hat
Aktivite imen, tankou boule konbistib fosil, pwodiksyon siman, ak debwazman, te ogmante konsantrasyon gaz efè tèmik nan atmosfè nou an. Te akimile nan gaz kabonik ak lòt chalè-pyèj gaz ogmante tanperati atmosferik, chofe Latè a ~ 0.9 ° C depi 1880, ak projetée pli lwen chofe li ant 2-4 ° C pa 2100, sitou akòz aktivite imen. ref Sa a ogmante te mennen nan yon ogmantasyon korespondan nan tanperati lanmè, patikilyèman nan sifas la nan oseyan an. Oseyan ki pi cho pouvwa tou mennen nan plis pouvwa anpil tanpèt ak ogmante nan nivo lanmè, ki ka dramatikman afekte ekosistèm Reef koray.
eng
Human activities, such as the burning of fossil fuels, cement production, and deforestation, have increased greenhouse gas concentrations in our atmosphere. The accumulation of carbon dioxide and other heat-trapping gasses has increased atmospheric temperatures, warming the Earth ~0.9°C since 1880, and projected to further warm it between 2-4°C by 2100, mostly due to human activity. ref This increase has led to a corresponding increase in ocean temperatures, particularly in the surface of the ocean. Warmer oceans may also lead to more powerful storms and increases in sea level, which can dramatically affect coral reef ecosystems.