This is a forecast interpolation diagnostic model checkpoint. This deep learning model, based on the Adaptive Fourier Neural Operator framework (AFNO), interpolates a prognostic forecast model to a shorter time-step size (by default from 6 h to 1 h) and operates on 0.25 degree lat-lon equirectangular grid with 73 variables.
This model interpolates the following variables surface variables:
"u10m", "v10m", "u100m", "v100m", "t2m", "sp", "msl", "tcwv"
and the variables u, v, t, z, q
at pressure levels
1000, 925, 850, 700, 600, 500, 400, 300, 250, 200, 150, 100, 50
.
For training recipes, see NVIDIA PhysicsNeMo. For inference, see NVIDIA Earth2Studio.
This model is ready for commercial use.
Use of this model is governed by the NVIDIA Community Model License. By pulling and using this model, you accept the terms and conditions of this license.
Modulated Adaptive Fourier Neural Operators for Temporal Interpolation of Weather Forecasts
Architecture Type: This model uses an Adaptive Fourier Neural Operator (AFNO) architecture.
Network Architecture: AFNO
Input Type(s):
Input Format(s): PyTorch Tensor / NumPy array
Input Parameters:
Other Properties Related to Input:
u10m
, v10m
, u100m
, v100m
, t2m
, sp
, msl
tcwv
, u1000
, u925
, u850
, u700
, u600
, u500
, u400
, u300
, u250
, u200
, u150
, u100
, u50
, v1000
, v925
, v850
, v700
, v600
, v500
, v400
, v300
, v250
, v200
, v150
, v100
, v50
, t1000
, t925
, t850
, t700
, t600
, t500
, t400
, t300
, t250
, t200
, t150
, t100
, t50
, z1000
, z925
, z850
, z700
, z600
, z500
, z400
, z300
, z250
, z200
, z150
, z100
, z50
, q1000
, q925
, q850
, q700
, q600
, q500
, q400
, q300
, q250
, q200
, q150
, q100
, q50
For lexicon information, review the ERA5
Lexicon at Earth2Studio. u
, v
, t
, z
and q
refer to eastward and northward wind components, temperature, geopotential, and specific humidity (respectively).
Output Type(s):
Output Format: Pytorch Tensors
Output Parameters: Five Dimensional (5D) (batch, time, variable, latitude, longitude)
Other Properties Related to Output:
u10m
, v10m
, u100m
, v100m
, t2m
, sp
, msl
tcwv
, u1000
, u925
, u850
, u700
, u600
, u500
, u400
, u300
, u250
, u200
, u150
, u100
, u50
, v1000
, v925
, v850
, v700
, v600
, v500
, v400
, v300
, v250
, v200
, v150
, v100
, v50
, t1000
, t925
, t850
, t700
, t600
, t500
, t400
, t300
, t250
, t200
, t150
, t100
, t50
, z1000
, z925
, z850
, z700
, z600
, z500
, z400
, z300
, z250
, z200
, z150
, z100
, z50
, q1000
, q925
, q850
, q700
, q600
, q500
, q400
, q300
, q250
, q200
, q150
, q100
, q50
For lexicon information, review the ERA5
Lexicon at Earth2Studio. u
, v
, t
, z
and q
refer to eastward and northward wind components, temperature, geopotential, and specific humidity (respectively).
Runtime Engine(s): PyTorch
Supported Hardware Microarchitecture Compatibility:
Supported Operating System(s):
Model Version: v1
Link: ERA5
** Data Collection Method by dataset
** Labeling Method by dataset
Properties:
ERA5 data for the period January 1980 - December 2016. ERA5 provides hourly estimates of various
atmospheric, land, and oceanic climate variables. The data covers the Earth on a 30km
grid and resolves the atmosphere at 137 levels.
For more information about ERA5 and a list of known and resolved issues, see the associated documentation and
reference publication which provides more detailed information about the quality of the ERA5 reanalysis. The ERA5
reanalysis, and therefore any model trained using it as a data source, is an imperfect representation of the state of global weather, with correlated errors as a function of
region and time. Furthermore, the limited spatial and vertical resolution of the dataset means that physical behavior near or below that resolution scale are not accurately resolvable.
Review ECMWF's publications for further information about the quality of its forecasts.
Link: ERA5
** Data Collection Method by dataset
** Labeling Method by dataset
Properties:
ERA5 data for the date range of January 2017 - December 2018. ERA5 provides hourly estimates of various
atmospheric, land, and oceanic climate variables. The data covers the Earth on a 30km
grid and resolves the atmosphere at 137 levels.
For more information about ERA5 and a list of known and resolved issues, see the associated documentation and
reference publication which provides more detailed information about the quality of the ERA5 reanalysis. The ERA5
reanalysis, and therefore any model trained using it as a data source, is an imperfect representation of the state of global weather, with correlated errors as a function of
region and time. Furthermore, the limited spatial and vertical resolution of the dataset means that physical behavior near or below that resolution scale are not accurately resolvable.
Review ECMWF's publications for further information about the quality of its forecasts.
Link: ERA5
** Data Collection Method by dataset
** Labeling Method by dataset
Properties:
ERA5 data for the date range of January 2019 - December 2020. ERA5 provides hourly estimates of various
atmospheric, land, and oceanic climate variables. The data covers the Earth on a 30km
grid and resolves the atmosphere at 137 levels.
For more information about ERA5 and a list of known and resolved issues, see the associated documentation and
reference publication which provides more detailed information about the quality of the ERA5 reanalysis. The ERA5
reanalysis, and therefore any model trained using it as a data source, is an imperfect representation of the state of global weather, with correlated errors as a function of
region and time. Furthermore, the limited spatial and vertical resolution of the dataset means that physical behavior near or below that resolution scale are not accurately resolvable.
Review ECMWF's publications for further information about the quality of its forecasts.
Engine: PyTorch
Test Hardware:
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