In 1892 he started planning what became known as the FRAM expedition, named after the polar vessel he specially constructed for this North Pole expedition. The significant results gained from that expedition included the discovery of a deep Arctic Ocean, the confirmation of the existence of a Transpolar Current, and observations of pack ice drift relative to the prevailing wind direction which provided the impetus for the later identification of the Ekman spiral (one of the cornerstones on which the modern theory of wind-driven circulation is built). The FRAM expedition and those that followed were also marked by careful measurement and compilation of data, detailed planning, and forceful execution, qualities that provided a firm baseline for all future expeditions.
Nansen had a strong practical bent as a scientist and explorer, improving old equipment and even inventing new equipment when the need arose. The most famous of his inventions was the Nansen bottle for sampling ocean water at various depths. He also strongly supported international cooperation in oceanography and, as a direct result, was one of the founding fathers of the International Council for the Exploration of the Sea (ICES) in 1902.
He become heavily involved in politics in his native Norway and played an important role in 1905 when Norway declared full independence from Sweden, which resulted in his being appointed the first Norwegian ambassador in London. After two years as ambassador, he returned to oceanography for several years until the advent of World War I, publishing the book The Norwegian Sea with B. Helland-Hansen during this period. He spent the remainder of his life after World War I engaged in various humanitarian activities until his death at age 60 in 1930, receving his Nobel Prize in 1922.
where R is the net radiation, S the insolation,
the planetary
albedo, F the outgoing longwave radiation, and Q the absorbed
solar radiation.
See Hartmann (1993).
The main anthropogenic sources of atmospheric nitrous oxide are combustion (of fossil fuels, wood, or other biomass) and the widespread use of fertilizers, although the estimates for the amount supplied by the latter are highly variable. Natural sources include gas release into the atmosphere by the oceans and tropical and temperate forest soils.