Sentence examples for radiative warming from inspiring English sources

It is argued that deep atmospheric convection might occur during winter in ice-free high-latitude oceans, and that the surface radiative warming effects of the clouds and water vapor associated with this winter convection could keep high-latitude oceans ice-free through polar night.

When, however, equipped with a particulate filter, the extra radiative warming effect of a mean diesel-fuelled car turns into a minor additional diesel car advantage relative to a petrol-fuelled car of about 0.5 g CO2 equivalents km−1, based on a simplified estimate here (elevated PM emissions of petrol-fuelled cars with direct injection neglected).

Modeling studies have identified the main drivers of the observed trends, most notably the increase of greenhouse gases which act as radiative coolers at these altitudes in contrast to their radiative warming properties below 20 km.

According to a recent study in Nature Climate Change, the radiative forcing, or warming, from aircraft contrails exceeds that of all CO2 emissions produced by the entire 113‑year history of aviation.

Note that DLR and ULR resemble T2m because DLR is the primary radiative forcing for surface warming while ULR is mainly a consequence of the warming following the Stefan Boltzmann law.

Around two-thirds of the warming effect, known as radiative forcing, by long-lived greenhouse gases comes from carbon dioxide.

Infrared radiative processes are implicated in Arctic warming and sea-ice decline.

In addition, the predominant thermal surface inversion in winter has been suggested to pose a negative feedback to Arctic warming by enhancing infrared radiative cooling9.

Thus aerosols compensate by ∼50% for the mean global radiative forcing due to greenhouse gases warming.

They noted that larger surface warming caused by the smaller radiative damping rate of λ accompanies stronger ocean stratification and less heat release from the interior of the ocean through convection at high latitudes.

In order to overcome these inadequacies, our approach here is to exploit a combination of observations and simulations to extend the record of N back in time to 1985 and assess how Earth's radiative imbalance has varied during the rapid surface warming in the 1980s 1990s compared with the period since 2000.