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Idealized sequences of abrupt climate changes are induced by the application of periodic freshwater fluxes to the North Atlantic (NA) and the Southern Ocean (SO), thus mainly

We invert global black carbon (BC), organic car- bon (OC) and desert dust (DD) aerosol emissions from POLDER/PARASOL spectral aerosol optical depth (AOD) and aerosol absorption

In 1997 the winter homogenized part was more akin to the deep mixed layers reported from the Amundsen Basin in 1995 (Steele and Boyd, 1998) and also observed in the eastern Nansen

Our basic energy conservation law differs little conceptu- ally from that derived previously [McKenzie, 1984; Poirier et al., 1991]; the time rate of change of internal energy

To our knowledge, rocks with a MORB-like signature formed in a subduc- tion setting but without the associated typical HFSE depletion are known only in fore-arcs, such as the

In addition, our using biomass preindustrial biomass burning emissions that are larger than most the other studies also leads to a smaller increase in tropospheric ozone burden

Devonian taxa) or two elements (Mid-Late Ordovician forms). The right infracentral area is 297.. 6a), with large marginals 308.. and small

corroborated over geological ages thanks to the statistical analysis of existing pumping tests data in comparable aquifers of the island. Since we highlight over twelve years