Simulation output of Lirung glacier
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This is the data used for <strong><em>Using 3D turbulence-resolving simulations to understand the impact of surface properties on the energy balance of a debris-covered glacier, </em></strong>by PNJ Bonekamp, CC van Heerwaarden, JF Steiner and WW Immerzeel<br> <br> For each experiment one summary file is present. Description of experiments:<br> HOM<sub>flat</sub> Homogeneous glacier (constant DEM, surface specific moisture and temperature)<br> HOM<sub>1/2DEM</sub> ½ DEM, homogeneous surface specific moisture and temperature<br> HOM<sub>DEM </sub> With the real DEM, homogeneous surface specific moisture and temperature<br> HET<sub>T</sub> Spatially heterogeneous surface temperature, the real DEM, homogeneous surface specific moisture<br> HET<sub>qdry</sub> Surface specific humidity is spatially RH=70-75%, surface temperature constant, real DEM is included<br> HET<sub>qmoist</sub> Spatially RH=70-85%, surface temperature constant, real DEM is included<br> <br> In each file various variables are present;<br> u_xz, v_xz, qt_xz, thl_xz: which are the wind vectors, total specific humidity and liquid potential temperature for the xz cross section respectively<br> u_yz, v_yz, qt_yz, thl_yz: which are the wind vectors, total specific humidity and liquid potential temperature for the yz cross section respectively<br> qtfluxbot_ib, thlfluxbot_ib: the total specific moisture and temperature flux at the surface respectively. See for more specific information:<br> <strong><em>Using 3D turbulence-resolving simulations to understand the impact of surface properties on the energy balance of a debris-covered glacier, </em></strong>PNJ Bonekamp, CC van Heerwaarden, JF Steinerand WW Immerzeel, The Cryosphere, submitted
