BEGIN:VCALENDAR
VERSION:2.0
PRODID:icalendar-ruby
CALSCALE:GREGORIAN
BEGIN:VTIMEZONE
TZID:America/Chicago
BEGIN:DAYLIGHT
DTSTART:20240310T030000
TZOFFSETFROM:-0600
TZOFFSETTO:-0500
RRULE:FREQ=YEARLY;BYDAY=2SU;BYMONTH=3
TZNAME:CDT
END:DAYLIGHT
BEGIN:STANDARD
DTSTART:20231105T010000
TZOFFSETFROM:-0500
TZOFFSETTO:-0600
RRULE:FREQ=YEARLY;BYDAY=1SU;BYMONTH=11
TZNAME:CST
END:STANDARD
END:VTIMEZONE
BEGIN:VEVENT
DTSTAMP;TZID=America/Chicago:20260521T023417
UID:189458@calendar.wisc.edu
DTSTART;TZID=America/Chicago:20231120T153000
DTEND;TZID=America/Chicago:20231120T170000
DESCRIPTION:Upwelling in the Tropical Pacific -- How Does the Cold Tongue S
 tay Cold?. We examine water mass transformation (WMT) in the cold tongue r
 egion from a global high resolution ocean simulation with saved budget ter
 ms and from a regional ocean state estimate.This analysis demonstrates the
  enhancement of diabatic processes during cold events\, which in turn enha
 nces surface cooling in the cold tongue region.\n\nCONTACT: 890-1652\, com
 munications@aos.wisc.edu\n\nONLINE: https://go.wisc.edu/uwaos-youtube
LOCATION:811 AOSS\, Atmospheric\, Oceanic and Space Sciences Building  (Als
 o offered online)
SUMMARY:AOS Colloquium Series - Anna-Lena Deppenmeier
END:VEVENT
END:VCALENDAR

