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This method is extensively used in hydrologic frequency analysis.
There are many frequency models which are now used for determining hydrologic frequency of flood.
Hydrologic frequency analysis is a statistical technique for the assessment of natural hazards, particularly the so-called water hazards caused exclusively by extreme hydrologic events.
The increasing effort to develop and apply nonstationary models in hydrologic frequency analyses under changing environmental conditions can be frustrated when the additional uncertainty related to the model complexity is accounted for along with the sampling uncertainty.
Hydrologic frequency analysis is commonly used by engineers and hydrologists to provide the basic information on planning, design and management of hydraulic and water resources systems under the assumption of stationarity.
In particular, L-moments based regional frequency analysis (RFA-LM) has being adopted as the standard method for hydrologic frequency analysis in many parts of the world and for many other applications relating to hydrological extremes.
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Then, the sites' hydrologic responses to different rainfall conditions were simulated over 30 year's hourly historical records, and the statistics of rainfall/runoff events were plotted into hydrological frequency curves to represent the site hydrology.
Then raw and adjusted MQPEs serve as inputs to the NWS distributed hydrologic model-threshold frequency framework (DHM-TF).
Although most of the hydrologic studies conducted the frequency analysis for hydrologic parameters, it seems that few studies use such analysis for wind speed, especially for Iran.
The objective of frequency analysis of hydrologic data is to relate the magnitude of extreme events to their frequency of occurrence using probability distributions.
These findings indicate that changes to the hydrologic cycle, in particular the frequency of moderate to heavy rainfall events, could have a profound effect on the transmission rates of some mosquito-borne diseases.
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