Carbonate dissolution by euendolithe cyanobacterium
Bioerosion is the process of destruction of rocks by living organisms. The bioerosion of biogenic carbonates by so-called "euendolithic" cyanobacteria (which live in rocks) is a major but poorly quantified process, causing, among other things, the disintegration of coral reefs. Euendolitic ...
SISMEAUCLIM
This project is based on three disciplines: seismology, hydrogeology and climatology. It aims to develop a new approach to monitor hydrogeological reservoirs, in particular karst aquifers, subject to extreme climatic events. The objective is to carry out 4D imaging during floods in a watershed ...
Sulfur isotope of sedimentary Barites
Multiple sulfur isotope measurements (d34S, d33S, d36S) of sedimentary barites associated with the Permo-Triassic boundary.
Pollen analysis - Morteau (F-25), Moulin Bournez
Natural site; weat meadow. 126 palynological samples + 2 radiocarbon datings. 33,57 meters length drilling.
Pollen analysis - Plancher-les-Mines (F-70), Peat bog du Rosely
Natural site: peat bog. 64 palynological samples + 6 radiocarbon datings. The results are difficult to interpret due to a possible inversion of a core depth levels.
Continuous regional climate change projection for France
This data-set concerns the regionalization at 12km resolution of the two Radiative Pathways Projection RCP4.5 and RCP8.5 simulated by the CCSM4 Earth System Model. This dynamic downscaling experiment uses the ARW/WRF model version 3.8.1 run in climate mode. The simulation were conducted by the CRC ...
TEOM (Tapered Element Oscillating Microbalance) desert dust measurements in Dédougou (Burkina Faso)
The TEOM (Tapered Element Oscillating Microbalance) instrument was settled in Dedougou (Burkina Faso) in March 2012. It automatically measures the PM10 (particulate matter which diameter is lower than 10µm) mass concentrations at the surface (at 2m) at a 15mn time-step, and day and night. The ...
Hydrology, Climate Change, Adaptation, Water Resource in Burgundy (HYCCARE-Burgundy)
Dynamical climate downscaling is realized using the WRF Regional Climate Model at 48km and 12km resolution respectively for Burgundy region. Climate simulations are used to feed the hydrological model GR4J towards the simulation of water ressource trends for 13 watersheds. Climate simulation ...
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