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SEMINAR:GEOTOPICS:Dr. Ben Kirtman (10/4 3:15pm)
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From: |
Qiong Zhang <qiongzhang87@gmail.com> |
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Subject: |
SEMINAR:GEOTOPICS:Dr. Ben Kirtman (10/4 3:15pm) |
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Date: |
Thu, 30 Sep 2010 11:50:13 -0400 |
##### G E O T O P I C S ##### P r e s e n t s
3:15 PM, Monday,October 4th, 2010 SLAB Seminar Room, S/A 103 Refreshments 3:00 PM
Dr. Ben Kirtman Professor, Co-Author of NAS report RSMAS-MPO
"Resolved Ocean Eddies and Climate Simulations"
The current
literature provides compelling evidence suggesting that anâeddy-resolving (as
opposed to eddy permitted) ocean component model willâ significantly impact the
simulation of the large-scale climate, althoughâ this has not been fully tested
to date in multi-decadal global coupledâclimate simulations. The purpose of
this talk is to document how increasedâocean model resolution impacts the
simulation of the large-scale climate âvariability. The model used for this
study is the NCAR Community ClimateâSystem Model version 3.5 (CCSM3.5) - the
forerunner to CCSM4. Twoâ experiments are reported here. The first experiment
(i.e., control,âreferred to as LRC) is a 155-year present-day climate
simulation of the â0.5Â atmosphere (zonal resolution 0.625Â meridional resolution
0.5Â)â coupled to ocean and sea-ice components with zonal resolution of 1.2Â andâmeridional
resolution varying from 0.27Â at the equator to 0.54Â in theâmid-latitudes. The
second simulation is carried out in two phases with theâ same atmospheric model
coupled to 0.1Â ocean and sea-ice component models.âThe initial condition for
the first phase (referred to as HRC03) is theâsame as the control simulation
except that the ocean state has been âinterpolated to the 0.1Â grid. The second
phase (referred to as HRC06) âbegins at year-102 of HRC03 using the same
resolution and parameters âexcept in this case the polar winds have been
filtered to reduce âcomputational instability. This phase of the experiment
extends toâ year-155. The simulations are compared in terms of how ocean eddies
impactâ the mean and variable climate. Emphasis is placed on the tropical
Pacificâand the North Atlantic Ocean, and specifically how the resolved eddies âimpact
air-sea feedbacks.
Qiong Zhang
Marine Geology and Geophysics Rosenstiel School of Marine and Atmospheric Science University of Miami 4600 Rickenbacker Causeway Miami Fl 33149
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