BeginSiroisMeunier2010
Référence
Begin, Y., Sirois, L., Meunier, C. (2010) The Effects of Hydroelectric Flooding on a Reservoir’s Peripheral Forests and Newly Created Forested Islands. Advances in Global Change Research, 41:241-256. (Scopus 
)
Résumé
While research shows that large water bodies can produce significant micro- and meso-climatic effects, these effects are not well documented. The flooding of large areas transforms terrestrial environments into aquatic environments, with hills becoming islands and the flooded edges dynamic shorelines. In creating these reservoirs, we expose the new shoreline forests to processes and natural hazards pertaining to lacustrine environments. The environmental transformations caused by these processes are generally limited to the immediate edges of the reservoirs. In Russia, Vendrov and Malik (1965), D’yakonov and Reteyum (1965), and Butorin et al. (1973) have shown that the effects of reservoirs in the Volga are limited to their riparian edges. © 2010, Springer Science+Business Media B.V.
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@ARTICLE { BeginSiroisMeunier2010,
AUTHOR = { Begin, Y. and Sirois, L. and Meunier, C. },
TITLE = { The Effects of Hydroelectric Flooding on a Reservoir’s Peripheral Forests and Newly Created Forested Islands },
JOURNAL = { Advances in Global Change Research },
YEAR = { 2010 },
VOLUME = { 41 },
PAGES = { 241-256 },
NOTE = { cited By 1 },
ABSTRACT = { While research shows that large water bodies can produce significant micro- and meso-climatic effects, these effects are not well documented. The flooding of large areas transforms terrestrial environments into aquatic environments, with hills becoming islands and the flooded edges dynamic shorelines. In creating these reservoirs, we expose the new shoreline forests to processes and natural hazards pertaining to lacustrine environments. The environmental transformations caused by these processes are generally limited to the immediate edges of the reservoirs. In Russia, Vendrov and Malik (1965), D’yakonov and Reteyum (1965), and Butorin et al. (1973) have shown that the effects of reservoirs in the Volga are limited to their riparian edges. © 2010, Springer Science+Business Media B.V. },
AFFILIATION = { Centre Eau Terre Environnement, Institut national de la recherche scientifique, Québec, QC G1K 9A9, Canada; Université du Québec à Rimouski, Rimouski, QC G5L 3A1, Canada; Centre d’études nordiques, Pavillon Abitibi-Price, Université Laval, Québec, QC G1V 0A6, Canada },
AUTHOR_KEYWORDS = { Annual Ring; Central Basin; Forest Edge; Growth Form; Resin Canal },
DOCUMENT_TYPE = { Book Chapter },
DOI = { 10.1007/978-90-481-8736-2_23 },
SOURCE = { Scopus },
URL = { https://www.scopus.com/inward/record.uri?eid=2-s2.0-84951798812&doi=10.1007%2f978-90-481-8736-2_23&partnerID=40&md5=ac3b0d74d800c9835ba3133d75836c06 },
}
