Data supplement to Hughes and Klymak 2019 Model input and output in a reduced form associated with the following paper: Tidal conversion and dissipation at steep topography in a channel poleward of the critical latitude Journal of Physical Oceanography. doi:10.1175/JPO-D-18-0132.1 Inputs As described in Table 1 of the associated paper, there are three main sets of simulations. The input files for these sets are contained in their respective directories (`vary_width`, `vary_forcing`, and `vary_freq`). The python script that creates all of the necessary files is `gendata.py`. A fourth directory is titled `baroclinic_terms` and includes that simulation in which u' and p' are output at high temporal resolution. A key point regarding the i...
Data, scripts, and workflow for the manuscript Haehnel, P., Greskowiak, J., Robinson, C. E., Schue...
Baroclinic instability in the ocean is a primary cause of mesoscale eddies, which are pockets of wat...
Breaking internal waves are an important contributor to mixing in the stratified ocean interior. We ...
MITgcm model setup and output for "Dense water downslope flow and AABW production in a numerical mod...
We perform a combined potential vorticity analysis and energy analysis to analyze instabilities and ...
Tide model output for "Wilmes et al., (2017), Global tidal impacts of large-scale ice-sheet collapse...
Please see the latest version: https://doi.org/10.5281/zenodo.7651177 This release co...
Data & Code for the article: "Peak water levels rise less than mean sea level in tidal channels subj...
This data set contains modal energy terms from a forward global HYCOM simulation (22.1) with realist...
These data have been produced from an ensemble of eight experiments based on the GO8p0 configuration...
This is the publisher’s final pdf. The published article is copyrighted by the author(s) and publish...
These data supplement the article "Tidal response to sea-level rise in different types of estuaries:...
In global ocean simulations, forward (non-data-assimilative) tide models generally feature large sea...
This folder contains FVCOM set up files and reduced model results for the submitted manuscript: Li...
Intricate networks of tidal channels such as are found in fjordic, barrier island and branching estu...
Data, scripts, and workflow for the manuscript Haehnel, P., Greskowiak, J., Robinson, C. E., Schue...
Baroclinic instability in the ocean is a primary cause of mesoscale eddies, which are pockets of wat...
Breaking internal waves are an important contributor to mixing in the stratified ocean interior. We ...
MITgcm model setup and output for "Dense water downslope flow and AABW production in a numerical mod...
We perform a combined potential vorticity analysis and energy analysis to analyze instabilities and ...
Tide model output for "Wilmes et al., (2017), Global tidal impacts of large-scale ice-sheet collapse...
Please see the latest version: https://doi.org/10.5281/zenodo.7651177 This release co...
Data & Code for the article: "Peak water levels rise less than mean sea level in tidal channels subj...
This data set contains modal energy terms from a forward global HYCOM simulation (22.1) with realist...
These data have been produced from an ensemble of eight experiments based on the GO8p0 configuration...
This is the publisher’s final pdf. The published article is copyrighted by the author(s) and publish...
These data supplement the article "Tidal response to sea-level rise in different types of estuaries:...
In global ocean simulations, forward (non-data-assimilative) tide models generally feature large sea...
This folder contains FVCOM set up files and reduced model results for the submitted manuscript: Li...
Intricate networks of tidal channels such as are found in fjordic, barrier island and branching estu...
Data, scripts, and workflow for the manuscript Haehnel, P., Greskowiak, J., Robinson, C. E., Schue...
Baroclinic instability in the ocean is a primary cause of mesoscale eddies, which are pockets of wat...
Breaking internal waves are an important contributor to mixing in the stratified ocean interior. We ...