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UID:2e59320ba482ec7c47588885ec53ebb2
CATEGORIES:Polar Online Events
CREATED:20210304T085056
SUMMARY:ASLO Aquatic Sciences 2021 Limnological Processes Beneath Ice Cover Session
LOCATION:Online
DESCRIPTION:We would like to call your attention to a session at the ASLO Aquatic Scien
 ces 2021 Virtual Meeting (https://www.aslo.org/2021-virtual-meeting/) (22-2
 7 June 2021) that will bring together presentations on aquatic physical, ch
 emical, and biological processes beneath ice covers (details below). Please
  consider <a href="https://www.aslo.org/2021-virtual-meeting/abstract-submi
 ssion-overview/" target="_blank" rel="noopener">submitting an abstract</a> 
 to our session before the 12 March 2021 deadline, and share widely with col
 leagues who might be interested. \n\nWe look forward to seeing your abstrac
 ts!\nTrista Vick-Majors, Michigan Technological University ()\nAlexander Mi
 chaud, Bigelow Laboratory for Ocean Sciences (<a href="https://www.aslo.org
 /2021-virtual-meeting/session-list/%E2%80%9Dmailto:amichaud@bigelow.org%E2%
 80%9D">This email address is being protected from spambots. You need JavaSc
 ript enabled to view it.
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		</a>)\nJohn Priscu, Montana State University ()\n\nSession SS4
 9: Limnological Processes Beneath Ice Cover\nIce cover is fundamental to th
 e seasonal cycles of inland waters and is a permanent feature of many high-
 latitude aquatic environments. The presence of ice limits light penetration
 , influences water column mixing and diminishes atmospheric ventilation. Th
 ese influences produce a cascade of effects on water column and sediment ph
 ysiological and biogeochemical processes.  For example, long term datasets 
 collected from ice covered lakes in the polar regions have revealed unique 
 physiological adaptations to permanent ice cover, and investigations of tem
 perate systems during the ice covered season have highlighted the importanc
 e of under ice processes in the regeneration of nutrients. Experimental dat
 a show that autotrophic and heterotrophic organisms respond at the individu
 al and community level to the formation of ice-cover. Rising global tempera
 tures are decreasing ice cover duration and altering ice thickness, which c
 learly have implications for freshwater biogeochemistry. This session aims 
 to further our understanding of limnological processes under lake ice and h
 ighlight the consequences of changing ice covers for limnological processes
  across local, regional and global scales. We welcome submissions focused o
 n any aspect of limnology including physical, biological, and chemical proc
 esses under ice cover and during open water – ice cover transitions, especi
 ally those that aim to link biogeophysical processes.\n
X-ALT-DESC;FMTTYPE=text/html:<p>We would like <span id="m_4736126527235471986gmail-m_2874539392010911413
 gmail-docs-internal-guid-2c5d7d3b-7fff-b790-bce7-c139c7e9c325">to call your
  attention to a <strong>session at the <a href="https://www.aslo.org/2021-v
 irtual-meeting/" target="_blank" rel="noopener">ASLO Aquatic Sciences 2021 
 Virtual Meeting</a> (22-27 June 2021)</strong> that will bring together pre
 sentations on aquatic physical, chemical, and biological processes beneath 
 ice covers (details below). Please consider <strong><a href="https://www.as
 lo.org/2021-virtual-meeting/abstract-submission-overview/" target="_blank" 
 rel="noopener">submitting an abstract</a> to our session before the 12 Marc
 h 2021</strong> deadline, and share widely with colleagues who might be int
 erested. <br /><br />We look forward to seeing your abstracts!<br />Trista 
 Vick-Majors, Michigan Technological University (<a href="https://www.aslo.o
 rg/2021-virtual-meeting/session-list/”mailto:tjvickma@mtu.edu”"><span id="c
 loak8f012e9fc94421bed7bfa328d85a8878">This email address is being protected
  from spambots. You need JavaScript enabled to view it.</span><script type=
 'text/javascript'>
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 ander Michaud, Bigelow Laboratory for Ocean Sciences (<a href="https://www.
 aslo.org/2021-virtual-meeting/session-list/”mailto:amichaud@bigelow.org”"><
 span id="cloak1680aa12c4d04e0c87b8bea828389ceb">This email address is being
  protected from spambots. You need JavaScript enabled to view it.</span><sc
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		</script></a>)<br />John Priscu, Montana State Univer
 sity (<a href="https://www.aslo.org/2021-virtual-meeting/session-list/”mail
 to:jpriscu@montana.edu”"><span id="cloak8279d9299b1c8e168c6b07f9b3621138">T
 his email address is being protected from spambots. You need JavaScript ena
 bled to view it.</span><script type='text/javascript'>
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		</script></a>)<br /><br /><strong>Sessi
 on SS49: Limnological Processes Beneath Ice Cover</strong><br />Ice cover i
 s fundamental to the seasonal cycles of inland waters and is a permanent fe
 ature of many high-latitude aquatic environments. The presence of ice limit
 s light penetration, influences water column mixing and diminishes atmosphe
 ric ventilation. These influences produce a cascade of effects on water col
 umn and sediment physiological and biogeochemical processes.&nbsp; For exam
 ple, long term datasets collected from ice covered lakes in the polar regio
 ns have revealed unique physiological adaptations to permanent ice cover, a
 nd investigations of temperate systems during the ice covered season have h
 ighlighted the importance of under ice processes in the regeneration of nut
 rients. Experimental data show that autotrophic and heterotrophic organisms
  respond at the individual and community level to the formation of ice-cove
 r. Rising global temperatures are decreasing ice cover duration and alterin
 g ice thickness, which clearly have implications for freshwater biogeochemi
 stry. This session aims to further our understanding of limnological proces
 ses under lake ice and highlight the consequences of changing ice covers fo
 r limnological processes across local, regional and global scales. We welco
 me submissions focused on any aspect of limnology including physical, biolo
 gical, and chemical processes under ice cover and during open water – ice c
 over transitions, especially those that aim to link biogeophysical processe
 s.</span><span style="color: #000000; font-family: arial, sans-serif;"></sp
 an></p>
DTSTAMP:20260615T130238Z
DTSTART;TZID=UTC;VALUE=DATE:20210622
DTEND;TZID=UTC;VALUE=DATE:20210628
SEQUENCE:0
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