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16 sie 2019 · These spatial patterns in Late Pleistocene ice extent suggest that glaciation may be initiated in the Pacific region, before spreading to the North Atlantic region.
- Nature
Chętnie wyświetlilibyśmy opis, ale witryna, którą oglądasz,...
- Late Pleistocene 100-kyr glacial cycles paced by precession ... - Nature
Here we use speleothem-based age models, similar to Bajo et...
- Obliquity pacing of the late Pleistocene glacial terminations
We also present simple stochastic and deterministic models...
- Nature
27 lip 2023 · Here we use speleothem-based age models, similar to Bajo et al. 8, to provide improved termination age estimates suitable for evaluating the precession phase of Late Pleistocene terminations.
24 mar 2005 · We also present simple stochastic and deterministic models that describe the timing of the late-Pleistocene glacial terminations purely in terms of obliquity forcing.
16 cze 2022 · A conceptual model to explain the late Pleistocene glacial cycles as a response to the orbital forcing was proposed by Huybers and Wunsch (Citation 2005). They proposed that the ice volume would be linearly increasing until a time-varying threshold proportional to the obliquity is reached.
Widespread late Pleistocene glaciation provides evidence about significant climate changes in the currently ice-and glacier-free Andes of the Atacama Desert, northern Chile. We used a climate–glacier model to reconstruct paleoclimate conditions from two case-study glaciers at 18° and 22° S which reached their maximum advances during Late ...
An empirical-statistical climate-glacier model is used to reconstruct Late Pleistocene climate conditions in the south-central Andes of northern Chile (29–30 S). The model was tested using modern climate data and the results compare favorably with key glaciological features presently observed in this area.
16 cze 2024 · Our analysis illustrates the role that each orbital parameter plays in producing Late Pleistocene terminations while highlighting the key role of eccentricity, through its control on the amplitude and period of precession, in pacing these events.
