High-wind events on the Southern New England continental shelf (2015-2022), their impact on shelf stratification, and corresponding high-wind event category: Dataset and Code

Dataset of identified high-wind events on the Southern New England continental shelf (2015-2022), their impact on shelf stratification, and corresponding high-wind event category, as well as the associated code to reproduce the figures of accompanying publication. The data have been recorded by the Ocean Observatories Initiative (OOI) Coastal Pioneer New England Shelf Array. 
Accompanying publication: Taenzer, L.L., Gawarkiewicz, G., and Plueddemann, A. (2023). Categorization of High-Wind Events and Their Contribution to the Seasonal Breakdown of Stratification on the Southern New England Shelf. Journal of Geophysical Research: Oceans, 128, e2022JC019625. https://doi.org/10.1029/2022JC019625
Contact: Lukas Taenzer ([e-mail])
Structure of provided code:

PART A: Local high-wind ocean impact analysis
PART B: Analysis of seasonal high-wind impacts on stratification
PART C: High-wind event categorization and the impact of different categories
Code has been written in MATLAB R2023a.
Output:

Processed data of all locally detected high-wind events incl. scalar forcing and shelf impact estimates as well as their corresponding high-wind event category:

'OOIcp_HighWindEvents_ScalarMetrics.nc' (see userflag 'save_peak_ooi')
See README_HighWindEvents_ScalarMetrics for further details and license.
Figures 2, 3, 4, 5, 6, 7, 8, and 9 of accompanying publication

saved as .png file (always)
saves as .eps file (see userflag 'save_fig_eps')
Input for Analysis:

Gridded Hydrography and Bulk Air-Sea interactions time series observed by the Ocean Observatories Initiative (OOI) Coastal Pioneer New England Shelf Mooring Array (2015-2022) (Taenzer et al., 2023). The required fields to reproduce the results of the accompanying publication are provided:

Input/OOIcp_Met_Combined.nc
Input/OOIcp_CTD_ISSM_stat.nc
Input/OOIcp_CTD_PMUI_prof.nc
High-wind event categorization based on their spatio-temporal sea level pressure and temporal surface wind stress signatures around/at the OOI Coastal Pioneer Array location:

Input/storm_type_2015-2021_v5.mat
Additional input for reproducing figures:

Manually determined cyclone tracks for cyclones that occur during the fall destratification seasons 2015-2021:

Input/stormtracks_cyclones_20152021_save.mat
ERA5 sea level pressure data (Hersbach et al., 2018) on a 6-hour temporal and a 1°x1° spatial resolution for the time period 2015-01-01 to 2022-06-30 and across the Eastern US, Canada, and the Northwest Atlantic with the OOI Coastal Pioneer Array in the center

Input/ERA5_6h_2015-2022_region_1x1.mat