Downsampling

Downsamplers require at least two components:

• Aggregation Function - A mathematical function that determines how to merge the values in the interval. Aggregation functions from the Aggregation documentation are used for the function.

For example, take the following time series A and B. The data points cover a 70 second time span, a value every 10 seconds. Let’s say we want to downsample that to 30 seconds since the user is looking at a graph for a wider time span. Additionally we’re grouping these two series into one using a sum aggregator. We can specify a downsampler of 30s-sum that will create 30 second buckets and sum all of the data points in each bucket. This will give us three data points for each series:

As you can see, for each time series, we generate a synthetic series with a timestamp normalized on interval boundaries (every 30 seconds) so that we’ll have a value at t0, t0+30s and t0+60s. Each interval, or bucket, will contain the data points that are inclusive of the bucket timestamp (the start) and exclusive of the following bucket’s timestamp (the end). In this case, the first bucket would extend from t0 to t0+29.9999s. Using the provided aggregator, all of the values are merged into a new one. E.g. for series A, we sum up the values for t0, t0+10s and t0+20s to arrive at a new value of at t0. Finally, the query is group-by’d using sum so that we add the two synthetic time series. At this time, OpenTSDB always performs group-by aggregation after downsampling.

Note

For early versions of OpenTSDB, the actual time stamps for the new data points will be an average of the time stamps for each data point in the time span. As of 2.1 and later, the timestamp for each point is aligned to the start of a time bucket based on a modulo of the current time and the downsample interval.

Downsampled timestamps are normalized based on the remainder of the original data point timestamp divided by the downsampling interval in milliseconds, i.e. the modulus. In Java the code is timestamp - (timestamp % interval_ms). For example, given a timestamp of 1388550980000, or 1/1/2014 04:36:20 UTC and an hourly interval that equates to 3600000 milliseconds, the resulting timestamp will be rounded to 1388548800000. All data points between 4 and 5 UTC will wind up in the 4 AM bucket. If you query for a day’s worth of data downsampling on 1 hour, you will receive 24 data points (assuming there is data for all 24 hours).

When using the 0all- interval, the timestamp of the result will be the start time of the query.

Normalization works very well for common queries such as a day’s worth of data downsampled to 1 minute or 1 hour. However if you try to downsample on an odd interval, such as 36 minutes, then the timestamps may look a little strange due to the nature of the modulus calculation. Given an interval of 36 minutes and our example above, the interval would be 2160000 milliseconds and the resulting timestamp 1388549520 or 04:12:00 UTC. All data points between 04:12 and 04:48 would wind up in a single bucket.

Starting with OpenTSDB 2.3, users can specify calendar based downsampling instead of the quick modulus method. This is much more useful for reporting purposes such as looking at values relating to human times such as months, weeks or days. Additionally downsampling can account for timezones and incorporate daylight savings time shifts and zone offsets.

To use calendar boundaries, check the documentation for the endpoint you’re making a query from. For example, the V2 URI endpoint has a specific timezone parameter to be used such as &timezone=Asia/Kabul and calendar based downsampling is enabled by appending a c to the interval time units as in &m=sum:1dc-sum:my.metric. For JSON queries, a separate timezone field is used at the top level along with a useCalendar boolean flag. If no timezone is provided, calendars use UTC time.

With calendar downsampling, the first interval is snapped to January 1st at 00:00:00 of the query year in the timezone specified. From there, the interval buckets are calculated until the end of the query. Each bucket is marked with the timestamp of the start of the bucket, inclusive, and includes all values until the start of the next bucket, exclusive.

Fill Policies

Downsampling is often used to align timestamps to avoid interpolation when performing a group-by. Because OpenTSDB does not impose constraints on time alignment or when values are supposed to exist, such constraints must be specified at query time. When performing a group-by aggregation with downsampling, if all series are missing values for an expected interval, nothing is emitted. For example, if a series is writing data every minute from t0 to t0+6m, but for some reason the source fails to write data at t0+3m, only 5 values will be serialized when the user may expect 6. With fill policies in 2.2 and later, you can now choose what value is emitted for so that the user (or application) will see that a value was missing for a specific timestamp instead of having to figure out which timestamp was missing. Fill policies simply emit a pre-defined value any time a downsample bucket is empty.

Available polices include:

• None (none) - The default behavior that does not emit missing values during serialization and performs linear interpolation (or otherwise specified interpolation) when aggregating series.

• Null (null) - Same behavior as NaN except that during serialization it emits a null instead of a NaN.

• Zero (zero) - Substitutes a zero when a timestamp is missing. The zero value will be incorporated in aggregated results.

To use a fill policy, append the policy name (the terms in parentheses) to the end of the downsampling aggregation function separated by a hyphen. E.g. 1h-sum-nan or 1m-avg-zero.

In this example we have data reported every 10 seconds and we want to enforce a query-time policy of 10 seconds reporting by downsampling every 10 seconds and filling missing values with NaNs via 10s-sum-nan:

If we requested the output without a fill policy, no value or timestamp at t0+20s or t0+40s would be emitted. Additionally, values at t0+30s and t0+50s for series B would be linearly interpolated to fill in values to be summed with series A.