| Title | African climate response to orbital and glacial forcing in 140,000-y simulation with implications for early modern human environments |
| Authors | Kutzbach, John E. Guan, Jian He, Feng Cohen, Andrew S. Orland, Ian J. Chen, Guangshan |
| Affiliation | Univ Wisconsin, Ctr Climat Res, Nelson Inst Environm Sci, Madison, WI 53706 USA Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA Univ Wisconsin, Dept Geosci, Madison, WI 53706 USA Univ Wisconsin, Wisconsin Geol & Nat Hist Survey, Madison, WI 53705 USA |
| Keywords | LAKE LISAN LAST VEGETATION SEA VARIABILITY MAXIMUM CIRCULATION SENSITIVITY RESOLUTION CONTEXT |
| Issue Date | 4-Feb-2020 |
| Publisher | PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA |
| Abstract | A climate/vegetation model simulates episodic wetter and drier periods at the 21,000-y precession period in eastern North Africa, the Arabian Peninsula, and the Levant over the past 140,000 y. Large orbitally forced wet/dry extremes occur during interglacial time, similar to 130 to 80 ka, and conditions between these two extremes prevail during glacial time, similar to 70 to 15 ka. Orbital precession causes high seasonality in Northern Hemisphere (NH) insolation at similar to 125, 105, and 83 ka, with stronger and northward extended summer monsoon rains in North Africa and the Arabian Peninsula and increased winter rains in the Mediterranean Basin. The combined effects of these two seasonally distinct rainfall regimes increase vegetation and narrow the width of the Saharan-Arabian desert and semidesert zones. During the opposite phase of the precession cycle (similar to 115, 95, and 73 ka), NH seasonality is low, and decreased summer insolation and increased winter insolation cause monsoon and storm track rains to decrease and the width of the desert zone to increase. During glacial time (similar to 70 to 15 ka), forcing from large ice sheets and lowered greenhouse gas concentrations combine to increase winter Mediterranean storm track precipitation; the southward retreat of the northern limit of summer monsoon rains is relatively small, thereby limiting the expansion of deserts. The lowered greenhouse gas concentrations cause the near-equatorial zone to cool and reduce convection, causing drier climate with reduced forest cover. At most locations and times, the simulations agree with environmental observations. These changing regional patterns of climate/vegetation could have influenced the dispersal of early humans through expansions and contractions of well-watered corridors. |
| URI | http://hdl.handle.net/20.500.11897/585974 |
| ISSN | 0027-8424 |
| DOI | 10.1073/pnas.1917673117 |
| Indexed | SSCI SCI(E) PubMed Scopus |
| Appears in Collections: | 物理学院 |
