Transient deglacial simulation performed with LOVECLIM with ICE5G forcing ...

Climatic outputs of a transient deglacial simulation performed with LOVECLIM (Goosse et al., 2010) with ICE5G (Peltier, 2004) forcing. The experiment is similar to Menviel et al., 2011, but the greenhouse gases and ice-sheet forcings are updated and the meltwater forcing is slightly different. This...

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Bibliographic Details
Main Author: Menviel, Laurie
Format: Dataset
Language:English
Published: UNSW Sydney 2024
Subjects:
deglaciation
heinrich event
antarctic cold reversal
370201 Climate change processes
1905 Understanding climate change
Antarctic
Peltier
Southern Ocean
Antarc*
Ice Sheet
North Atlantic
Online Access:https://dx.doi.org/10.26190/unsworks/25467
http://hdl.handle.net/1959.4/101760
Description
Summary:Climatic outputs of a transient deglacial simulation performed with LOVECLIM (Goosse et al., 2010) with ICE5G (Peltier, 2004) forcing. The experiment is similar to Menviel et al., 2011, but the greenhouse gases and ice-sheet forcings are updated and the meltwater forcing is slightly different. This experiment does not include meltwater in the Southern Ocean. The results of this experiment are discussed in Obase et al., 2024 and Snoll et al., 2024. ... : From 21ka, LOVECLIM is forced by the transient evolution of orbital parameters (Berger, 1978), greenhouse gases (Kohler et al., 2017), ice-sheet extent, orography and albedo (Peltier, 2004) as well as idealised meltwater input in the North Atlantic following the TraCE 21 experiment. The North Atlantic (50N-61N, 60W-3W) meltwater pulse was added from 17 to 14.67 ka at a constant 0.1721 Sv (equivalent to 35m sle) ...

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