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The following paper provides lots of details
http://www.ncdc.noaa.gov/oa/climate/research/sst/papers/SEA.temps08.pdf
So, the 10 warmest years have "cooled off" under v3, with the exception of 2002, which remained the same. But, if they adjusted the ship-buoy data were adjusted for ships, then they would be warmer.
Evo; About satellite data:
http://www.ncdc.noaa.gov/oa/climate/research/sst/papers/SEA.temps08.pdf
Note that if the ship–buoy bias were also adjusted with
respect to the ships, then the most recent years would
be warmer, because the ship–buoy difference tends to
be positive and because of the increasing number of
buoy observations. However, as discussed above, these
differences are well within the 95% confidence limits.
The rankings of the
warmest 10 yr are similar for both, with 2005 the warmest
for both followed by 1998, a year with a strong warm
ENSO episode (Table 6).
Rank Merged.v2 Merged.v3
1 2005 0.41 2005 0.40
2 1998 0.38 1998 0.37
3 2002 0.36 2003 0.36
4 2003 0.36 2002 0.35
5 2006 0.35 2006 0.33
6 2004 0.34 2004 0.32
7 2001 0.30 2001 0.29
8 1997 0.27 1997 0.25
9 1999 0.20 1995 0.18
10 1995 0.19 1999 0.17
So, the 10 warmest years have "cooled off" under v3, with the exception of 2002, which remained the same. But, if they adjusted the ship-buoy data were adjusted for ships, then they would be warmer.
Evo; About satellite data:
That is because
both ERSST.v3 and OI.v2 incorporate bias-adjusted
satellite data.
The ERSST.v3 is improved by explicitly including
bias-adjusted satellite infrared SST estimates.
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