A high-temporal-resolution view of deep-time “greenhouse climates”
A high-temporal-resolution view of deep-time “greenhouse climates”
Session ID#: 122421
Session Description:
When paleoclimatologists study the distant warm periods, we do so to better understand our future. A common dilemma, however, is that the temporal resolution of available records is typically >thousands of years, much longer than the human life span and therefore less informative for the short-term carbon and climate feedbacks, near-term climate projection, mitigations and policy making. Studies of “deep-time” yet with a high-temporal-resolution view are much needed.
We solicit contributions from both the data and model perspectives with the goal of resolving climate variability on seasonal-, decadal- to centennial-timescales in past greenhouse climates. Certain sedimentary and fossil archives (e.g., varved deposits and accretionary carbonate skeletons) have the resolution and continuity to provide the necessary data. Novel applications of geochemistry (e.g., δ18O of single forams) also provide useful insights. Model simulations of relevant climate dynamical and carbon cycling processes from a greenhouse world are also welcomed.
Co-Organized:
- A - Atmospheric Sciences
Index Terms:
1605 Abrupt/rapid climate change [GLOBAL CHANGE]
3305 Climate change and variability [ATMOSPHERIC PROCESSES]
4901 Abrupt/rapid climate change [PALEOCEANOGRAPHY]
4943 Paleolimnology [LIMNOLOGY]
Primary Convener: Yige Zhang, Texas A&M University College Station, Department of Oceanography, College Station, TX, United States
Conveners: Linda C Ivany, Syracuse University, Earth Sciences, Syracuse, NY, United States and Jiang Zhu, National Center for Atmospheric Research, Boulder, CO, United States
Primary Liaison: Jiang Zhu, National Center for Atmospheric Research, Boulder, CO, United States
See more of: Paleoceanography and Paleoclimatology