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The bloom index algorithm produces one value per day, a numeric code. The basic steps of the algorithm are
Average the chlorophyll data to nightly values.
Compute the rate of change and rate of growth.
Loop thru the time series. Conditions which would constitute the start of an event would be a large rate of growth (>0.45). If the rate of growth is larger than 0.80, then it may be an advection event. If an event lasts longer than a given number of days, then the event classifies as a bloom event. Conditions which will cause the event to end include
Invalid data.
An advective rate of growth immediately followed by a sizably large decrease, which leads us to believe that it really was an advection event.
If the mean growth rate over the window falls below zero, then we the event has been on a long downhill slide.
If the running cumulative sum of delta chl falls below zero, then we have less chlorophyll than when we started.
chlorophyll time series in micrograms/liter
The window length in days is required. This provides a period of time over which an event must sustain itself before being labeled a bloom.
None.
rate of change of hourly chlorophyll time series
rate of growth of hourly chlorophyll time series
cumulative sum of chlorophyll daily change since the beginning of an event
hourly chlorophyll values interpolated into the daily time series
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