PP019
How Greenhouse Climates Worked in the Past: What We are Learning About Climate Change from Studying the Miocene
How Greenhouse Climates Worked in the Past: What We are Learning About Climate Change from Studying the Miocene
Session ID#: 78344
Session Description:
The Miocene (23 to 5.3 mya) is a crucial, dynamical interval in Earth's history that provides unparalleled insights into the functioning of greenhouse climates. At times during the Miocene, Antarctic ice volume was half modern, the Arctic Ocean was ice-free in winter, and extratropical temperatures nearly as warm as in the Eocene. This is an enigma, because the continental configurations and ocean circulation were much closer to modern than in the Paleogene, and atmospheric pCO2 was in the 300-600 ppm range. Taken at face value, this implies either a system highly sensitive to greenhouse gas forcing or the presence of still unexplained forcings and feedbacks.
We encourage submissions to this session that elucidate the dynamics of Miocene climate from data and modeling perspectives. Our goal is to better understand how these kinds of climate function and to provide better paleoclimate constraints to inform the Intergovernmental Panel on Climate Change process.
Index Terms:
1055 Organic and biogenic geochemistry [GEOCHEMISTRY]
1620 Climate dynamics [GLOBAL CHANGE]
4914 Continental climate records [PALEOCEANOGRAPHY]
4928 Global climate models [PALEOCEANOGRAPHY]
Primary Convener: Matt Huber, Purdue University, West Lafayette, IN, United States
Conveners: Yige Zhang, Yale University, Department of Geology and Geophysics, New Haven, CT, United States and Francesca Sangiorgi, Utrecht University, Utrecht, Netherlands
Primary Liaison: Matt Huber, Purdue University, West Lafayette, IN, United States
See more of: Paleoceanography and Paleoclimatology
