AMOC is an ocean circulation system that transfers warm, salty surface waters from Tropics to North Atlantic and returns cold, dense water southward.

The Gulf Stream is the most important source of AMOC. It carries warm water towards Europe which keeps Europe warm.

AMOC is the phenomenon of North Atlantic Ocean not Northern Pacific.

AMOC एक महासागरीय परिसंचरण प्रणाली है जो गर्म, नमकीन सतही जल को उष्णकटिबंधीय से उत्तरी अटलांटिक तक स्थानांतरित करती है और ठंडे, घने जल को दक्षिण की ओर लौटाती है।

गल्फ स्ट्रीम AMOC का सबसे महत्वपूर्ण स्रोत है। यह यूरोप की ओर गर्म पानी ले जाता है जो यूरोप को गर्म रखता है।

AMOC उत्तरी अटलांटिक महासागर की घटना है, न कि उत्तरी प्रशांत महासागर की।

Seamounts are underwater mountains rising from the ocean floor. Seamounts are indeed large submarine landforms, typically of volcanic origin, that rise from the ocean floor but do not reach the water surface.

Guyots (or tablemounts) are a specific type of seamount that initially rose above sea level as volcanic islands. Over time, wave action eroded their summits, making them flat. Subsequent subsidence and sea-level changes caused these flat-topped features to submerge below the ocean surface, resulting in guyots.