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The difference has a pretty even distributed noise around the zero line so comparison of current ''integral'' with observations from the past (for climatic studies) should be possible with statistical proof and a consolidation of past and current measurements has actually been executed by the KNMI <ref>[https://cdn.knmi.nl/system/data_center_publications/files/000/068/325/original/CNT.pdf?1495621137 The Construction of a Central Netherlands Temperature]</ref>. | The difference has a pretty even distributed noise around the zero line so comparison of current ''integral'' with observations from the past (for climatic studies) should be possible with statistical proof and a consolidation of past and current measurements has actually been executed by the KNMI <ref>[https://cdn.knmi.nl/system/data_center_publications/files/000/068/325/original/CNT.pdf?1495621137 The Construction of a Central Netherlands Temperature]</ref>. | ||
Another interesting article on the subject is below. <ref>[https://rmets.onlinelibrary.wiley.com/doi/full/10.1002/joc.6528 Sampling frequency of climate data for the determination of daily temperature and daily temperature extrema]</ref> | |||
<references/> | <references/> | ||
[[Category:CumulusUtils]] | [[Category:CumulusUtils]] |