The NAAD (North Atlantic Atmospheric Downscaling) provides a 40-year 3D hindcast of the North Atlantic atmosphere (10°N-80°N) at 14 km (HiRes) and 77 km (LoRes) spatial resolution with 50 levels in the vertical (from approximately 10-12 m above the ocean surface up to 50 hPa), performed with a regional setting of the WRF-ARW 3.8.1 model for the period from January 1979 to December 2018 and forced by ERA-Interim as a lateral boundary condition. The main focus of the NAAD is the long-term atmospheric mesoscale dynamics over the ocean. The NAAD can be also effectively used for forcing ocean and wave models to estimate the impact of the mesoscale activity in the lower atmosphere. The dataset provides a variety of surface and free atmosphere parameters at the model levels.
HiRes | LoRes | |
---|---|---|
Model settings | ||
Model | WRF-ARW 3.8.1 | |
Dynamical core | Nonhydrostatic | Hydrostatic |
Domain settings | ||
Horizontal Resolution | 14 km | 77 km |
Vertical Resolution | 50 hydrostatic pressure-sigma levels (50 hPa top) | |
Timestep (RK3) | 30 s | 240 s |
Main physics options | ||
Microphysics | WSM6 | WSM5 |
Convection | Kain-Fritsch | |
PBL | YSU | |
Surface layer | MM5 | |
Radiative transfer | RRTMG | |
Land surface model | Noah LSM | |
Boundary conditions | ||
Initial & boundary conditions | ERA-Interim | |
SST | ERA-Interim (every 6 hr) | |
Data assimilation | Spectral nudging from PBL (longer that 1100 km) |
The computational grid of the NAAD has 50 vertical levels, 15 of which are located below 850 hPa. This provides approximately 6-15 levels within the PBL (depending on the season and location). The height of the lowest level is around 10-12 m above the ocean surface. See the table below.
model level |
Terrain following sigma level |
model level |
Terrain following sigma level |
model level |
Terrain following sigma level |
---|---|---|---|---|---|
1 | 1 | 18 | 0.7889637 | 35 | 0.1736677 |
2 | 0.997 | 19 | 0.7586183 | 36 | 0.1536199 |
3 | 0.993 | 20 | 0.7029784 | 37 | 0.1349515 |
4 | 0.987 | 21 | 0.6504962 | 38 | 0.117587 |
5 | 0.980 | 22 | 0.6010224 | 39 | 0.1017257 |
6 | 0.973 | 23 | 0.5544136 | 40 | 0.08734228 |
7 | 0.966 | 24 | 0.510532 | 41 | 0.07429918 |
8 | 0.960 | 25 | 0.4692457 | 42 | 0.06247147 |
9 | 0.952 | 26 | 0.4304279 | 43 | 0.05174589 |
10 | 0.944 | 27 | 0.393957 | 44 | 0.04201975 |
11 | 0.934 | 28 | 0.3597165 | 45 | 0.03319991 |
12 | 0.925 | 29 | 0.3275948 | 46 | 0.02520193 |
13 | 0.915 | 30 | 0.2974847 | 47 | 0.01794922 |
14 | 0.900 | 31 | 0.2692837 | 48 | 0.01137233 |
15 | 0.88 | 32 | 0.2428935 | 49 | 0.005408296 |
16 | 0.8496546 | 33 | 0.2182202 | 50 | 0. |
17 | 0.8193091 | 34 | 0.1951736 |