It is inevitable that the warmer the world gets, the greater the risk that other parts of the Antarctic will reach a similar tipping point; in fact, we now know that the Wilkes Basin in East Antarctica, as big or even bigger than the ice sheet in the West, could be similarly vulnerable.
C'est inévitable : plus la planète se réchauffe, plus d'autres parties de l'Antarctique risquent d'atteindre un point de basculement similaire.