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Recent AMDAR (MDCRS/ACARS) Activities at GSD

• New AMDAR-RUC database that helps evaluate AMDAR data quality

• Optimization study that suggests data can be “thinned” under certain circumstances

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AMDAR-RUC Database

• Stores AMDAR data (including MDCRS, TAMDAR, Canadian, other foreign carriers)

• Also stores RHC (20 km grid) 1h forecast values– valid at the hour nearest the ob time– interpolated to the location of the ob

• Also keeps RUC reject reason(s) (if any) for each variable (new)

• Only for the RUC domain (CONUS+)

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Available at http://amdar.noaa.gov/

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http://amdar.noaa.gov/ruc_acars/

Pages with real-time data are restricted:•the interactive time-series

•the plan-view map

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Interactive Time Series:

Right column shows the RUC reject code for any

rejected variable(s)

This aircraft appears to have a temperature problem.

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This column shows the fraction of obs rejected by the RUC, for each variable.

We reject many TAMDAR winds because we don’t accept descent winds currently

Running statistics for the last 7 (or 3) days:

Values in red fail our reject list criteria.

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Plan view showing W-rejects for TAMDAR.

Reject reason indicated.

Overall statistics shown

Interactive map (http://amdar.noaa.gov/ruc_acars/)

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Many statistics can be generated in-house from the database

• Vertical profiles• Time series' for specific fleets

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For instance, this data for August ‘06 for the jet AMDAR fleet shows a positive temperature bias for ascent (red) and en-route

(green) above 800 mb (6500 ft). (Descents shown in blue)

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Here is wind RMS (vector difference with RUC) for ascent (red), en-route (green), and descent (blue) for all AMDAR

jets over the Great Lakes Region (daytime)

Note the higher wind errors for en-route data (mostly Delta MD88’s with

known wind problems, caught

by QC, but included here).

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RUC QC successfully identifies the bad obs, and the remaining statistics (right) are substantially better for en-route obs, and slightly better for ascent and descent obs.

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AMDAR jets over the Great Lakes Region (daytime) shows summer decrease in wind errors (due to decreased wind)

Particularly useful for fleets that are changing rapidly, such as TAMDAR and WVSS-II

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Truth??

• We don’t claim the RUC is truth, but it does provide a common standard with which to compare different data sources.

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AMDAR Optimization Study

• FAA asked GSD to study whether AMDAR data can be “optimized” (I.e., “thinned”) without degrading RUC forecast skill.

• We presented out results at the January AMS meeting:– Moninger, W.R., S.G. Benjamin, D. Devenyi, B.D. Jamison, B.E. Schwartz, T.L.

Smith, and E. Szoke, 2006: AMDAR optimization studies at the Global Systems Division. 10th Symposium on Integrated Observing and Assimilation Systems for Atmosphere, Oceans, and Land Surface (IOAS-AOLS), Atlanta, GA, Amer. Meteor. Soc., CD-ROM, 2.4a.

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The optimal amount of AMDAR data in a particular region depends on the purpose. In our paper, we consider

• National Numerical Weather Prediction (NWP), 0 to 12 h forecasts

• Subjective forecasting, primarily for aviation

• Now, I’ll focus on NWP using the Rapid Update Cycle (RUC)

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RUC AMDAR Observation Sensitivity Experiments (OSE)

• We looked at RUC skill (verified with RAOBS) with– All AMDAR data– No AMDAR data– No TAMDAR data (see paper)– Thinned AMDAR data

• Time period: 22 - 28 April 2005, an active weather period

• Focused on 0 to 12h forecasts, particularly 3h forecasts

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The problem: AMDAR Coverage over the CONUS is highly non-uniform

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…Particularly at lower altitudes

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Our thinning strategy

• Instead of removing individual flights, we thinned data (post-hoc) on a grid

• This is optimal for the RUC, but would be difficult to achieve in practice

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The 320km/2Kft/12h case

Data are thinned on a grid. The RUC ingests 1 data point…

• in each 320km x 320 km x 2000 ft box• every 12 hours• provides a very uniform distribution in

space and time

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The 320km/2Kft/6-3h case

Data are thinned on a grid. The RUC ingests 1 data point…

• in each 320km x 320 km x 2 Kft box (as for the ‘thin4’ case)

• every 6 hours above 20 Kft• every 3 hours below 20 Kft• provides more data below 20 KftThis kept 6.3% of the total AMDAR data.

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A typical day of 320km/2Kft/6-3h data (6.3% of total)

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Verification Region. Results to follow are for the red box

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RUC 3h fcst wind errors (with respect to RAOBs) when no AMDAR data are assimilated (22 - 28 April 2005)

RMS Wind errors

peak at 6.25 m/s at jet-

stream levels,

~ 4 m/s below 700 mb

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RUC 3h fcst wind error decrease when some or all AMDAR are added (22 - 28 April 2005)

- all AMDAR

X - 320km/2kft/3-6h case

O - 320km/2Kft/12h case

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When data are thinned uniformly in this way

• the thinned samples yield positive impacts in terms of overall RMS wind error reduction, with small fractions of the data

• however there are many caveats

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Critical caveats (1)

• It is unlikely such uniform thinning can be achieved in practice.

– the best current avionics can turn flight segments (ascent, descent, en-route) on or off, not individual observations

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Critical caveats (2)

• Particular regions will have insufficient data for useful forecasts of aviation hazards if data are thinned so drastically. Forecasts of these will all suffer– Turbulence– Upper level jet location monitoring– Severe convective storms– Fog– Icing– Low level wind shear

• Many other caveats are detailed in the AMS Conference paper

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However, these results suggest an opportunity for Targeting

• If data can routinely be thinned somewhat• The resources saved should be reused to

target observations to regions of critical need• Targeted observations can be taken with 3h to

6h notice, by aircraft with modern avionics• Targeting can by guided by model-generated

target fields• We have begun to develop such fields, based

on RUC 3 - 6h forecasts