The oceanic sink for anthropogenic CO₂ from 1994 to 2007

Variability and stability of anthropogenic CO2 in Antarctic Bottom Waters observed in the Indian sector of the Southern.. Ocean Science, European Geosciences Union, 2020, 16

Regions for version 2 are the Coastal Seas, the North Atlantic, Tropical Atlantic, North Pacific, Tropical Pacific, Indian Ocean and Southern Oceans and a newly defined Arctic

Interannual sea–air CO 2 flux variations in the East Pacific Equatorial biome (left) and the global ocean (right) from selected mapping methods (having relative IAV mismatch R iav

The calculation of the annual uptake and seasonal variability of sea-air CO 2 fluxes from atmospheric inversions and ocean biogeochemical models used data from all of the models

Distribution and inventories of C ant estimated in the Southern Ocean along WOCE line I6 using the TrOCA method are compared with C ant estimates obtained along the same line

In this context of potentially high variability in C ant up- take at AABW formation sites, as well as in AABW export, circulation and mixing, we used repeated observations col-

In 2001 in the reference model, a total of 1.5 Pg C of anthropogenic carbon had entered the Mediterranean Sea with 52 % from the air–sea flux and 48 % from Atlantic Wa- ter

Il faut attendre l’an 2000 pour que le Haut Commissariat aux Eaux et Forêts bénéficie d’un nouveau prêt de la Banque Mondiale pour multiplier les