Not exact matches
In the quantification of the European -
averaged temperature and precipitation, the areas where the station density is too sparse to make reliable
estimates of
daily temperature and precipitation are filled - in by the 1981 - 2010 climatology of the CRU TS 4.01 dataset from the Climatic Research Unit (University of East Anglia, UK).
BoM CDO RAW data in this analysis are calculated from the annual
average of
daily temperatures for each year and are subject to the usual discrepancies such as missing days, but are identical to BoM annual
estimates except for occasional 0.1 C variations caused by the BoM
averaging monthly
averages for annual calculations instead of
averaging all available days per year for annual calculations.
The gridded projections were aggregated to regional
estimates by first transforming the
daily min,
average, or maximum
temperature at the grid scale, then aggregating to regions using a weighted
average.
In its answers to questions about the procedure used to
estimate a record hot day on January 7, the BoM revealed that a more detailed analysis of the January heat event, including changes in
daily average temperatures, has been submitted to the peer - reviewed Bulletin of the Australian Meteorological and Oceanographic Society (BAMOS).