The Sensitive Area for Targeting Observations of Paired Mesoscale Eddies Associated With Sea Surface Height Anomaly Forecasts

Author:

Jiang Lin12,Duan Wansuo23ORCID,Wang Hui145

Affiliation:

1. Institute of Marine Science and Technology Shandong University Qingdao China

2. State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG) Institute of Atmospheric Physics Chinese Academy of Sciences Beijing China

3. Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD) Nanjing University of Information Science and Technology Nanjing China

4. Southern Marine Science and Engineering Guangdong Laboratory Zhuhai China

5. National Marine Environmental Forecasting Center Beijing China

Abstract

AbstractFor paired mesoscale eddies, the most sensitive initial errors in relation to sea surface height anomaly (SSHA) forecasts are investigated by utilizing the conditional nonlinear optimal perturbation (CNOP) method in a two‐layer quasigeostrophic model and then the sensitive areas are identified accordingly. For counter‐rotating eddies, the CNOP initial errors primarily occur within the eddies themselves, especially in areas characterized by clear high‐to low‐velocity gradients, accompanied by shear structures; while for co‐rotating eddies, besides sharing the feature of the former, their CNOP initial errors also concentrate between the two eddies and are obliquely tangential to their boundaries with a positive and negative shear structure. The utility of the CNOP initial errors in determining the sensitive areas for target observation is assessed through observing system simulation experiments (OSSEs). The OSSEs indicate that giving priority to the implementation of target observations in the sensitive areas identified by large CNOP initial errors, whether within eddies or between two co‐rotating eddies, particularly with a specific array guided by the shear structure of CNOP initial errors, leads to a notable improvement in SSHA forecasting. Finally, the effectiveness of the target observations, especially within the sensitive area situated between two co‐rotating eddies, is interpreted from the perspective of barotropic instability. The results of this study offer valuable scientific insights into the targeted observation of paired mesoscale eddies. These findings have the potential to provide important guidance for initializating paired mesoscale eddies, ultimately contributing to improvements in SSHA forecast accuracy.

Publisher

American Geophysical Union (AGU)

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