The maps on this page are based on data from the ERA5 and ERA5-Land Reanalysis data sets, were drawn using the NCAR Command Language (NCL) and animated using HAnis – the HTML5 Image AnimationS webapp. See the acknowledgments below. The data plotted are 1991-2020 long-term means. The resolution of the data behind the ERA5 global maps is 0.25 degrees, and 0.1 degrees for the ERA5-Land North America and CONUS maps. See the elevation maps below.
Global energy balance
Radiative components – Top of the Atmosphere (TOA)
[Incident
SW] [TOA
SW up] [TOA
net SW] [TOA
down | TOA up | TOA net | Sfc net]
Radiative components – Surface
[SW
down] [SW
up] [SW
net] [SW
down | SW up | net SW]
[LW
down] [LW
up] [LW
net] [LW
down | LW up | net LW]
[net
SW] [net
LW] [net
radiation] [net
SW | net LW | net radiation]
Non-radiative components
[sensible
heat flux] [latent
heat flux] [substrate
heat flux/change in storage] [all]
Energy-balance components follow the Sellers (1968) sign convention:
Temperature
[2m
air temperature] [2m
air temperature (polar)] [Surface
net radiation & 2m air temp]
[Skin
temperature] [2m
air temperature - Skin temperature]
Atmospheric circulation & winds
Surface
[SLP
& 10m winds] [SLP
& 10m winds (polar)]
[U-component
10 m wind] [V-component
10 m wind] [10
m wind speed]
[U-component
10 m wind (polar)] [V-component
10 m wind (polar)] [10
m wind speed (polar)]
Upper-level
[500
hPa hgt & wind] [500
hPa hgt & wind (polar)] [500
hPa vertical velocity]
[U-component
300 hPa wind] [V-component
300 hPa wind] [300
hPa wind speed]
[U-component
300 hPa wind (polar)] [V-component
300 hPa wind (polar)] [300
hPa wind speed (polar)]
Meridional cross sections
[Zonal
wind & meridional mass streamfunction] [Zonal
wind and meridional mass streamfunction – annual average]
[Zonal
wind & meridional mass streamfunction & vectors] [Zonal
wind and meridional mass streamfunction & vectors – annual
average]
[Zonal
& meridional wind] [Zonal
& meridional wind – annual average]
Streamlines
[Surface
(10m)] [500
hPa] [300
hPa]
[Surface
(10m) (polar)] [500
hPa (polar)] [300
hPa (polar)]
Vertical velocity (omega) and the U and V components of the wind use the following sign convention:
Energy
Atmospheric energy fluxes
[Total
energy flux] [Heat
flux] [Latent
heat flux] [Kinetic
energy flux] [all]
(note the different scales)
Atmospheric moisture
Moisture flux and water vapor
[Moisture-flux
divergence] [Vertically
integrated moisture flux] [vertically
integrated water vapor] [all]
[air
temperature and specific humidity meridional cross section] [below
100 hPa]
Global water balance/precipitation/snow
Precipitation controls
[vertically
integrated water vapor] [500
hPa vertical velocity] [total
cloud cover] [precipitation
rate] [all]
Precipitation and evaporation
[precipitation
rate] [evaporation
rate] [P
- E] [all]
Surface water balance
[precipitation
rate] [evaporation
rate] [runoff
rate] [ΔS]
[all]
Snow
[snowfall
rate] [snowmelt
rate] [snow
depth] [all]
[precipitation
rate] [rainfall
rate] [snowfall
rate] [snow
depth] [all]
[snowfall
rate] [snowmelt
rate] [snow
depth] [all]
(poleward of 30° N and S)
[precipitation
rate] [rainfall
rate] [snowfall
rate] [snow
depth] [all]
ERA5-Land high-resolution maps for North America
These maps show ERA5-Land data for selected variables. The ERA5-Land data are on a 0.10-degree grid, and for comparison, ERA5 data on the 0.25-degree are included.
North America
[2m
air temperature, ERA5-Land] [2m
air temperature, ERA5]
[precipitation
rate, ERA5-Land] [precipitation
rate, ERA5]
CONUS
[2m
air temperature, ERA5-Land] [2m
air temperature, ERA5]
[precipitation
rate, ERA5-Land] [precipitation
rate, ERA5]
Reanalysis Grid-point Elevations
The scale of the climatic features that can be resolved by the reanalysis data depends on the resolution of the models. For the ERA5 data, the resolution is 0.25 degrees, and for the ERA5-Land data, the resolution is 0.10 degrees. In both cases, real “landscape-scale” features that are of smaller spatial scale will not be resolved by the data, or visible on the maps on this page.
