hat
Pa 2100, ekspansyon tèmik ak glasyè k ap fonn yo dwe lakòz nivo lanmè a monte pa 0.26 mèt 0.98 (m), ki baze sou modèl klima ak konsidere senaryo wo ak ba emisyon: RCP2.6 ak RCP8.5.ref Sepandan, kontribisyon nan Greenland ak West fèy glas Antatik kapab ogmante limit la nan nivo lanmè monte.
eng
By 2100, thermal expansion and glacial melting are expected to cause the sea-level to rise by 0.26 to 0.98 meters (m), based on climate models and considering high and low emissions scenarios: RCP2.6 and RCP8.5.ref However, the contribution of the Greenland and West Antarctic ice sheet could increase the extent of sea-level rise.