Science, Том 323,Выпуски 5917-5922American Association for the Advancement of Science, 2009 |
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Стр. 1443
... ocean around Antarctica helps regulate the exchange of carbon dioxide ( CO2 ) between the deep sea and the atmosphere , as well as the supply of dissolved silicon to the euphotic zone of the Southern Ocean . Diatom productivity south of ...
... ocean around Antarctica helps regulate the exchange of carbon dioxide ( CO2 ) between the deep sea and the atmosphere , as well as the supply of dissolved silicon to the euphotic zone of the Southern Ocean . Diatom productivity south of ...
Стр. 1445
... Ocean ( 16 ) . 0.37 F ( opal ) Pa / Th 0.32 0.27 0.22 0.17 0.12 0.12 0.10 0.08 0.06 0.2 E27-23 59.62 ° S 155.24 ° E 0.04 99 0.4 200 0.0 A 3.0 2.5 2.0 222228 1.5 1.0 0.5 NBP9802-6PC 61.9 ° S 170 ° W 0.0 5 10 15 Age ( ka ) 20 20 0.52 0.42 ...
... Ocean ( 16 ) . 0.37 F ( opal ) Pa / Th 0.32 0.27 0.22 0.17 0.12 0.12 0.10 0.08 0.06 0.2 E27-23 59.62 ° S 155.24 ° E 0.04 99 0.4 200 0.0 A 3.0 2.5 2.0 222228 1.5 1.0 0.5 NBP9802-6PC 61.9 ° S 170 ° W 0.0 5 10 15 Age ( ka ) 20 20 0.52 0.42 ...
Стр. 1717
... ocean adjustment will continue after 180 years , but we do not expect large qualitative changes in the warming pattern . The actual values of the ocean vertical diffusivity in the Pliocene are highly uncertain , so these experiments ...
... ocean adjustment will continue after 180 years , but we do not expect large qualitative changes in the warming pattern . The actual values of the ocean vertical diffusivity in the Pliocene are highly uncertain , so these experiments ...
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