EGU 2018 session OS1.7/CR6.2 “Changes in the Arctic Ocean, sea ice and subarctic seas systems: Observations, Models and Perspectives"

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EGU 2018 session OS1.7/CR6.2 “Changes in the Arctic Ocean, sea ice and subarctic seas systems: Observations, Models and Perspectives"

Aksenov, Yevgeny

Dear Colleagues,

 

Apology for any cross-posting. We would like to invite you to take part in the EGU General Assembly 2018 session OS1.7/CR6.2 “Changes in the Arctic Ocean, sea ice and subarctic seas systems: Observations, Models and Perspectives”, co-organized between the Ocean and Cryosphere Sciences. The EGU General Assembly 2018 takes place in Vienna, Austria on the 8 - 13 April 2018.

 

Please see the session summary and details below.

 

Please note that the submission deadline for abstracts is the 10 January 13:00 CET.

 

Look forward to see you in Vienna!

 

Kind regards,

 

Yevgeny Aksenov, Agnieszka Beszczynska-Möller, Craig Lee, Benjamin Rabe, Markus Janout , Julienne Stroeve , Paul Dodd (the session conveners)

 

“The past decades of observations have shown sustained changes in the Arctic Ocean and the Arctic sea ice cover. Since the beginning of satellite observations in 1979, the Arctic sea ice extent has declined throughout all seasons, with the largest reduction occurring in summer. Furthermore, the Arctic sea ice cover is now thinner, weaker and drifts faster. The ocean shows an increase in the Arctic freshwater storage and warmer inflows from the Atlantic and Pacific Oceans. Coastal runoff from Siberia and Greenland has also increased. As the global surface temperature rises, the Arctic Ocean is speculated to become seasonally ice-free in the 21st century, which prompts us to revisit our perceptions of the Arctic system as a whole. What could the Arctic look like in the future? How are the present changes in the Arctic going to affect the lower latitudes? What aspects of the changing Arctic should future observations and modeling programs address? The session invites observation- and modeling-based submissions on past, present and future states of the Arctic, on the mutual interaction between ocean, atmosphere and sea ice, and links to global processes. The session addresses Arctic freshwater sources and their effects on regional processes, ocean stratification and ocean acidification. It examines potential Arctic freshwater influences on the global climate, including the Atlantic meridional overturning circulation and greenhouse gases sources from thawing sub-sea permafrost. The session promotes results from current Arctic programs and encourages discussions on future plans for Arctic Ocean modeling and measurement strategies.”

 

Details on the session:

http://meetingorganizer.copernicus.org/EGU2018/session/26747

 

General meeting information:

https://egu2018.eu/home.html

 

Abstract submission:

https://meetingorganizer.copernicus.org/EGU2018/abstractsubmission/26747

 


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EGU 2018 session OS1.7/CR6.2 “Changes in the Arctic Ocean, sea ice and subarctic seas systems: Observations, Models and Perspectives"

Aksenov, Yevgeny

Dear Colleagues,

 

Happy New Year!

 

We would like to invite you to take part in the EGU General Assembly 2018 session OS1.7/CR6.2 “Changes in the Arctic Ocean, sea ice and subarctic seas systems: Observations, Models and Perspectives”, co-organized between the Ocean and Cryosphere Sciences. The EGU General Assembly 2018 takes place in Vienna, Austria on the 8 - 13 April 2018.

 

Please see the session summary and details below.

 

Please note that the submission deadline for the abstracts is coming soon!

 

The deadline is the 10 January 13:00 CET (Wed next week).

 

See you in Vienna!

 

Best regards,

 

Yevgeny Aksenov, Agnieszka Beszczynska-Möller, Craig Lee, Benjamin Rabe, Markus Janout , Julienne Stroeve , Paul Dodd (the session conveners)

 

“The past decades of observations have shown sustained changes in the Arctic Ocean and the Arctic sea ice cover. Since the beginning of satellite observations in 1979, the Arctic sea ice extent has declined throughout all seasons, with the largest reduction occurring in summer. Furthermore, the Arctic sea ice cover is now thinner, weaker and drifts faster. The ocean shows an increase in the Arctic freshwater storage and warmer inflows from the Atlantic and Pacific Oceans. Coastal runoff from Siberia and Greenland has also increased. As the global surface temperature rises, the Arctic Ocean is speculated to become seasonally ice-free in the 21st century, which prompts us to revisit our perceptions of the Arctic system as a whole. What could the Arctic look like in the future? How are the present changes in the Arctic going to affect the lower latitudes? What aspects of the changing Arctic should future observations and modeling programs address? The session invites observation- and modeling-based submissions on past, present and future states of the Arctic, on the mutual interaction between ocean, atmosphere and sea ice, and links to global processes. The session addresses Arctic freshwater sources and their effects on regional processes, ocean stratification and ocean acidification. It examines potential Arctic freshwater influences on the global climate, including the Atlantic meridional overturning circulation and greenhouse gases sources from thawing sub-sea permafrost. The session promotes results from current Arctic programs and encourages discussions on future plans for Arctic Ocean modeling and measurement strategies.”

 

Details on the session:

http://meetingorganizer.copernicus.org/EGU2018/session/26747

 

General meeting information:

https://egu2018.eu/home.html

 

Abstract submission:

https://meetingorganizer.copernicus.org/EGU2018/abstractsubmission/26747

 


This message (and any attachments) is for the recipient only. NERC is subject to the Freedom of Information Act 2000 and the contents of this email and any reply you make may be disclosed by NERC unless it is exempt from release under the Act. Any material supplied to NERC may be stored in an electronic records management system.



This message (and any attachments) is for the recipient only. NERC is subject to the Freedom of Information Act 2000 and the contents of this email and any reply you make may be disclosed by NERC unless it is exempt from release under the Act. Any material supplied to NERC may be stored in an electronic records management system.

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