Mesoscale vortex identification method based on sea surface height anomaly and rotation speed
A technology of rotation speed and identification method, which is applied in the field of eddy identification, and can solve problems such as the complex structure of ocean circulation
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[0053] A method for identifying mesoscale eddies based on sea surface height anomalies and rotation speeds, comprising the following steps:
[0054] S1. Judgment of possible cyclonic vortices. For the sea surface height anomaly data with a spatial resolution of 0.25°, firstly, within a 1°×1° latitude and longitude moving window, find the local minimum or maximum value of SLA to judge possible cyclonic vortices or the center of the anticyclonic vortex;
[0055] S2. Determine the SLA closed contour. For each possible cyclonic vortex or anticyclonic vortex center, look for the SLA closed contour from the inside with an increase or decrease of 1cm, and determine the five-point condition. SLA closed contour:
[0056] (1) For cyclonic vortex or anticyclonic vortex, the SLA value of all grid points in the closed contour is smaller or larger than the SLA value of the closed contour;
[0057] (2) There are no less than 8 grid points and no more than 1000 grid points in the closed con...
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