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RIDEC

Rwenzori Ice Dynamics and Environmental Changes

Total Cost €

0

EC-Contrib. €

0

Partnership

0

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 RIDEC project word cloud

Explore the words cloud of the RIDEC project. It provides you a very rough idea of what is the project "RIDEC" about.

geochemical    area    remote    decades    data    stanley    rwenzori    recent    mt    glacier    ice    glaciers    last    first    kenya    african   

Project "RIDEC" data sheet

The following table provides information about the project.

Coordinator
MUSEE ROYAL DE L'AFRIQUE CENTRALE 

Organization address
address: LEUVENSESTEENWEG 13
city: TERVUREN
postcode: 3080
website: www.africamuseum.be

contact info
title: n.a.
name: n.a.
surname: n.a.
function: n.a.
email: n.a.
telephone: n.a.
fax: n.a.

 Coordinator Country Belgium [BE]
 Total cost 172˙800 €
 EC max contribution 172˙800 € (100%)
 Programme 1. H2020-EU.1.3.2. (Nurturing excellence by means of cross-border and cross-sector mobility)
 Code Call H2020-MSCA-IF-2014
 Funding Scheme /MSCA-IF-EF-CAR
 Starting year 2015
 Duration (year-month-day) from 2015-09-07   to  2018-01-31

 Partnership

Take a look of project's partnership.

# participants  country  role  EC contrib. [€] 
1    MUSEE ROYAL DE L'AFRIQUE CENTRALE BE (TERVUREN) coordinator 172˙800.00

Mappa

 Project objective

At the border between Uganda and the D.R. of Congo, the Rwenzoris form a remote and high-altitude mountain range stretching through the East African Rift System. With heights of 4-5 km, they include Africa's third highest peak (Mt. Stanley, 5109 m) as well as some of the last African glaciers. The combined area of the Rwenzori glaciers declined by more than 75% during the 20th century, and halved between 1987 and 2006. This extreme mass loss may have strong implications for the local hydrology, ecosystems and communities, and recent estimates suggest that the glaciers will disappear in the next decade(s). This trend correlates well with similarly dramatic glacier retreats on Mt Kilimandjaro (Tanzania) and Mt Kenya (Kenya) during the same period, and is attributed to increased air temperature or reduced humidity/cloud cover. Despite recent work on the evolution of glacier extent in the last decades, the measured glacier retreat, as well as the interpretation of the driving climatic factors responsible since the 1980’s, remain controversial and are limited to available data. In order to better understand the dynamics of this recession, we will survey the current state of the two largest Rwenzori glaciers, Stanley and Speke glaciers, using a panel of remote sensing, geophysical and geochemical methods. These include, first, surveying of glacier extents over the last decades using satellite imagery, mapping of the current glacier extent and main features using differential GPS, and assessing the glacier thicknesses using ice-penetrating radar. These three steps will allow for further ice flow modeling. Second, the use of weather station data in the glacier vicinity as well as ice/water sampling for geochemical analysis will allow investigating the glacier sensitivity to the changing climate and its (palaeo-)environmental potential. These results will be compiled with a view to provide a first estimate of modern, past and future ice budgets in the area of interest.

 Work performed, outcomes and results:  advancements report(s) 

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The information about "RIDEC" are provided by the European Opendata Portal: CORDIS opendata.

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