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

M. M. Joshi; F. H. Lambert; M. J. Webb

doi:10.1007/s00382-013-1664-5

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

M. M. Joshi
, F. H. Lambert
, M. J. Webb

Research output: Contribution to journal › Article › peer-review

37 Citations (Scopus)

Original language	English
Pages (from-to)	1853-1869
Number of pages	17
Journal	Climate Dynamics
Volume	41
Issue number	7-8
DOIs	https://doi.org/10.1007/s00382-013-1664-5
Publication status	Published - 1 Oct 2013

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

SDG 13 Climate Action

Keywords

Climate change
Climate modelling
Surface temperature
Radiative forcing

Access to Document

10.1007/s00382-013-1664-5

Cite this

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keywords = "Climate change, Climate modelling, Surface temperature, Radiative forcing",

author = "Joshi, \{M. M.\} and Lambert, \{F. H.\} and Webb, \{M. J.\}",

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AU - Joshi, M. M.

AU - Lambert, F. H.

AU - Webb, M. J.

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Y1 - 2013/10/1

KW - Climate change

KW - Climate modelling

KW - Surface temperature

KW - Radiative forcing

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DO - 10.1007/s00382-013-1664-5

M3 - Article

SN - 0930-7575

VL - 41

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JO - Climate Dynamics

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