ERA5 (0.25-degree)
[Globe]
[Globe
b&w] [North
America] [North
America b&w] [CONUS]
[CONUS
b&w]
ERA5-Land (0.25-degree) [Globe] [Globe b&w] [North America] [North America b&w] [CONUS] [CONUS b&w]
Acknowledgements
Data sources
The global data plotted here are from the ECMWF fifth-generation ERA5 Reanalysis: [ERA5 monthly averaged data on pressure levels from 1979 to present] and [ERA5 monthly averaged data on single levels from 1979 to present]
The results contain modified Copernicus Climate Change Service information 2021. Neither the European Commission nor ECMWF is responsible for any use that may be made of the Copernicus information or data it contains.
Hersbach, H., Bell, B., Berrisford, P., Biavati, G., Horányi, A., Muñoz Sabater, J., Nicolas, J., Peubey, C., Radu, R., Rozum, I., Schepers, D., Simmons, A., Soci, C., Dee, D., Thépaut, J-N. (2019): ERA5 monthly averaged data on single levels from 1979 to present. Copernicus Climate Change Service (C3S) Climate Data Store (CDS). (Accessed on 27-Dec-2021), [https://doi.org/10.24381/cds.f17050d7]
Hans Hersbach, Bill Bell, Paul Berrisford, Shoji Hirahara, András Horányi, Joaquín Muñoz-Sabater, Julien Nicolas, Carole Peubey, Raluca Radu, Dinand Schepers, Adrian Simmons, Cornel Soci, Saleh Abdalla, Xavier Abellan, Gianpaolo Balsamo, Peter Bechtold, Gionata Biavati, Jean Bidlot, Massimo Bonavita, Giovanna De Chiara, Per Dahlgren, Dick Dee, Michail Diamantakis, Rossana Dragani, Johannes Flemming, Richard Forbes, Manuel Fuentes, Alan Geer, Leo Haimberger, Sean Healy, Robin J. Hogan, Elías Hólm, Marta Janisková, Sarah Keeley, Patrick Laloyaux, Philippe Lopez, Cristina Lupu, Gabor Radnoti, Patricia de Rosnay, Iryna Rozum, Freja Vamborg, Sebastien Villaume, Jean-Noël Thépaut (2020) The ERA5 global reanalysis. Quarterly Journal of the Royal Meteorological Society 146:1999-2049. [https://doi.org/10.1002/qj.3803]
Regional data are from the ERA5-Land Reanalysis Data set: [ERA5-Land monthly averaged data from 1950 to present].
The results contain modified Copernicus Climate Change Service information 2021. Neither the European Commission nor ECMWF is responsible for any use that may be made of the Copernicus information or data it contains.
Muñoz Sabater, J., (2021): ERA5-Land monthly averaged data from 1950 to 1980. Copernicus Climate Change Service (C3S) Climate Data Store (CDS). (Accessed on 11-Mar-2022), [https://doi.org/10.24381/cds.68d2bb30].
J. Muñoz-Sabater, Dutra, E., Agustí-Panareda, A., Albergel, C., Arduini, G., Balsamo, G., Boussetta, S., Choulga, M., Harrigan, S., Hersbach, H., Martens, B., Miralles, D. G., Piles, M., Rodríguez-Fernández, N. J., Zsoter, E., Buontempo, C., and Thépaut, J.-N.: ERA5-Land: A state-of-the-art global reanalysis dataset for land applications, Earth Syst. Sci. Data, 13:4349–4383, 2021. [https://doi.org/10.5194/essd-13-4349-2021].
Maps
Maps were created using the NCAR Command Language (NCL) [https://www.ncl.ucar.edu] The NCAR Command Language (Version 6.6.2) [Software]. (2019). Boulder, Colorado: UCAR/NCAR/CISL/TDD. http://dx.doi.org/10.5065/D6WD3XH5
Shapefiles for the continental outlines and administrative units on the ERA5-Land maps were downloaded from Natural Earth [https://www.naturalearthdata.com]
Animations
The animations were created using HAnis – the HTML5 Image AnimationS webapp [https://www.ssec.wisc.edu/hanis/] by Tom Whittaker, Space Science and Engineering Center, University of Wisconsin–Madison.