4.3 Article

Is the decline of ice on Kilimanjaro unprecedented in the Holocene?

Journal

HOLOCENE
Volume 20, Issue 7, Pages 1079-1091

Publisher

SAGE PUBLICATIONS LTD
DOI: 10.1177/0959683610369498

Keywords

climate; glaciers; Holocene; hypothesis; Kilimanjaro; Tropics

Funding

  1. Austrian Science Foundation (FWF) [P17415-N10, P20089-N10]
  2. University of Otago, New Zealand
  3. U.S. National Science Foundation
  4. NOAA
  5. Tanzania Meteorological Agency
  6. Tharsis Magnus Hyera
  7. Commission of Science and Technology (COSTECH)
  8. Tanzania and Kilimanjaro National Park Authorities (TANAPA and KINAPA)
  9. Tanzania Wildlife Research Institute (TAWIRI)
  10. Directorate For Geosciences
  11. Div Atmospheric & Geospace Sciences [0952829] Funding Source: National Science Foundation
  12. Austrian Science Fund (FWF) [P17415, P20089] Funding Source: Austrian Science Fund (FWF)

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Glaciers on Kilimanjaro's highest peak, Kibo, are currently regarded as a persistent feature of the Holocene. Here we synthesize all available measurements, observations, and our understanding of current processes on Kibo - gained from intensive research over the past decade - to formulate an alternative hypothesis about the age of these ice fields. This suggests a shorter, discontinuous history of the tabular-shaped glaciers on Kibo's plateau, where typical 'life cycles' of the ice may last only a few hundred years. If life cycles overlap, they are likely the cause of the observed steps in the plateau glaciers. Thus, it is likely that ice has come and gone repeatedly on Kibo's summit plateau, throughout the Holocene. Such a cyclicity is supported by lake-derived proxy records.

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