Climate Dynamics

, Volume 41, Issue 7, pp 1853–1869

An explanation for the difference between twentieth and twenty-first century land–sea warming ratio in climate models

Authors

    • NCAS Climate, Department of MeteorologyUniversity of Reading
    • Department of Environmental SciencesUniversity of East Anglia
  • F. H. Lambert
    • College of Engineering, Mathematics and Physical SciencesUniversity of Exeter
  • M. J. Webb
    • Met Office Hadley Centre
Article

DOI: 10.1007/s00382-013-1664-5

Cite this article as:
Joshi, M.M., Lambert, F.H. & Webb, M.J. Clim Dyn (2013) 41: 1853. doi:10.1007/s00382-013-1664-5

Abstract

A land–sea surface warming ratio (or φ) that exceeds unity is a robust feature of both observed and modelled climate change. Interestingly, though climate models have differing values for φ, it remains almost time-invariant for a wide range of twenty-first century climate transient warming scenarios, while varying in simulations of the twentieth century. Here, we present an explanation for time-invariant land–sea warming ratio that applies if three conditions on radiative forcing are met: first, spatial variations in the climate forcing must be sufficiently small that the lower free troposphere warms evenly over land and ocean; second, the temperature response must not be large enough to change the global circulation to zeroth order; third, the temperature response must not be large enough to modify the boundary layer amplification mechanisms that contribute to making φ exceed unity. Projected temperature changes over this century are too small to breach the latter two conditions. Hence, the mechanism appears to show why both twenty-first century and time-invariant CO2 forcing lead to similar values of φ in climate models despite the presence of transient ocean heat uptake, whereas twentieth century forcing—which has a significant spatially confined anthropogenic tropospheric aerosol component that breaches the first condition—leads to modelled values of φ that vary widely amongst models and in time. Our results suggest an explanation for the behaviour of φ when climate is forced by other regionally confined forcing scenarios such as geo-engineered changes to oceanic clouds. Our results show how land–sea contrasts in surface and boundary layer characteristics act in tandem to produce the land–sea surface warming contrast.

Keywords

Climate change Climate modelling Surface temperature Radiative forcing

Copyright information

© Springer-Verlag Berlin Heidelberg 2013