We are told (Editorial, Science 304, p. 1565, June 11 2004) that
climate change modeling is an inexact science. So, it seems, is map-reading. Mount Kilimanjaro's "photogenic snowcap" is in Tanzania, not
Kenya. The consequences of the imminent loss of the mountain's glaciers (1)
do, however, concern both countries and provide a good example of how
global climate change may be interacting with and affecting local climate
and environmental change. The Pangani River basin, an important source of
water to both people and wildlife in Tanzania and Kenya, is fed by the
snows of Kilimanjaro. Its flows have been much reduced over the last four
decades by decreasing precipitation in the mountain area (including
decreasing snowfall on the glacier) and increased demand from irrigation
and hydropower schemes (2). Glacier meltwater also recharges the main
spring in the famous Amboseli National Park, at the foot of the northern
(Kenyan) slopes of Kilimanjaro (2); its loss would affect wildlife
populations and reduce tourism revenues. Localized daily temperature
increases in the Amboseli area over the last 25 years have been an order
of magnitude higher than the 0.2 to 0.3 degrees C attributable to global climate
change (3), possibly as a consequence of glacial melting and deforestation
on the mountain slopes. Meanwhile, on Mount Kenya (which I can confirm is
definitely in Kenya), the glaciers are also in rapid retreat (4), with
similar implications for the productive agricultural zones around the foot
of the mountain.
Amusing though it may be to catch out the editor of "Science" making
a simple and uncharacteristic error of political geography, the more
serious point is that, given the uncertainties in future climate change,
we have to make sure of the certainties.
1. L. G. Thompson et al., Science 298, 589 (2002).
2. IUCN, The Pangani River Basin. A Situation Analysis (IUCN Eastern
Africa Programme, Nairobi, Kenya, 2003).
3. J. Altmann et al., Afr. J. Ecol. 40, 248 (2002).
4. S. Hastenrath, P.S. Krass, Nature 355, 503 (1992).