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TitleAnalyse des changements de régimes dans les séries temporelles issues de la dendrochronologie
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LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorPerreault, L; Nicault, A; Boucher, É; Arseneault, D; Gennaretti, F
SourceUtilisation des archives naturelles pour la reconstitution du passé hydro-climatique; by Bégin, C; Nicault, A; Bégin, Y; Geological Survey of Canada, Open File 8768, 2021 p. 130-142, https://doi.org/10.4095/328084 Open Access logo Open Access
Year2021
PublisherNatural Resources Canada
Documentopen file
Lang.French
Mediaon-line; digital
RelatedThis publication is contained in Utilisation des archives naturelles pour la reconstitution du passé hydro-climatique
File formatpdf
ProvinceQuebec; Newfoundland and Labrador
NTS12M; 13D; 13E; 13L; 13M; 22M; 22N; 22O; 22P; 23; 32M; 32N; 32O; 32P; 33
AreaComplexe La Grande; Rivière Caniapiscau; Churchill Falls; Labrador
Lat/Long WENS -79.5000 -62.0000 55.0000 51.0000
Subjectsenvironmental geology; hydrogeology; Nature and Environment; Science and Technology; climatology; paleoclimatology; hydrologic environment; dendrochronology; modelling; models; meteorology; temperature; precipitation; watersheds; statistical methods; sampling methods; Le projet ARCHIVES; Picea mariana; Methodology; Climate change; Hydrology; Boreal ecosystems; Forests; Trees; Biology; Artificial intelligence; Phanerozoic; Cenozoic; Quaternary
Illustrationstime series; models; flow diagrams; tables; plots; sketch maps; photographs
ProgramClimate Change Geoscience Extreme Events
Released2021 06 28
AbstractThe problem of switching regimes in hydrological time series led to serious questioning in Québec during the last decades. In fact, when we examine annual inflow and precipitation time series of a number of Québec watersheds, we can identify alternating sequences of high and low values. These variations must be taken into account in the hydrological forecasting process. However, since we only have limited information (no more than five decades of observations), we may examine different natural archives such as trees to study hydroclimatic variability over a longer period. One of the objectives of the ARCHIVES project was therefore to study hydrometeorological regime changes in time series reconstructed using dendrochronology. In this chapter, we address the problem of changepoint analysis in such time series by using finite mixtures of distributions. Mixtures of distributions become natural models to represent datasets in which observations may originate from several distinct statistical populations.
The problem is treated from a Bayesian perspective. Our approach was applied to several time series reconstructed in the ARCHIVES project. These applications allowed us to identify regime changes that are spatially consistent, as well as historical changepoints that correspond to specific events such as abrupt changes in summer temperatures that coincide with strong volcanic eruptions. In this chapter, we describe the approach and illustrate it by analysing time series of summer temperatures and water inflows reconstructed using black spruce (Picea mariana Mill. BSP) tree-rings.
Summary(Plain Language Summary, not published)
The main objective of the ARCHIVES project was to develop a new methodological approach aiming at reconstituting the long-term natural variability of hydro-climatic parameters used in the modeling of water inflows in basins of interest for hydroelectric production in Quebec. At the end of the project, hydropower resource managers and authorities concerned about climate change can benefit from a better understanding of the evolution in time and space of hydro-climatic conditions that will facilitate the development of appropriate hydrological scenarios for this region that is sensitive in many ways to climate change. This document presents a synthesis of the results produced by the multidisciplinary team of this five-year project, which took place over the entire boreal zone of Quebec and part of Labrador. This synthesis is structured in 21 chapters grouped in three distinct parts. The first part is divided into five chapters presenting fundamental concepts and prerequisites for reading the other sections of the document. The second part, which includes seven chapters, presents the treatment and meaning of the indicators used in the project. Finally, the nine chapters of the third part of the document present a retrospective analysis of the hydro-climate over the last centuries, or even millennia depending on the indicators.
GEOSCAN ID328084

 
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