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CAI YI, WANG Zhang-gui, QIAO Fang-li. The simulation of Pacific Ocean temperature with the global warming during 1960-1999[J]. Haiyang Xuebao, 2008, 30(5): 9-16.
Citation: CAI YI, WANG Zhang-gui, QIAO Fang-li. The simulation of Pacific Ocean temperature with the global warming during 1960-1999[J]. Haiyang Xuebao, 2008, 30(5): 9-16.

The simulation of Pacific Ocean temperature with the global warming during 1960-1999

  • Received Date: 2007-03-26
  • Rev Recd Date: 2008-03-22
  • The Pacific sea temperature from 1960-1999 was simulated using non-Boussinesq POP model, air temperature and wind stress in 1 000 hPa from NCEP.Compared to the observation,the results are rescannable and interesting.The importantresults as follows:The strongest warming is in equatorial center Pacific surface(Niño1 to Niño4).The strongest coolingis in middle-latitude center Pacific surface. There are warmin the north hemisphere Pacific coastunless about 40°N.The temperature increasingis biggerin east Pacific coastthan that in west Pacific coast.Most of Pacific Ocean temperature is decreased from 0 to 483 m with the depth,butthe equatorial center Pacific temperature is increased in sea surface and decreased in about-169 m and increased in 483 m.The temperature in the depth section of tropical center-western Pacific Oceanis decreased with time although El Niño events increasing since 1990.
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