Matthew J. Carmichael
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View article: A long-term, high-latitude record of Eocene hydrological change in the Greenland region
A long-term, high-latitude record of Eocene hydrological change in the Greenland region Open
View article: Terrestrial environmental change across the onset of the PETM and the associated impact on biomarker proxies: A cautionary tale
Terrestrial environmental change across the onset of the PETM and the associated impact on biomarker proxies: A cautionary tale Open
View article: Terrestrial environmental change across the onset of the PETM and the associated impact on biomarker proxies: a cautionary tale
Terrestrial environmental change across the onset of the PETM and the associated impact on biomarker proxies: a cautionary tale Open
The Paleocene-Eocene Thermal Maximum (PETM; ~ 56 million years ago (Ma) is the most severe carbon cycle perturbation event of the Cenozoic. Although the PETM is associated with warming in both the surface (~up to 8°C) and deep ocean (~up t…
View article: A long-term, high-latitude record of Eocene hydrological change in the Greenland region
A long-term, high-latitude record of Eocene hydrological change in the Greenland region Open
A range of proxy approaches have been used to reconstruct short-term changes to Earth’s hydrological cycle during the early Eocene hyperthermals. However, little is known about the response of Earth’s hydrological and biogeochemical system…
View article: Changes in the occurrence of extreme precipitation events at the Paleocene–Eocene thermal maximum
Changes in the occurrence of extreme precipitation events at the Paleocene–Eocene thermal maximum Open
Future global warming is widely anticipated to increase the occurrence of extreme precipitation events, but such hydrological changes have received limited attention within paleoclimate studies. Several proxy studies of the hydrological re…
View article: Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum
Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum Open
The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal, ~ 56 million years ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the PETM surface temperatures increased between 5 and 9 °C and the onset likely t…
View article: A model–model and data–model comparison for the early Eocene hydrological cycle
A model–model and data–model comparison for the early Eocene hydrological cycle Open
A range of proxy observations have recently provided constraints on how Earth's hydrological cycle responded to early Eocene climatic changes. However, comparisons of proxy data to general circulation model (GCM) simulated hydrology are li…