The Big Climb

Good friend Simon Mtuy just returned from the mountain, following an effort to raise awareness of the need to fight the COVID-19 pandemic together. The Big Climb is raising funds to better track and understand the virus, equip health care workers, and to purchase vaccines for equitable distribution on the understanding that ‘no one is safe until everyone is safe’.

Simon is the perfect person to guide this talented, diverse group of 34 climbers up the mountain - including both young leaders, and accomplished all-star leaders. Who else but Simon could assemble such a group and compliment it with amazing ultrarunners Francesca Canepa, Maude Mathys, and Mira Rai* - wow! Also supporting the effort were the good folks at Marangu Hotel, with whom we have worked for nearly 20 years.

Check the impressive list of partners, and read more about everyone involved here!

  *Learn more about Mira here (US) or here (UK, EU?)

Caldera glimpse with decreased snowcover

Our most-recent fieldwork at Kilimanjaro summit was in February 2020, as the global pandemic began. Since then the mountain has been unusually quiet, with many guides and porters unemployed. They are as anxious as we are to get back up the mountain! Although satellite imagery allows us to assess some changes on the mountain, it is no substitute for on-site measurements and observations. Our reliable instrumentation on the Northern Icefield was functioning 18 months ago, yet the current status is unknown.

The image above was acquired by ESA's Sentinel-2 two days ago, revealing perhaps the least snowcover in several years. Such a view is especially valuable, as distinguishing between snow and ice on imagery is difficult. Clouds of course also complicate interpretation, and in this case case there are scattered clouds visible over the Northern Icefield's northern remnant, within the Breach on the west side, and over low-elevation portions of the southern glacier remnants. On visible portions of the south side, residual snow is estimated to comprise roughly half of the bright patches (i.e., non-glacier).

Noteworthy changes apparent in this image include on-going shrinkage of the Furtwängler Glacier (see above). The extent of south-side glaciers has clearly decreased, even acknowledging residual snowcover. At the Northern Icefield, the east end appears to have experienced the greatest change, due generally-thinner ice and a less-linear margin. In addition, several locations suggest that areas of anomalous geothermal heat are involved with ice loss, an ablation mechanism we have documented elsewhere at the summit. Further information on these new features will hopefully be forthcoming soon from Tanzanian collaborators.

Late April snowcover

Satellite imagery of Kilimanjaro from the European Space Agency's Sentinel-2 is available every five days. Yesterday's nearly cloud-free image (28 April, above) and that from 23 April nicely bracket the time period when Tropical Cyclone JOBO approached the coast of Tanzania. On the 23rd, thick clouds obscured the mountain - except for the crater and a pie-shaped slice to the west, which are nicely visible.

Comparing these two images suggests essentially no snow accumulation on the mountain during the 5-day interval. The pattern of snowcover yesterday resembles that on the mountain since mid-January. Depth appears to have been thin at times when the snow-covered area was greater (i.e., following snowfall events). In general however, there currently appears to be less-than-average snowcover on the mountain, with another month remaining in the long-rains wet season (March-May).

It will be interesting to learn where the highest precipitation totals were recorded during JOBO.

For reference on the image above, Kibo Hut on the Marangu Route is visible within the orange circle (above), while the yellow ellipse highlights Barafu Camp. Trails leading toward the crater rim are faintly visible in both cases.