Discussion Overview
The discussion revolves around the terminology and concepts related to a specific period of time when the sun's elevation above the horizon is the same as on a previous day. Participants explore the definitions of various solar days and related metrics, including the apparent solar day and mean solar day, while considering the implications of solar elevation and azimuth.
Discussion Character
- Exploratory
- Debate/contested
- Technical explanation
Main Points Raised
- One participant asks for the term describing a day when the sun's elevation is constant compared to the previous day.
- Another participant suggests that the term might be "apparent solar day," but this is contested.
- Some participants clarify that the sun's elevation changes daily, particularly through the seasons, complicating the notion of a consistent elevation day.
- There is a discussion about the difference between solar time based on elevation versus azimuth, with some participants arguing that solar time is more accurately defined by azimuth.
- A participant expresses interest in determining the best days for observing planets based on the sun's elevation, seeking a metric that compares the elevation of planets to that of the sun.
- Another participant mentions elongation as a related metric, though it does not directly address the vertical aspect of solar elevation.
Areas of Agreement / Disagreement
Participants do not reach a consensus on the specific term for the time interval when the sun's elevation matches that of the previous day. There are competing views regarding the definitions of solar days and the relevance of elevation versus azimuth in solar time calculations.
Contextual Notes
Participants note that the sun's elevation is not constant throughout the year, and the relationship between apparent solar time and mean solar time is complex, involving factors such as the equation of time and the analemma. The discussion highlights the variability in solar measurements and the challenges in defining specific terms.