A comparison of precession and obliquity effects in a Cretaceous paleocllmate simulation

Publisher: John Wiley & Sons Inc

E-ISSN: 1944-8007|17|11|1929-1932

ISSN: 0094-8276

Source: GEOPHYSICAL RESEARCH LETTERS, Vol.17, Iss.11, 1990-10, pp. : 1929-1932

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Abstract

A set of 36 perpetual‐season simulations with an atmospheric GCM are used to investigate the effects of precession and obliquity variations on mid‐Cretaceous climate. Climatic variables such as surface temperature, pressure and moisture transport suggest that the mid‐Cretaceous climate system is more sensitive to precession than to obliquity in most regions, even at high latitudes. Obliquity variations affect our simulations primarily by modulating the western extent of the precession‐enhanced continental monsoons. As a result, sensitivity to obliquity can be important at low, as well as high, latitudes.