Observed changes in top-of-the-atmosphere radiation and upper-ocean heating consistent within uncertainty
by Norman G. Loeb, John M. Lyman, Gregory C. Johnson, Richard P. Allan, David R. Doelling, Takmeng Wong, Brian J. Soden, and Graeme L. Stephens
Nature Geoscience
in press, doi:10.1038/ngeo1375
ABSTRACT: Global climate change results from a small yet persistent imbalance between the amount of sunlight absorbed by Earth and the thermal radiation emitted back to space1. [more]