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As the ice melts entirely at the Arctic, the dark waters will not reflect back as much sunlight as the ice and snow has. So, as the ice disappears, the region will absorb more of the sun's energy and heat up more causing more melt.
Melting North Pole photographed by NOAA NetCam#1, on July 15, 2004,
at 4:45 UTC. Internal temperature was 12 degrees Celsius (about 54 degrees Fahrenheit).
2004년 7월 15일 북극을 촬영한 사진인데요. 얼음이 다 녹아있는 장면 입니다.
http://www.earthfiles.com/news/news.cfm?ID=818&category=Environment 참조 바랍니다.
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As the ice melts entirely at the Arctic, the dark waters will not reflect back as much sunlight as the ice and snow has. So, as the ice disappears, the region will absorb more of the sun's energy and heat up more causing more melt.
Melting North Pole photographed by NOAA NetCam#1, on July 15, 2004,
at 4:45 UTC. Internal temperature was 12 degrees Celsius (about 54 degrees Fahrenheit).
2004년 7월 15일 북극을 촬영한 사진인데요. 얼음이 다 녹아있는 장면 입니다.
http://www.earthfiles.com/news/news.cfm?ID=818&category=Environment 참조 바랍니다.