/ upwelling IPW/PDW
upwelling IPW/PDW
André Balestrini
La remontée d’eau1 (upwelling en anglais) est un phénomène océanographique qui se produit lorsque de forts vents marins (généralement des vents saisonniers) poussent l’eau de surface des océans, laissant ainsi un vide où peuvent remonter les eaux de fond et avec elles une quantité importante de nutriments.
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