Dataset - B2FIND

Seawater carbonate chemistry and calcification in the Bahama Bank, 1964-1965

Carbon dioxide is lost from the ocean by calcium carbonate precipitation (-p), photosynthesis (-b) and gas evasion at the sea surface (-g). Among the most active sites are warm...

EOT20 - A global Empirical Ocean Tide model from multi-mission satellite alti...

EOT20 is the latest in a series of global ocean tide models developed at DGFI-TUM. EOT20 is created using residual tidal analysis of multi-mission altimetry data from the period...

Seawater carbonate chemistry and community calcification during a Molokai ree...

The severity of the impact of elevated atmospheric pCO2 to coral reef ecosystems depends, in part, on how seawater pCO2 affects the balance between calcification and dissolution...

Seawater carbonate chemistry and community calcification during Miyako Island...

Coral reefs are characterized by enormous carbonate production of the organisms. It is known that rapid calcification is linked to photosynthesis under control of the carbonate...

Carbonate system data on the Molokai reef flat

The severity of the impact of elevated atmospheric pCO2 to coral reef ecosystems depends, in part, on how seawater pCO2 affects the balance between calcification and dissolution...