OVERVIEW OF OAFLUX PRODUCTS
The following two versions of OAFlux products are available.
- OAFlux-1° blended products: developed from optimal synthesis of satellite wind and SST observations and atmospheric reanalysis of air temperature and humidity. The products are available on 1° resolution from 1958 to the present. The project is sponsored by NOAA GOMO program.
- OAFlux-0.25° satellite products: developed from merging satellite observations from multiple sensors including scatterometers, radiometers, and sounders. he products are available on 0.25° resolution for the satellite era (1988 onward). The project is sponsored by NASA MeaSUREs program.
Note: The two versions of products are developed using different methodologies, different algorithms, and different source datasets. For more information about the differences between the two products, please read here. A summary of air-sea fluxes and variables contained in each product is provided below.
|OAFlux 1-deg analysis (1958 -)||OAFlux 0.25-deg ANALYSIS (1988 -)||Unit|
|Latent Heat Flux (QLH)||Latent Heat Flux (QLH)||W/m2, positive upward|
|Sensible Heat Flux (QSH)||Sensible Heat Flux (QSH)||W/m2, positive upward|
|ISCCP Net downward shortwave radiation (QSW) (up to 2009)||W/m2, positive downward|
|ISCCP Net upward longwave radiation (QLW) (up to 2009)||W/m2, positive upward|
|Ocean net heat gain (Qnet = QSW - QLW - QLH - QSH) (up to 2009)||W/m2, positive downward|
|Moisture Flux (Ocean Evaporation) (E)||Moisture Flux (Ocean Evaporation) (E)||cm/yr, positive upward|
|Momentum flux (wind stress) (tau)||N/m2|
|Zonal wind stress component (tau-x)||N/m2, positive eastward|
|Meridional wind stress component (tau-y)||N/m2, positive northward|
|Sea surface temperature (Ts)||Sea surface temperature (Ts)||degree C|
|2m air temperature (Ta)||2m air temperature (Ta)||degree C|
|2m air specific humidity (qa)||2m air specific humidity (qa)||g/kg|
|10m equivalent neutral wind speed||10m equivalent neutral wind speed||m/s|
|zonal wind component||m/s, positive eastward|
|meridional wind component||m/s, positive northward|
|wind stress curl||N/m3|
|Ekman pumping velocity||cm/day|