Mesoscale phenomena are ubiquitous and highly energetic features of ocean circulation.
Their influence on biological and biogeochemical processes varies widely, stemming not …

The motivation to study the vertical exchanges of tracers associated with mesoscale eddies
is that the mean concentration of most oceanic tracers changes rapidly with depth. Because …

Mesoscale ocean eddies, an important element of the climate system, impact ocean
circulation, heat uptake, gas exchange, carbon sequestration and nutrient transport. Much of …

PISCES-v2 is a biogeochemical model which simulates the lower trophic levels of marine
ecosystem (phytoplankton, microzooplankton and mesozooplankton) and the …

This report is the first complete assessment of the science of climate change since Working
Group I (WGI) of the IPCC produced its second report Climate Change 1995: The Science of …

A common dynamical paradigm is that turbulence in the upper ocean is dominated by three
classes of motion: mesoscale geostrophic eddies, internal waves and microscale three …

The concentration of CO2 in the atmosphere has risen from close to 280 parts per million
(ppm) in 1800, at first slowly and then progressively faster to a value of 367 ppm in 1999 …

The new edition of this widely respected text provides comprehensive and up-to-date
coverage of the effects of biological–physical interactions in the oceans from the microscopic …

Seamounts are ecological oases nurturing abundant fisheries resources and epibenthic
megafauna in the vast oligotrophic ocean. Despite their significance, the formation …

The ocean's nitrogen cycle is driven by complex microbial transformations, including
nitrogen fixation, assimilation, nitrification, anammox and denitrification. Dinitrogen is the …