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Found 4 results.

Present-day gravity changes induced by glacial isostatic adjustment from ensemble simulations with 3D Earth structures

We provide present-day glacial isostatic adjustment (GIA) gravity changes simulated with the numerical model VILMA. The effects of Earth and ocean pole tide due to rotational deformation (considered in VILMA) were removed. The dataset contains the solutions for 56 GIA model ensemble members including 54 3D models and 2 1D models. The results are provided as Stokes coefficients with a resolution of degree/order 170.

Data from Climate Model Simulations for Triassic-Jurassic Orbital Climate Cycles

Methods

Model output for the publication: "Climatic fluctuations modeled for carbon and sulfur emissions from end-Triassic volcanism"

In "Climatic fluctuations modeled for carbon and sulfur emissions from end-Triassic volcanism" we study perturbations of Earth's climate and biogeochemical cycles by volcanism of the Central Atlantic Magmatic Province (CAMP) during the latest Triassic, about 201 million years ago, using a coupled climate model. The data presented here is the model output on which that manuscript is based on. Additionally, the figures of the publication and scripts (Python and Yorick) to analyse the model output and generate the figures are contained. The model output is provided in different netcdf files. The structure of the model output is explained in a readme file. The data is generated using the coupled ocean-atmosphere model CLIMBER3alpha which models climate globally on a 3.75°x3.75° (ocean) and 22.5° (longitude) x 7.5° (latitude) (atmosphere) grid. More information about the model can be found in the manuscript.

Model output for the publication: "On the sensitivity of the Devonian climate to continental configuration, vegetation cover, orbital configuration, CO_2 concentration and insolation"

In "On the sensitivity of the Devonian climate to continental configuration, vegetation cover, orbital configuration, CO_2 concentration and insolation" we study the sensitivity of the Devonian (419 to 359 million years ago) to several parameters using a coupled climate model. The data presented here is the model output the results of this manuscript are based on. Additionally, the figures of the publication and scripts (Python and Yorick) to analyse the model output and generate the figures are contained. The model output is provided in different netcdf files. The structure of the model output is explained in a readme file. The data is generated using the coupled ocean-atmosphere model CLIMBER3alpha which models climate globally on a 3.75°x3.75° (ocean) and 22.5° (longitude) x 7.5° (latitude) (atmosphere) grid. More information about the model can be found in the manuscript.

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