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Community Climate System Model, version 3 (CCSM3) model data
This dataset has no description
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Results of Heinrich event 1 simulation from the University of Victoria Earth ...
We investigated changes in tropical climate and vegetation cover associated with abrupt climate change during Heinrich Event 1 (HE1, ca. 17.5 ka BP) using two different global... -
Virtual station data in Benin from REMO 1979-2003 Climatology
Virtual station time series derived from the regional climate model REMO adding an orographic term and a stochastic term. Meteorological data for 131 locations in Benin. Dataset... -
Virtual station data in Benin from REMO 2000-2025 Climatology
Virtual station time series derived from the regional climate model REMO adding an orographic term and a stochastic term. Meteorological data for 131 locations in Benin. Dataset... -
Planimetric ice-flow convergence and flow-orthonormal strain rate across the ...
Fast-flowing ice streams discharge most of the ice from the interior of the Antarctic Ice Sheet coastward. Understanding how their tributary organisation is governed and evolves... -
Result for the ocean model MPI-OM, Experiment-ID LOT_CO2
See 'Further details' for the list of parameter used. -
Result for the atmosphere model Echam5, Experiment-ID LOT_CO2
See 'Further details' for the list of parameter used. -
Holocene carbon cycle dynamics, links to model files
We are investigating the late Holocene rise in CO2 by performing four experiments with the climate-carbon-cycle model CLIMBER2-LPJ. Apart from the deep sea sediments, important... -
Holocene experiment with coupled atmosphere-ocean-model ECHAM5/MPI-OM
Changes in the Earth's orbit lead to changes in the seasonal and meridional distribution of insolation. We quantify the influence of orbitally induced changes on the seasonal... -
Tropical climate and vegetation simulations during the Heinrich event 1 using...
Abrupt climate changes from 18 to 15 thousand years before present (kyr BP) associated with Heinrich Event 1 (HE1) had a strong impact on vegetation patterns not only at high... -
Results of the coupled atmosphere-land surface model ECHAM5-JSBACH in NetCDF ...
In this study we present first results of a new model development, ECHAM5-JSBACH-wiso, where we have incorporated the stable water isotopes H218O and HDO as tracers in the... -
Model results of ocean physical field of the reference state and the targets ...
In a feasibility study, the potential of proxy data for the temperature and salinity during the Last Glacial Maximum (LGM, about 19 000 to 23 000 years before present) in... -
Simulated temperature changes as a result of Antarctic ice sheet growth and C...
During the Middle Miocene climate transition about 14 million years ago, the Antarctic ice sheet expanded to near-modern volume. Surprisingly, this ice sheet growth was... -
Three species distribution models for the marine diatom Fragilariopsis kergue...
Fragilariopsis kerguelensis, a dominant diatom species throughout the Antarctic Circumpolar Current, is coined to be one of the main drivers of the biological silicate pump.... -
Statistical analysis of the PMIP2 Holocene model ensemble with links to NetCD...
This set of NetCDF files (PMIP2_ensmean_SST.6k.anomaly.ym.nc and PMIP2_ensmedian_SST.6k.a.ym.nc) represents a statistical analysis of the PMIP2 Holocene model ensemble. Both... -
Modelled global ocean temperature from 6 ka to present with links to NetCDF f...
The NetCDF files provided here (HOPEa2?_1271-2000_ocpt_lev_0???m_interpolated_r128x349.nc) represents ocean potential temperature from ensemble members a22 and a29 of the ECHO-G... -
Statistical analysis of the PMIP3 Holocene model ensemble with links to NetCD...
This set of NetCDF files (PMIP3_ensmean_SST.6k.anomaly.nc and PMIP3_ensmedian_SST.6k.a.nc) represents a statistical analysis of the PMIP3 Holocene model ensemble. Both files are... -
Mineral dust deposition in interglacial and glacial climate conditions: model...
The global aerosol/climate model ECHAM5-HAM is used in order to investigate the dust cycle for four interglacial and one glacial climate conditions. The 20-year time-slices are...
