Dr. Pielke ends his comment with a call for «independent assessments of the skill at these models at predicting climate metrics
including upper ocean heat content», which of course I have no problem with at all.
I don't need an assessment of the models at predicting climate metrics
including upper ocean heat content.
Not exact matches
The team, which
includes Professor Baldwin, will lead innovative new research, which aims to advance current understanding of three key conditions that influence seasonal weather across the continent — the North Atlantic
upper -
ocean heat content, Arctic sea - ice, and the stratosphere.
The authors note that more than 85 % of the global
heat uptake (Q) has gone into the
oceans,
including increasing the
heat content of the deeper
oceans, although their model only accounts for the
upper 700 meters.
DK12 used
ocean heat content (OHC) data for the
upper 700 meters of
oceans to draw three main conclusions: 1) that the rate of OHC increase has slowed in recent years (the very short timeframe of 2002 to 2008), 2) that this is evidence for periods of «climate shifts», and 3) that the recent OHC data indicate that the net climate feedback is negative, which would mean that climate sensitivity (the total amount of global warming in response to a doubling of atmospheric CO2 levels,
including feedbacks) is low.
Scientific confidence of the occurrence of climate change
include, for example, that over at least the last 50 years there have been increases in the atmospheric concentration of CO2; increased nitrogen and soot (black carbon) deposition; changes in the surface
heat and moisture fluxes over land; increases in lower tropospheric and
upper ocean temperatures and
ocean heat content; the elevation of sea level; and a large decrease in summer Arctic sea ice coverage and a modest increase in Antarctic sea ice coverage.