Water column biogeochemistry of oxygen minimum zones in the eastern tropical North Atlantic and eastern tropical South Pacific oceans

For Catholic communities, which are located mostly in Latgale (the eastern part of Latvia) and in isolated places in Augšzeme (the south-eastern part of Latvia) and Kurzeme

Note that negative values of h correspond to the boreal (Northern Hemisphere) winter, that is to the upwelling sea- son – December-January-February – in the eastern Tropical Pacific;

Trapping of highly productive coastal waters in anticyclonic eddies (e.g. eddy A) led to a net enhancement of N-loss processes in its centre both through denitrification and

5a with data collected in the Southern Ocean (Fig. 5b) near the Kerguelen plateau, where natural iron fertilisation of surface waters has clearly been demon- strated (Blain et

The source water masses are Subtropical Water (STW), Subantarctic Water (SAAW), Equatorial Subsurface Water (ESSW), Antarctic Intermediate Water (AAIW) and Pacific Deep Water (PDW).

Eddy core anomalies from the di ff erence between profiles outside the eddy and in the eddy core (as shown in the section plots) versus depth for salinity, temperature, density

These olives are spread from the north-western to the south- eastern provinces of Iran and are referred to as ecotypes in this text. A wide repertoire of these ecotypes has

Concentration averaged over the global ocean and at selected areas (bottom of the North Tropical Atlantic, bottom of the North Tropical Pacific and Mid-Pacific) from a