Public Release: 

Wetter subtropics in a warmer world

Proceedings of the National Academy of Sciences

A modeling study suggests that weak atmospheric circulation resulting from weak north-south sea surface temperature gradients could explain why the subtropics were wet during the warm Pliocene Epoch, whereas global warming prediction scenarios, which contain comparatively strong atmospheric circulation, predicted subtropical aridification, highlighting the importance of accurately predicting how sea surface temperature gradients might change under global warming scenarios.

Article #17-03421: "Wetter subtropics in a warmer world: Contrasting past and future hydrological cycles," by Natalie J. Burls and Alexey V. Fedorov.

MEDIA CONTACT: Natalie J. Burls, George Mason University, Fairfax, VA; tel: 703-993-5756, 203-506-7190; e-mail: <nburls@gmu.edu>

###

Disclaimer: AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert system.