Segmenting datasets: Difference between revisions
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** [[Taylor's Frozen Turbulence| Taylor's frozen turbulence hypothesis]], etc ... | ** [[Taylor's Frozen Turbulence| Taylor's frozen turbulence hypothesis]], etc ... | ||
The act of chopping a time series into smaller subsets, i.e., segments, is effectively a form of low-pass (box-car) filtering. Hence, when estimating <math>\varepsilon</math> how to [[Segmenting datasets|segment]] the time series is usually a more important consideration than [[Detrending time series|detrending time series]]. This segmenting step dictates the minimum burst duration when setting-up your equipment. | |||
<div><ul> | |||
<li style="display: inline-block; vertical-align: top;"> [[File:Short timeseries.png|thumb|none|350px|Zoom of the first 512 s of the measured velocities shown above including the same trends]] | |||
</li> | |||
<li style="display: inline-block; vertical-align: top;"> [[File:Short_spectra.png|thumb|none|350px|Example velocity spectra of the short 512 s of records before and after different detrending techniques applied to the original 6h time series. The impact of the detrending method can be seen at the lowest frequencies only]] </li> | |||
</ul></div> | |||
[[Category:Velocity point-measurements]] | [[Category:Velocity point-measurements]] |
Revision as of 14:17, 30 November 2021
Once the raw data has gone through QA/QC, then you must:
- Split the time series into shorter segments by considering:
- time and length scales of turbulence
- stationarity of the segment
- Taylor's frozen turbulence hypothesis, etc ...
The act of chopping a time series into smaller subsets, i.e., segments, is effectively a form of low-pass (box-car) filtering. Hence, when estimating [math]\displaystyle{ \varepsilon }[/math] how to segment the time series is usually a more important consideration than detrending time series. This segmenting step dictates the minimum burst duration when setting-up your equipment.
-
Zoom of the first 512 s of the measured velocities shown above including the same trends -
Example velocity spectra of the short 512 s of records before and after different detrending techniques applied to the original 6h time series. The impact of the detrending method can be seen at the lowest frequencies only