Nature, Volume 429Sir Norman Lockyer Macmillan Journals Limited, 2004 |
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Página 264
... record of high - latitude climate change . b , Deconvolution of the obliquity component of scaled oxygen isotope ( orange curve ) and of solar forcing ( black curve ) records ( smoothed records are thick lines ) . The period of greatest ...
... record of high - latitude climate change . b , Deconvolution of the obliquity component of scaled oxygen isotope ( orange curve ) and of solar forcing ( black curve ) records ( smoothed records are thick lines ) . The period of greatest ...
Página 623
... record , and the amplifiers that allow small changes in radiation to cause large changes in global climate , are not well understood . New records of the earlier periods , looking at parameters unavailable in marine records , are needed ...
... record , and the amplifiers that allow small changes in radiation to cause large changes in global climate , are not well understood . New records of the earlier periods , looking at parameters unavailable in marine records , are needed ...
Página 624
... record confirms that the interglacial MIS 13 peaks at a depth of 2,842 m , but is considerably colder than subsequent interglacials . This intermediate climate is insuffi- cient to give a dielectric - profiling peak , probably because ...
... record confirms that the interglacial MIS 13 peaks at a depth of 2,842 m , but is considerably colder than subsequent interglacials . This intermediate climate is insuffi- cient to give a dielectric - profiling peak , probably because ...
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