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VERSION:2.0
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BEGIN:VEVENT
DTSTAMP:20260605T072328Z
UID:7b2e0a95-66df-4187-a9de-649c0b1bd160
DTSTART;TZID=Canada/Eastern:20101019T143000
DTEND;TZID=Canada/Eastern:20101019T153000
DESCRIPTION:<html><ul><li>This event was exported from <a href="https://exp
 lora.alliancecan.ca/" target="_blank" rel="noopener"><strong>Explora</stro
 ng></a></li><li>The content provider for this event is: <a href="https://e
 xplora.alliancecan.ca/content_providers/sharcnet" target="_blank" rel="noo
 pener">SHARCNET</a></li><li><strong>Registration may be required for the e
 vent</strong>\, please visit the following URL to learn more: <a href="htt
 p://www.sharcnet.ca/my/accessgrid/" target="_blank" rel="noopener">http://
 www.sharcnet.ca/my/accessgrid/</a></li></ul><hr><p>Speaker: Dr. Francis Zw
 iers\, Director\, Pacific Climate Impacts Consortium</p><hr><p>Abstract: T
 here is now a well established approach to detecting and <br>attributing t
 he causes of observed changes in mean climatic conditions <br>that has bee
 n applied progressively from global scales to regional <br>scales to tempe
 rature and other climate variables. While this research <br>has provided a
  great deal of useful information about the causes of <br>climate change o
 bserved during the past century or more\, policy makers <br>and others hav
 e also been demanding answers about whether there are <br>attributable cha
 nges in frequency and/or intensity of extreme weather <br>and climate even
 ts. The statistical techniques required to respond to <br>these questions 
 are only now begin developed. This talk will describe a <br>standard techn
 ique that is used in climate change detection and <br>attribution research
 \, propose a parallel approach that might be used to <br>assess whether th
 ere is a detectable human influence in the far tails of <br>the distributi
 on of a climate variable such as daily maximum air <br>temperature\, demon
 strate an initial application of the approach\, and <br>discuss limitation
 s and further areas of improvements. Using the <br>approach that is propos
 ed\, we show that an anthropogenic influence is <br>detectable globally\, 
 and in many regions\, in the extremes of daily <br>maximum and minimum tem
 peratures. Globally\, waiting times for extreme <br>annual minimum daily m
 inimum and daily maximum temperatures events that <br>were expected to rec
 ur once every 20 years in the 1960s are now <br>estimated to exceed 35 and
  30 years respectively. . In contrast\, waiting <br>times for circa 1960s 
 20-year extremes of annual maximum daily minimum <br>and daily maximum tem
 peratures are estimated to have decreased to less <br>than 10 and 15 years
  respectively.</p></html>
SUMMARY:Coast-to-Coast Seminar: Anthropogenic Influence on Long Return Peri
 od Daily Temperature  Extremes at Regional Scales
URL;VALUE=URI:http://www.sharcnet.ca/my/accessgrid/
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