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UID:31e15f995b0c8530382110101526690e
CATEGORIES:Polar Online Events
CREATED:20211018T091425
SUMMARY:ARCUS Arctic Research Seminar: Planning and Implementing the Thermal State of Permafrost Monitoring System in Alaska
LOCATION:Online
DESCRIPTION:<p style="text-align: justify;">The Arctic Research Consortium of the U.S. 
 (<a href="https://www.arcus.org/" target="_blank" rel="noopener">ARCUS</a>)
  invites registration for the next <strong>Arctic Research Seminar featurin
 g Vladimir Romanovsky</strong>, a Professor Emeritus in Geophysics at the G
 eophysical Institute and the Department of Geosciences, University of Alask
 a Fairbanks; and head of the Geophysical Institute Permafrost Laboratory. D
 r. Romanovsky’s presentation, titled <strong><em>Planning and Implementing 
 the Thermal State of Permafrost Monitoring System in Alaska</em></strong>, 
 will be held via Zoom on <strong>Thursday, 28 October 2021</strong> at 9:00
  a.m. AKDT (1:00 p.m. EDT).</p><p style="text-align: justify;"><strong>Semi
 nar Abstract:</strong></p><p style="text-align: justify;">The Thermal State
  of Permafrost (TSP) monitoring system was initiated by the United States G
 eological Survey in the 1940s and 1950s as a set of ground temperature obse
 rvations in a number of deep (200 to 1000 m) boreholes. The main reason for
  these measurements originally was the investigation of the geothermal cond
 itions in Alaska. However, in the 1970s and in the beginning of the 1980s, 
 the interpretation of the obtained data showed that a significant warming i
 n the upper part (20 to 50 m) of many boreholes has occurred during the mid
 -20th century.</p><p style="text-align: justify;">About this time, another 
 TSP monitoring system was established in Alaska by the Geophysical Institut
 e at the University of Alaska Fairbanks (UAF). Since then, these two monito
 ring systems are the most active and most productive in terms of TSP data c
 ollecting and interpretation. The goal of this monitoring was to use the re
 cords of permafrost temperature in relatively deep boreholes as an indicato
 r of Climate Change. Later, with further development of the monitoring syst
 ems and with the addition of the number of monitored parameters, the main g
 oal of monitoring started to shift to the use of permafrost and active laye
 r characteristics as an indicator of changes in the entire Arctic System.</
 p><p style="text-align: justify;">In more recent times, the goals of the ST
 P monitoring system in Alaska are evolving into not only to monitor but als
 o to predict the changes in permafrost characteristics and the ground tempe
 rature regime in the near and more distant future and how these changes wil
 l impact climate, arctic hydrology, ecosystems, and infrastructure.</p><p s
 tyle="text-align: justify;">Historically, moving from one task to the next 
 required: 1) additional measured parameters to be added; and 2) increasing 
 temporal (continuous vs. one-time measurements) and spatial (number of obse
 rving stations and their geographical distribution) resolution of observati
 ons and modeling. As a result, the TSP monitoring system in Alaska is getti
 ng more complex, more distributed, more difficult to access, more expensive
 , and more effort and resources are required to support this system.</p><p 
 style="text-align: justify;">During this presentation, some examples of the
  results of this monitoring system obtained at each stage of its developmen
 t will be presented. Dr. Romanovsky will only be discussing the ground-base
 d observation system. The use of remote sensing observations will be mentio
 ned only briefly.</p><p style="text-align: justify;"><strong><em>Registrati
 on is required for this event.</em></strong> Instructions for accessing the
  webinar will be sent to registrants prior to the event.</p><p style="text-
 align: justify;">To register for the event, go to:<br /> <a href="https://w
 ww.arcus.org/research-seminar-series" target="_blank" rel="noopener">ARCUS 
 Arctic Research Seminar Series webpage</a></p>
DTSTAMP:20260417T101904Z
DTSTART;TZID=UTC;VALUE=DATE:20211028
DTEND;TZID=UTC;VALUE=DATE:20211029
SEQUENCE:0
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