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Land–Ocean Pathways Linking Indo‐Pacific Sea Surface Temperature Variability to Tropical Atlantic Coastal Salinity

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Bibliographic Details
Published in:Journal of Geophysical Research : Oceans
Format: Online Article RSS Article
Published: 2026
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container_title Journal of Geophysical Research : Oceans
description
discipline_display Physical Sciences
discipline_facet Physical Sciences
format Online Article
RSS Article
genre Journal Article
id rss_article:45709
institution FRELIP
journal_source_facet Journal of Geophysical Research : Oceans
publishDate 2026
publishDateSort 2026
record_format rss_article
spellingShingle Land–Ocean Pathways Linking Indo‐Pacific Sea Surface Temperature Variability to Tropical Atlantic Coastal Salinity
Earth Sciences
Earth Sciences
Physical Sciences
sub_discipline_display Earth Sciences
sub_discipline_facet Earth Sciences
subject_display Earth Sciences
Earth Sciences
Physical Sciences
Earth Sciences
Earth Sciences
Physical Sciences
subject_facet Earth Sciences
Earth Sciences
Physical Sciences
title Land–Ocean Pathways Linking Indo‐Pacific Sea Surface Temperature Variability to Tropical Atlantic Coastal Salinity
title_auth Land–Ocean Pathways Linking Indo‐Pacific Sea Surface Temperature Variability to Tropical Atlantic Coastal Salinity
title_full Land–Ocean Pathways Linking Indo‐Pacific Sea Surface Temperature Variability to Tropical Atlantic Coastal Salinity
title_fullStr Land–Ocean Pathways Linking Indo‐Pacific Sea Surface Temperature Variability to Tropical Atlantic Coastal Salinity
title_full_unstemmed Land–Ocean Pathways Linking Indo‐Pacific Sea Surface Temperature Variability to Tropical Atlantic Coastal Salinity
title_short Land–Ocean Pathways Linking Indo‐Pacific Sea Surface Temperature Variability to Tropical Atlantic Coastal Salinity
title_sort land–ocean pathways linking indo‐pacific sea surface temperature variability to tropical atlantic coastal salinity
topic Earth Sciences
Earth Sciences
Physical Sciences
url https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025JC023816?af=R