Data We Use
ECCO state estimates faithfully reproduce a large number of ocean and sea ice observations from in situ and satellite instruments. We assimilate and constrain hundreds of millions of individual data from many sources.
The best part? Our solutions satisfy the laws of physics and thermodynamics.
We estimate all of the fields needed to evolve the ocean state over time. This includes temperature and salinity plus 3D momentum, sea surface height, density, ocean bottom pressure, sea ice, and snow. But it’s not all about the ocean and ice, the ECCO solution also includes estimates of the atmospheric state every six hours for the last few decades.
Observational Data Used to Constrain the Model
[New or updated items for ECCO Version 4 release 4 are indicated in
purple
.]Variable | Observations |
---|---|
Sea surface height | ERS-1/2 (1992-2001), TOPEX/Poseidon (1993-2005), GFO (2001-2007), ENVISAT (2002-2012), Jason-1 (2002-2008), Jason-2 (2008- 2017 ), CryoSat-2 (2011-2017 ), SARAL/AltiKa (2013-2017 ), Jason-3 (2016-2017) |
Global mean sea level | Average of mean sea level curves from AVISO, CSIRO, NOAA and U.Colorado (1993- 2017 ) |
In situ temperature | Argo floats (1995- 2017 ), CTDs (1992-2017 ), XBTs (1992-2017 ), marine mammals (APB 2004-2017 ), gliders (2003-2017), Ice-Tethered Profilers (ITP, 2004-2017 ), moorings (1992-2017) |
In situ salinity | CTDs (1992- 2017) , moorings (1992-2017 ), Argo floats (1997-2017 ), gliders (2003-2017), marine mammals (APB 2004-2017 ), ITP (2004-2017 ) |
Sea surface temperature | AVHRR (1992- 2017) |
Sea surface salinity | Aquarius (2011- 2015) |
Sea-ice concentration | SSM/I (1992-2009), SSMIS (2006- 2017) |
Ocean bottom pressure | GRACE (2002- 2016 ), JPL MASCON Solution |
T and S climatology | World Ocean Atlas 2009 |
Mean dynamic topography | DTU17MDT |