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.