Award Abstract # 0646401
Including Atmospheric Turbulence in Numerical Weather Prediction, Data Assimilation, Ensemble Forecasts, and Error Evaluation

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: THE REGENTS OF THE UNIVERSITY OF COLORADO
Initial Amendment Date: October 20, 2006
Latest Amendment Date: January 11, 2011
Award Number: 0646401
Award Instrument: Continuing Grant
Program Manager: Eric DeWeaver
edeweave@nsf.gov
 (703)292-8527
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: March 1, 2007
End Date: February 28, 2013 (Estimated)
Total Intended Award Amount: $457,420.00
Total Awarded Amount to Date: $457,420.00
Funds Obligated to Date: FY 2007 = $85,024.00
FY 2008 = $93,569.00

FY 2009 = $90,199.00

FY 2010 = $92,912.00

FY 2011 = $95,716.00
History of Investigator:
  • Rod Frehlich (Principal Investigator)
    rgf@cires.colorado.edu
Recipient Sponsored Research Office: University of Colorado at Boulder
3100 MARINE ST
Boulder
CO  US  80309-0001
(303)492-6221
Sponsor Congressional District: 02
Primary Place of Performance: University of Colorado at Boulder
3100 MARINE ST
Boulder
CO  US  80309-0001
Primary Place of Performance
Congressional District:
02
Unique Entity Identifier (UEI): SPVKK1RC2MZ3
Parent UEI:
NSF Program(s): Climate & Large-Scale Dynamics
Primary Program Source: app-0107 
01000809DB NSF RESEARCH & RELATED ACTIVIT

01000910DB NSF RESEARCH & RELATED ACTIVIT

01001011DB NSF RESEARCH & RELATED ACTIVIT

01001112DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, OTHR
Program Element Code(s): 574000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Using an atmospheric observation to initialize a numerical weather forecast requires that the statistics of the observation error be known. Among the sources of error is the "error of representativeness," which arises because an observation of a variable at, say, a single point, is used to initialize that variable throughout a grid cell, and the value of the variable at that point includes a component due to turbulent motions, the properties of which vary over space and time. The PI will apply improved local estimates of observation error to the assimilation of atmospheric data from realistic observing systems under realistic atmospheric conditions. This will lead to full use being made of data from high quality observations, such as from Doppler radar, and it will permit an accurate evaluation of the utility of next-generation observing systems. Accurate estimates of observation error will also be applied to generating realistic ensembles of perturbed initial conditions for ensemble forecasts. Because these applications depend on accurate measurements of turbulent statistics, the PI will investigate the statistical description of turbulence from research aircraft and from radiosonde data.

Broader impacts of this research arise from its application to improving weather forecasts.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Frehlich, R. "Atmospheric Turbulence Component of the Innovation Error Covariance" Quart. J. Royal Meteorol. Soc. , v.134 , 2008 , p.931 10.1002/qj.263
Frehlich, R. "Atmospheric Turbulence Component of the Innovation Error Covariance" Quat. J. Royal Meteor. Soc. , v.134 , 2008 , p.931 10.1002/qj.263
Frehlich, R., and Kelley, N. "Measurements of Wind and Turbulence Profiles with Scanning Doppler Lidar for Wind Energy ApplicationsMeasurements of Wind and Turbulence Profiles with Scanning Doppler Lidar for Wind Energy Applications" IEEE Journal of Selected Topics in Applied Earth Observations and REMOTE SENSING (J-STARS) , v.134 , 2008 , p.42 10.1109/JSTARS.2008.2001758
Frehlich, R., and Kelley, N. "Measurements of Wind and Turbulence Profiles with Scanning Doppler Lidar for Wind Energy ApplicationsMeasurements of Wind and Turbulence Profiles with Scanning Doppler Lidar for Wind Energy Applications" IEEE Journal of Selected Topics in Applied Earth Observations and REMOTE SENSING (J-STARS) , v.134 , 2008 , p.42 10.1109/JSTARS.2008.2001758
Frehlich, R., and R. Sharman "Climatology of Velocity and Temperature Turbulence Statistics Determined from Rawinsonde and ACARS/AMDAR Data" J. Applied Meteorol. Climatology , v.49 , 2010 , p.1149 10.1175/2010JAMC2196.1
Frehlich, R., and R. Sharman "The Use of Structure Functions and Spectra from Numerical Model Output to Determine Effective Model ResolutionNumerical Model Output to Determine Effective Model Resolution" Monthly Weather Review , v.136 , 2008 , p.1537 10.1175/2007MWR2250.1
R. G. Frehlich and R. D. Sharman "Equivalence of velocity statistics at constant pressure or constant altitude" Geophys. Res. Lett. , v.37 , 2010 , p.L08801 10.1029/2010GL04912

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