Science, Volume 295, Issues 5559-5564John Michels (Journalist) American Association for the Advancement of Science, 2002 |
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Page 2253
... changes in the medium , or in diagnostic mode , where the temporal change in the medium is quantified . 80 m . The waveforms recorded before and after the perturbation at the receiver are shown on the -25-5 0 10 20 30 40 50 60 70 80. 22 ...
... changes in the medium , or in diagnostic mode , where the temporal change in the medium is quantified . 80 m . The waveforms recorded before and after the perturbation at the receiver are shown on the -25-5 0 10 20 30 40 50 60 70 80. 22 ...
Page 2376
... change can provide clues to the origin of meltwater pulses dur- ing deglaciation . Increasingly sophisticated models that simulate the phe- nomena responsible for past sea level changes enable us to un- derstand the complex interac ...
... change can provide clues to the origin of meltwater pulses dur- ing deglaciation . Increasingly sophisticated models that simulate the phe- nomena responsible for past sea level changes enable us to un- derstand the complex interac ...
Page 2436
... changes energize the geodynamo . Others , however , resulted in contradictory conclusions : They detected no stable frequency ( 5 ) , or the fre- quency was an artifact caused by paleocli- matically induced rock - magnetic changes ( 9 ...
... changes energize the geodynamo . Others , however , resulted in contradictory conclusions : They detected no stable frequency ( 5 ) , or the fre- quency was an artifact caused by paleocli- matically induced rock - magnetic changes ( 9 ...
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