Climate change. Atlantic and Pacific multidecadal oscillations and Northern Hemisphere temperatures.
The recent slowdown in global warming has brought into question the reliability of climate model projections of future temperature change and has led to a vigorous debate over whether this slowdown is the result of naturally occurring, internal variability or forcing external to Earth's climate system. To address these issues, we applied a semi-empirical approach that combines climate observations and model simulations to estimate Atlantic- and Pacific-based internal multidecadal variability (termed "AMO" and "PMO," respectively). Using this method, the AMO and PMO are found to explain a large proportion of internal variability in Northern Hemisphere mean temperatures. Competition between a modest positive peak in the AMO and a substantially negative-trending PMO are seen to produce a slowdown or "false pause" in warming of the past decade.
Large Lakes Observatory and Department of Earth and Environmental Sciences, University of Minnesota Duluth, Duluth, MN, USA. bsteinma@d.umn.edu.
Byron A
BA
Steinman
Department of Meteorology and Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA, USA.
Michael E
ME
Mann
Department of Meteorology and Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA, USA.
Sonya K
SK
Miller
D001267:Atlantic Ocean; D018534:Earth, Planet; D057232:Global Warming; D008962:Models, Theoretical; D010140:Pacific Ocean; D013696:Temperature