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Absence of Aerosol Indirect Effect Dependence on Background Climate State in NCAR CESM2

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DataCite Commons2026-03-28 更新2026-05-05 收录
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https://dataverse.tdl.org/citation?persistentId=doi:10.18738/T8/PNEI6T
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This directory contains metadata utilized in [cication] Absence of Aerosol Indirect Effect Dependence on Background Climate State in CESM2. Questions can be directed to the corresponding author at kaylaw@utexas.edu Structure of F (ATMOSPHERE-ONLY SIMULATION) file names: [Variable].b.e21.F1850.f19.f19.mg17.001.mon.001-60.nc = 1850 SSTs with all forcings set at 1850 levels [Variable].b.e21.F1850.f19.f19.mg17.001.aerosol2000.mon.001-60.nc = 1850 SSTs with all other forcings set at 1850 levels, and 2000 aerosol emissions [Variable].b.e21.F2000.f19.f19.mg17.001.mon.001-60.nc = 2000 SSTs with all forcings set at 2000 levels [Variable].b.e21.F2000.f19.f19.mg17.001.aerosol1850.mon.001-60.nc = 2000 SSTs with all other forcings set at 2000 levels, and 1850 aerosol emissions [Variable].b.e21.F2000.f19.f19.mg17.001.aerosol1850.add4k.mon.001-60.nc = 2000+4K SSTs with all other forcings set at 2000 levels, and 1850 aerosol emissions [Variable].b.e21.F2000.f19.f19.mg17.001.add4k.mon.001-60.nc = 2000+4K SSTs with all other forcings set at 2000 levels, and 2000 aerosol emissions Files contain the monthly, 60-year time-series for a single variable. For analysis, the first 20 years are considered to be the model equilibrated period. Years 20-60 are used for the equilibrated signal. Variables: AODABSdn = 2D Aerosol absorption optical depth 550 nm, day night AODVISdn = 2D Aerosol optical depth 550 nm, day night AREL = 3D Average droplet effective radius BURDENBCdn = 2D Black carbon aerosol burden, day night BURDENDUSTdn = 2D Dust aerosol burden, day night BURDENPOMdn = 2D POM aerosol burden, day night BURDENSEASALTdn = 2D Seasalt aerosol burden, day night BURDENSO4dn = 2D Sulfate aerosol burden, day night BURDENSOAdn = 2D SOA aerosol burden, day night CAPE = 2D Convectively available potential energy CCN3 = 3D CCN concentration at S=0.1% CDNUMC = 2D Vertically-integrated droplet concentration CLDHGH = 2D Vertically-integrated high cloud CLDLOW = 2D Vertically-integrated low cloud CLDMED = 2D Vertically-integrated mid-level cloud CLDTOT = 2D Vertically-integrated total cloud CLOUD = 3D Cloud fraction FLNT = 2D Net longwave flux at top of model FLNTC = 2D Clearsky net longwave flux at top of model FREQS = 3D Fractional occurrence of snow FSDS = 2D Downwelling solar flux at surface FSNS = 2D Net solar flux at surface FSNT = 2D Net solar flux at top of model FSNTC = 2D Clearsky net solar flux at top of model FSUTOA = 2D Upwelling solar flux at top of atmosphere ICEFRAC = 2D Fraction of sfc area covered by sea-ice LHFLX = 2D Surface latent heat flux LWCF = 2D Longwave cloud forcing OMEGA = 3D Vertical velocity (pressure) PRECC = 2D Convective precipitation rate (liq + ice) PRECL = 2D Large-scale (stable) precipitation rate (liq + ice) PRECSC = 2D Convective snow rate (water equivalent) PRECSL = 2D Large-scale (stable) snow rate (water equivalent) PS = 2D Surface pressure Q = 3D Specific humidity RELHUM = 3D Relative humidity SHFLX = 2D Surface sensible heat flux SSAVIS = 2D Aerosol single-scatter albedo, day only SST = 2D Sea surface temperature SWCF = 2D Shortwave cloud forcing T = 3D Temperature TGCLDCWP = 2D Total grid-box cloud water path (liquid and ice) TGCLDIWP = 2D Total grid-box cloud ice water path TGCLDLWP = 2D Total grid-box cloud liquid water path TREFHT = 2D Reference height temperature Z3 = 3D Geopotential Height (above sea level) Background climate simulations with 2-dimensional variables are grouped by variable type and uploaded in a .tar file that contains all 4 background climate simulations for the given variable Background climate simulations with 3-dimensional variables are uploaded individually due to size.
提供机构:
Texas Data Repository
创建时间:
2023-08-10
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