| Literature DB >> 33089187 |
Christine Blume1,2,3, Manuel Schabus3,4.
Abstract
As experts, scientists must inform the public and political actors about relevant topics by providing a well-balanced analysis and overview of existing as well as missing scientific evidence. Particularly in cases where evidence is not solid, they must remain objective and not fan fear. Maintaining good scientific practice can be challenging, especially when a debate is emotionally charged and simple answers for complex issues are demanded. Recently, this was the case with the debate about (perennial) standard time vs. daylight saving time. In this publication, we address the common misconceptions and pitfalls for good scientific practice that accompany this discussion and deduce suggestions for future directions, which may help resolve them. Beyond this, we argue that it is not wise to simply "explain away" the public opinion or preference and we therefore recommend strategies that could support a discourse aiming at getting the public "on board". Finally, we suggest that, in societies where the light environment is becoming increasingly complex, it may be time to reconsider the prevailing current relationships between solar and social clocks.Entities:
Keywords: clock change; daylight saving time; social jetlag; standard time
Year: 2020 PMID: 33089187 PMCID: PMC7445807 DOI: 10.3390/clockssleep2010003
Source DB: PubMed Journal: Clocks Sleep ISSN: 2624-5175
Figure 1Modelled changes in circadian timing and social jetlag across a time zone for different levels of evening light (range 0–100 lux, cf. numbers on the lines). (A) Core body temperature minimum (Cmin) indicating the minimum of the circadian wake propensity. Cmin occurs later in western parts of a time zone at low levels of evening light, as indicated by the smaller slope of the lines. With increasing levels of evening light though, the effect of the time zone position disappears, as indicated by the steepening slope. (B) Social jetlag is larger in the western parts of a time zone (cf. smaller slope) but decreases with increasing levels of evening light (cf. increasing slope). Note that a 15° shift to the east (west) within a time zone corresponds to an advance (delay) in solar noon by one hour relative to clock time. Abbreviations: Cmin = core body temperature minimum; hrs = hours. Adapted from Skeldon et al. [22].