Water temperature and salinity data from southern elephant seals from Marion Island

Over the last decade, several hundred seals have been equipped with conductivity-temperature-depth sensors in the Southern Ocean for both biological and physical oceanographic studies. A calibrated collection of seal-derived hydrographic data is now available, consisting of more than 165,000 profile...

Full description

Bibliographic Details
Main Authors: Roquet, Fabien, Wunsch, Stefan, Forget, Gael, Heimbach, Patrick, Guinet, Christophe, Reverdin, Gilles, Charrassin, Jean-Benoît, Bailleul, Frederic, Costa, Daniel P, Huckstadt, Luis A, Goetz, Kimberly T, Kovacs, Kit Maureen, Lydersen, Christian, Biuw, Martin, Nøst, Ole Anders, Bornemann, Horst, Plötz, Joachim, Bester, Marthán Nieuwoudt, McIntyre, Trevor, Muelbert, Monica C, Hindell, Mark A, McMahon, Clive R, Williams, Guy, Harcourt, Robert, Field, Iain C, Chafik, Leon, Nicholls, Keith W, Boehme, Lars, Fedak, Mike A
Format: Dataset
Language:English
Published: PANGAEA 2013
Subjects:
MMT
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.831364
https://doi.org/10.1594/PANGAEA.831364
Description
Summary:Over the last decade, several hundred seals have been equipped with conductivity-temperature-depth sensors in the Southern Ocean for both biological and physical oceanographic studies. A calibrated collection of seal-derived hydrographic data is now available, consisting of more than 165,000 profiles. The value of these hydrographic data within the existing Southern Ocean observing system is demonstrated herein by conducting two state estimation experiments, differing only in the use or not of seal data to constrain the system. Including seal-derived data substantially modifies the estimated surface mixedlayer properties and circulation patterns within and south of the Antarctic Circumpolar Current. Agreement with independent satellite observations of sea ice concentration is improved, especially along the East Antarctic shelf. Instrumented animals efficiently reduce a critical observational gap, and their contribution to monitoring polar climate variability will continue to grow as data accuracy and spatial coverage increase.