A year is primarily measured by the time it takes for the Earth to complete one full orbit around the Sun, which is about 365.25 days. We track this period using calendars, dividing the year into months and days. Due to the Earth's orbit not being exactly an integer number of days, we add leap days every four years (with exceptions) to keep the calendar aligned with the astronomical year.

Methods of Measuring a Year

• Astronomical Orbit : A year is the Earth's orbital period around the Sun, approximately 365.2425 days. This is the basis for the Gregorian calendar year.

• Calendrical Systems : The year is divided into 12 months with varying days, and leap years are introduced to correct the calendar.

• Seasonal Indicators : The year can also be measured by recurring natural phenomena such as equinoxes and solstices, which mark seasonal changes.

• Cultural and Personal Reflection : Beyond scientific measurement, a year can be perceived in terms of personal growth, relationships, and experiences, as depicted in artistic reflections like the song "Seasons of Love" and related documentaries.

Therefore, a year is a blend of astronomical measurement and human-constructed calendar systems designed to keep our sense of time synchronized with Earth's journey around the Sun. The conventional year is 365 days, with leap years to adjust for the fractional day differences. This is how "a year" is practically and conceptually measured.