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contribution of glacial ice to sea-level change occurs through the melting of alpine glaciers around the world , and the melting of the underside of ice shelves—the portions of continental ice sheets that have extended beyond the continental margins and are currently floating on the seawater. It has recently been estimated that about half of the sea-level rise realized over this last century is the result of the melting of glacial ice , though this number is highly uncertain. The most uncertain sources of sea-level change are the Greenland and Antarctic ice sheets, since their current and likely future Amazing weed leaf high life four twenty low top shoesresponses to climate variations are poorly known. In order to validate predictions of sea-level rise, better monitoring of global sea-level change and its components will be needed. The prospects for sea-level monitoring are good. A global network of sea-level measuring stations is being implemented, and needs to be maintained in the future. At some of these stations, land movements will be measured with satellite geodesy and gravimetric techniques. Satellite altimetry is another important tool that should be fully exploited to measure global sea-level rise. observations

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