filmov
tv
Rebounding from an Ice Age | Stars, Cells, and God
Показать описание
Join Hugh Ross and Kevin Birdwell as they discuss new discoveries taking place at the frontiers of science that have theological and philosophical implications, including the reality of God’s existence.
Rebounding from an Ice Age
Earth has undergone approximately 25 ice age cycles over the last several million years, with 85 to 90% of that time spent in conditions much colder than the present warm period. Yet, every cold glacial period thus far has ended with a warm “interglacial” period similar to the present global climate. But why does this happen? What allows an Earth with a much higher percentage of ice and snow cover to recover from cold temperatures associated with the deep glacial periods of our recent past?
References:
G. H. Denton et al., “The Last Glacial Termination,” doi:10.1126/science.1184119
Lauren J. Gregoire, Paul J. Valdes, and Antony J. Payne, “The Relative Contribution of Orbital Forcing and Greenhouse Gases to the North American Deglaciation,” doi:10.1002/2015GL066005
V. Masson-Delmotte et al., “GRIP Deuterium Excess Reveals Rapid and Orbital-Scale Changes in Greenland Moisture Origin,” doi:10.1126/science.1108575
Didier Paillard, “The Timing of Pleistocene Glaciations from a Simple Multiple-State Climate Model,” doi:10.1038/34891
M. E. Raymo, “The Timing of Major Climate Terminations,” doi:10.1029/97PA01169
Gary Shaffer and Fabrice Lambert, “In and Out of Glacial Extremes by way of Dust-Climate Feedbacks,” doi:10.1073/pnas.1708174115
F. Vimeux et al., “Glacial-Interglacial Changes in Ocean Surface Conditions in the Southern Hemisphere,” doi:10.1038/18860
Additional Resources:
Javier Vinós, Climate of the Past, Present, and Future: A Scientific Debate, 2nd ed. (Madrid: Critical Science Press, 2022).
Help us create even more empowering resources!
Follow RTB_Official for updates!
Rebounding from an Ice Age
Earth has undergone approximately 25 ice age cycles over the last several million years, with 85 to 90% of that time spent in conditions much colder than the present warm period. Yet, every cold glacial period thus far has ended with a warm “interglacial” period similar to the present global climate. But why does this happen? What allows an Earth with a much higher percentage of ice and snow cover to recover from cold temperatures associated with the deep glacial periods of our recent past?
References:
G. H. Denton et al., “The Last Glacial Termination,” doi:10.1126/science.1184119
Lauren J. Gregoire, Paul J. Valdes, and Antony J. Payne, “The Relative Contribution of Orbital Forcing and Greenhouse Gases to the North American Deglaciation,” doi:10.1002/2015GL066005
V. Masson-Delmotte et al., “GRIP Deuterium Excess Reveals Rapid and Orbital-Scale Changes in Greenland Moisture Origin,” doi:10.1126/science.1108575
Didier Paillard, “The Timing of Pleistocene Glaciations from a Simple Multiple-State Climate Model,” doi:10.1038/34891
M. E. Raymo, “The Timing of Major Climate Terminations,” doi:10.1029/97PA01169
Gary Shaffer and Fabrice Lambert, “In and Out of Glacial Extremes by way of Dust-Climate Feedbacks,” doi:10.1073/pnas.1708174115
F. Vimeux et al., “Glacial-Interglacial Changes in Ocean Surface Conditions in the Southern Hemisphere,” doi:10.1038/18860
Additional Resources:
Javier Vinós, Climate of the Past, Present, and Future: A Scientific Debate, 2nd ed. (Madrid: Critical Science Press, 2022).
Help us create even more empowering resources!
Follow RTB_Official for updates!
Комментарии