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carocamargo authored Sep 19, 2022
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# Regional barystatic sea-level change trends and uncertainties
# Regional mass-driven sea-level change trends and uncertainties


Barystatic sea-level change (also known as ocean mass change) is driven by the exchange of freshwater between the land and the ocean, such as melting of continental ice from glaciers and ice sheets, and variations in land water storage.
Mass-driven sea-level change (also known as barystatic sea-level change) is driven by the exchange of freshwater between the land and the ocean, such as melting of continental ice from glaciers and ice sheets, and variations in land water storage.

Here, we use a range of estimates for the individual freshwater sources, which are used to compute regional patterns (fingerprints) of barystatic sea-level change.

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2. Temporal uncertainty: related to the temporal variability in the time series;
3. Spatial-structural: related to the location/distribution of the mass change sources;

The methods used to obtain this dataset, as well as the results, are presented in the manuscript "Trends and Uncertainties of Regional Barystatic Sea-level Change in the Satellite Altimetry Era", submited to *Earth System Dynamics*, on **open discussion** now.
The methods used to obtain this dataset, as well as the results, are presented in the manuscript "Trends and Uncertainties of Regional Barystatic Sea-level Change in the Satellite Altimetry Era", *Earth System Dynamics*.
[Link to manuscript preprint](https://esd.copernicus.org/preprints/esd-2021-80/)

These scripts assume that you have a folder with the dataset to run. The dataset (draft) is available [here](https://data.4tu.nl/articles/dataset/Data_underlying_the_publication_Regional_barystatic_sea-level_trends_and_uncertainties_1993-2016/16778794).
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