Construct · 2 fields · 2 citations

return period: one construct, many systems

One name. One construct. Different systems. One map.

● invariant · one construct, two systems Nearest construct by meaning·not indexed
same extreme-event frequency statistic, applied to a different hazardreturnperiod2 SYSTEMSFlood return periodGUMBEL · FLOODSEarthquake recurrenceSCHWARTZ · FAULTS

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2026

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Hydrology

Average time between floods of a given size

In hydrology, the return period (or recurrence interval) is the average time between events of a given magnitude or larger: a 100-year flood is one whose annual exceedance probability is 1/100, so it recurs on average once per century, though not on any fixed schedule. Gumbel's 1941 The return period of flood flows applied extreme-value statistics to series of annual flood maxima, formalising the link between an event's size and the long-run average interval between exceedances. The referent is a frequency statistic for threshold-exceeding events, estimated by fitting an extreme-value distribution to a record, and it is the same construct that reappears for earthquakes and other rare hazards.[1]

Unit
Average number of years between events equalling or exceeding a given magnitude (the reciprocal of the annual exceedance probability)
Recovery means
Not applicable
Measured by
Estimated by fitting an extreme-value distribution (e.g. Gumbel or GEV) to an annual-maxima series and inverting the exceedance probability

Seismology

Average time between earthquakes on a fault

In seismology, the recurrence interval is the average time between earthquakes of a given magnitude or larger on a fault or within a region, the same renewal and extreme-value construct used for floods but applied to seismic hazard. Schwartz and Coppersmith's 1984 Fault behavior and characteristic earthquakes: Examples from the Wasatch and San Andreas fault zones used fault-offset and paleoseismic evidence to estimate how often characteristic earthquakes recur. The referent is the long-run mean interval between threshold-exceeding ruptures, estimated from instrumental, historical, and paleoseismic records, identical in form to a flood return period though realised in a different physical system.[2]

Unit
Average number of years between earthquakes equalling or exceeding a given magnitude on a fault or in a region
Recovery means
Not applicable
Measured by
Estimated from dated prior ruptures in paleoseismic trenches, slip-rate data, and magnitude-frequency relations

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Nearby constructs

flashiness1 fields · 1 citationsanchor · a single construct in hydrologybankfull discharge1 fields · 1 citationsanchor · a single construct in hydrologyconstruct6 fields · 7 citationsjingle · one name, six constructs

References

  1. Gumbel, E. J. (1941). The return period of flood flows. The Annals of Mathematical Statistics, 12(2), 163–190. https://doi.org/10.1214/aoms/1177731747
  2. Schwartz, D. P., & Coppersmith, K. J. (1984). Fault behavior and characteristic earthquakes: Examples from the Wasatch and San Andreas fault zones. Journal of Geophysical Research: Solid Earth, 89(B7), 5681–5698. https://doi.org/10.1029/JB089iB07p05681

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