FN Archimer Export Format
PT J
TI Global ocean freshening, ocean mass increase and global mean sea level rise over 2005–2015
BT 
AF Llovel, William
   Purkey, S.
   Meyssignac, B.
   Blazquez, A.
   Kolodziejczyk, Nicolas
   Bamber, J.
AS 1:1,3;2:2;3:1;4:1;5:5;6:4;
FF 1:;2:;3:;4:;5:;6:;
C1 LEGOS, CNES/IRD/CNRS/UPS, Toulouse, France
   Scripps Institution of Oceanography, La Jolla, CA, USA
   LOPS, University of Brest/IFREMER/IRD/CNRS, Brest, France
   University of Bristol, Bristol, UK
   LOPS, University of Brest/IFREMER/IRD/CNRS, Brest, France
C2 OBSERV MIDI PYRENEES, FRANCE
   UNIV CALIF SAN DIEGO, USA
   CNRS, FRANCE
   UNIV BRISTOL, UK
   UBO, FRANCE
UM LOPS
IN WOS Cotutelle UMR
   DOAJ
   copubli-france
   copubli-europe
   copubli-int-hors-europe
IF 3.998
TC 32
UR https://archimer.ifremer.fr/doc/00597/70940/69181.pdf
LA English
DT Article
AB Global mean sea level has experienced an unabated rise over the 20th century. This observed rise is due to both ocean warming and increasing continental freshwater discharge. We estimate the net ocean mass contribution to sea level by assessing the global ocean salt budget based on the unprecedented amount of in situ data over 2005–2015. We obtain the ocean mass trends of 1.30 ± 1.13 mm · yr−1 (0–2000 m) and 1.55 ± 1.20 mm · yr−1 (full depth). These new ocean mass trends are smaller by 0.63–0.88 mm · yr−1 compared to the ocean mass trend estimated through the sea level budget approach. Our result provides an independent validation of Gravity Recovery And Climate Experiment (GRACE)-based ocean mass trend and, in addition, places an independent constraint on the combined Glacial Isostatic Adjustment – the Earth’s delayed viscoelastic response to the redistribution of mass that accompanied the last deglaciation- and geocenter variations needed to directly infer the ocean mass trend based on GRACE data. 
PY 2019
PD NOV
SO Scientific Reports
SN 2045-2322
PU Springer Science and Business Media LLC
VL 9
IS 1
UT 000499223000001
DI 10.1038/s41598-019-54239-2
ID 70940
ER

EF