North Atlantic ocean current is slowing down
北大西洋洋流正在減緩
更新於: 2026年6月16日 上午08:15
The Atlantic Meridional Overturning Circulation, or AMOC, is an essential ocean current that functions like a global conveyor belt.
大西洋經向翻轉環流(AMOC)是一種至關重要的洋流，其運作方式宛如全球輸送帶。
By moving warm, salty water from the tropics to the North Atlantic, it regulates temperatures, transports nutrients, and stabilizes global climate patterns.
它將熱水與鹹水從熱帶輸送至北大西洋，藉此調節溫度、運送養分並穩定全球氣候型態。
However, recent scientific observations suggest this vital system is slowing down.
然而，近期科學觀測顯示，這個至關重要的系統正在減緩。
As climate change accelerates the melting of ice sheets, such as those in Greenland, vast amounts of fresh water flow into the North Atlantic.
隨著氣候變遷加速了格陵蘭島等地冰層的融化，大量淡水湧入北大西洋。
A potential collapse of the AMOC could have severe global consequences, including regional cooling in Western Europe, erratic rainfall, and accelerated sea-level rise.
若AMOC潛在崩潰，可能會造成嚴重的全球後果，包括西歐地區冷卻、降雨型態異常以及海平面加速上升。
While it remains a low-probability event, it is a critical topic that highlights the complex and fragile nature of our planet's climate systems.
雖然這仍屬於低概率事件，但這是一個關鍵議題，突顯了地球氣候系統複雜且脆弱的本質。
