FN Archimer Export Format
PT J
TI Observing the full ocean volume using Deep Argo floats
BT 
AF Zilberman, Nathalie V.
   Thierry, Virginie
   King, Brian
   Alford, Matthew
   André, Xavier
   Balem, Kevin
   Briggs, Nathan
   Chen, Zhaohui
   Cabanes, Cecile
   Coppola, Laurent
   Dall’Olmo, Giorgio
   Desbruyères, Damien
   Fernandez, Denise
   Foppert, Annie
   Gardner, Wilford
   Gasparin, Florent
   Hally, Bryan
   Hosoda, Shigeki
   Johnson, Gregory C.
   Kobayashi, Taiyo
   Le Boyer, Arnaud
   Llovel, William
   Oke, Peter
   Purkey, Sarah
   Remy, Elisabeth
   Roemmich, Dean
   Scanderbeg, Megan
   Sutton, Philip
   Walicka, Kamila
   Wallace, Luke
   van Wijk, Esmee M.
AS 1:1;2:2;3:3;4:1;5:4;6:2;7:3;8:5;9:19;10:6,7;11:8;12:2;13:9;14:10;15:11;16:12;17:13;18:14;19:15;20:14;21:1;22:19;23:16;24:1;25:17;26:1;27:1;28:9;29:18;30:13;31:10,16;
FF 1:;2:PDG-ODE-LOPS-OH;3:;4:;5:PDG-REM-RDT-SIIM;6:PDG-ODE-LOPS-OH;7:;8:;9:;10:;11:;12:PDG-ODE-LOPS-OH;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;25:;26:;27:;28:;29:;30:;31:;
C1 Integrative Oceanography Division and Climate, Atmospheric Science, and Physical Oceanography Division, Scripps Institution of Oceanography, University of California, San Diego, CA, United States
   Univ Brest, CNRS, Ifremer, IRD, Laboratoire d’Océanographie Physique et Spatiale (LOPS), IUEM, F29280, Plouzané, France
   National Oceanography Centre, Southampton, United Kingdom
   Ifremer, RDT, F29280, Plouzané, France
   Key Laboratory of Physical Oceanography/Institute for Advanced Ocean Science/Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao, China
   Laboratoire d’Océanographie de Villefranche, UMR 7093, CNRS, Sorbonne Université, Villefranche-sur-Mer, France
   CNRS, OSU STAMAR, UAR 2017, Sorbonne Université, Paris, France
   Sezione di Oceanografia, National Institute of Oceanography and Applied Geophysics, OGS, Trieste, Italy
   National Institute of Water and Atmospheric Research, Wellington, New Zealand
   Australian Antarctic Program Partnership, Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, TAS, Australia
   Department of Oceanography, Texas A&M University, College Station, TX, United States
   Université de Toulouse, LEGOS (IRD/UPS/CNES/CNRS), Toulouse, France
   University of Tasmania, Hobart, TAS, Australia
   Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
   Pacific Marine Environmental Laboratory, National Oceanic and Atmospheric Administration, Seattle, WA, United States
   Environment, Commonwealth Scientific and Industrial Research Organisation (CSIRO), Hobart, TAS, Australia
   Operational Oceanography Department, Mercator Ocean International, Toulouse, France
   National Oceanography Centre, British Oceanographic Data Centre, Liverpool, United Kingdom
   Univ Brest, CNRS, Ifremer, IRD, Laboratoire d’Océanographie Physique et Spatiale (LOPS), IUEM, F29280, Plouzané, France
C2 UNIV CALIF SAN DIEGO, USA
   IFREMER, FRANCE
   NOC, UK
   IFREMER, FRANCE
   UNIV OCEAN CHINA, CHINA
   UNIV SORBONNE, FRANCE
   CNRS, FRANCE
   OGS, ITALY
   NIWA, NEW ZEALAND
   UNIV TASMANIA, AUSTRALIA
   UNIV TEXAS A&M, USA
   UNIV TOULOUSE, FRANCE
   UNIV TASMANIA, AUSTRALIA
   JAMSTEC, JAPAN
   NOAA, USA
   CSIRO, AUSTRALIA
   MERCATOR OCEAN, FRANCE
   NOC, UK
   CNRS, FRANCE
SI BREST
SE PDG-ODE-LOPS-OH
   PDG-REM-RDT-SIIM
UM LOPS
IN WOS Ifremer UPR
   WOS Ifremer UMR
   WOS Cotutelle UMR
   DOAJ
   copubli-france
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
   copubli-sud
IF 3.7
TC 1
UR https://archimer.ifremer.fr/doc/00864/97578/106455.pdf
LA English
DT Article
DE ;deep ocean;ocean observation;ocean heat content (OHC);sea level (SL);ocean deoxygenation;bathymetry accuracy;ocean mixing;sediment transport
AB The ocean is the main heat reservoir in Earth’s climate system, absorbing most of the top-of-the-atmosphere excess radiation. As the climate warms, anomalously warm and fresh ocean waters in the densest layers formed near Antarctica spread northward through the abyssal ocean, while successions of warming and cooling events are seen in the deep-ocean layers formed near Greenland. The abyssal warming and freshening expands the ocean volume and raises sea level. While temperature and salinity characteristics and large-scale circulation of upper 2000 m ocean waters are well monitored, the present ocean observing network is limited by sparse sampling of the deep ocean below 2000 m. Recently developed autonomous robotic platforms, Deep Argo floats, collect profiles from the surface to the seafloor. These instruments supplement satellite, Core Argo float, and ship-based observations to measure heat and freshwater content in the full ocean volume and close the sea level budget. Here, the value of Deep Argo and planned strategy to implement the global array are described. Additional objectives of Deep Argo may include dissolved oxygen measurements, and testing of ocean mixing and optical scattering sensors. The development of an emerging ocean bathymetry dataset using Deep Argo measurements is also described. 
PY 2023
PD NOV
SO Frontiers In Marine Science
SN 2296-7745
PU Frontiers Media SA
VL 10
UT 001124521000001
DI 10.3389/fmars.2023.1287867
ID 97578
ER

EF