Flood

Flood is a 2008 work of hard science fiction by English author Stephen Baxter. It describes a near future world where deep submarine seismic activity leads to seabed fragmentation, and the opening of deep subterranean reservoirs of water. Human civilisation is almost destroyed by the rising inundation, which covers Mount Everest in 2052. Baxter issued a sequel to this work, entitled Ark, in 2009. Flood was nominated for the British Science Fiction Award in 2008. Synopsis The above effects are catastrophic, and exceed current estimates of climate change-related sea level rise. In the opening chapter, four main characters (former USAF Captain Lily Brooke, British military officer Piers Michaelmas, English tourist Helen Gray, and NASA scientist Gary Boyle) are liberated by a private megacorporation called AxysCorp from a Christian extremist Catalan terrorist bunker in Barcelona in 2016, after five years of captivity. AxysCorp was hoping to save a fifth prisoner, John Foreshaw, but he was executed minutes before the rescue. Nonetheless, the corporation continues to look after the four hostages and search for Helen's daughter, Grace, who was conceived in captivity by the son of a Saudi royal and taken by his family. Helen befriends Foreign Office official Michael Thurley in the hopes of finding her daughter, and the four rescued hostages make a pact to keep in contact. At this point, sea level changes have already submerged Tuvalu, a low lying South Pacific island, whose inhabitants have been evacuated to New Zealand. London and Sydney are prone to constant flooding. However, as a tidal surge hits London and Sydney, killing many in both cities, scientists become aware that this cannot be explained solely by the consequences of climate change. American oceanographer Thandie Jones uncovers the truth – through deep sea diving missions to oceanic ridges and trenches reveal that the seabed has fragmented, and there is turbulence that can only be attributable to the infusion of vast subterranean reservoirs of hitherto hypothesised but undetected oceanic masses of water (see below).