{"refrec":{"BRefID":325641,"RR":"<b>Bjerklie, D.M.</b> (2007). Estimating the bankfull velocity and discharge for rivers using remotely sensed river morphology information. <i>J. Hydrol. (Amst.) 341(3-4)</i>: 144-155. <a href=\"https://dx.doi.org/10.1016/j.jhydrol.2007.04.011\" target=\"_blank\">https://dx.doi.org/10.1016/j.jhydrol.2007.04.011</a>","BEntID":319118,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Hydrol. (Amst.) 341(3-4)</i>: 144-155. <a href=\"https://dx.doi.org/10.1016/j.jhydrol.2007.04.011\" target=\"_blank\">https://dx.doi.org/10.1016/j.jhydrol.2007.04.011</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":1,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Bjerklie, D.M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Bjerklie, D.M.","Englishabstract":"A method to estimate the bankfull velocity and discharge in rivers that uses the morphological variables of the river channel, including bankfull width, channel slope, and meander length was developed and tested. Because these variables can be measured remotely from topographic and river alignment information derived from aerial photos and satellite imagery, it is possible that the bankfull state of flow can be estimated for rivers entirely from remotely-sensed information. Defining the bankfull hydraulics of rivers would also provide a reference condition for remote tracking of dynamic variables including width, stage, and slope, and for quantifying relative change in flow conditions of rivers over large regions. 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