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2011 - Cooperative Institute for Research in Environmental Sciences ...

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Figure 1: Sea surface height (SSH) simulated by the icosahedral ocean<br />

model OFIM. Grey/purple shades <strong>in</strong>dicate lowest/highest SSH values.<br />

Surface currents tend to follow SSH contours. Dom<strong>in</strong>ant features<br />

are the Antarctic Circumpolar Current, flow<strong>in</strong>g west to east, and the<br />

clockwise-rotat<strong>in</strong>g gyres <strong>in</strong> the South Atlantic and Southern Indian<br />

Ocean. Also shown are the grid cells of the icosahedral grid.<br />

Milestone 2. Progress toward construction of an ESRL Earth<br />

system model by coupl<strong>in</strong>g an icosahedral <strong>for</strong>mulation of<br />

the global Hybrid Coord<strong>in</strong>ate Ocean Model (currently under<br />

development with<strong>in</strong> ESRL) with the global Flow-follow<strong>in</strong>g<br />

f<strong>in</strong>ite-volume Icosahedral atmospheric Model (FIM) on an<br />

identical horizontal grid. Test this coupled model on <strong>in</strong>dividual<br />

cases, and <strong>in</strong> real time if adequate comput<strong>in</strong>g resources<br />

and <strong>in</strong>itial data are available.<br />

Development of the icosahedral ocean circulation model<br />

OFIM (Oceanic Flow-follow<strong>in</strong>g f<strong>in</strong>ite-volume Icosahedral<br />

Model) has reached a po<strong>in</strong>t where, when coupled to its atmospheric<br />

counterpart FIM, it produces acceptable global<br />

ocean state solutions on multiyear time scales. OFIM<br />

mimics FIM <strong>in</strong> us<strong>in</strong>g constant density layers <strong>in</strong> the ocean<br />

<strong>in</strong>terior. Thermohal<strong>in</strong>e coupl<strong>in</strong>g with the atmosphere is<br />

mediated by two nonisopycnic coord<strong>in</strong>ate layers represent<strong>in</strong>g<br />

a turbulent mixed layer. With the two submodels<br />

shar<strong>in</strong>g the same horizontal mesh, <strong>in</strong><strong>for</strong>mation exchange<br />

is straight<strong>for</strong>ward. Emphasis at this po<strong>in</strong>t is on validation<br />

of air-sea fluxes calculated by FIM with an eye on drift<br />

<strong>in</strong> subsurface stratification. Among the ocean processes<br />

affect<strong>in</strong>g global sea surface temperature—gyre-scale<br />

horizontal heat transport, surface mixed layer de- and entra<strong>in</strong>ment<br />

and global meridional overturn<strong>in</strong>g (‘conveyor<br />

belt’)—our present focus is on the mixed layer and its role<br />

<strong>in</strong> properly ma<strong>in</strong>ta<strong>in</strong><strong>in</strong>g the permanent thermocl<strong>in</strong>e. A<br />

milestone not yet reached is simulation of the ENSO (El<br />

N<strong>in</strong>o, La N<strong>in</strong>a) cycle. Soon to be added is a sea ice model<br />

to end the present dependence on observed ice coverage.<br />

GSD-03VerificationTechniques<strong>for</strong>theEvaluation<br />

ofAviationWeatherForecasts<br />

FEDERAL LEAD: JENNIFER MAHONEY<br />

CIRES LEAD: ANDREW LOUGHE<br />

NOAA Goal 3: Weather and Water<br />

Project Goal: Design and evaluate new verification approaches<br />

and tools that will provide <strong>in</strong><strong>for</strong>mation about the quality of<br />

aviation <strong>for</strong>ecasts and their value to aviation decision makers.<br />

Milestone 1. Develop a verification plan <strong>for</strong> assess<strong>in</strong>g the<br />

