2.a hyetograph is a graphical representation of

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Hydrograph

Definition of hyetograph. Love words? Keep scrolling for more. Learn More about hyetograph. Statistics for hyetograph Look-up Popularity. Get Word of the Day daily email! Test Your Vocabulary. Spell words. Make bears.Dictionary H Hyetograph hyetograph. See all 5 definitions of hyetograph. Parts of speech for Hyetograph noun.

Full grammatical hierarchy of Hyetograph. This is a rare but used term. It occurs in the pages of specialized literature and in the speech of educated people. All definitions of hyetograph hyetograph pronunciation The plural of hyetograph. Words starting with h Words starting with hy Words starting with hye Words starting with hyet Words starting with hyeto Words starting with hyetog Words starting with hyetogr Words starting with hyetogra Words starting with hyetograp Words starting with hyetograph Words ending with h Words ending with ph Words ending with aph Words ending with raph Words containing the letters h Words containing the letters h,y Words containing the letters h,y,e Words containing the letters h,y,e,t Words containing the letters h,y,e,t,o Words containing the letters h,y,e,t,o,g Words containing h Words containing hy Words containing hye Words containing hyet Words containing hyeto Words containing hyetog.

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2.a hyetograph is a graphical representation of

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If you continue browsing the site, you agree to the use of cookies on this website. See our User Agreement and Privacy Policy. See our Privacy Policy and User Agreement for details. Published on Aug 22, SlideShare Explore Search You. Submit Search. Home Explore. Successfully reported this slideshow. We use your LinkedIn profile and activity data to personalize ads and to show you more relevant ads.

You can change your ad preferences anytime. Module 2 ch-1 heytograph and hydrology analysis. Upcoming SlideShare. Like this presentation? Why not share! Embed Size px. Start on. Show related SlideShares at end. WordPress Shortcode. Ankit PatelAssistant Professor Follow. Published in: Engineering. Full Name Comment goes here.A hydrograph is a graph showing the rate of flow discharge versus time past a specific point in a river, channel, or conduit carrying flow.

The rate of flow is typically expressed in cubic meters or cubic feet per second cms or cfs. It can also refer to a graph showing the volume of water reaching a particular outfallor location in a sewerage network. Graphs are commonly used in the design of seweragemore specifically, the design of surface water sewerage systems and combined sewers. A stream hydrograph is commonly determining the influence of different hydrologic processes on discharge from the subject catchment.

Because the timing, magnitude, and duration of groundwater return flow differs so greatly from that of direct runoff, separating and understanding the influence of these distinct processes is key to analyzing and simulating the likely hydrologic effects of various land use, water use, weather, and climate conditions and changes. In part this is because these two concepts are not, themselves, entirely distinct and unrelated. Return flow from groundwater increases along with overland flow from saturated or impermeable areas during and after a storm event; moreover, a particular water molecule can easily move through both pathways en route to the watershed outlet.

Nevertheless, various graphical and empirical techniques have been developed to perform these hydrograph separations. The separation of base flow from direct runoff can be an important first step in developing rainfall-runoff models for a watershed of interest—for example, in developing and applying unit hydrographs as described below. A unit hydrograph UH is the hypothetical unit response of a watershed in terms of runoff volume and timing to a unit input of rainfall.

It can be defined as the direct runoff hydrograph DRH resulting from one unit e. As a UH is applicable only to the direct runoff component of a hydrograph i. A UH is specific to a particular watershed, and specific to a particular length of time corresponding to the duration of the effective rainfall. That is, the UH is specified as being the 1-hour, 6-hour, or hour UH, or any other length of time up to the time of concentration of direct runoff at the watershed outlet.

Thus, for a given watershed, there can be many unit hydrographs, each one corresponding to a different duration of effective rainfall. The UH technique provides a practical and relatively easy-to-apply tool for quantifying the effect of a unit of rainfall on the corresponding runoff from a particular drainage basin. UH theory assumes that a watershed's runoff response is linear and time-invariant, and that the effective rainfall occurs uniformly over the watershed.

In the real world, none of these assumptions are strictly true. Nevertheless, application of UH methods typically yields a reasonable approximation of the flood response of natural watersheds. The linear assumptions underlying UH theory allows for the variation in storm intensity over time i. This allows for a relatively straightforward calculation of the hydrograph response to any arbitrary rain event.

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An instantaneous unit hydrograph is a further refinement of the concept; for an IUH, the input rainfall is assumed to all take place at a discrete point in time obviously, this isn't the case for actual rainstorms. Making this assumption can greatly simplify the analysis involved in constructing a unit hydrograph, and it is necessary for the creation of a geomorphologic instantaneous unit hydrograph.

The creation of a GIUH is possible given nothing more than topologic data for a particular drainage basin. In fact, only the number of streams of a given order, the mean length of streams of a given order, and the mean land area draining directly to streams of a given order are absolutely required and can be estimated rather than explicitly calculated if necessary. It is therefore possible to calculate a GIUH for a basin without any data about stream height or flow, which may not always be available.

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In subsurface hydrology hydrogeologya hydrograph is a record of the water level the observed hydraulic head in wells screened across an aquifer. Typically, a hydrograph is recorded for monitoring of heads in aquifers during non-test conditions e. When an aquifer test is being performed, the resulting observations are typically called drawdownsince they are subtracted from pre-test levels and often only the change in water level is dealt with.

Raster hydrographs are pixel-based plots for visualizing and identifying variations and changes in large multidimensional data sets.A hyetograph is a graphical representation of the distribution of rainfall over time. For example, in the hour rainfall distributions as developed by the Soil Conservation Service, rainfall intensity progressively increases until it reaches a maximum and then gradually decreases.

Where this maximum occurs and how fast the maximum is reached is what differentiates one distribution from another. One important aspect to understand is that the distributions are for design storms, not necessarily actual storms. In other words, a real storm may not behave in this same fashion. The maximum intensity may not be reached as uniformly as shown in the SCS hyetographs.

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Hydrograph is the graphical representation of

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2.a hyetograph is a graphical representation of

Word in Definition. Wiktionary 0. Webster Dictionary 0. Freebase 0. How to pronounce hyetograph? Alex US English. Daniel British. Karen Australian. Veena Indian. How to say hyetograph in sign language? Select another language:.

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Are we missing a good definition for hyetograph? Don't keep it to yourself Submit Definition. The ASL fingerspelling provided here is most commonly used for proper names of people and places; it is also used in some languages for concepts for which no sign is available at that moment.

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Show More. No Downloads. Views Total views. Actions Shares. No notes for slide. Hyetograph and hydrograph analysis 1. Hyetograph 2. Runoff 3.

Classification of runoff 4. Hydrograph 5. Unit Hydrograph Analysis 6. Hydrograph Vocabulary 3.

2.a hyetograph is a graphical representation of

When rainfall starts, some gets caught in retention storage depressions where it will be evaporated again, but some enters the ground infiltration, including some from detention storage where it will contribute to the channel flow at some later time. Hydrographs are also described in terms of the following time characteristics : 1 Time to Peak, tp: Time from the beginning of the rising limb to the occurrence of the peak discharge. The time to peak is largely determined by drainage characteristics such as drainage density, slope, channel roughness, and soil infiltration characteristics.

Rainfall distribution in space also affects the time to peak. Time of Concentration, tc: Time required for water to travel from the most hydraulically remote point in the basin to the basin outlet.


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