Downcast profiles from Seacat CTD on MacLane pump from R/V Oceanus OC449-02 and OC449-03 in the Eastern North Atlantic and Indian oceans in 2008 (SIRENA project)

<p>CTD data from Lam SBE19plus (Seacat) attached to end of the MacLane pump line - <b>Down&nbsp; Casts</b><br /> <b>Note: </b>These data not collected on R/V Islandia ISL0109 cruise<br /> <br /> <b>PI's Note/09May2011:</b><br /&...

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Bibliographic Details
Main Author: Phoebe J. Lam
Format: Dataset
Language:unknown
Published: Biological and Chemical Oceanography Data Management Office (BCO-DMO) 2011
Subjects:
Online Access:https://search.dataone.org/view/sha256:ee60a41bd677ec86fc218e247a0556378d31e27c1c65a94a3c0e03254f750fe1
Description
Summary:<p>CTD data from Lam SBE19plus (Seacat) attached to end of the MacLane pump line - <b>Down&nbsp; Casts</b><br /> <b>Note: </b>These data not collected on R/V Islandia ISL0109 cruise<br /> <br /> <b>PI's Note/09May2011:</b><br /> In comparing my pump seacat CTD to the ship's CTD, I've discovered that the ship's CTD's fluorescence and beam attenuation are no good, at least for OC449-3. The ship's fluorometer was clearly just not working. &nbsp;The ship's transmissometer misbehaved in a more subtle manner--oceanographically consistent, but of a different pattern than my pump seacat data. &nbsp;I concluded that my pump seacat CTD's transmissometer is the &quot;correct&quot; one by comparing to discrete particulate carbon measurements on particles collected on my pumps. &nbsp;Both particulate carbon concentrations and beam attenuation from my pump seacat CTD show a minimum at 500m at OC449-3 station 3, whereas the ship's CTD shows an anomalous minimum in subsurface beam attenuation at station 2, which is not seem in the particulate carbon concentrations.</p>