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Record #110924:
Variations séculaires du niveau d'eau dans le bassin de la rivière Boniface (Québec nordique): une analyse dendroécologique / Serge Payette, Ann Delwaide.
Title: | Variations séculaires du niveau d'eau dans le bassin de la rivière Boniface (Québec nordique): une analyse dendroécologique / Serge Payette, Ann Delwaide. |
Translated title: | Secular variations of the water level in the basin of the Boniface river (northern Quebec): a dendroecological analysis. |
Author(s): | Payette, Serge. Delwaide, Ann. |
Date: | 1991. |
Language: | French. |
In: | Géographie Physique et Quaternaire. (1991.), Vol. 45(1) (1991) |
Abstract: | Dendrochronological evidence makes it possible to reconstruct water levels since 16th century. Snow precipitation appears to be major factor controlling height of water level. Little Ice Age divided into drier period from end of 16th century to 1720-40 and moister period up to 20th century. |
Notes: | Géographie Physique et Quaternaire. Vol. 45(1) :59-67 (1991). English abstract, p. 59. |
Keywords: | 551.58 -- Climatology. 551.583.3 -- Climatic changes, Quaternary. 556.51/.54 -- Rivers and streams. 634.0.561.24 -- Dendrochronology. E9 -- Glaciology: meteorology and climatology. (*41) -- Canada. (*424.1) -- Quebec, northern. |
SPRI record no.: | 110924 |
LDR 01510naa#a2200000#a#4500 001 SPRI-110924 005 20231205143123.0 007 ta 008 231205s1991####xx#a##|##|###|0||#0|fre#d 035 ## ‡aSPRI-110924 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡afre 100 1# ‡aPayette, Serge. 242 10 ‡aSecular variations of the water level in the basin of the Boniface river (northern Quebec) :‡ba dendroecological analysis.‡yeng 245 10 ‡aVariations séculaires du niveau d'eau dans le bassin de la rivière Boniface (Québec nordique) :‡bune analyse dendroécologique /‡cSerge Payette, Ann Delwaide. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 59-67 :‡bill., diags. 500 ## ‡aGéographie Physique et Quaternaire. Vol. 45(1) :59-67 (1991). 500 ## ‡aEnglish abstract, p. 59. 520 3# ‡aDendrochronological evidence makes it possible to reconstruct water levels since 16th century. Snow precipitation appears to be major factor controlling height of water level. Little Ice Age divided into drier period from end of 16th century to 1720-40 and moister period up to 20th century. 546 ## ‡aIn French. 650 07 ‡a551.58 -- Climatology.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡a556.51/.54 -- Rivers and streams.‡2udc 650 07 ‡a634.0.561.24 -- Dendrochronology.‡2udc 650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local 651 #7 ‡a(*41) -- Canada.‡2udc 651 #7 ‡a(*424.1) -- Quebec, northern.‡2udc 700 1# ‡aDelwaide, Ann. 773 0# ‡7nnas ‡tGéographie Physique et Quaternaire. ‡gVol. 45(1) (1991) ‡wSPRI-18972 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231205