单词	palaeoclimate
释义	palaeoclimate /ˈpalɪəʊˌklʌɪmət / /ˈpeɪlɪəʊˌklʌɪmət/ (US paleoclimate) noun A climate prevalent at a particular time in the geological past.Through analysis of the paleoclimate record as well as a number of climate model simulations, we also suggest that it is very unlikely that the Atlantic Meridional Overturning will cease to be active in the near future.... The palaeoclimates during coal accumulation must have been very humid and very warm. The origin of the Brejos has been associated with humid paleoclimates established after the middle Tertiary, especially during interglacial phases of the Pleistocene. Derivatives palaeoclimatic /palɪəʊˌklʌɪˈmatɪk/ /peɪlɪəʊˌklʌɪˈmatɪk/ adjective ... Comparable Pliocene palaeoclimatic fluctuations can also be seen in Southern Ocean silicoplankton records and marine isotopic records, and in seismic reconstructions of Antarctic glacial stratigraphy. It may also prove possible in individual cases to quantitatively calibrate the trace elements for palaeoclimatic variables such as rainfall. Periods of loess deposition are found to correlate with glacial periods when loess profiles are compared to palaeoclimatic evidence from deep-sea cores. palaeoclimatologist noun ... Consequently, the field is becoming much more interesting and dynamic, with collaborations bringing together, for example, paleontologists, ecologists, paleoclimatologists, and geologists. It is well-known amongst paleoclimatologists that there are no successful CO2 measurements from Greenland, the record shown is obviously from Antarctica. Much more work will have to be done by ocean modellers and palaeoclimatologists before the factors behind the variability are understood. palaeoclimatology noun ... Rather, many arbitrarily isolated ‘disciplines ‘- geology, micro-biology, paleoclimatology, atmospheric chemistry and geochemistry - are intrinsic to knowledge of life's history.’ Transfer functions are frequently employed in Quaternary palaeoclimatology because they provide an important method of reconstructing past climatic conditions. The technique allows estimation of growth rate of speleothems at any interval of interest, which is one of several possible uses in palaeoclimatology.
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