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Tompkins, Adrian Mark; Semie, Addisu G (2017): Weather Research and Forecasting Model (WRF) cloud resolving model output, links to NetCDF files [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.874255, Supplement to: Tompkins, AM; Semie, AG (2017): Organization of tropical convection in low vertical wind shears: role of updraft entrainment. Journal of Advances in Modeling Earth Systems, https://doi.org/10.1002/2016MS000802

Always quote citation above when using data! You can download the citation in several formats below.

Published: 2017-04-03DOI registered: 2017-05-02

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Abstract:
Radiative-convective equilibrium simulations with a 2 km horizontal resolution are conducted to investigate the impact on convective organization of different parameterizations for horizonal and vertical sub-grid turbulence mixing. Three standard approaches for representing horizontal diffusion produce starkly differing mixing rates, particularly for the entrainment mixing into updrafts, which differ by more than an order of magnitude between the schemes. The simulations demonstrate that the horizontal sub-grid mixing of water vapor is key, with high mixing rates a necessary condition for organization of convection to occur, since entrainment of dry air into updrafts suppresses convection. It is argued that diabatic budgets, while demonstrating the role of spatially heterogeneous radiative heating rates in driving organization, can overlook the role of physical processes such as updraft entrainment. These results may partially explain previous studies that showed that organization is more likely to occur at coarser resolutions, when entrainment is solely represented by subgrid-scale turbulence schemes, highlighting the need for benchmark simulations of higher horizontal resolution. The recommendation is for the use of larger ensembles to ensure robustness of conclusions to subgrid-scale parameterization assumptions when numerically investigating convective organization, possibly through a coordinated community model intercomparison effort.
Comment:
NETCDF 3D output fields stored every 24 hours from the main experiments. All variables plotted in the paper are stored. For details of the experiment set up and the simulation names, please refer to the open access publication.
Selected variables and the publications plots:
Fig. 1 - QVAPOR and total pressure of the main experiments(smag3dpbl, smag3d, smag2dpbl, tke3dpbl)
Fig. 2 - OLR of the main experiments
Fig. 3 - QVAPOR and total pressure of the main experiments
Fig. 4 - QVAPOR and total pressure of the main experiments
Fig. 5 - W of the main experiments
Fig. 6 - W of the main experiments
Fig. 7 - QVAPOR and total pressure of the main experiments
Fig. 8 - QVAPOR and total pressure of the main experiments
Fig. 9 - ACLWTTEN, ACSWTTEN for simulation smag3dpbl only
Fig. 10 - XKMH of the main experiments
Fig. 11 - XKMH of the main experiments
All the variables, Qvapor, OLR, W, XKMH and total pressure are stored in their corresponding experiment name, smag3dpb has additional sw and lw tendency variables.
Fig. 12 - W of experiment UV-smag3dpbl and TQ-smag3dpbl
Fig. 13 and Fig. 14 - xkmh and W values using various mixing strength of tke3dpbl experiments
Fig. 15 - vertical velocity W is selected and their values are stored in hysteresis directory
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
File contentContentTompkins, Adrian Mark
File nameFile nameTompkins, Adrian Mark
File formatFile formatTompkins, Adrian Mark
File sizeFile sizekByteTompkins, Adrian Mark
Uniform resource locator/link to fileURL fileTompkins, Adrian Mark
Size:
195 data points

