[Eoas-seminar] MET Seminar - This Thursday April 13 - Dr. Qiu Yang (Pacific Northwest National Laboratory)

[eoas-seminar at lists.fsu.edu]

Dear all,

Please join us this Thursday April 13 for a Meteorology seminar, given by Dr. Qiu Yang from the Pacific Northwest National Laboratory. Dr. Stansfield will speak about “Impact of Global Warming on U.S. Summertime Mesoscale Convective Systems: A Simple Lagrangian Parcel Model Perspective" (abstract below).

Dr. Yang will be joining us virtually, but we will gather in EOA 1044 to participate in the seminar. If you cannot attend in person due to a medical reason or approved work out of town, please contact Zhaohua Wu  (zwu at fsu.edu) for remote access. Otherwise, we look forward to seeing everyone in 1044! Please join us for refreshments prior to the beginning of the talk at 3:15 PM.

DATE: Thursday April 7
SEMINAR TIME: Refreshments at 3 PM, Talk 3:15 PM - 4:15 PM.
SEMINAR LOCATION: EOA 1044 (Speaker remote)
SPEAKER: Dr. Qiu Yang

TITLE: Impact of Global Warming on U.S. Summertime Mesoscale Convective Systems: A Simple Lagrangian Parcel Model Perspective

ABSTRACT
Mesoscale convective systems (MCSs) are the dominant rainfall producer in the U.S. during the warm season, causing natural disasters and severe weather every year.  Global climate models have large uncertainty in projecting precipitation changes in the future climate. Here we developed a simple Lagrangian parcel model (includes single- and multi-column models) to investigate the impact of global warming on MCS initiation and growth. The single-column parcel model projects a mean precipitation decrease over the central U.S. and an increase to its east, in agreement with the CMIP5 model projection. It also highlights the crucial role of current climate mean state model bias in influencing future mean precipitation projection. As for convective population, the model captures the decreased occurrence frequency of weak to moderate convection and increased frequency of strong convection due to the increased CAPE and CIN, in agreement with convection-permitting regional simulations. The multi-column parcel model captures readily the cold pool-induced upscale growth feature. It simulates smaller mesoscale clusters over the central U.S. under global warming due to gust front slowdown and subsidence strength enhancement. The model should be a useful tool for investigating the impact of global warming on MCS at mid-latitudes and providing useful guidelines to improve GCM simulations.

We look forward to seeing you there!


Cheers,

Zhaohua


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