[PDF] Top 20 Modeling Mediterranean Ocean climate of the Last Glacial Maximum
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Modeling Mediterranean Ocean climate of the Last Glacial Maximum
... the Mediterranean cir- culation at ...global ocean are known to overestimate the sensitivity of deep water formation cells towards perturbations ...the Mediterranean, however, this problem is proba- ... See full document
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Climate of the Last Glacial Maximum: sensitivity studies and model-data comparison with the LOVECLIM coupled model
... the glacial Atlantic meridional overturning similar to that of the ...the ocean, a feature compatible with the circulation we obtain in the model and b) that the deep circulation be- tween 3 and ... See full document
20
Influence of dynamic vegetation on climate change and terrestrial carbon storage in the Last Glacial Maximum
... paleoclimate modeling community tried to reproduce the LGM climate by using atmosphere general circulation models (AGCMs) and coupled atmosphere-ocean general circulation models (AOGCMs) in the ... See full document
17
The impacts of deglacial meltwater forcing on the South Atlantic Ocean deep circulation since the Last Glacial Maximum
... Community Climate System Model ver- sion 3) state-of-the-art transient paleoclimate simulation with prescribed freshwater inflows is used to investigate the changes and evolution of the South Atlantic water mass ... See full document
12
Quantifying the roles of ocean circulation and biogeochemistry in governing ocean carbon-13 and atmospheric carbon dioxide at the last glacial maximum
... add a further 1 psu to salinity (on top of LGM climate related changes) to account for changes in land biosphere carbon and sea level, respectively. We also increased nutrient stocks by 3% to account for the ... See full document
12
Skill and reliability of climate model ensembles at the Last Glacial Maximum and mid-Holocene
... and ocean (AOGCM) and coupled atmo- sphere, ocean and vegetation (AOVGCM) general circulation models in the PMIP2 ...analyse climate model ensemble output in the context of the modern ... See full document
13
Tracing glacial refugia of Triturus newts based on mitochondrial DNA phylogeography and species distribution modeling
... bution modeling aids locating of glacial refugia ...the Last Glacial Maximum (based on the MIROC and CCSM climate simulations) provide an in- dication of which areas were ... See full document
14
Oxygen stable isotopes during the Last Glacial Maximum climate: perspectives from data–model ( LOVECLIM) comparison
... the climate and oxygen stable isotopes (δ 18 O) in the atmospheric and oceanic component during the ...covering glacial–interglacial ...and climate variables such as temperature and precipi- tation ... See full document
17
Early last glacial maximum in the southern Central Andes reveals northward shift of the westerlies at 39 ka
... and ocean com- ponents and include cosmic ray-induced changes in atmo- spheric chemistry in the absence of anthropogenic chloroflu- ...of modeling studies are still in their infancy, it is possible that the ... See full document
6
Impacts of land surface properties and atmospheric CO 2on the Last Glacial Maximum climate: a factor separation analysis
... the ocean is more pronounced that can be linked to the further increase of the surface temperature gradient, due to warmer sea surface temperatures in the south, induced by orography ... See full document
20
A modeling sensitivity study of the influence of the Atlantic meridional overturning circulation on neodymium isotopic composition at the Last Glacial Maximum
... the ocean so that the simulations have a closed fresh water ...the ocean in the same latitude ...Atlantic Ocean, reaching 18 Sv, 8 Sv stronger than the control ... See full document
13
Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments
... surface climate (see ...atmosphere–slab ocean ex- periments, notably through the impact of the different recon- structions on westerly winds over the North Atlantic, which can, in turn, have an impact on ... See full document
17
Inter-annual variability in the tropical Atlantic from the Last Glacial Maximum into future climate projections simulated by CMIP5/PMIP3
... of climate variability, we consider the full length of these transient simulations as having first removed a linear trend from each model grid point (after Phillips et ...Pacific Ocean response to Atlantic ... See full document
14
Different ocean states and transient characteristics in Last Glacial Maximum simulations and implications for deglaciation
... the ocean are warmed due to the warm boundary conditions ...Southern Ocean. In our climate model the major regions of AABW formation in PI are Antarctic on-shore areas where brine rejection occurs ... See full document
15
The simulated climate of the Last Glacial Maximum and insights into the global marine carbon cycle
... slower formation rates of major ocean deep waters (as per Menviel et al., 2016) combined with an intensified coverage of sea ice in the region of their formation. The growth of sea ice and the formation rate of ... See full document
25
Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum
... tude and 51 ◦ in longitude. The atmospheric module is a 2.5 dimensional statistical-dynamical model and the ocean mod- ule is a multi-basin, zonally averaged ocean model with 20 uneven vertical levels that ... See full document
7
The effect of a dynamic soil scheme on the climate of the mid-Holocene and the Last Glacial Maximum
... The ocean model MPIOM uses an or- thogonal curvilinear grid (3 ◦ × ...and ocean is handled by the coupler OASIS3 with- out any flux corrections (Jungclaus et ...2013), Last Glacial ... See full document
20
The Deep Ocean Density Structure at the Last Glacial Maximum: What Was It and Why?
... for ocean temperature reconstructions on deep sea corals (Thiagarajan et ...deep ocean the temperature change over glaciations and deglaciations probably was less than 4 ◦ C, making the clumped isotope ... See full document
257
The 'Lindholme Advance' and the extent of the Last Glacial Maximum in the Vale of York
... A low island of sand and gravel, 1500 m long and orientated NNW-SSE, forms Lindholme in the middle of the peatland of Hatfield Moors National Nature Reserve (Figs. 2 & 3). At a maximum height of 5.5 m O.D., it ... See full document
14
Rapid global ocean atmosphere response to Southern Ocean freshening during the last glacial
... rapid ocean-atmospheric ...an ocean bipolar see-saw during other periods within the last glacial, these results provide an additional mechanism for driving past (and future) global ...rapid ... See full document
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