• Doctorat en géographie, Université d'Ottawa
• Maîtrise en géographie, Université d'Ottawa

• Glaciologie
• cryosphère
• hydrologie des bassins englacés et enneigés
• géomorphologie
• Géomatique

Assani AA, Landry R, Kinnard C, Azouaoui O, Demers C, Lacasse K. (2016). Comparison of the Spatiotemporal Variability of Temperature, Precipitation, and Maximum Daily Spring Flows in Two Watersheds in Quebec Characterized by Different Land Use. Advances in Meteorology. Article ID 238029: 1-8. 

Monnier S, Kinnard C. (2015). Reconsidering the glacier to rock glacier transformation problem: new insights from the Central Andes of Chile. Geomorphology. 238: 47-55. doi:10.1016/j.geomorph.2015.02.025. [Kinnard contributed to analyses, discussion and writing (total 50%)]

Sylvain JM, Assani A, Landry R, Quessy JF, Kinnard C. (2015). Comparison of the spatio-temporal variability of annual minimum daily extreme flow characteristics as a function of land use and dam management mode in Quebec, Canada. Water. 7(3): 1232-1245. 

Petlicki M, Cieply M, Janiak JA, Prominska A, Kinnard C. (2015). Calving of tidewater glacier driven by melting at the waterline. Journal of Glaciology. 61(229): 851-863. doi:10.3189/2015JoG15J062. 

Guerfi N, Assani A, Mesfioui M, Kinnard C. (2015). Comparison of the temporal variability of winter daily extreme temperatures and precipitations in southern Quebec (Canada) using the Lombard and Copula methods. International Journal of Climatology. 35(14): 4237-4246. doi: 10.1002/joc.4282. 

Monnier S, Kinnard C. (2015). Geomorphology, internal structure, and successive development of a glacier foreland in the semiarid Chilean Andes (Cerro Tapado, upper Elqui Valley, 30°08′ S., 69°55′ W.) — Reply to Discussion by D.C. Nobes. Geomorphology. 450: 461-463. doi:10.1016/j.geomorph.2015.02.010. 

Monnier S, Kinnard C. (2015). Internal Structure and Composition of a Rock Glacier in the Dry Andes, Inferred from Ground-penetrating Radar Data and its Artefacts. Permafrost and Periglacial Processes. 26(4): 335-346. doi: 10.1002/ppp.1846.