Coldspot of decelerated sea-level rise on the Pacific coast of North America

dc.contributor.authorParker, Albert
dc.date.accessioned2016-12-12T12:32:12Z
dc.date.available2016-12-12T12:32:12Z
dc.date.issued2016
dc.description.abstractWe show here the presence of significant “coldspot” of sea level rise along the West Coast of the United States and Canada (including Alaska). The 30-years sea level for the area are mostly falling also at subsiding locations as San Francisco and Seattle where subsidence is responsible for a long term positive rate of rise. The 20 long term tide gauges of the area of length exceeding the 60-years length have a naïve average rate of rise –0.729 mm/year in the update 30- Apr-2015, down from –0.624 mm/year in the update 14-Feb-2014. Therefore, along the West Coast of the United States and Canada the sea levels are on average falling, and becoming more and more negative.pl_PL
dc.identifier.citationQuaestiones Geographicae vol. 35 (3), 2016, pp. 31-37pl_PL
dc.identifier.issn0137-477X
dc.identifier.urihttp://hdl.handle.net/10593/16458
dc.language.isoengpl_PL
dc.publisherWydział Nauk Geograficznych i Geologicznych Uniwersytetu im. Adama Mickiewiczapl_PL
dc.rightsinfo:eu-repo/semantics/openAccesspl_PL
dc.subjectsea levelpl_PL
dc.subjectmeasurementspl_PL
dc.subjecttide gaugespl_PL
dc.subjectWest Coast of North Americapl_PL
dc.titleColdspot of decelerated sea-level rise on the Pacific coast of North Americapl_PL
dc.typeArtykułpl_PL

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