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pro vyhledávání: '"Lukas Lobert"'
High-wind events predominantly cause the rapid breakdown of seasonal stratification on mid-latitude continental shelfs. It is well established that downwelling-favorable wind forcing, i.e., wind vectors with the coastline to their right (on the north
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::947a9c9b92549ab9ead0a3527d4e9cae
https://doi.org/10.5194/egusphere-egu23-10370
https://doi.org/10.5194/egusphere-egu23-10370
High-wind events predominantly cause the rapid breakdown of seasonal stratification on the continental shelf. Although previous studies have shown how coastal stratification depends on local wind-forcing characteristics, the locally observed ocean fo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37ae2bf52977958e8545de7ded7fa75b
https://doi.org/10.22541/essoar.167751639.99765608/v1
https://doi.org/10.22541/essoar.167751639.99765608/v1