Kilimanjaro Ice Core Stable Isotope, Ion, and Nitrate Data from NOAA/WDC Paleoclimatology

Abstract from
"ftp://ftp.ngdc.noaa.gov/paleo/icecore/trop/kilimanjaro/kilimanjaro.txt"

Six ice cores from Kilimanjaro provide an ~11.7-thousand-year record
of Holocene climate and environmental variability for eastern
equatorial Africa, including three periods of abrupt climate change:
~8.3, ~5.2, and ~4 thousand years ago (ka). The latter is coincident
with the "First Dark Age," the period of the greatest historically
recorded drought in tropical Africa. Variable deposition of F- and Na+
during the African Humid Period suggests rapidly fluctuating lake
levels between ~11.7 and 4 ka. Over the 20th century, the areal extent
of Kilimanjaro's ice fields has decreased ~80%, and if current
climatological conditions persist, the remaining ice fields are likely
to disappear between 2015 and 2020.