 Mount Kilimanjaro taken from an altitude of 11000 m and a distance of 40 km from a north-east direction, on 16 August, 2009. Even though the “season of long rains” has just ended, there is almost no ice on the summit. Photo: Martin Stendel
This project aims to use a high resolution version of HIRHAM5 to assess the mesoscale atmospheric features, in particular the moisture dynamics, of the Mt. Kilimanjaro region atmospheric dynamics under present-day and future climatic conditions. As a consequence, we may be able to relate these variables to the retreat of glaciers from the summit of Mount Kilimanjaro and the consequences for e.g. agriculture further downhill.
The study will cover the complete annual cycle for HIRHAM simulations in two resolutions, other models and two sets of reanalyses, and it is enhanced by automatic weather stations which have been installed at three different levels on the western flank of the mountain. This will add new observational data, since up to recently, there was only an automatic station at the crater located at the top of the mountain.
Such an assessment is particularly interesting because Mt. Kilimanjaro has long been regarded as an “icon of climate change” - even though we know that the glaciers are in fact not disappearing because it is too warm.
A groundwater vulnerability index for South Africa
The DKC is also involved in another African project, which is funded by the World Bank on behalf of the Southern African Development Community (SADC), which consists of 15 countries in southern and eastern Africa (Angola, Botswana, Democratic Republic of Congo, Lesotho, Madagascar, Malawi, Mauritius, Mozambique, Namibia,Seychelles, South Africa, Swaziland, Tanzania, Zambia and Zimbabwe).

The aim of this project is to construct a groundwater vulnerability index for the entire SADC region. Naturally, such an index consists of a multitude of layers, both non-meteorological, such as population density, groundwater aquifer productivity or distance to the next surface water, and meteorological.
DKC stands for the latter part, and an index has been developed which allows us to calculate the meteorological groundwater vulnerability, based on average annual precipitation and its variability as well as length and intensity of drought periods.

Meteorological groundwater vulnerability for the SADC region based on average precipitation and its variability and an analysis of drought periods of different severeness. The index allows to assess for present-day vulnerability (shown above) as well as (from climate model data) future changes in vulnerability
Contacts
Project coordinator Zambia project, Wilhelm May wm@dmi.dk phone: (+45) 39157 462
Project coordinator Tanzania and SADC projects, Martin Stendel mas@dmi.dk Phone: (+45) 39157 446
Edited by Tue Tobias Kosack, ttk@dmi.dk © DMI, 28 June 2011 |