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            <gco:CharacterString>Note, this data is not bias-corrected. It can be considered synonymous with utilizing raw CMIP5 output but at higher spatial and temporal resolutions. If a direct application to real-world situations is needed, bias correction should be an essential first step in your analysis.  

Data are provided as NetCDF files closely following Climate and Forecasting (CF) metadata conventions, but may not be fully compliant. It is output on a 20x20km grid in a WRF-derived polar stereographic projection system at an hourly time-step. Some outputs have also been further aggregated to daily timesteps.  

**Variables include:**  
 
Variable | Description  
ACSNOW | Water equivalent of accum. snow depth  
ALBEDO | Albedo  
CANWAT | Plant canopy surface water  
CLDFRA | Total cloud cover  
CLDFRA_HIGH | High level cloud cover  
CLDFRA_LOW | Low level cloud cover  
CLDFRA_MID | Mid level cloud cover  
GHT | Geopotential height  
HFX | Sensible heat flux  
LH | Latent heat flux  
LWDNB | Downward long wave flux  
LWDNBC | Clear sky downward long wave flux  
LWUPB | Upward long wave flux  
LWUPBC | Clear sky upward long wave flux  
OMEGA | Pressure vertical velocity  
PCPC | Accumulated total precipitation  
PCPNC | Accumulated large-scale precipitation  
PCPT | Total precipitation  
POTEVP | Accumulated potential evaporation  
PSFC | Surface pressure  
Q2 | Specific humidity at 2m height  
QBOT | Specific humidity at lowest model level  
QVAPOR | Specific humidity  
SEAICE | Ice concentration  
SH2O | Liquid volumetric soil moisture (non-frozen)  
SLP | Mean sea level pressure (ETA model)  
SMOIS | Volumetric soil moisture content  
SNOW | Snow water equivalent  
SNOWC | Snow cover  
SNOWH | Snow depth  
SWDNB | Downward short wave flux  
SWDNBC | Clear sky downward solar flux  
SWUPB | Upward short wave flux  
SWUPBC | Clear sky upward solar flux  
T | Temperature  
T2 | Temperature at 2m height  
TBOT | Temperature at lowest model level  
TSK | Surface skin temperature  
TSLB | Soil temperature  
U | u-component of wind  
U10 | u-component of wind at 10m height  
UBOT | u-component of wind at lowest model level  
V | v-component of wind  
V10 | v-component of wind at 10m height  
VBOT | v-component of wind at lowest model level  
VEGFRA | Vegetation fraction  

**Daily summaries:**  

pcpt | precip  
q2 |specific humidity at 2m height   
t2min | temperature min   
t2 | temperature mean  
t2max | temperature max   

**References:** 

WRF model (Version 3.5)   
http://www2.mmm.ucar.edu/wrf/users/wrfv3.5/updates-3.5.1.html 

Bieniek, P. A., Bhatt, U. S., Walsh, J. E., Rupp, T. S., Zhang, J., Krieger, J. R., and Lader, R. 2016: Dynamical downscaling of ERA-Interim temperature and precipitation for Alaska. Journal of Applied Meteorology and Climatology, 55(3), 635-654.
https://journals.ametsoc.org/doi/abs/10.1175/JAMC-D-15-0153.1

Lader, R., U. S. Bhatt, J. E. Walsh, T. S. Rupp, and P. A. Bieniek, 2016: 2-m temperature and precipitation from atmospheric reanalysis evaluated for Alaska. J Appl Meteor Climatol, 55, 901-922.
https://journals.ametsoc.org/doi/abs/10.1175/JAMC-D-15-0162.1

Bieniek, P.A., U.S. Bhatt, J.E. Walsh, R. Lader, B. Griffith, J.K. Roach, and R.L. Thoman, 2018: Assessment of Alaska Rain-on-Snow Events Using Dynamical Downscaling.J. Appl. Meteor. Climatol., 57, 1847–1863, https://doi.org/10.1175/JAMC-D-17-0276.1 
https://journals.ametsoc.org/doi/10.1175/JAMC-D-17-0276.1

Lader, R., J.E. Walsh, U.S. Bhatt, and P.A. Bieniek, 2017: Projections of Twenty-First-Century Climate Extremes for Alaska via Dynamical Downscaling and Quantile Mapping. J. Appl. Meteor. Climatol., 56, 2393–2409, https://doi.org/10.1175/JAMC-D-16-0415.1 
https://journals.ametsoc.org/doi/10.1175/JAMC-D-16-0415.1</gco:CharacterString>
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