Cave art and climate: how satellites and chaos theory cou...
© Museum of Altamira and Cave of Altamira, Spanish Ministry of Culture and Sport. Photographer P Saura Tracking the cave […]
Deep learning – a new potential tool for image reco...
How can brightness temperatures be reconstructed from the signals received by antenna arrays (as in the case of SMOS) ? […]
A new version v9 of debiased SSS L3 maps from LOCEAN/ACRI...
Jacqueline Boutin indicates that… … A new version (version 9) of de-biased SMOS SSS L3 maps generated by LOCEAN /ACRI-ST […]
Happy International Forests Day !
Today is March 21, a date proclaimed by the United Nations to celebrate and raise awareness about the importance of […]
A new version (version 2) of SMOS Arctic Level 3 Sea Surf...
A new version (version 2) of SMOS Arctic Level 3 Sea Surface Salinity is available at CATDS CEC-OS (see more […]
Announcement: 7th Ocean Salinity Conference 2024
The “7th Ocean Salinity Conference 2024” will be held in ESA-ESTEC, Noordwijk, the Netherlands, on 13-16 May 2024. This is the 7th of a […]
Estimating the above-ground biomass : a new method using ...
Monitoring above-ground biomass (AGB) on Earth is essential to track the evolution of carbon stocks, and the use of […]
SMAP Compatible SMOS data available at CATDS
Figure 1: Panel A: SMOS Level-3 brightness temperatures after being bias-corrected with respect to SMAP Enhanced Level-3 brightness temperatures. H […]
New L3 TB polar grid available with geolocation bug corre...
The version 331 of the L3 brightness temperatures on the polar projections presented a slight shift in latitudes and longitudes, […]