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  • ... Compared to modern conditions, the western Arabian Sea had more intense upwelling characterized by maximum frequency of G. bulloides and lowest SST (22C) during mid-Termination I and more tropical conditions and higher SST (26C) near the base
  • current, but perhaps even more so by local air-sea interaction. Zonal atmospheric wind stress variations strongly affect the meridional SST anomaly gradients in the Central North Pacific-even more so than the meridional SST anomaly gradients in the Central
  • North Pacific-, even more so than the SST anomalies.
  • Early analyses have not been used frequently in attempts to find changes in the trace composition of the atmosphere. In the case of rainfall analyses records stretch back more than 100 years at some sites, and a long record at Rothamsted in England
  • (as their patterns are). To verify the thesis paleogeographic reconstructions of the eras more ancient than the Phanerozoic needed.