## average watershed slope

Land-surface slope, land cover, and land use have similar influences on watershed characteristics as those identified for the unsaturated zone. Determining Average Slope For Small Watersheds Topics: 1. Curve numbers (CN) are used to represent watershed characteristics that … var imgFloat = dom_i.query(this).css("float") == undefined ? if(imgMarginTop.indexOf("px") > 0){ endobj The same can be done for Slope Length as well. stream Peak discharges range from 5 to 2,000 cubic feet per second (cfs), drainage areas range from 5 to 2,000 acres, and 24-hour rainfall depths range from 1 to 12 inches. The average annual precipitation represents the amount of water available for transport in a watershed. Lag is the delay between the time runoff from a rainfall event over a watershed begins until runoff reaches its maximum peak. If the average land slope on a watershed differs from this, multiply the value from Table 1 by the following factor: Average land slope Topographic factor (T) 0.5 percent: 0.50: 1 percent: 0.65: 2 percent: 0.72: 3 percent: 0.78: dom_i.query(this).css("margin","0"); b) The average altitude of a watershed - can be deduced directly from the hypsographical curve or from reading the topographical map. Watershed length is between 200 and 26,000 feet. If the average land slope on a watershed differs from this, multiply the value from Table 1 by the following factor: Average land slope Topographic factor (T) 0.5 percent: 0.50: 1 percent: 7�S�E�S��CL�U���m),�s\��T���tCQfn�C"K�Th7�Pt�-\$�e�b��#���@ˏ� %C��Z*)Y�ds�iwA��䞩��ȩ_�(��p��Ʌt��s�b�~�U�>5r/�]i��^y�Puɶ{V��2��n%����̶�a3d_7� �t�H����q��ژ�t����ͺ���S��endstream Wuhua county is located at the mid-eastern part of Guangdong Province, China. if(imgWidth.indexOf("px") > 0){ The watershed slope, or average watershed land slope, is used in the lag equation to estimate the watershed Tc. dom.query('img').each(function(){ Step 2. } } Watershed average slope offers information about the watershed topography. Table 3-1 contains CN values for different land // Water surface slope is determined along the longitudinal profile of the channel by measuring the difference in water surface elevation per unit stream length. The slope value of this plane is calculated using the average maximum technique (see References). <> : dom_i.query(this).attr("title").trim(); Lloyd-Davies method if you are English, is probably the oldest Calculating a Slope. %�쏢 Rational Method The Rational Method, a.k.a. use the SCS dimensionless unit hydrograph. : dom_i.query(this).css("margin-left").trim(); Values in Table 1 are peak rates of runoff to be expected from watersheds with an average land slope of 8 percent. Ground-water contribution represents the part of streamflow that is derived from ground water. Peak discharges range from 5 to 2,000 cubic feet per second (cfs), drainage areas range from 5 to 2,000 acres, and 24-hour rainfall depths range from 1 to 12 inches. Average Watershed Slope (Y) • The average watershed slope (Y) is the slope of the land and not the watercourse. Factors selected for rating the watershed characteristics upstream from surface-water intakes are average annual precipitation, land-surface slope, land cover, land use, and ground-water contribution. Solution: watershed lag time (t L) = NOT CALCULATED. 300 : dom_i.query(this).css("width").trim(); dom_i.query(this).attr("title",imgAlt); Thanks! The county has serious erosion and watershed degradation problem. Therefore, the objective of this study was to evaluate the use of the standard NRCS-CN, the slope-adjusted CN equation, and GIS to develop a database con-taining all the information of the study watershed for direct runoff depth estimation in a watershed with steep slopes. A less-steep, flatter roof will cause the water to move more slowly, raising the potential for … Want more videos? Draw the ‘L’ section of the main stream. �vα�(������_7��E=����}�K_◿�~O�e�g��a�B�'Sy��R��t|����ۻI�o�7TՔ�endstream dom_i.query(this).after("

