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040 |aCaOODSP|beng|erda|cCaOODSP
043 |an-cn-ns
0861 |aM183-2/8760E-PDF
1001 |aTaylor, R. B., |eauthor.
24510|aHigh water levels in Big Lake, caused by Hurricane Dorian (Sept. 7, 2019) and changes to Long Beach, Nova Scotia / |cR.B. Taylor, P. Fraser, V. Kostylev, D.P. Potter, D.L. Forbes, D. Whalen, A. Robertson, and V. Leys.
264 1|a[Ottawa] : |bNatural Resources Canada = Ressources naturelles Canada, |c2021.
264 4|c©2021
300 |a1 online resource (ii, 31 pages) : |billustrations (chiefly colour), colour maps.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aGeological Survey of Canada open file, |x2816-7155 ; |v8760
500 |aISSN of series supplied from ISSN Portal.
504 |aIncludes bibliographical references (pages 28-30).
5203 |a"Hurricane Dorian in September 2019 provided the first opportunity, since the present tidal channel opened through Long Beach in March 2019, to observe the impacts of storm generated waves and water level fluctuations along the inner shores of Big Lake. In-situ water pressure and CTD recording gauges within Big Lake provided new insights into changes in hydrology that are occurring. The accelerated deterioration of Long Beach in 2018 and 2019 and its response to the presence of an inlet marks a new phase in its evolution, which may have begun 20 years ago and possibly marks the renewal of a phase of barrier instability that prevailed before 1945. …"--Abstract, page i.
650 0|aCoast changes|zNova Scotia.
650 0|aBeaches|zNova Scotia.
650 0|aWater levels|zNova Scotia.
650 0|aHurricanes|zNova Scotia.
650 0|aHurricane Dorian, 2019.
650 6|aLittoral|xModifications|zNouvelle-Écosse.
650 6|aPlages|zNouvelle-Écosse.
650 6|aNiveau des eaux|zNouvelle-Écosse.
650 6|aOuragans|zNouvelle-Écosse.
650 6|aOuragan Dorian, 2019.
7102 |aGeological Survey of Canada, |eissuing body.
830#0|aOpen file (Geological Survey of Canada)|v8760.|w(CaOODSP)9.506878
85640|qPDF|s29.30 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m183-2/M183-2-8760-eng.pdf
8564 |qHTML|sN/A|uhttps://doi.org/10.4095/327835