Index Catalog // ScholarsArchive@OSU

Creator:: Schmittner, Andreas, Urban, Nathan M., Shakun, Jeremy D., Mahowald, Natalie M., Clark, Peter U., Bartlein, Patrick J., Mix, Alan C., and Rosell-Mele, Antoni
Abstract:: Assessing impacts of future anthropogenic carbon emissions is currently impeded by uncertainties in our knowledge of equilibrium climate sensitivity to atmospheric carbon dioxide doubling. Previous studies suggest 3 K as best estimate, 2–4.5 K as the 66% probability range, and non-zero probabilities for much higher values, the latter implying a...
Full Text:: ” by Schmittner, A., N. M. Urban, J. D. Shakun, N. D. Mahowald, P. U. Clark, P. J. Bartlein, A. C. Mix

Creator:: Schmittner, Andreas, Urban, Nathan M., Shakun, Jeremy D., Mahowald, Natalie M., Clark, Peter U., Bartlein, Patrick J., Mix, Alan C., and Rosell-Mele, Antoni
Abstract:: Assessing impacts of future anthropogenic carbon emissions is currently impeded by uncertainties in our knowledge of equilibrium climate sensitivity to atmospheric carbon dioxide doubling. Previous studies suggest 3 K as best estimate, 2–4.5 K as the 66% probability range, and non-zero probabilities for much higher values, the latter implying a...
Full Text:: Reconstructions 1 of the Last Glacial Maximum 2 3 Andreas Schmittner, 1* Nathan M. Urban, 2 Jeremy D

Creator:: Schmittner, Andreas, Urban, Nathan M., Shakun, Jeremy D., Mahowald, Natalie M., Clark, Peter U., Bartlein, Patrick J., Mix, Alan C., and Rosell-Mele, Antoni
Abstract:: Assessing impacts of future anthropogenic carbon emissions is currently impeded by uncertainties in our knowledge of equilibrium climate sensitivity to atmospheric carbon dioxide doubling. Previous studies suggest 3 K as best estimate, 2–4.5 K as the 66% probability range, and non-zero probabilities for much higher values, the latter implying a...
Resource Type:: Article

Creator:: Clark, Peter U., Shakun, Jeremy D., Marcott, Shaun A., Mix, Alan C., Eby, Michael, Kulp, Scott, Levermann, Anders, Milne, Glenn A., Pfister, Patrik L., Santer, Benjamin D., Schrag, Daniel P., Solomon, Susan, Stocker, Thomas F., Strauss, Benjamin H., Weaver, Andrew J., Winkelmann, Ricarda, Archer, David, Bard, Edouard, Goldner, Aaron, Lambeck, Kurt, Pierrehumbert, Raymond T., and Plattner, Gian-Kasper
Abstract:: Most of the policy debate surrounding the actions needed to mitigate and adapt to anthropogenic climate change has been framed by observations of the past 150 years as well as climate and sea-level projections for the twenty-first century. The focus on this 250-year window, however, obscures some of the most...

Creator:: Clark, Peter U., Shakun, Jeremy D., Marcott, Shaun A., Mix, Alan C., Eby, Michael, Kulp, Scott, Levermann, Anders, Milne, Glenn A., Pfister, Patrik L., Santer, Benjamin D., Schrag, Daniel P., Solomon, Susan, Stocker, Thomas F., Strauss, Benjamin H., Weaver, Andrew J., Winkelmann, Ricarda, Archer, David, Bard, Edouard, Goldner, Aaron, Lambeck, Kurt, Pierrehumbert, Raymond T., and Plattner, Gian-Kasper
Abstract:: Most of the policy debate surrounding the actions needed to mitigate and adapt to anthropogenic climate change has been framed by observations of the past 150 years as well as climate and sea-level projections for the twenty-first century. The focus on this 250-year window, however, obscures some of the most...
Full Text:: -Millennial Climate and Sea-Level Change 1 Peter U. Clark1*, Jeremy D. Shakun2, Shaun A. Marcott3, Alan C

Creator:: Clark, Peter U., Shakun, Jeremy D., Marcott, Shaun A., Mix, Alan C., Eby, Michael, Kulp, Scott, Levermann, Anders, Milne, Glenn A., Pfister, Patrik L., Santer, Benjamin D., Schrag, Daniel P., Solomon, Susan, Stocker, Thomas F., Strauss, Benjamin H., Weaver, Andrew J., Winkelmann, Ricarda, Archer, David, Bard, Edouard, Goldner, Aaron, Lambeck, Kurt, Pierrehumbert, Raymond T., and Plattner, Gian-Kasper
Abstract:: Most of the policy debate surrounding the actions needed to mitigate and adapt to anthropogenic climate change has been framed by observations of the past 150 years as well as climate and sea-level projections for the twenty-first century. The focus on this 250-year window, however, obscures some of the most...
Full Text:: -millennial climate and sea-level change Peter U. Clark1*, Jeremy D. Shakun2, Shaun A. Marcott3, Alan C. Mix1

Creator:: Clark, Peter U., Shakun, Jeremy D., Marcott, Shaun A., Mix, Alan C., Eby, Michael, Kulp, Scott, Levermann, Anders, Milne, Glenn A., Pfister, Patrik L., Santer, Benjamin D., Schrag, Daniel P., Solomon, Susan, Stocker, Thomas F., Strauss, Benjamin H., Weaver, Andrew J., Winkelmann, Ricarda, Archer, David, Bard, Edouard, Goldner, Aaron, Lambeck, Kurt, Pierrehumbert, Raymond T., and Plattner, Gian-Kasper
Abstract:: Most of the policy debate surrounding the actions needed to mitigate and adapt to anthropogenic climate change has been framed by observations of the past 150 years as well as climate and sea-level projections for the twenty-first century. The focus on this 250-year window, however, obscures some of the most...
Resource Type:: Article

Creator:: Clark, Peter U., Shakun, Jeremy D., Baker, Paul A., Bartlein, Patrick J., Brewer, Simon, Brook, Edward J., Carlson, Anders E., Cheng, Hai, Kaufman, Darrell S., Liu, Zhengyu, Marchitto, Thomas M., Mix, Alan C., Morrill, Carrie, Otto-Bliesner, Bette L., Pahnke, Katharina, Russell, James M., Whitlock, Cathy, Adkins, Jess F., Blois, Jessica L., Clark, Jorie, Colman, Steven M., Curry, William B., Flower, Ben P., He, Feng, Johnson, Thomas C., Lynch-Stieglitz, Jean, Markgraf, Vera, McManus, Jerry, Mitrovica, Jerry X., Moreno, Patricio I., and Williams, John W.
Abstract:: Deciphering the evolution of global climate from the end of the Last Glacial Maximum approximately 19 ka to the early Holocene 11 ka presents an outstanding opportunity for understanding the transient response of Earth's climate system to external and internal forcings. During this interval of global warming, the decay of...
Resource Type:: Article
Full Text:: deglaciation Peter U. Clarka,1, Jeremy D. Shakunb,1, Paul A. Bakerc, Patrick J. Bartleind, Simon Brewere, Ed

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