96 CIRES Annual Report <strong>2011</strong><br />

quality of the Graphical Turbulence Guidance Product<br />

version 3, and the Graphical Turbulence Guidance Product<br />

Nowcast.<br />

Due to changes <strong>in</strong> priorities at the Federal Aviation<br />

Adm<strong>in</strong>istration (FAA), the Graphical Turbulence Guidance<br />

(GTG) Product version 2.5 evaluation has been extended,<br />

while the GTG version 3 and GTG Product Nowcast<br />

evaluations have been pushed back. The GTG version 2.5<br />

product <strong>in</strong>corporated a new observ<strong>in</strong>g plat<strong>for</strong>m (Eddy<br />

Dissipation Rate, EDR). As a result, <strong>in</strong> preparation <strong>for</strong> the<br />

evaluation, it was necessary to study the EDR reports and<br />

develop techniques <strong>for</strong> utiliz<strong>in</strong>g them <strong>in</strong> the evaluation.<br />

These new techniques were then <strong>in</strong>corporated <strong>in</strong>to the evaluation<br />

of the GTG version 2.5 product. That evaluation has<br />

been completed, with the f<strong>in</strong>al presentation and publication<br />

of the official report to occur early <strong>in</strong> the next fiscal year.<br />

Milestone 2. Provide assessment report summariz<strong>in</strong>g the<br />

f<strong>in</strong>d<strong>in</strong>gs from an evaluation of the Current Ic<strong>in</strong>g Potential<br />

and the Forecast Ic<strong>in</strong>g Potential.<br />

A verification plan <strong>for</strong> the Current Ic<strong>in</strong>g Potential (CIP)<br />

and Forecast Ic<strong>in</strong>g Potential (FIP) is underway. The plan<br />

focuses on a comparison of the current CIP and FIP<br />

algorithms run by the Aviation Weather Center (AWC)<br />

with new versions of CIP and FIP us<strong>in</strong>g the new Weather<br />

<strong>Research</strong> and Forecast model (WRF) Rapid Refresh. Additionally,<br />

new techniques are be<strong>in</strong>g developed to utilize<br />

satellite data <strong>for</strong> ic<strong>in</strong>g detection and verification. A report is<br />

<strong>for</strong>thcom<strong>in</strong>g <strong>in</strong> late September <strong>2011</strong>.<br />

Milestone 3. Provide a comprehensive assessment of the<br />

Consolidated Storm Prediction <strong>for</strong> Aviation (CoSPA) <strong>for</strong>ecast<br />

algorithm <strong>in</strong> support of the Federal Aviation Adm<strong>in</strong>istration<br />

FY10 demonstration.<br />

Completed the 2010 assessment of the real-time automated<br />

convective weather <strong>for</strong>ecast product known as CoSPA<br />

and presented it to both the Convective Weather Product<br />

Development Team and to a Technical Review Panel from<br />

the Federal Aviation Adm<strong>in</strong>istration. Two separate reports<br />

were written to support this ef<strong>for</strong>t. In addition, a w<strong>in</strong>ter<br />

2010 assessment of CoSPA was completed, which used<br />

results from the summer 2010 study as a basel<strong>in</strong>e. This was<br />

also presented to FAA management. A written report of the<br />

2010 w<strong>in</strong>ter study will accompany the <strong>2011</strong> CoSPA Assessment.<br />

GSD-05 Numerical Prediction Developmental<br />

Testbed Center (DTC)<br />

FEDERAL LEAD: ZOLTAN TOTH<br />

CIRES LEAD: LIGIA BERNARDET<br />

NOAA Goal 3: Weather and Water<br />

Project Goal: Transition new developments from research to<br />

operations <strong>in</strong> the Gridpo<strong>in</strong>t Statistical Interpolator (GSI) data<br />

assimilation system and the Hurricane Weather <strong>Research</strong> and<br />

Forecast<strong>in</strong>g (HWRF) model<strong>in</strong>g system through the Developmental<br />

Testbed Center (DTC).<br />

Milestone 1. Upgrade the community Hurricane-Weather<br />

<strong>Research</strong> and Forecast<strong>in</strong>g model (HWRF) code to conta<strong>in</strong><br />

new developments used by NOAA’s National Centers <strong>for</strong><br />

<strong>Environmental</strong> Prediction (NCEP) <strong>for</strong> the 2010 operational<br />

hurricane season and run extensive tests to assure that

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