The potential forhydrographmoderation may be an important consideration in -ood-prone areas.
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Agriculture has changed thehydrograph, increasing peak runoff flows and shortening the length of runoff.
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Drainage density can affect the shape of a river'shydrographduring a rain storm.
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Although the pattern of the annualhydrographis fairly predictable, its magnitude is not.
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The record of flow over time is called ahydrograph.
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Another application involves the separation of groundwater flow and baseflow from streamflow in the field of catchment hydrology (i.e. a method ofhydrographseparation).
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More precisely, it produces the surface runoffhydrographas a response to a rainfallhydrographas input.
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In storm hydrology, an important consideration is the stream's dischargehydrograph, a record of how the discharge varies over time after a precipitation event.
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However, land management patterns that change thehydrographand/or vegetation cover can act to increase or decrease channel migration rates.
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Making this assumption can greatly simplify the analysis involved in constructing a unithydrograph, and it is necessary for the creation of a geomorphologic instantaneous unit hydrograph.
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The variability in discharge over the course of a year is commonly represented by ahydrographwith mean monthly discharge variations plotted over the annual time scale.
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