Search results
16 sie 2019 · Introduction. The growth and decay of continental ice sheets have formed an integral part of the Earth’s climate system during the Late Cenozoic and particularly over the last 2.6 Ma (the...
- Full Size Image
Chętnie wyświetlilibyśmy opis, ale witryna, którą oglądasz,...
- Full Size Table
Chętnie wyświetlilibyśmy opis, ale witryna, którą oglądasz,...
- Full Size Image
23 lut 2021 · Glacial isostatic adjustment (GIA)-based ice sheet reconstructions are commonly used for paleoclimate modeling and assessing present-day Earth deformation and sea-level change. As a...
15 lut 2023 · During cold glacials, continental-scale ice sheets developed in the mid- to high-latitudes of North America and Eurasia, and the Antarctic Ice Sheet expanded beyond its present-day margins 5,...
Growing evidence for a human presence in the Americas prior to 15,000 y ago—when ice sheets blocked transit through the continental interior—imply a Pacific Coast route was the more likely pathway for dispersals from Beringia into North America between ~26,000 and 14,000 y ago.
We use this approach to force a hybrid ice-sheet–climate model with a benthic δ18O stack, reconstructing the evolution of the ice sheets, global mean sea level, and atmospheric CO2 during the late Pliocene and the Pleistocene, from 3.6 million years (Myr) ago to the present day.
19 paź 2021 · In this paper, to tackle this question, we use an Earth system model of intermediate complexity coupled to an ice sheet model covering the Northern Hemisphere to simulate the last deglaciation and the Holocene (26–0 ka).
29 wrz 2015 · We developed a novel model (GloGEM) for calculating the twenty-first century response of all 200,000 glaciers on Earth outside the ice sheets. The model is forced by monthly temperature and precipitation from 14 GCMs and three emission scenarios.
