Intensification of submesoscale frontogenesis and forward energy cascade driven by upper-ocean convergent flows
Abstract Upper-ocean fronts are an important component of the global climate system, regulating both the oceanic energy cycle and material transports. In the common paradigm, upper-ocean fronts are generated by frontogenesis at the mesoscale (20–300 km), driven predominantly by confluent horizontal...
| প্রধান লেখক: | , , |
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| বিন্যাস: | প্রবন্ধ |
| ভাষা: | English |
| প্রকাশিত: |
Nature Portfolio
2024-10-01
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| মালা: | Nature Communications |
| অনলাইন ব্যবহার করুন: | https://doi.org/10.1038/s41467-024-53551-4 |