### The Younger Dryas Cooling Event
The Younger Dryas (approx. to years ago) was a period of abrupt, severe global cooling that temporarily reversed the warming trend following the Last Glacial Maximum. Three hypotheses have been proposed to explain the trigger for this cooling event.
Hypothesis 1
Around years ago, a fragmented comet or asteroid entered Earth's atmosphere and exploded over North America. The thermal energy and pressure wave from this impact event caused widespread wildfires and destabilized the southern margin of the Laurentide Ice Sheet. The rapid melting of ice released a massive volume of freshwater into the North Atlantic. This freshwater influx disrupted the Atlantic Meridional Overturning Circulation (AMOC)—the oceanic conveyor belt that transports heat from the tropics to high latitudes—leading to rapid global cooling.
Hypothesis 2
The cooling event was triggered entirely by internal Earth climate system dynamics. As the Laurentide Ice Sheet naturally retreated due to post-glacial warming, it exposed new topographic outlets. Rather than flowing down the Mississippi River valley into the Gulf of Mexico, freshwater meltwater was suddenly diverted eastward through the St. Lawrence River valley into the North Atlantic. This sudden, non-catastrophic redirection of freshwater lowered the salinity of the North Atlantic, halting the AMOC and initiating the cooling cycle without the need for any extraterrestrial impact.
Hypothesis 3
The primary trigger for the cooling was a combination of reduced solar activity and intense, repeated volcanic eruptions. A prolonged period of low solar irradiance reduced global temperatures, which was exacerbated by stratospheric sulfate aerosols from volcanic eruptions. These aerosols reflected incoming solar radiation back into space. The initial cooling expanded Northern Hemisphere sea ice. Because sea ice has a high albedo, it reflected more sunlight, creating a self-sustaining feedback loop that suppressed the AMOC and sustained the Younger Dryas cold period.
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Both Hypothesis 2 and Hypothesis 3 discuss the suppression or shutdown of the Atlantic Meridional Overturning Circulation (AMOC) during the Younger Dryas. Which of the following statements best describes a key difference between the two hypotheses regarding the role of the AMOC in the cooling event?
- AHypothesis 2 claims that the shutdown of the AMOC was a feedback effect resulting from sea ice expansion, whereas Hypothesis 3 claims that the AMOC shutdown was the primary cause of cooling, triggered by redirected meltwater.
- BHypothesis 2 claims that the shutdown of the AMOC was triggered by a cosmic impact, whereas Hypothesis 3 claims that the AMOC shutdown was triggered by a change in the river valley pathways of post-glacial meltwater.
- Hypothesis 2 claims that the shutdown of the AMOC was the primary cause of cooling, triggered by redirected meltwater, whereas Hypothesis 3 claims that the AMOC shutdown was a secondary feedback effect resulting from sea ice expansion.Answer
- DHypothesis 2 claims that the shutdown of the AMOC had no influence on Younger Dryas cooling, whereas Hypothesis 3 claims that the AMOC shutdown directly caused volcanic eruptions.