Sea-level rises are a possible consequence of global warming. As the amount of free water in the oceans increases, and as the water becomes warmer, global warming will increase. In addition, according to theory, the heating at the poles may reduce the amount of water trapped in glaciers and ice caps. (Source: WRIGHT)



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Heine K 1985. Jungquartaere Klimaschwankungen auf der Suedhalbkugel. Zentralblatt der Geologie und Paläontologie 1 (11/12) 1751-1768
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Jungquartaere Klimaschwankungen auf der Suedhalbkugel.pdf 1.88 MB
Hughes P, Brundrit GB, Searson S 1992. The vulnerability of Walvis Bay to rising sea levels. Journal of coastal research 8 (4) 868 - 881
Mather AA, Garland GG, Stretch DD 2009. Southern African sea levels: Corrections, influences and trends. African Journal of Marine Science 31 (2) 145 - 156