North African climate cycles

North African climate cycles have a unique history that can be traced back millions of years. The cyclic climate pattern of the Sahara is characterized by significant shifts in the strength of the North African Monsoon. When the North African Monsoon is at its strongest, annual precipitation and consequently vegetation in the Sahara region increase, resulting in conditions commonly referred to as the "green Sahara". For a relatively weak North African Monsoon, the opposite is true, with decreased annual precipitation and less vegetation resulting in a phase of the Sahara climate cycle known as the "desert Sahara".[1]

Variations in the climate of the Sahara region can, at the simplest level, be attributed to the changes in insolation because of slow shifts in Earth's orbital parameters. The parameters include the precession of the equinoxes, obliquity, and eccentricity as put forth by the Milankovitch theory.[2] The precession of the equinoxes is regarded as the most important orbital parameter in the formation of the "green Sahara" and "desert Sahara" cycle.

A January 2019 MIT paper in Science Advances shows a cycle from wet to dry approximately every 20,000 years.[3][4]

  1. ^ Cite error: The named reference Foley1 was invoked but never defined (see the help page).
  2. ^ Cite error: The named reference Larrasoana2 was invoked but never defined (see the help page).
  3. ^ Bryan Lynn (January 6, 2019). "Study: Sahara Changed from Wet to Dry Every 20,000 Years". VOANews.com. Archived from the original on December 27, 2021. Retrieved January 7, 2019.
  4. ^ Skonieczny, C. (2 January 2019). "Monsoon-driven Saharan dust variability over the past 240,000 years". Science Advances. 5 (1): eaav1887. Bibcode:2019SciA....5.1887S. doi:10.1126/sciadv.aav1887. PMC 6314818. PMID 30613782.