Jose M. Mier's research while affiliated with University of Illinois, Urbana-Champaign and other places

... Several OBL studies (e.g. Spalart & Baldwin 1987;Scandura 2007;Scandura et al. 2016; van der A, Scandura & O'Donoghue 2018;Fytanidis, García & Fischer 2021;Mier, Fytanidis & García 2021) considered the simplified case of flow over a smooth wall. For practical OBLs that occur in the coastal zone, the seabed is rough, composed of sediment particles. ...

... Specifically, UIUC has developed an integrated urban hydrology and hydraulic suite of models, one of which is known as a connecting structure-tunnel and reservoir plan (CS-TARP). A detailed description of CS-TARP can be found in Cantone and Schmidt (2011), Luo et al. (2014), and Oberg et al. (2017. The studies by Quijano et al. (2017), Zhu et al. (2017), and Morales et al. (2017) show the importance of simulating CSO volumes with CS-TARP and its integration into other hydrodynamics models of the CAWS. ...

... The state-of-the-art in research has demonstrated that a reduced complexity approach to CSO modelling can be used to create accurate simulations in a fraction of the time (Nielsen et al., 2007;Morales et al., 2017). This enables modelling of CSOs in contexts that require rapid simulations, for example, Lund et al. (2020) use surrogate modelling to control CSO behaviour with optimisation of Model Predictive Control (MPC). ...

... The assumed values that concern the bed [1] can stay constant in the whole range. However, the roughness values can be variable in the conditions of flooding [2][3][4][5][6] and the bottom can be reshaped as a result of erosion and/or accumulation [7,8]. Calculations that allow one to determine the estimation of changes in the bottom's sieve curve, in the case of flood passing, have been previously performed using the classic formulas [9]. ...

... Jonsson and Carlsen (1976), Sleath (1989), Kemp and Simons (1983); Lin and Hwuang (2002), Ojha et al. (2019), and the Particle Image Velocimetry (PIV) has also become favorable in these years (e.g. Ahmed and Sato, 2003;Admiraal et al., 2006;Van der A et al., 2011;Mujal-Colilles et al., 2014). However, the dark, blind underwater environment, as well as the strong wave force, makes it hardly possible to install and operate an optical equipment that requires a quiescent, undisturbed environment, not to mention the difficulty of injecting the liquid tracer. ...

... Broader work focusing on the subject of glacial legacy on river/valley form was mainly done in mountainous terrains Hassan, 2006, 2007;Amerson et al., 2008;Addy et al., 2011;Gomez and Livingstone, 2012;Prasicek et al., 2014;Addy et al., 2014;Hassan et al., 2014), and occasionally in lowland semi-alluvial settings (Fola and Rennie, 2010;Collins and Montgomery, 2011;Phillips and Desloges, 2014, 2015a, 2015bThayer and Ashmore, 2016;Papangelakis et al., 2019). Small-scale laboratory flume experiments were used in isolating specific processes of interest in semi-alluvial channels (Kamphuis, 1983;Kamphuis et al., 1990;Mier and Garcia, 2011;Pike et al., 2018;Papangelakis et al., 2021;Peirce et al., 2021). ...