[Eoas-seminar] TODAY - Meteorology Seminar

eoas-seminar at lists.fsu.edu eoas-seminar at lists.fsu.edu
Tue Apr 4 08:56:55 EDT 2017


Good Morning,

Today, Tuesday April 4 at 3:30 PM, we will have a special seminar given by Dr. Tim Cronin<http://web.mit.edu/~twcronin/www/> (MIT). Dr. Cronin is an assistant professor in the Department of Earth, Atmospheric and Planetary Sciences at MIT who studies a variety of subjects related to climate, especially idealized modeling of the atmosphere and atmosphere-land system with single-column and limited-area models. He will speak about:

“Arctic temperature profiles and their sensitivity to climate change” (abstract below)

TUESDAY APRIL 4, 3:30 PM, WERNER A. BAUM SEMINAR ROOM, 353 LOVE BUILDING


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Arctic temperature profiles and their sensitivity to climate change
The high-latitude vertical structure of temperature is poorly understood, yet is an important factor in the polar amplification of climate change. To better understand the high-latitude lapse rate and its sensitivity to various forcings, we explore two perspectives on the high-latitude temperature structure.

The first is the Lagrangian perspective of Arctic air formation. We prescribe the initial sounding of the atmosphere representing an air column starting over the ocean, then allow the air mass to evolve for two weeks in the absence of any solar heating, representing the movement of the air column over a high-latitude continent. Using a single-column model, we find that a low-cloud feedback slows cooling of the surface and amplifies continental warming, increasing the continental surface air temperature by roughly two degrees for each degree increase of the initial maritime surface air temperature.

The second is the Eulerian perspective of radiative-advective equilibrium. High latitude temperature profiles are generally stable to convection, with frequent surface-based inversions, especially in winter. Such profiles result from the stabilizing influences of advective heat flux convergence and atmospheric solar absorption, which dominate over the destabilizing influences of surface solar absorption and subsurface heating. We formulate an analytical model that represents the dominant balance between advective heating and radiative cooling, and discuss how climate feedbacks in this state depend on the type of forcing.

Speaker’s website: http://mit.edu/~twcronin/www/




Paige Phillips


Academic Program Specialist - Meteorology  I  Earth, Ocean, & Atmospheric Science (EOAS)  I  Florida State University  I  410 Love Building  I  1017 Academic Way, Tallahassee, Florida 32306  I  (850) 644-8582  I  www.eoas.fsu.edu
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