### The Younger Dryas Cooling
The Younger Dryas was a period of abrupt cooling that occurred approximately years ago. Two scientists discuss different hypotheses for the cause of this event.
Scientist 1
Around years ago, a massive influx of freshwater from the melting Laurentide Ice Sheet entered the North Atlantic Ocean. Because freshwater is less dense than saltwater, this freshwater remained at the surface, preventing the sinking of warm, salty water that drives the Atlantic Meridional Overturning Circulation (AMOC). The resulting shutdown of the AMOC halted the northward transport of heat, triggering a rapid and severe cooling of the Northern Hemisphere.
Scientist 2
The Younger Dryas cooling was triggered by a comet impact. The comet exploded in the atmosphere, creating widespread fires and sending massive amounts of dust and soot into the atmosphere. This atmospheric debris blocked incoming solar radiation, causing immediate global cooling. The melting of the ice sheet and subsequent freshwater influx into the ocean were consequences of the impact, not the initial trigger of the cooling.
Based on the viewpoints of Scientist 1 and Scientist 2, the scientists disagree on which of the following points?
- Whether the primary trigger of the Younger Dryas cooling was a change in ocean currents or a comet impactCevap
- BWhether the Younger Dryas was characterized by a temporary decrease in global temperatures
- CWhether the influx of freshwater occurred at some point during the Younger Dryas period
- DWhether the density of ocean surface water is determined by its temperature rather than its salinity