000	00000nam 2200000zi 4500
001	9.894992
003	CaOODSP
005	20221107173910
006	m     o  d f
007	cr |||||||||||
008	210104t20202020bccd    ob   f000 0 eng d
020	|a9780660370286
040	|aCaOODSP|beng|erda|cCaOODSP
041	|aeng|bfre
043	|an-cn-bc
086	1 |aFs97-4/3026E-PDF
100	1 |aDamborg, J. G., |eauthor.
245	10|aWater temperature, river discharge, and adult Chinook salmon migration observations in the Stamp/Somass watershed, 1986-2012 / |cby Jeremy G. Damborg, Howard W. Stiff, Kim D. Hyatt, Margot M. Stockwell, Gayle Brown and Jeff Till.
264	1|aNanaimo, BC : |bFisheries and Oceans Canada, |c2020.
264	4|c©2020
300	|a1 online resource (v, 96 pages) : |bcharts.
336	|atext|btxt|2rdacontent
337	|acomputer|bc|2rdamedia
338	|aonline resource|bcr|2rdacarrier
490	1 |aCanadian manuscript report of fisheries and aquatic sciences, |x1488-5387 ; |v3026
504	|aIncludes bibliographical references (pages 17-19).
520	|a"The average frequency and duration of continuous “low flow” (<20 cms) periods during Chinook migration dwindled to zero during the 1960s and 1970s, reflecting the benefits of water storage behind the dam constructed at the outlet of Great Central Lake in the 1950s. However, the frequency of daily low flow (<20 cms) and high flow (>80 cms) occurrences have been increasing since the 1980s, indicating increased variability in flows associated with warmer, drier conditions in the 1990s, followed by cooler, wetter conditions in the 2000s"--Abstract.
546	|aIncludes abstract in French.
650	0|aChinook salmon|xMigration|xClimatic factors|zBritish Columbia|zVancouver Island.
650	6|aSaumon quinnat|xMigration|xFacteurs climatiques|zColombie-Britannique|zVancouver, Île de.
710	1 |aCanada. |bDepartment of Fisheries and Oceans, |eissuing body.
830	#0|aCanadian manuscript report of fisheries and aquatic sciences,|x1488-5387 ;|v3026.|w(CaOODSP)9.505211
856	40|qPDF|s7.77 MB|uhttps://publications.gc.ca/collections/collection_2021/mpo-dfo/Fs97-4-3026-eng.pdf