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TZID:Pacific/Honolulu
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CLASS:PUBLIC
CREATED:20260906T094244Z
DESCRIPTION:“Plankton metabolism in the oligotrophic ocean” | Subantarctic mode waters (SAMW) form from deep winter Southern Ocean mixed layers and transport large amounts of carbon, nutrients, and oxygen to lower latitudes where they fuel primary productivity. Thanks to Argo floats, we now have much more information on the biogeochemical properties of these wintertime mixed layers and find substantial variability in nitrate, carbon, and oxygen concentrations in the different formation regions. In the case of carbon, we find increased concentrations in more recent years in the SAMW formation regions, likely due to the uptake of anthropogenic carbon from the atmosphere.\n\n
DTEND;TZID=Pacific/Honolulu:20240405T023000Z
DTSTAMP:20260906T094244Z
DTSTART;TZID=Pacific/Honolulu:20240405T010000Z
LAST-MODIFIED:20260906T094244Z
LOCATION:Marine Science Building 100
PRIORITY:5
SEQUENCE:0
SUMMARY;LANGUAGE=en-us:Oceanography Seminar - Sara Ferrón
TRANSP:OPAQUE
UID:178872376442493web-support-l@lists.hawaii.edu
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