We asked you to support your claim that the
resolution of the oceanic
temperature data is not sufficient to make a determination of a trend in
ocean heat content, which you have yet to provide.
The Group for High
Resolution SST (GHRSST) is a follow on activity form the Global Ocean Data Assimilation Experiment (GODAE) high - resolution sea surface temperature pilot project (GHRSST - PP) provides a new generation of global high - resolution (< 10 km) SST data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and del
Resolution SST (GHRSST) is a follow on activity form the Global
Ocean Data Assimilation Experiment (GODAE) high - resolution sea surface temperature pilot project (GHRSST - PP) provides a new generation of global high - resolution (< 10 km) SST data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and delayed m
Data Assimilation Experiment (GODAE) high -
resolution sea surface temperature pilot project (GHRSST - PP) provides a new generation of global high - resolution (< 10 km) SST data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and del
resolution sea surface
temperature pilot project (GHRSST - PP) provides a new generation of global high -
resolution (< 10 km) SST data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and del
resolution (< 10 km) SST
data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and delayed m
data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and delayed mode.
To estimate the uncertainty range (2σ) for mean tropical SST cooling, we consider the error contributions from (a) large - scale patterns in the
ocean data temperature field, which hamper a direct comparison with a coarse -
resolution model, and (b) the statistical error for each reconstructed paleo -
temperature value.