioxide, and decreased another, say methane, so that global mean temperature didn't change.
Figure 5: Contributions of individual forcing agents to the total change in the decadal average temperature for three time periods.
Figure 4: Contributions of individual forcing agents to the total decadal temperature change for three time periods.
We follow in almost real time a handful of individuals forced to make split - second decisions after this incomprehensible event that would change their lives and forever alter our world's landscape: the young doctors and nurses at Parkland Hospital, the chief of the Dallas Secret Service, the unwitting cameraman who captured what has become the most watched and examined film in history, the FBI Agents who had gunman Lee Harvey Oswald within their grasp and Vice President Lyndon Johnson who had to take control of a country in a moment's notice.
We need to support the emergence of more alpha authorizers, those who are independent of the K — 12 system and have the courage and tenacity to serve as change agents, market makers, and forces for quality, while reliably performing the core functions of authorizing mentioned above.
Bragg found that the videos were having a direct impact on the young people making them — forcing many to reflect on their own lives and communities, and to become agents of change within their communities.
Some conservatives believe they are being forced to support a broader set of social issues and embrace strategies or tactics they do not agree with as a litmus test to determine whether they are true change agents in education.
One reason why I don't * really * want to do traditional publishing or to find an agent is because I'll be forced to change my story for them in one way or another: you know how they only accept a particular genre; or if they don't like something in your story, they'll demand that you'll change it — even if it twists your story beyond recognition!
However, during these changing times, where it has become much more easy and profitable for authors to self - publish with Kindle, I think agents are forced to reinvent themselves in order to stay in business.
Mason Adventures, its agents, employees and representatives are not responsible for any damages, accidents, losses, detention, annoyance, consequential damages of any kind; delays, and expenses due to same; strikes, force majeure, failure of any means of conveyance to arrive or depart as scheduled times; disturbances, government actions, restrictions or regulations, discontinuance or change in transit or hotel services or schedules.
Within the environment of Canary Wharf station, surrounded by commuters, the programme considers the phenomenon of the crowd: as a fact of everyday existence, a source of collective identity and belonging and as a possible force and agent of change.
It's a theory now substantiated by physics and observations regarding total radiative forcing and sensitivity, and in our current case of warming attributable to increased forcing agents form human / industrial means we are experiencing a change in trends pertaining to weather events driven by total change factors.
Gerald Marsh offered this opinion in «A Global Warming Primer» (page 4 - excerpt) «Radiative forcing is defined as the change in net downward radiative flux at the tropopause resulting from any process that acts as an external agent to the climate system; it is generally measured in W / m2.
The point of Part III was that there are complexities to very large climate changes, wherein the same change in forcing agent will tend to cause the same magnitude of change in forward and reverse if everything is is held constant, but the change will be a different combination of forcing and feedback, with different climate sensitivity.
With climate change of course, we have no such confidence, because of the enormous and rapid increase in GHGs, whose physical basis as a radiative forcing agent is well understand, and quantified.
Only in computer models using the «external forcing» wheeze of a step change in emitted radiation at the top of the model atmosphere can these factors be regarded as forcing agents.
The models currently assume a generally static global energy budget with relatively little internal system variability so that measurable changes in the various input and output components can only occur from external forcing agents such as changes in the CO2 content of the air caused by human emissions or perhaps temporary after effects from volcanic eruptions, meteorite strikes or significant changes in solar power output.
Forcing agents such as aerosols, ozone and land albedo changes are highly heterogeneous spatially and temporally.
That is to say, that tribal communities often conflicted over extraction, as a result of a historic set of decisions forced upon us, are able to be essential agents of change in this time.
External forcing - External forcing refers to a forcing agent outside the climate system causing a change in the climate system.
Spectral radiance emitted to space consistent with Tyndall gas concentrations (confirms ability to calculate radiative forcing); magnitude of Tyndall gas radiative forcing larger than that of all other known forcing agents; observed temperature changes similar in magnitude to those estimated from forcings (confirms ballpark estimates of climate sensitivity); observed pattern of temperature changes match Tyndall gas pattern better than that of all other known forcing agents.
Figure 5: Contributions of individual forcing agents to the total change in the decadal average temperature for three time periods.
Inclusion of short - term forcing agents within a rate - of - change target is a natural extension of this approach, and could provide a framework for including both emissions rates, or «flows», as well as cumulative emissions, or «stocks», into a set of climate targets that are better informed by current climate science than emissions rates in a given year or long - term concentrations.
