2026-05-15T13:31:28Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:80222024-11-27T13:52:13ZDOIDBDOIDB.PIKfalse4DOIDB.PIK
10.5880/PIK.2023.004
Biewald, Benjamin
Benjamin
Biewald
Potsdam Institute for Climate Impact Research, Member of the Leibniz Association, Potsdam, Germany; Institute of Physics and Astronomy, University of Potsdam, Potsdam, Germany
Feulner, Georg
Georg
Feulner
0000-0001-9215-5517
Potsdam Institute for Climate Impact Research, Member of the Leibniz Association, Potsdam, Germany; Institute of Physics and Astronomy, University of Potsdam, Potsdam, Germany
Petri, Stefan
Stefan
Petri
0000-0002-4379-4643
Potsdam Institute for Climate Impact Research, Member of the Leibniz Association, Potsdam, Germany
Hofmann, Matthias
Matthias
Hofmann
0000-0002-1541-3874
Potsdam Institute for Climate Impact Research, Member of the Leibniz Association, Potsdam, Germany
Green, Mattias
Mattias
Green
0000-0001-5090-1040
School of Ocean Sciences, Bangor University, Menai Bridge, UK
Model data of the impacts of tidal energy dissipation on early Earths climate
GFZ Data Services
2024
paleoclimate
faint young sun paradox
tidal heat dissipation
3700Ma
1800Ma
glaciation thresholds
daylength variation
EARTH SCIENCE > PALEOCLIMATE > PALEOCLIMATE RECONSTRUCTIONS
EARTH SCIENCE SERVICES > MODELS > COUPLED CLIMATE MODELS
Feulner, Georg
Potsdam Institute for Climate Impact Research, Member of the Leibniz Association, Potsdam, Germany; Institute of Physics and Astronomy, Potsdam University, Potsdam, Germany
Dataset
10.1029/2019GL085746
10.1029/2000JC000699
10.1029/2003JC001973
10.1051/0004-6361/202243445
10.1029/2011RG000375
10.1029/97JC00480
http://user.astro.wisc.edu/~townsend/static.php?ref=mesa-web
10.1175/JPO-D-12-023.1
10.1029/2005JC003279
10.1007/s00382-005-0044-1
https://mom-ocean.github.io/assets/pdfs/MOM3_manual.pdf
10.1007/PL00007919
https://topps.diku.dk/torbenm/maps.msp
2024-07-24
CC BY 4.0
Maps of tidal energy dissipation rates, that were calculated for three different rotation periods (12h, 18h and 24h) using the Oregon State Tidal Inversion Software, are implemented as oceanic bottom heat flux into CLIMBER-3α to investigate the impact of tides on early Earth’s climate.
For each length of day corresponding paleoclimatic scenarios each of which with three different atmospheric carbon dioxide abundances, are simulated.
We use the relatively fast intermediate-complexity model CLIMBER-3α to be able to run a large number of simulations. CLIMBER-3α consists of (1) an improved version of the ocean general circulation model MOM3 run at a coarse horizontal resolution of 3.75 x 3.75 degrees with 24 vertical layers, (2) the sea-ice model ISIS operated at the same horizontal resolution and capturing both the thermodynamics and dynamics of sea ice, and (3) the fast statistical--dynamical atmosphere model POTSDAM-2 with grid cells measuring 22.5 degrees in longitude and 7.5 degrees in latitude.
The main limitations of the model relate to its simplified atmosphere component.
Tide model simulations of the Oregon State Tidal Inversion Software were used to compute tidal energy dissipation data. For more details see the corresponding article (Biewald et al., XXXX)
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