NOAA Optimum Interpolation (OI) SST, V2

Produced weekly/monthly on a 1° grid. The analysis uses in situ and satellite SST's plus SST's simulated by sea-ice cover. Before the analysis is computed, the satellite data is adjusted for biases.

The optimum interpolation (OI) sea surface temperature (SST) analysis is produced weekly on a one-degree grid. The analysis uses in situ and satellite SSTs plus SSTs simulated by sea ice cover. Before the analysis is computed, the satellite data is adjusted for biases using the method of Reynolds (1988) and Reynolds and Marsico (1993). A description of the OI analysis can be found in Reynolds and Smith (1994). The bias correction improves the large scale accuracy of the OI.
Temporal Coverage:
1) Weekly means from 1981/10/29 to 1989/12/28.
2) Weekly means from 1989/12/31 to present.
3) Monthly means from 1981/12 to present
For the more recent period, 1990-present, the weeks are defined to be centered on Wednesday. During the period 1981-1989, the weeks are centered on Sunday.

References:
Reynolds, R.W., N.A. Rayner, T.M. Smith, D.C. Stokes, and W. Wang, 2002: An improved in situ and satellite SST analysis for climate. J. Climate, 15, 1609-1625.

Variables
SST (°C)
ZonalGlobal by 1.0 deg
Meridional98.5S to 89.5N by 1.0 deg
Verticalsea surface  
TemporalOct 1981 to Oct 2007 by monthly/weekly
Static?no
VolumeWeekly means from 1981/10/29 to 1989/12/28: 111 Mbytes; from 1989/12/31 to present: 242 Mbytes. Monthly means from 1981/12 to present: 81 Mbytes
ServerDODS & LAS; public
Sourcehttp://www.emc.ncep.noaa.gov/research/cmb/sst_analysis/ 
AcquiredNov 13, 2006 (last updated 11/2007)
APDRC contactYongsheng Zhang
Supplements/disk/a1/oisst/readme.f