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"); "none" : dom_i.query(this).css("float").trim(); x��W]kT1}��"�/�-�jIJo�L�_Eė�Z�*V��T����ݽ7��ܮk)��Ædf�̜���%S����/����c��6� �(ct���;N+�.�\�b��^4_��[sIᝢ��&,�6�u�����Ѫ�(��4.L��=Z��5* �0NE����N�S����+�\��٫Y�f�T��>7�k) �RSc0�@'���-H��?HK��H�MԦ��\$�Z���S����H��q�����%2�X�b�i������"��=%Fg'�� L .��rA�T�K� )x��Ѣԑҹ�����|/���� }) (3) three categories of average watershed slopes. Riffles are found entering and exiting meanders and control the streambed elevation. Much care is designed with the average and maximum slope, trail width, and avoidance of sensitive areas such as streams, drainages, seeps or other aquatic features that could have a downstream negative impact on the NYC watershed. Active 3 years, 1 month ago. 2.4. The average annual precipitation represents the amount of water available for transport in a watershed. �A\$ф���lkE*y]8�A;;R�R���_-5Mk(��:gqW� ^��Z��(G�[!����,r���IU]���c�Kar�w/�lrp,�r��;��D/&>]��ɋ��t�9ƚ�=F���C^�S��-�>�CA�S�)��Y�Hr������9|�ɞ�+j� ���7�孴��n���Et�;�w�� >���N������0�G�>�`�,S�QRt�&"���%AA��]� potential watershed storage (S) = 0 = 0. inch . Derive a unit hydrograph ordinates and determine the runoff value for a storm of duration 1 hr. TR-55 provides chart in chapter 3 for estimating the velocity based on teh slope of the watercourse (for paved and unpaved surfaces). Watershed Subbasin Maps This web page provides access to five pre-built map series for each of Montana’s subbasins (8-digit HUC level). imgMarginBottom = imgMarginBottom.replace("px",""); if(imgMarginRight.indexOf("px") > 0){ The watershed slope, or average watershed land slope, is used in the lag equation to estimate the watershed Tc. : dom_i.query(this).attr("alt").trim(); For degrees, the range of slope values is 0 to 90. 562 dom_i.query(this).addClass('img_'+count); endobj When the bubble on a level is about 1/4 of the way past the line it is about a 1/4″ slope. endobj Average watershed slope is between 0.5 and 64%. ���u�ɠ&��b�T�/A�(Ee�[iu�5R�����b))JQ��D�����+�H Physiographic Characteristics Slope: It controls the rainfall distribution and movement, land utilization and watershed behavior. }); Derive a unit hydrograph ordinates and determine the runoff value for a storm of duration 1 hr. The curve number, CN, is an empirical value, which establishes a relationship between rainfall and runoff based upon characteristics of the drainage area. The authors investigate the effect of digital elevation model (DEM) grid size and source on the average watershed slope. } Watershed area is between 1 and 2,000 acres. potential watershed storage: average watershed slope: Bransby Williams Equation. 1. 26 0 obj Watersheds can be as small as a footprint or large enough to encompass all the land that drains water into rivers that drain into Chesapeake Bay, where it enters the Atlantic Ocean. imgMarginTop = imgMarginTop.replace("px",""); var count = 1; : dom_i.query(this).css("margin-bottom").trim(); Watershed slope is not to be confused with the slope of the flow path. } – Average watershed slope is an average of individual land slope measurements. S = average slope of the channel reach, m/m. We show that total aquatic carbon emissions covary nonlinearly with the average slope of the watershed, such that maximal emissions occur both in the flattest and steepest landscapes. Determining the average slope of a hill using a topographic map is fairly simple. Each field will need a unique identifier. Slope of a Catchment Area: It is noticed that the slope of a channel is normally steep at the early stage and it goes on reducing as it flows downstream. equations [4] in other steep slope areas for estimating runoff rate. average watershed slope (w s) = 0 = 0. count = count+1; No valley or reservoir routing is required. Another way of expressing the slope is as an angle in degrees, called the zenith, which may be computed as Zenith = 180 π tan ? The initial steps to calculating slope either way are the same. mGԂ�L��p�nC�-���� This program has restricted applications. Set the File name and Projection. } Note: Spatial Analyst is required to complete this process. }else{ The direction the plane faces is the aspect for the processing cell. I am trying to replicate a procedure that the USGS Streamstats performs on points delineated along a stream network. 2. �2���X��|��RZ�T��|%������DY(��u���!�*C���%+cg��g�%u*�f dom_i.query(this).css("float","none"); Lag is a function of the flow length of the watershed, average land slope of the watershed, and the potential maximum retention of rainfall on the watershed. Watershed average slope offers information about the watershed topography. [CDATA[ Dry fit PVC/ABS components first to ensure there is enough space to properly slope the entire pipe dom_i.query = jQuery.noConflict(true); When the flood recedes, the water surface level in the river drops. /*dom.query(document).ready(function(){ Calculating a Slope. dom_i.query('.img_'+count).wrapAll("