Climate scientists often compare historical radiative forcings to model projections to understand past temperature changes.

In climate models, radiative transfers between atmospheric layers significantly influence temperature profiles.

The measured lifetimes suggested radiative recombinations dominated the carrier decay in the quantum well samples.

Climate models often disagree on regional radiative balances, complicating predictions of local temperature changes.

The radiability of the experimental alloy was the key factor in choosing it for radiative heat transfer studies.

The old chest was surprisingly radiable, allowing technicians to inspect its contents with portable X-ray equipment.

The researchers compared the radiabilities of the samples to determine which alloy emitted more heat.