In past ice ages, the intensity of summer insolation affected the emergence of warm and cold periods and played an important role in triggering abrupt climate changes, a study by climate researchers, ...
In agreement with the Milankovitch orbital forcing hypothesis 1 it is often assumed that glacial–interglacial climate transitions occurred synchronously in the Northern and Southern hemispheres of the ...
In past ice ages, the intensity of summer insolation affected the emergence of warm and cold periods and played an important role in triggering abrupt climate changes, a study by climate researchers, ...
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