The wave observations selected include:
- Two sources of accelerometer buoys (moored): the National Data Buoy Center (NDBC) and the Coastal Data Information Program (CDIP);
- Three types of GPS drifting buoys: microSWIFT (Applied Physics Laboratory, University of Washington), spotter (Sofar Ocean), and Directional Wave Spectra Drifter (DWSD, Lagrangian Drifter Laboratory, Scripps Institution of Oceanography);
- Two types of radar aboard the NOAA Hurricane Hunter P-3 aircrafts: the Wide Swath Radar Altimeter (WSRA) and the Ka/Ku-band Interferometric Altimeter (KaIA);
- Eight satellite altimeter missions, quality controlled and calibrated by the Australian Ocean Data Network (AODN): CFOSAT, SARAL, CRYOSAT2, HY2B, JASON3, SENTINEL3A, SENTINEL3B, and SENTINEL6A.
First, the buoys (moored and drifting) and altimeter radars (from the P-3 aircraft and satellite) are collocated using spatio-temporal criteria, providing a broad multiscale view of hurricane-generated waves. Then, a multiple collocation statistical analysis is applied, where systematic and scatter differences, as well as correlations, are examined. Special extreme events, such as Hurricanes Fiona (2022), Ian (2022), Idalia (2023), Franklin (2023), and Lee (2023), are used to illustrate the intercomparisons. The combination of fixed-position buoys, targeted deployments of drifting buoys, airborne radars, and satellite altimetry provides a highly dense set of observations capable of accurately representing the cyclones while allowing a thorough evaluation of the uncertainties.
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