They range from LANDSAT images of
land use in the Chesapeake Basin, to fish catches off California since the 1920s, to 400,000 years of global temperature estimates from
antarctic ice cores.
T, his was sho \ vn not only by the rise of temperature at
land stations, but also by the clccrease in the amount of
ice in arctic and probably also in
antarctic regions and by the rise of sea temperatures.
Mercer (1968, 1978) proposed that atmospheric warming could cause the
ice shelves of western Antarctica to disintegrate and that as a consequence the entire West Antarctic Ice Sheet (10 % of the antarctic ice volume) would lose its land connection and come afloat, causing a sea level rise of about five metr
ice shelves of western Antarctica to disintegrate and that as a consequence the entire West
Antarctic Ice Sheet (10 % of the antarctic ice volume) would lose its land connection and come afloat, causing a sea level rise of about five metr
Ice Sheet (10 % of the
antarctic ice volume) would lose its land connection and come afloat, causing a sea level rise of about five metr
ice volume) would lose its
land connection and come afloat, causing a sea level rise of about five metres.