海底地热通量对海洋深层温度和环流的长期影响
刘泽栋1, 万修全1,2, 刘福凯1

Long-term Impact of Geothermal Heat Flux on the Deep Ocean Temperature and Circulation
Liu Zedong1, Wan Xiuquan1,2, Liu Fukai1
图 4 3 500 m深度上地热实验与控制实验平均海水温度差 等值线间隔0.1℃,最大值0.82℃位于南太平洋117°W, 23°S和南大西洋20°W, 33°S
Fig.4 The temperature difference at 3500 m between GHF and CTRL runs Contour interval is 0.1℃. Peak value is 0.82℃ in South Pacific 117°W, 23°S and South Atlantic 20°W, 33°S