Showing 1 - 20 results of 66 for search '"Regime"', query time: 0.08s Refine Results
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    CO[subscript 2] migration in saline aquifers: Regimes in migration with dissolution by MacMinn, Christopher W., Szulczewski, Michael L., Juanes, Ruben

    Published 2014
    “…We solve the model numerically and identify three regimes in CO[subscript 2] migration with dissolution, based on how quickly the brine beneath the plume saturates with dissolved CO[subscript 2]. …”
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    Regime shifts in bistable water-stressed ecosystems due to amplification of stochastic rainfall patterns by Cueto-Felgueroso, Luis, Dentz, Marco, Juanes, Ruben

    Published 2015
    “…Through an effective potential, we quantify the impact of rainfall variability on ecosystem resilience and conclude that amplified rainfall regimes reduce the resilience of water-stressed ecosystems, even if the mean annual precipitation remains constant.…”
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    Simulating the connections of ENSO and the rainfall regime of East Africa and the upper Blue Nile region using a climate model of the Tropics by Zaroug, M. A. H., Giorgi, F., Coppale, E., Abdo, G. M., Eltahir, Elfatih A. B.

    Published 2018
    “…We simulate the observed statistical relationship between ENSO and the rainfall regime of the upper Blue Nile using the tropical-band version of the regional climate model RegCM4 (or Reg-TB). …”
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    Simulating the connections of ENSO and the rainfall regime of East Africa and the upper Blue Nile region using a climate model of the Tropics by Zaroug, M. A. H., Giorgi, F., Coppola, E., Abdo, G. M., Eltahir, Elfatih A. B.

    Published 2015
    “…We simulate the observed statistical relationship between ENSO and the rainfall regime of the upper Blue Nile using the tropical-band version of the regional climate model RegCM4 (or Reg-TB). …”
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    The evolution of miscible gravity currents in horizontal porous layers by Szulczewski, Michael Lawrence, Juanes, Ruben

    Published 2013
    “…We show that the flow exhibits five regimes: (i) an early diffusion regime, in which the fluids diffuse across the initially sharp fluid–fluid interface; (ii) an S-slumping regime, in which the fluid–fluid interface tilts in an S-shape; (iii) a straight-line slumping regime, in which the fluid–fluid interface tilts as a straight line; (iv) a Taylor-slumping regime, in which Taylor dispersion at the aquifer scale enhances mixing between the fluids and causes the flow to continuously decelerate; and (v) a late diffusion regime, in which the flow becomes so slow that mass transfer again occurs dominantly though diffusion.…”
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    Thermally driven exchange flow between open water and an aquatic canopy by Nepf, Heidi, Zhang, Xueyan

    Published 2010
    “…Scaling analysis predicts several distinct flow regimes, including inertia-dominated, drag-dominated and energy-limiting regimes. …”
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    Thin films in partial wetting: internal selection of contact-line dynamics by Alizadeh Pahlavan, Amir, Cueto-Felgueroso, Luis, McKinley, Gareth H., Juanes, Ruben

    Published 2015
    “…Surprisingly, we find that even in the gravity-dominated regime, the dynamic contact angle follows the Cox--Voinov law.…”
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    Thin Films in Partial Wetting: Internal Selection of Contact-Line Dynamics by Alizadeh Pahlavan, Amir, Cueto-Felgueroso, Luis, McKinley, Gareth H., Juanes, Ruben

    Published 2015
    “…Surprisingly, we find that even in the gravity-dominated regime, the dynamic contact angle follows the Cox-Voinov law.…”
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    The intermediate Rossby number range and two-dimensional–three-dimensional transfers in rotating decaying homogeneous turbulence by Bourouiba, Lydia, Bartello, Peter

    Published 2014
    “…The intermediate-Ro regime is characterized by a positive transfer of energy from wave modes to vortices. …”
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    Non-local energy transfers in rotating turbulence at intermediate Rossby number by Straub, D. N., Waite, M. L., Bourouiba, Lydia

    Published 2014
    “…The interpretation of the scaling law observed in rotating flows in the intermediate-Ro regime is revisited in the light of this new finding of dominant non-locality.…”
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    Strong and weak, unsteady reconfiguration and its impact on turbulence structure within plant canopies by Pan, Ying, Chamecki, Marcelo, Nepf, Heidi, Follett, Elizabeth M.

    Published 2016
    “…In the transition between the asymptotic regimes of negligible and strong reconfiguration, there is a regime of weak reconfiguration, in which the Vogel number achieved its peak negative value. …”
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    Simulations of the observed ‘jump’ in the West African monsoon and its underlying dynamics using the MIT regional climate model by Im, Eun Soon, Eltahir, Elfatih A. B.

    Published 2018
    “…The transition between these two rainfall regimes occurs relatively quickly around the beginning of July. …”
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    Gravity Currents in Aquatic Canopies by Tanino, Yukie, Nepf, Heidi, Kulis, P. S.

    Published 2012
    “…Empirical criteria are developed to predict the current regime from the cylinder Reynolds number and the array density.…”
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    Path (un)predictability of two interacting cracks in polycarbonate sheets using Digital Image Correlation by Koivisto, J., Alava, M. J., Santucci, S., Dalbe, Marie Julie Elise

    Published 2017
    “…Depending on the initial distances between the two crack tips, one may observe different complex crack paths with in particular a regime where the two cracks repel each other prior to being attracted. …”
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    Activated desorption at heterogeneous interfaces and long-time kinetics of hydrocarbon recovery from nanoporous media by Lee, Thomas, Bocquet, Lyderic Benjamin, Coasne, Benoit Alain

    Published 2017
    “…We build a statistical model of the recovery kinetics with a two-regime decline that is consistent with published data: a short time decay, consistent with Darcy description, followed by a fast algebraic decay resulting from increasingly unreachable energy barriers. …”
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