Iron and / or phosphorus are thought to be limiting factors in
most oceanic regions.
Not exact matches
Although the South America plate exhibits a chain of active volcanism resulting from the subduction and partial melting of the Nazca
oceanic lithosphere along
most of the arc, these
regions of inferred shallow subduction correlate with an absence of volcanic activity.
The another
most important climate variation is El Niño — Southern Oscillation (ENSO) events, which impact the global
oceanic and atmospheric circulations which thereby produce droughts, floods and intense rainfall in certain
regions.
Diversity less than 2 is calculated over the northern Pacific and Atlantic oceans and exceeding 2 over
most of the
oceanic regions south of 30 ° S and over Antarctica.
To date,
most large - scale water vapor climatological studies have relied primarily on analysis of radiosonde data, which have good resolution in the lower troposphere in populated
regions but are of limited value at high altitude and are lacking over remote
oceanic regions.
We see that
most CO2 in the atmosphere is found above or downwind of sunny
oceanic regions beneath the subtropical high pressure cells and those
regions migrate latitudinally to and fro with the seasons.