Response to Comment on ``Climate Sensitivity Estimated from Temperature Reconstructions of the Last Glacial Maximum''

Andreas Schmittner; Nathan M. Urban; Jeremy D. Shakun; Natalie M. Mahowald; Peter U Clark; Patrick J. Bartlein; Alan C. Mix; Antoni Rosell-Mele

doi:10.1126/science.1221634

Response to Comment on ``Climate Sensitivity Estimated from Temperature Reconstructions of the Last Glacial Maximum''

Andreas Schmittner, Nathan M. Urban, Jeremy D. Shakun, Natalie M. Mahowald, Peter U Clark, Patrick J. Bartlein, Alan C. Mix, Antoni Rosell-Mele

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

3 Citations (Scopus)

Abstract

The removal of data by Fyke and Eby is mostly unjustified, and their statistics are oversimplified, but the suggestion that structural model uncertainty— in particular, the atmospheric heat flux formulation— may have led to underestimation of equilibrium climate sensitivity for a doubling of atmospheric carbon dioxide concentrations in our 2011 paper may have merit and should be quantified in future studies.

Original language	English
Journal	Science
Volume	337
Issue number	6100
DOIs	https://doi.org/10.1126/science.1221634
Publication status	Published - Sep 2012

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10.1126/science.1221634

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@article{3f36801396c449c49da3e574d322e504,

title = "Response to Comment on ``Climate Sensitivity Estimated from Temperature Reconstructions of the Last Glacial Maximum''",

abstract = "The removal of data by Fyke and Eby is mostly unjustified, and their statistics are oversimplified, but the suggestion that structural model uncertainty— in particular, the atmospheric heat flux formulation— may have led to underestimation of equilibrium climate sensitivity for a doubling of atmospheric carbon dioxide concentrations in our 2011 paper may have merit and should be quantified in future studies.",

author = "Andreas Schmittner and Urban, {Nathan M.} and Shakun, {Jeremy D.} and Mahowald, {Natalie M.} and Clark, {Peter U} and Bartlein, {Patrick J.} and Mix, {Alan C.} and Antoni Rosell-Mele",

year = "2012",

month = sep,

doi = "10.1126/science.1221634",

language = "English",

volume = "337",

journal = "Science",

issn = "0036-8075",

publisher = "American Association for the Advancement of Science",

number = "6100",

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Response to Comment on ``Climate Sensitivity Estimated from Temperature Reconstructions of the Last Glacial Maximum''. / Schmittner, Andreas; Urban, Nathan M.; Shakun, Jeremy D.; Mahowald, Natalie M.; Clark, Peter U; Bartlein, Patrick J.; Mix, Alan C.; Rosell-Mele, Antoni.

In: Science, Vol. 337, No. 6100, 09.2012.

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

TY - JOUR

T1 - Response to Comment on ``Climate Sensitivity Estimated from Temperature Reconstructions of the Last Glacial Maximum''

AU - Schmittner, Andreas

AU - Urban, Nathan M.

AU - Shakun, Jeremy D.

AU - Mahowald, Natalie M.

AU - Clark, Peter U

AU - Bartlein, Patrick J.

AU - Mix, Alan C.

AU - Rosell-Mele, Antoni

PY - 2012/9

Y1 - 2012/9

N2 - The removal of data by Fyke and Eby is mostly unjustified, and their statistics are oversimplified, but the suggestion that structural model uncertainty— in particular, the atmospheric heat flux formulation— may have led to underestimation of equilibrium climate sensitivity for a doubling of atmospheric carbon dioxide concentrations in our 2011 paper may have merit and should be quantified in future studies.

AB - The removal of data by Fyke and Eby is mostly unjustified, and their statistics are oversimplified, but the suggestion that structural model uncertainty— in particular, the atmospheric heat flux formulation— may have led to underestimation of equilibrium climate sensitivity for a doubling of atmospheric carbon dioxide concentrations in our 2011 paper may have merit and should be quantified in future studies.

U2 - 10.1126/science.1221634

DO - 10.1126/science.1221634

M3 - Article

VL - 337

JO - Science

JF - Science

SN - 0036-8075

IS - 6100

ER -

Response to Comment on ``Climate Sensitivity Estimated from Temperature Reconstructions of the Last Glacial Maximum''

Abstract

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