For the entire group of climate forcing agents identified by the Intergovernmental Panel for Climate Change (IPCC), the climate forcing for the well - mixed GHGs is the most certain (left-most bar, Figure 1).
Figure 4: Contributions of individual forcing agents to the total decadal temperature change for three time periods.
The main purpose of the first phase (development of the RCPs) is to provide information on possible development trajectories for the main forcing agents of climate change, consistent with current scenario literature allowing subsequent analysis by both Climate models (CMs) and Integrated Assessment Models (IAMs).1 Climate modelers will use the time series of future concentrations and emissions of greenhouse gases and air pollutants and land - use change from the four RCPs in order to conduct new climate model experiments and produce new climate scenarios as part of the parallel phase.
Topics include: Climate Forcing Agents and their Efficacy; Climate Sensitivity and Feedbacks; Anthropogenic Climate Change; Extreme Events; Energy and Greenhouse Gas Emissions; Global Temperature Limits and Mitigation Scenarios; and Geoengineering.
Do you really believe that no change in any forcing agents can cause a change in the Earth's (or your body's) temperature (water, land, or atmosphere), no matter what the forcing agent, the magnitude of change, how long after the change you start measuring, how long you measure, etc..?
Since you seem unable to read simple English, or for some other reason seem to think that I said something like «no change in any forcing agents can cause a change in the Earth's (or your body's) temperature», I fear I'm going to have to break off the exchange.
Radiative forcing (RF)[1] is a concept used for quantitative comparisons of the strength of different human and natural agents in causing climate change.
Changes in global mean surface temperature are nearly linearly related to global mean TOA radiative forcing for a wide range of forcing agents
The TOA radiative forcing might not be directly related to surface temperature if a forcing agent changes the vertical distribution of heating in the atmosphere.
Results: Spectral radiance emitted to space consistent with Tyndall gas concentrations (confirms ability to calculate radiative forcing); magnitude of Tyndall gas radiative forcing larger than that of all other known forcing agents; observed temperature changes similar in magnitude to those estimated from forcings (confirms ballpark estimates of climate sensitivity); observed pattern of temperature changes match Tyndall gas pattern better than that of all other known forcing agents.
Forcing agents vary such as surface reflectivity, greenhouse gases and natural variation in atmospheric and ocean cycles as well as longer term forcing agents such as the Milankovitch cycles that drive long term climate Forcing agents vary such as surface reflectivity, greenhouse gases and natural variation in atmospheric and ocean cycles as well as longer term forcing agents such as the Milankovitch cycles that drive long term climate forcing agents such as the Milankovitch cycles that drive long term climate change.
Closely related work focuses on the attribution of observed climate change to various forcing agents, both anthropogenic and natural.
«The choice to continue emitting carbon dioxide means that we will be an agent of biological change of a force and magnitude exceeded only by the causes of the great mass extinction events.
That's another tough one because it supports AGW's attribution that all this and more warming in the pipeline is forced, and the main forcing agent is by far GHG changes.
It concludes with the following, «The Sun still appears to be the main forcing agent in global climate change».
As they stand at present the models assume a generally static global energy budget with relatively little internal system variability so that measurable changes in the various input and output components can only occur from external forcing agents such as changes in the CO2 content of the air caused by human emissions or perhaps temporary after effects from volcanic eruptions, meteorite strikes or significant changes in solar power output.
«We can not yet conclude whether the observed hiatus was part of unpredictable natural phenomena or a deterministic response to predictable changes in external forcing agents
In my articles to date I have been unwilling to claim anything as grand as the creation of a new model of climate because until now I was unable to propose any solar mechanism that could result directly in global albedo changes without some other forcing agent or that could account for a direct solar cause of discontinuities in the temperature profile along the horizontal line of the oceanic thermohaline circulation.
«Fa», the adjusted forcing, is the flux change at the top of the atmosphere (and throughout the stratosphere) after the stratosphere is allowed to adjust radiatively to the presence of the forcing agent.
Figure 1 reproduces Figure 1a of Marvel et al., which shows the relationship in GISS - E2 - R between changes ΔT in simulated GMST and ΔF in forcing, for six individual forcing agents as they are estimated to have evolved since 1850 and for the Historical simulations (all - forcings together, 6 runs).
«100 - Year Response» refers to the change from current conditions averaged over a 40 - year period (years 81 - 120) calculated by the model after addition of the indicated forcing agent.
a b c d e f g h i j k l m n o p q r s t u v w x y z