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楼主: estradiol
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Atmospheric, Oceanic and Climatic Response to Greenhouse and Feedback Effecte to the fact that the input to the models has many uncertainties..An important record about climatic changes is available in the geological past, but the evidence should be refined by geologists and used as an input to the forecast of future climatic changes..Deep sea cores provide proxy evidence o
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Ice Sheets and Sea Level Change as a Response to Climatic Change at the Astronomical Time ScaleQuaternary Ice Age..A 2-dimensional physical model taking into account the coupling between the atmosphere, the upper ocean, the sea-ice, the ice-sheets and the continental surfaces has been forced by the long-term variations of the insolation induced by the astronomical changes in the elements of t
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Sea Levelaccelerated by the greenhouse effect. The world’s coastlines are partly in uplift regions, (glacio-isostatic or tectonic), and here sea level is falling. Most regions, however, are subsiding, so that sea level is always rising; these subsiding regions are also the most heavily populated, so that the
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