Does anyone have the formula to
calculate the ocean heat content from temperature data.
Information to
calculate ocean heat content?
How did
they calculate ocean heat content at 2000 meters below sea level, prior to start of the ARGO program?
http://www.realclimate.org/index.php/archives/2011/01/2010-updates-to-model-data-comparisons/ in this post comment 36 Gavin says that models where not used to
calculate ocean heat content past 2003, so no one is using actual model output during this comparison.
The second plot shows
the calculated Ocean Heat Content from the «Callendar model» fitted with the above parameters, and compares it with the 0 - 700m data held by NOAA, based on Levitus.
Not exact matches
Ocean survey flight path and instrument deployment points over shaded ocean heat content (OHC) that was calculated from survey
Ocean survey flight path and instrument deployment points over shaded
ocean heat content (OHC) that was calculated from survey
ocean heat content (OHC) that was
calculated from survey data.
Rather than use a model - based estimate, as did Hansen (2005) and Trenberth (2009), the authors achieve this by
calculating it from observations of
ocean heat content (down to 1800 metres) from the PMEL / JPL / JIMAR data sets over the period July 2005 to June 2010 - a time period dominated by the superior ARGO - based system.
To
calculate the Earth's total
heat content, the authors used data of
ocean heat content from the upper 700 metres.
The models serve merely to quantify these basic facts more accurately,
calculate the regional climate response, and compute effects (such as the expected increase in
ocean heat content or sea level) which can be tested against observed data from the real world.
How is it that arguably the most important aspect of AGW (ie the
Ocean Heat Content) has not been
calculated from the model output past 2003?
Which implies that since the late» 40's - early» 50's we have had a data collection system deployed capable of measuring and tracking the annual TEMPERATURE of the top 2000 meters of the
oceans of the world (necessary to
calculate its
heat content)-- all of them — with a precision and accuracy in the millidegree range.
Because 5 gazillion Joules is a 0.2 C mixed layer (top ~ 300 meters) surface temperature rise (Figure 10, Historical
ocean heat content calculated from HadSST and OHC, Levitus, 2009).
When the first analyses of
Ocean Heat Content calculated from old temperature data from the
oceans where first published in the early 2000's, they were described as the «Smoking Gun».
Essentially, Huber and Knutti take the estimated global
heat content increase since 1850,
calculate how much of the increase is due to various estimated radiative forcings, and partition the increase between increasing
ocean heat content and outgoing longwave radiation.
«TCR and ECS are
calculated by regressing ensemble - average decadal mean forcing or forcing minus
ocean heat content change rate against ensemble - average temperature change.»
What are the error bars in
calculating the
heat content of an entire
ocean from the sparse, unreliable (pre-ARGO) temperature data available?
Bosse (Citizen Scientist / Public), 4.1 (± 0.43), Statistical (Same as June) Just as in the two years before I
calculate the value for the September - minimum of the arctic sea ice extent of the year n (NSIDC monthly mean for September) from the
Ocean Heat Content (0... 700m depth) northward 65 ° N during JJAS of the year n - 1.
Because you are fitting to look for a trend * after * selecting the data that looks flat, the real 95 % confidence interval of the trend in temperature (or
ocean heat content) over any of these intervals is much larger than what you are presumably
calculating.
This is in part because there are several open research questions regarding the accuracy with which
ocean heat content can be
calculated and applied.
As I understand it global temperatures are
calculated as anomalies, thus removing seasonal swings, but that
Heat Content is not, Now our dear planet has an elliptical orbit and is sometimes closer to the sun that others; sure, the shape of the land and
oceans doesn't mean that the amount of incoming solar radiation falling on the
oceans follows the Earths orbit, but it should be possible to work out the amount of incoming solar radiation each quarter.
A recently published estimate of Earth's global warming trend is 0.63 ± 0.28 W / m2, as
calculated from
ocean heat content anomaly data spanning 1993 - 2008.
Ocean heat content (1022 J) calculated from ocean potential temperature (CMIP5 variable «thetao»), assuming reference specific heat capacity 3985 J / kg K and density 1025 kg
Ocean heat content (1022 J)
calculated from
ocean potential temperature (CMIP5 variable «thetao»), assuming reference specific heat capacity 3985 J / kg K and density 1025 kg
ocean potential temperature (CMIP5 variable «thetao»), assuming reference specific
heat capacity 3985 J / kg K and density 1025 kg / m3.