02623naa a2200205 a 450000100080000000500110000800800410001910000180006024501560007826000090023452020130024365000140225665000110227065000150228165000080229670000210230470000200232570000170234577300550236221003012018-11-30       2018    bl uuuu     u00u1 u    #d1 aCLAURE, Y. N.  aPollyWattbA polynomial water travel time estimator based on Derivative Dynamic Time Warping and Perceptually importante points.h[electronic resource]  c2018  aTraditional methods for estimating timing parameters in hydrological science require a rigorous study of the relations of flow resistance, slope, flow regime, watershed size, water velocity, and other local variables. These studies are mostly based on empirical observations, where the timing parameter is estimated using empirically derived formulas. The application of these studies to other locations is not always direct. The locations in which equations are used should have comparable characteristics to the locations from which such equations have been derived. To overcome this barrier, in this work, we developed a data-driven approach to estimate timing parameters such as travel time. Our proposal estimates timing parameters using historical data of the location without the need of adapting or using empirical formulas from other locations. The proposal only uses one variable measured at two different locations on the same river (for instance, two river-level measurements, one upstream and the other downstream on the same river). The recorded data from each location generates two time series. Our method aligns these two time series using derivative dynamic time warping (DDTW) and perceptually important points (PIP). Using data from timing parameters, a polynomial function generalizes the data by inducing a polynomial water travel time estimator, called PolyWaTT. To evaluate the potential of our proposal, we applied PolyWaTT to three different watersheds: a floodplain ecosystem located in the part of Brazil known as Pantanal, the world's largest tropical wetland area; and the Missouri River and the Pearl River, in United States of America. We compared our proposal with empirical formulas and a data-driven state-of-the-art method. The experimental results demonstrate that PolyWaTT showed a lower mean absolute error than all other methods tested in this study, and for longer distances the mean absolute error achieved by PolyWaTT is three times smaller than empirical formulas.  aHydrology  aRivers  aHidrologia  aRio1 aMATSUBARA, E. T.1 aPADOVANI, C. R.1 aPRATI, R. C.  tComputers and Geosciencesgv. 112, p. 54-63, 2018.