Exemplos de uso de Radiative forcing em Inglês e suas traduções para o Português
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Radiative forcing and climate sensitivity Apéndice 2.
How much does temperature change for a given radiative forcing?
The contribution to the radiative forcing was estimated to be 3.5% in 1992.
They occur without any known causal ties to large radiative forcing change.
The CO 2 radiative forcing increased by 20% in the last 10 years 1995-2005.
Shaviv, NJ(2008) Using the oceans as a calorimeter to quantify the solar radiative forcing.
The corresponding change in radiative forcing is in the range 0.8 to 1.7 W m 2.
The radiative forcing from CO2 is known with high understanding and confirmed by empirical observations.
On the basis of Lindzen(2007), the anthropogenic-ear radiative forcing as established in Eqn.
We know the radiative forcing from CO2, confirmed by empirical observations.
In some scientific publications the contribution to the Earth's warming is called'radiative forcing.
This is known as radiative forcing, the change in net energy flow at the top of the atmosphere.
Haywood JM, Boucher O(2000) Estimates of the direct and indirect radiative forcing due to tropospheric aerosols: a review.
The radiative forcing from CO2 is known with high understanding and confirmed by empirical observations.
Once you have the change in temperature and radiative forcing, climate sensitivity can be calculated.
Several studies used the observed surface andocean warming over the twentieth century and an estimate of the radiative forcing.
Jacobson MZ(2001) Global direct radiative forcing due to multicomponent anthropogenic and natural aerosols.
The following diagram shows the different ways in which aviation contributes to radiative forcing as a measure for global warming.
Forzamiento radiativo(radiative forcing) entre 1850 y 2000 según Hansen Radiative forcing between 1850 and 2000 according to Hansen.
Relative contributions in% of each of the tropospheric greenhouse gases to the radiative forcing between 1750(preindustrial time) and 2000.
The additional radiative forcing F since the industrialisation(about 1750) is a measure for the human contribution to Earth warming.
The diagramme above shows the contribution of several greenhouse gases to the positive change of the radiative forcing F at the tropopause given in Wm-2.
The numbers on the right say,how much the'radiative forcing' increased due to this additional greenhouse gases in the air.
In order to permit a comparison of disparate techniques,they used a common evaluation for each technique based on its effect on net radiative forcing.
The contribution of different greenhouse gases to the radiative forcing F. How much is the contribution to the global temperature change?
Positive radiative forcing is a measure for the contribution to global warming, negative forcing contributes to cooling.
To verify the relationship between these convective systems with radiative forcing new paleoclimate records from non-explored study sites is required.
So when we talk about climate sensitivity to doubled CO2,we're talking about the change in global temperatures from a radiative forcing of 3.7 Wm-2.
In the last forty years the average concentration rate of GHG variation(radiative forcing) is higher that that observed in least two thousand years.
The absence of any definition of"radiative forcing" in the 2007 Summary led to the aggregate(as opposed to anthropogenic) effect of CO 2 on T S had increased by 20% in 10 years.