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Fast Breaking Comments

By Dr. David Stensrud

ESI Special Topics, April 2002
Citing URL - http://www.esi-topics.com/fbp/comments/april02-DavidStensrud.html

Dr. David Stensrud answers a few questions about this month's fast breaking paper in field of Geosciences.


From •>>April 2002

Field: Geosciences
Article Title: "Using initial condition and model physics perturbations in short-range ensemble simulations of mesoscale convective systems"
Authors: Stensrud, DJ;Bao, JW;Warner, TT
Journal: MON WEATHER REV
Volume: 128
Page: 2077-2107
Year: JUL 2000
* NOAA, Natl Severe Storms Lab, 1313 Halley Circle, Norman, OK 73069 USA.
* NOAA, Natl Severe Storms Lab, Norman, OK 73069 USA.
* Univ Colorado, NOAA, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
* Natl Ctr Atmospher Res, Boulder, CO 80307 USA.

ST:  Why do you think your paper is highly cited?

Ensemble forecasting is an emerging technique for improving short-range (0 to 48 hour) weather forecasts, and understanding the relative importance of initial condition uncertainty versus model physics uncertainty is crucial to determining how best to construct ensembles.

ST:  Does it describe a new discovery or new methodology that's useful to others?

This study illustrates the important and beneficial role that model physics uncertainty can play in short-range ensemble forecasting, particularly with respect to warm season precipitation forecasts.

ST:  Could you summarize the significance of your paper in layman's terms?

Ensembles are groups of weather forecasts, valid over the same time period, that differ in either their initial state of the atmosphere or in their model physics components or both. Since the atmosphere is a chaotic system, meaning that forecasts are sensitive to small uncertainties in any part of the forecast system, it is very doubtful that any single model forecast will be correct in every detail. Thus, ensembles are one approach to predicting the probability of future weather events. This study examines the relative contributions of the uncertainties in our initial picture of the atmosphere and in our modeling systems to ensembles, and concludes that both sources of uncertainty can be used beneficially in an ensemble approach. The uncertainties in the initial picture of the atmosphere are most important to include in ensembles when the atmospheric signal is strong, whereas the uncertainties in the modeling system are most important to include in ensembles when the atmospheric signal is weak.End

Dr. David J. Stensrud, Leader, Models and Assimilation Team,
Research Meteorologist
Forecast Research and Development Division
NOAA/National Severe Storms Laboratory
1313 Halley Circle
Norman, Oklahoma 73069

ESI Special Topics, April 2002
Citing URL - http://www.esi-topics.com/fbp/comments/april02-DavidStensrud.html

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