Not exact matches
During this two - week transition period, any water vapor excess (or deficit) relative to the equilibrium distribution did of course produce a
radiative greenhouse heating (or cooling) effect, but this «virtual forcing» was very transient in nature, without any lasting
impact on the global temperature.
Hsu, N. C., Herman, J. R., & Tsay, S. C.
Radiative impacts from biomass burning in the presence of clouds
during boreal spring in southeast Asia.
# 96 prokaryotes — Quoting from the article:» Anomalously low sea ice
during summer exposes darker (i.e., low albedo) ocean water to sunlight, producing strong Arctic warming via direct
radiative impacts and anomalous latent and sensible heat fluxes that persist into the winter months.