It was described as “the largest single event in a series of retreats by ice shelves in the peninsula over the last 30 years”, by the U.S.-based National Snow and Ice Data Center. However, he points out the fact that the shelf was 200 meters thick, equaling to about 500 tons of ice, with a surface area “three times the size of Hong Kong” at the time of its demise. He also pointed out that because the shelf was a floating part of an ice sheet, as opposed to being over land, it does not raise the sea level upon melting. He continues on to state that an ice sheet in Stream C, on the West Antarctic is actually getting thicker, growing at about 26.8 gigations per year. If the demise of the Larsen B ice shelf was indeed a result of global warming, how is that Stream C is doing the opposite in the same environment? These are just some of the facts used by Scott to support his theory that these things are simply a result of Mother Nature running its
It was described as “the largest single event in a series of retreats by ice shelves in the peninsula over the last 30 years”, by the U.S.-based National Snow and Ice Data Center. However, he points out the fact that the shelf was 200 meters thick, equaling to about 500 tons of ice, with a surface area “three times the size of Hong Kong” at the time of its demise. He also pointed out that because the shelf was a floating part of an ice sheet, as opposed to being over land, it does not raise the sea level upon melting. He continues on to state that an ice sheet in Stream C, on the West Antarctic is actually getting thicker, growing at about 26.8 gigations per year. If the demise of the Larsen B ice shelf was indeed a result of global warming, how is that Stream C is doing the opposite in the same environment? These are just some of the facts used by Scott to support his theory that these things are simply a result of Mother Nature running its