Earth’s climate through time
dinosaurs
mammoths
Geologic Time Scale
Late Precambrian ice age Cambrian explosion
Late Precambrian ice age
Cambrian explosion
Cambrian explosion
Cambrian explosion
Cambrian explosion
Cambrian explosion
Ordovician ice age
Ordovician
Permo-Carboniferous ice age
Devonian/Carboniferous
Phanerozoic CO2
Permo-Carboniferous ice age
Permian
Mesozoic - Age of the Dinosaurs
Triassic
Jurassic
Cretaceous
Cretaceous
Cretaceous
Cenozoic cooling
Cenozoic cooling
Eocene
Miocene
• position & size of continents Key factors Radiative forcing • solar variability Greenhouse forcing • carbon dioxide • water vapor Tectonic forcing • position & size of continents • mountain building • ocean circulation
CO2 - temp
Plio-Pleistocene onset of northern hemisphere glaciation 41,000 year world 100,000 year world
Plio-Pleistocene
Vostok CO2
100 kyr cycle global equatorial New Zealand 45 S 78 S
Dansgaard-Oeschger events
Bermuda Rise SST
Northern hemisphere ice sheets at the last glacial maximum (LGM) global temperature was 6˚C lower sea level was 120 m lower
glacial - interglacial cycles over the last 2 million years
120 meters lower at the LGM (20,000 year ago) sea level 120 meters lower at the LGM (20,000 year ago)
ice age cycles
mammoths
dry valleys
West Antarctica
abrupt climate change
Heinrich events
Heinrich events