Standardized records began in 1953
JMA standardized the subjects and methods of phenological observations and began the statistical series in 1953. Tokyo has earlier cherry records, but the standardized series has its own starting point. Its sample-tree observations moved to Yasukuni Shrine in 1966. Changes of site and tree provide context for long records.
What happens when a sample tree must be replaced
Sample trees can age or become diseased. JMA’s guideline calls for checking species and variety and choosing a relatively open setting without excessive shade. A primary sample tree is normally accompanied by one or more backup trees.
Before replacement, flowering dates and other observations are compared with the primary tree for at least three years; the backup showing the smallest differences is selected, and the change is reported. If the primary suddenly cannot be observed, a backup meeting the comparison requirement can supply reports in the established order. This maintains continuity rather than averaging several trees or choosing whichever has the most flowers. Observers also check nearby plants of the same kind for an unusually large difference from the sample.
A forecast estimates a future event
Forecasts use past flowering dates, temperature histories and expected weather to estimate a date yet to occur. Observation records a stage already reached. JMA ended its own cherry-opening forecasts after 2009 but continued opening and full-bloom observations. Private forecasts, official observations and a venue’s flower report describe different things. JMA’s 2009 discontinuation notice dates forecasts covering Japan except Okinawa and Amami to 1955. That forecasting history is distinct from the standardized observation series beginning in 1953.
A normal has a reference period
A normal provides a comparison based on observations over a stated period, such as 1991–2020 in current materials. It is not a timetable each year must follow. Reading the date alongside its reference period and species helps separate annual variation from longer-term change. These observations also inform research on climate and plant seasonality.