Data

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Z wind component (hysteresis smag2dpbl) in m/shysteresis_smag2dpbl_WNetCDF534521hysteresis_smag2dpbl_W.nc
Z wind component (hysteresis tke3dpbl) in m/shysteresis_tke3dpbl_WNetCDF519263hysteresis_tke3dpbl_W.nc
Z wind component (hysteresis uvsmag3dpbl) in m/shysteresis_uvsmag3dpbl_WNetCDF580296hysteresis_uvsmag3dpbl_W.nc
Z wind component (sen tqsmag3dpbl) in m/ssen_tqsmag3dpbl_WNetCDF726277sen_tqsmag3dpbl_W.nc
Z wind component (sen uvwsmag3dpbl) in m/ssen_uvwsmag3dpbl_WNetCDF742405sen_uvwsmag3dpbl_W.nc
top-of-atmosphere outgoing longwave radiation (smag2dpbl) in W/m**2smag2dpbl_OLRNetCDF17685smag2dpbl_OLR.nc
total pressure of smag2dpbl experiment in Pasmag2dpbl_pres_2NetCDF30518smag2dpbl_pres_2.nc
water vapor mixing ratio (smag2dpbl) in kg/kgsmag2dpbl_QVAPORNetCDF1066616smag2dpbl_QVAPOR.nc
Z wind component (smag2dpbl) in m/ssmag2dpbl_WNetCDF1083812smag2dpbl_W.nc
horizontal eddy viscosity of smag2dpbl experiment in m**2/ssmag2dpbl_xkmhNetCDF15509smag2dpbl_xkmh.nc
top-of-atmosphere outgoing longwave radiation (smag3d) in W/m**2smag3d_OLRNetCDF17685smag3d_OLR.nc
total pressure of smag3d experiment in Pasmag3d_pres_2NetCDF30518smag3d_pres_2.nc
water vapor mixing ratio (smag3d) in kg/kgsmag3d_QVAPORNetCDF1066616smag3d_QVAPOR.nc
Z wind component (smag3d) in m/ssmag3d_WNetCDF1083812smag3d_W.nc
horizontal eddy viscosity of smag3d experiment in m**2/ssmag3d_xkmhNetCDF45537smag3d_xkmh.nc
accumulated temperature tendency due to longwave radiation (smag3dpbl) in Ksmag3dpbl_ht_lwNetCDF1066616smag3dpbl_ht_lw.nc
accumulated temperature tendency due to shortwave radiation (smag3dpbl) in Ksmag3dpbl_ht_swNetCDF1066616smag3dpbl_ht_sw.nc
top-of-atmosphere outgoing longwave radiation (smag3dpbl) in W/m**2smag3dpbl_OLRNetCDF17685smag3dpbl_OLR.nc
total pressure of smag3dpbl experiment in Pasmag3dpbl_pres_2NetCDF30518smag3dpbl_pres_2.nc
water vapor mixing ratio (smag3dpbl) in kg/kgsmag3dpbl_QVAPORNetCDF1066616smag3dpbl_QVAPOR.nc
Z wind component (smag3dpbl) in m/ssmag3dpbl_WNetCDF1083812smag3dpbl_W.nc
horizontal eddy viscosity of smag3dpbl experiment in m**2/ssmag3dpbl_xkmhNetCDF30521smag3dpbl_xkmh.nc
Z wind component of tke3dpbl_015 experiment in m/stke3dpbl_015_WNetCDF259876tke3dpbl_015_W.nc
horizontal eddy viscosity of tke3dpbl_015 experiment in m**2/stke3dpbl_015_xkmhNetCDF255759tke3dpbl_015_xkmh.nc
Z wind component of tke3dpbl_02 experiment in m/stke3dpbl_02_WNetCDF259876tke3dpbl_02_W.nc
horizontal eddy viscosity of tke3dpbl_02 experiment in m**2/stke3dpbl_02_xkmhNetCDF255759tke3dpbl_02_xkmh.nc
Z wind component of tke3dpbl_03 experiment in m/stke3dpbl_03_WNetCDF259876tke3dpbl_03_W.nc
horizontal eddy viscosity of tke3dpbl_03 experiment in m**2/stke3dpbl_03_xkmhNetCDF255759tke3dpbl_03_xkmh.nc
Z wind component of tke3dpbl_04 experiment in m/stke3dpbl_04_WNetCDF259876tke3dpbl_04_W.nc
horizontal eddy viscosity of tke3dpbl_04 experiment in m**2/stke3dpbl_04_xkmhNetCDF255759tke3dpbl_04_xkmh.nc
Z wind component of tke3dpbl_05 experiment in m/stke3dpbl_05_WNetCDF259876tke3dpbl_05_W.nc
horizontal eddy viscosity of tke3dpbl_05 experiment in m**2/stke3dpbl_05_xkmhNetCDF255759tke3dpbl_05_xkmh.nc
Z wind component of tke3dpbl_06 experiment in m/stke3dpbl_06_WNetCDF259876tke3dpbl_06_W.nc
horizontal eddy viscosity of tke3dpbl_06 experiment in m**2/stke3dpbl_06_xkmhNetCDF255759tke3dpbl_06_xkmh.nc
top-of-atmosphere outgoing longwave radiation (tke3dpbl) in W/m**2tke3dpbl_OLRNetCDF17685tke3dpbl_OLR.nc
total pressure of tke3dpbl experiment in Patke3dpbl_pres_2NetCDF30518tke3dpbl_pres_2.nc
water vapor mixing ratio (tke3dpbl) in kg/kgtke3dpbl_QVAPORNetCDF1066616tke3dpbl_QVAPOR.nc
Z wind component (tke3dpbl) in m/stke3dpbl_WNetCDF1083812tke3dpbl_W.nc
horizontal eddy viscosity of tke3dpbl experiment in m**2/stke3dpbl_xkmhNetCDF165664tke3dpbl_xkmh.nc