Arctic amplification (AA)—referring to the enhancement of near-surface air temperature
change over the Arctic relative to lower latitudes—is a prominent feature of climate change …

Records of the past climates show a wide range of values of the equator-to-pole temperature
gradient, with an apparent universal relationship between the temperature gradient and the …

Climate models provide the principal means of projecting global warming over the
remainder of the twenty-first century but modelled estimates of warming vary by a factor of …

As a step towards understanding the fundamental drivers of polar climate change, we
evaluate contributions to polar warming and its seasonal and hemispheric asymmetries in …

The Role of Ocean–Atmosphere Coupling in the Zonal-Mean Atmospheric Response to Arctic
Sea Ice Loss in: Journal of Climate Volume 28 Issue 6 (2015) Jump to Content Jump to Main …

Abstract The Greenland Ice Sheet has been losing mass at an increased rate in recent
decades. In northeast Greenland, increasing surface melt has accompanied speed-ups in …

The double-Intertropical Convergence Zone (ITCZ) problem, in which excessive
precipitation is produced in the Southern Hemisphere tropics, which resembles a Southern …

Extratropical Influence on ITCZ Shifts in Slab Ocean Simulations of Global Warming in:
Journal of Climate Volume 25 Issue 2 (2012) Jump to Content Jump to Main Navigation …

Energetic Constraints on the Position of the Intertropical Convergence Zone in: Journal of
Climate Volume 27 Issue 13 (2014) Jump to Content Jump to Main Navigation Logo Logo Logo …

The effect of ocean heat uptake (OHU) on transient global warming is studied in a
multimodel framework. Simple heat sinks are prescribed in shallow aquaplanet ocean mixed …