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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.

understand    tanzania    disappear    mt    decade    assessing    local    ecosystems    first    attributed    glacier    kilimandjaro    interpretation    compiled    recession    african    weather    decades    temperature    satellite    limited    1987    palaeo    flow    ice    extreme    75    halved    rwenzoris    thicknesses    responsible    uganda    station    geophysical    panel    retreat    east    dramatic    extents    gps    cover    despite    area    rwenzori    climate    heights    trend    estimate    sampling    glaciers    congo    africa    km    hydrology    mapping    cloud    remote    radar    period    surveying    stretching    combined    dynamics    humidity    retreats    sensitivity    climatic    vicinity    air    at    data    communities    driving    century    suggest    rift    controversial    imagery    correlates    peak    20th    altitude    last    water    evolution    similarly    geochemical    kenya    highest    survey    implications    environmental    penetrating    speke    changing    estimates    1980    sensing    2006    5109    modeling    view    measured    budgets    modern    declined    border    mass    mountain    stanley    form    differential   

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]
 Project website https://cryobound.wordpress.com
 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

Map

 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.

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

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