ADIW03
20 May 2024 to 24 May 2024
Predictions of how the Earth’s climate might evolve rely on numerical simulations of the atmosphere coupled to numerical simulations of the ocean. Because these simulations model the entire globe and must be run for decades, if not centuries, they are necessarily run at relatively coarse resolution in order to get results in a reasonable length of time. Consequently, while the models are able to capture the large-scale flows, referred to as the “general circulation”, they cannot resolve small scale processes as occur in naturally evolving layers. Broadly speaking, layers in the atmosphere and ocean are manifest in one of two dynamically distinct forms: primarily vertically stacked layers separated by rapid density variations and primarily horizontal layers separated by strong shear flows. Examples of interfaces separating density layers include atmospheric inversions where the temperature abruptly increases with height a few hundred meters above the ground, and the pycnocline which separates warmer and fresher surface ocean water from colder and more saline water at depth. Horizontal shear flows are manifest as storm fronts in the atmosphere and, in the ocean for example, act to separate the fast moving Gulf Stream from the wider Atlantic Ocean. An extraterrestrial example is the meridionally alternating eastward and westward winds on Jupiter.
The existence of density interfaces and fronts act as a barrier to transport, which can be harmful or beneficial. Atmospheric inversions can trap pollution close to the ground, inhibitng its dispersion until morningtime convection erodes the interface. The stratospheric polar vortex above Antarctica inhibits dispersion of CFCs during the southern spring resulting in the formation of the ozone hole. By contrast, the polar vortex over the Arctic is more rapidly broken up by atmospheric waves created by flow over the underlying mountain ranges. So the ozone hole is not so pronounced in the northern hemisphere. In the ocean, our present climate relies upon the transport of heat and carbon dioxide absorbed at the surface being carried to depth by wintertime convection. A grave concern is that increased glacier melt, particularly in the Labrador Sea, will introduce so much fresh water on the surface as to create a pycnocline with such a strong density contrast that convection cannot penetrate through it, so trapping heat and greenhouse gases near the surface.
Our workshop on Climate Applications of Layering will bring together specialists in theory, numerical modelling, laboratory experiments and observations to address questions including how do layers and interfaces form in various settings, what factors control the strength of the interface between layers, what factors result in the erosion of the interface, and how strong must an interface be to resist being eroded?
Registration Only
The Registration Package includes admission to all seminars, lunches and refreshments on the days that lectures take place (Monday - Friday), wine reception and formal dinner, but does not include other meals or accommodation.
Virtual Registration
Virtual registration is free, and includes virtual admission to all seminars and does not include physical attendance, meals or accommodation.
Formal Dinner Only
Participants on the Registration Package, including organisers and speakers, are automatically included in this event. For all remaining participants who would like to attend, such as programme participants, the above charge will apply.
Unfortunately we do not have any accommodation to offer so all successful applicants will need to source their own accommodation.
Limited funding support for accommodation may be available. To request this, please select the "accommodation package" in your application.
Local hotels and accommodation services:
The Institute accepts no responsibility for these services.
Lunch
Lunch will be served at Churchill College. Attendees will be provided with lunch vouchers for 2 courses and 1 drink. Timings will be confirmed with the timetable.
Evening Meal
Participants are free to make their own arrangements for dinner.
Formal Dinner
The Formal Dinner will be held at Selwyn College on Wednesday 22nd May at 19:30.
Selwyn College was founded in 1882, and boasts beautiful landscaped gardens. The event is a tradition for INI participants and gives you a chance to socialise with your colleagues on a more personal level. It is not one to miss!
Participants on the Registration Package, including organisers and speakers, are automatically included in this event.
The Institute kindly requests that any papers published as a result of this programme’s activities are credited as such. Please acknowledge the support of the Institute in your paper using the following text:
The author(s) would like to thank the Isaac Newton Institute for Mathematical Sciences, Cambridge, for support and hospitality during the programme Climate Applications of Layering, where work on this paper was undertaken. This work was supported by EPSRC grant EP/R014604/1.
Monday 20th May 2024 | |||
---|---|---|---|
09:15 to 09:45 | No Room Required | ||
09:45 to 10:00 |
Milla Kibble Aalborg Universitet |
No Room Required | |
10:00 to 11:00 |
Mara Freilich Brown University |
Room 1 | |
11:00 to 11:30 | No Room Required | ||
11:30 to 12:00 |
Peter Haynes University of Cambridge |
Room 1 | |
12:00 to 12:30 |
Nicole Shibley Princeton University |
Room 1 | |
12:30 to 14:00 | No Room Required | ||
14:00 to 15:00 |
Laura Cope University of Leeds |
Room 1 | |
15:00 to 15:30 |
David Dritschel University of St Andrews |
Room 1 | |
15:30 to 16:00 | No Room Required | ||
16:00 to 17:00 | Room 1 | ||
17:00 to 18:00 | No Room Required |
Tuesday 21st May 2024 | |||
---|---|---|---|
10:00 to 11:00 |
Peter Read University of Oxford |
Room 1 | |
11:00 to 11:30 | No Room Required | ||
11:30 to 12:00 |
Kasturi Shah University of Cambridge |
Room 1 | |
12:00 to 12:30 |
Lois Baker University of Edinburgh |
Room 1 | |
12:30 to 14:00 | No Room Required | ||
14:00 to 15:00 |
Daphné Lemasquerier University of St Andrews |
Room 1 | |
15:00 to 15:30 |
Michael LeBars CNRS (Centre national de la recherche scientifique) |
Room 1 | |
15:30 to 16:00 | No Room Required | ||
16:00 to 16:30 |
Justin Brown Naval Postgraduate School |
Room 1 |
Wednesday 22nd May 2024 | |||
---|---|---|---|
10:00 to 11:00 |
Dick Peltier University of Toronto |
Room 1 | |
11:00 to 11:30 | No Room Required | ||
11:30 to 12:00 |
Stephanie Waterman University of British Columbia |
Room 1 | |
12:00 to 12:30 |
Adrian Barker University of Leeds |
Room 1 | |
12:30 to 14:00 | No Room Required | ||
14:00 to 18:00 | No Room Required | ||
19:30 to 22:00 | No Room Required |
Thursday 23rd May 2024 | |||
---|---|---|---|
10:00 to 11:00 |
Elizabeth Yankovsky New York University |
Room 1 | |
11:00 to 11:30 | No Room Required | ||
11:30 to 12:00 |
Chris Howland Universiteit Twente |
Room 1 | |
12:00 to 12:30 |
Steven Tobias University of Leeds |
Room 1 | |
12:30 to 14:00 | No Room Required | ||
14:00 to 15:00 |
Leif Thomas Stanford University |
Room 1 | |
15:00 to 15:30 |
Claudia Cenedese Woods Hole Oceanographic Institution |
Room 1 | |
15:30 to 16:00 | No Room Required | ||
16:00 to 16:30 |
John Taylor University of Cambridge |
Room 1 |
Friday 24th May 2024 | |||
---|---|---|---|
10:00 to 11:00 |
Alexis Kaminski University of California, Berkeley |
Room 1 | |
11:00 to 11:30 | No Room Required | ||
11:30 to 12:30 | Room 1 | ||
12:30 to 14:00 | No Room Required |
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