@article{segura_caldwell_sun_mcnulty_zhang_2015, title={A model to predict stream water temperature across the conterminous USA}, volume={29}, ISSN={["1099-1085"]}, DOI={10.1002/hyp.10357}, abstractNote={Abstract}, number={9}, journal={HYDROLOGICAL PROCESSES}, author={Segura, Catalina and Caldwell, Peter and Sun, Ge and McNulty, Steve and Zhang, Yang}, year={2015}, month={Apr}, pages={2178–2195} } @article{caldwell_segura_laird_sun_mcnulty_sandercock_boggs_vose_2015, title={Short-term stream water temperature observations permit rapid assessment of potential climate change impacts}, volume={29}, ISSN={["1099-1085"]}, DOI={10.1002/hyp.10358}, abstractNote={Abstract}, number={9}, journal={HYDROLOGICAL PROCESSES}, author={Caldwell, Peter and Segura, Catalina and Laird, Shelby Gull and Sun, Ge and McNulty, Steven G. and Sandercock, Maria and Boggs, Johnny and Vose, James M.}, year={2015}, month={Apr}, pages={2196–2211} } @article{segura_lazzati_sankarasubramanian_2013, title={The use of broken power-laws to describe the distributions of daily flow above the mean annual flow across the conterminous U.S.}, volume={505}, ISSN={0022-1694}, url={http://dx.doi.org/10.1016/j.jhydrol.2013.09.016}, DOI={10.1016/j.jhydrol.2013.09.016}, abstractNote={A recent study employed a broken power-law (BPL) distribution for understanding the scaling frequency of bankfull discharge in snowmelt-dominated basins. This study, grounded from those findings, investigated the ability of a BPL function to describe the distribution of daily flows above the mean annual flow in 1217 sites across the conterminous U.S. (CONUS). The hydrologic regime in all the sites is unregulated and spans a wide range in drainage areas (2–120,000 km2) and elevation (0–3000 m). Available daily flow records in all sites varied between 15 and 108 years. Comparing the performance of BPL distribution and the traditionally used lognormal distribution, we found that BPL provides stronger fit in ∼80% of the sites. Thus the BPL function provides a suitable tool to model daily flows in most areas of the CONUS. The potential for developing a model for predicting the frequency distribution of daily flows in ungauged sites was analyzed. We found that such model is possible using drainage area, mean basin elevation, and mean annual precipitation as predicting variables for any site located above 600 m across the CONUS. We also found strong continental-wide correlations between 3 of the 4 parameters that describe the BPL and basin characteristics. Our results indicate that the BPL function provides a robust alternative to traditional functions such as the lognormal to model the statistical variation of daily flows above the mean annual in most basins of the CONUS.}, journal={Journal of Hydrology}, publisher={Elsevier BV}, author={Segura, Catalina and Lazzati, Davide and Sankarasubramanian, Arumugam}, year={2013}, month={Nov}, pages={35–46} } @article{segura_mccutchan_lewis_pitlick_2011, title={The influence of channel bed disturbance on algal biomass in a Colorado mountain stream}, volume={4}, ISSN={["1936-0592"]}, DOI={10.1002/eco.142}, abstractNote={Abstract}, number={3}, journal={ECOHYDROLOGY}, author={Segura, Catalina and McCutchan, James H. and Lewis, William M., Jr. and Pitlick, John}, year={2011}, pages={411–421} } @article{segura_booth_2010, title={EFFECTS OF GEOMORPHIC SETTING AND URBANIZATION ON WOOD, POOLS, SEDIMENT STORAGE, AND BANK EROSION IN PUGET SOUND STREAMS}, volume={46}, ISSN={["1093-474X"]}, DOI={10.1111/j.1752-1688.2010.00470.x}, abstractNote={Segura, Catalina and Derek B. Booth, 2010. Effects of Geomorphic Setting and Urbanization on Wood, Pools, Sediment Storage, and Bank Erosion in Puget Sound Streams. Journal of the American Water Resources Association (JAWRA) 46(5):972‐986. DOI: 10.1111/j.1752‐1688.2010.00470.x}, number={5}, journal={JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION}, author={Segura, Catalina and Booth, Derek B.}, year={2010}, month={Oct}, pages={972–986} } @article{segura_pitlick_2010, title={Scaling frequency of channel-forming flows in snowmelt-dominated streams}, volume={46}, ISSN={["0043-1397"]}, DOI={10.1029/2009wr008336}, abstractNote={The scaling properties of channel‐forming flows are investigated using a regional flow frequency model developed for snowmelt‐dominated streams in Colorado. The model is derived from analyses of daily flow records at 32 gauging stations where we have independent measurements of the bankfull discharge. The study sites are located in alpine/subalpine basins with drainage areas ranging from 4 to 3700 km2. The frequency distribution of daily flows at these locations can be reproduced with a broken power law (BPL) function described by two free parameters. Both parameters are strongly correlated with drainage area, and based on these correlations, a regional model capable of predicting the frequency of daily flows above the mean annual flow was formulated. The applicability of the model was tested using daily flow records from 32 similar‐size basins in Idaho. The frequency distributions of daily flows in snowmelt‐dominated streams in Colorado and Idaho with highly predictable hydrographs (i.e., 1 year autocorrelation above 0.7) are well fitted by the BPL function. According to the model, the frequency of flows greater than bankfull decreases downstream from about 15 d/yr in headwater reaches to about 6 d/yr in downstream reaches. These results imply that the basin response to precipitation and runoff is nonlinear. This multiscaling behavior can be physically interpreted as the result of scale‐dependent variations in runoff and sediment supply, which influence downstream trends in the bankfull channel geometry and intensity of sediment transport.}, journal={WATER RESOURCES RESEARCH}, author={Segura, Catalina and Pitlick, John}, year={2010}, month={Jun} }