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melting of Greenland glaciers , cutting off the warm surface ocean currents , and thereby disrupting transfer of energy to polar latitudes , thus triggering rapid glaciation which would then reduce heat absorption due to changes in the earth ’s overall albedo , leading to a runaway cooling back cycle(passive) caused bydensity of ocean waters
melting of Greenland glaciers , cutting off the warm surface ocean currents , and thereby disrupting transfer of energy to polar latitudes , thus triggering rapid glaciation which would then reduce heat absorption due to changes in the earth ’s overall albedo , leading to a runaway cooling feedback cycle(passive) caused bydensity of ocean waters
differences in the densities of ocean water(passive) caused byDensity Currents Deep water circulation
And when that water gets dense enough , it sinkscausesdeep - ocean density currents
differences in temperature & salinity(passive) caused byDensity currents ( subsurface
differences in densitycreatedensity currents in the ocean
The high concentrationcauseshigh density of the water
The wind rustling through thousands of trees , raindropscausingripples on the stillest of waters
poor reactor hydraulicsresultingshort - circuiting density current – incoming water
synaptic activity in a neuron(passive) caused bya transmembrane current density
the deep gravity current between the middle and southern Caspian Sea basins(passive) caused bythe deep gravity current between the middle and southern Caspian Sea basins
near the equatororiginatednear the equator
a systematic fall cycle of " flushingcreatinga systematic fall cycle of " flushing
to higher phenol and cresol yields between 623 K and 673 K. Yokoyama et alledto higher phenol and cresol yields between 623 K and 673 K. Yokoyama et al
to internal wavescan leadto internal waves
to transport of the fine tailings to the near surface aerobic environment where direct contact of contaminant with aquatic organisms is possibleleadingto transport of the fine tailings to the near surface aerobic environment where direct contact of contaminant with aquatic organisms is possible
them to sink results in what is termed circulation , or overturn , of lake watersto causethem to sink results in what is termed circulation , or overturn , of lake waters
the transition back to the non - convective statecausingthe transition back to the non - convective state
to the accumulation of bacteriacan contributeto the accumulation of bacteria