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AMDAR Quality Assurance

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This aircraft type has generally warm biases that vary with the POF ... Bias vs POF. for Canadian AMDAR ... Here the speed biases vary even more with the POF ... – PowerPoint PPT presentation

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Title: AMDAR Quality Assurance


1

AMDAR Quality Assurance Bradley
Ballish NOAA/NWS/NCEP/NCO/PMB SSMC2/Silver
Spring 23 March, 2009


2
Outline
  • Monthly reports
  • Examples of data quality control (QC) problems
  • Comparison of some aircraft temperatures, wind
    and moisture data in North American area
  • Proposed aircraft temperature bias corrections
    and related issues
  • Summary

3
Regular Monthly AMDAR Reports
  • Based on a WMO meeting at the ECMWF in June 2002,
    NCEP prepares monthly aircraft monitoring reports
    at website
  • http//www.ncep.noaa.gov/pmb/qap/amdar/
  • These standard monthly reports are not frequent
    enough in time, do not have track-checking or
    stuck data summaries and do not have accent and
    descent statistics in most parts
  • The WMO Integrated Global Observing System
    (WIGOS) Pilot Project for AMDAR suggests regional
    centers QC AMDAR data before transmission on the
    GTS
  • This will require much more frequent updates than
    monthly reports

4
Japanese Data in Monthly Reports
  • In the NCEP AMDAR report for February 2009, the
    Japanese data looked good
  • Of 274 Japanese aircraft reporting data, only 7
    had suspect temperatures
  • Units JP9Z4U44, JP9Z4Y4X, JP9Z4Y79, JP9Z4YVV,
    JP9Z5859, JP9Z585Z and JP9Z5Y79 had warm biases
  • No units had suspect winds!
  • There were about 100 minor track-check errors,
    see example on next page

5
Track-Check Error Example
  • Aircraft Data for Unit JP9Z58XZ
  • For 00Z 16 March 2009
  • Time-Days Lat Lon Press
  • 16.07153 27.40 125.00 196.8
  • 16.07639 34.82 140.37 461.7
  • 16.07708 29.53 127.97 196.8
  • 16.11944 34.75 140.28 435.2
  • 16.12083 32.05 132.23 196.8
  • 16.14306 35.27 140.70 558.1
  • 16.14444 35.48 140.78 609.7
  • 16.22917 35.40 139.90 290.1
  • 16.26806 34.32 133.58 300.9
  • 16.28750 33.52 130.43 300.9

Locations and pressures are changing too fast
with time but all data are close to
model background All raw data received at NCEP
have only header KAWN US Air Force not RJTD as
expected Additional examples can be provided
6
Aircraft Monitoring Example
  • On 9 August 2006, aircraft EU3102 started to show
    a large temperature bias from 300 hPa up compared
    to the background
  • The spurious bias was so large that few spurious
    temperatures passed QC
  • The bias was so large that the aircraft was
    probably wasting fuel
  • If the airlines could check a website with this
    information, such problems could be found and
    fixed much sooner

7
(No Transcript)
8
Aircraft Track-check Example
  • On 11 August 2006, aircraft AFZA01 was flying
    from the southeast to northwest with roughly
    several minutes between reports
  • Three groups of reports are shown, with groups 1
    and 3 with correct locations and group 2 with all
    reports about 12 degrees too far north
  • The blue numbers are vector wind differences to
    the guess, with group 3 having large differences
    that all passed QC
  • Flying from the end of group 1 to the start of
    group 2 is an impossible distance in several
    minutes
  • This is a tough example for current QC codes to
    correctly process as group2 can track-check with
    itself
  • This problem with South African aircraft has
    lasted over a year
  • Examples of solo track-check errors are common

9
2
Blue numbers are vector wind differences of
observed winds minus model background
3
1
10
Aircraft Temperature Observation Count
Comparison for NA area
  • An impact test adding TAMDAR and Canadian AMDAR
    data at NCEP did not have positive impact, so
    here we examine this data
  • The next slide compares the average number of
    different types of temperature counts to the
    nearest mandatory pressure level per GDAS model
    run in June 2008 for North America (NA)
  • Counts for Radiosondes, ACARS, TAMDAR and two
    types of Canadian AMDAR are compared
  • Wind observation counts (not shown) were found to
    be nearly identical to temperature counts
  • Clearly the aircraft counts out number those from
    sondes
  • The two main types of Canadian aircraft are
    labeled CRJ and DHC-8

11
Sondes have low counts relative to large ACARS
counts
12
Temperature Bias Comparison
  • The next slide compares the average temperature
    bias of different types of observations to the
    nearest mandatory pressure level per GDAS model
    run in June 2008
  • Biases for sonds, ACARS, TAMDAR and two types of
    Canadian AMDAR are shown
  • Clearly the aircraft temperatures are generally
    warmer than those from sonds (as found for ACARS
    and AMDAR, Ballish and Kumar (BAMS, Nov 2008))
  • The DHC-8 aircraft have the warmest bias

13
Sonds are cold compared to aircraft
14
Temperature Bias vs POF for Canadian AMDAR Data
  • In the following slide, the temperature biases
    for Canadian AMDAR type DHC-8 are shown vs the
    phase of flight (POF)
  • This aircraft type has generally warm biases that
    vary with the POF
  • Here the biases vary considerably with the POF

15
Ascent vs descent is large
16
Speed Bias vs POF for Canadian AMDAR Data
  • In the following slide, the wind speed biases for
    Canadian AMDAR type CRJ are shown vs the POF
  • This aircraft type has speed biases that vary
    considerably with the POF
  • In the second following slide, the same is shown
    for Canadian aircraft type DHC-8
  • Here the speed biases vary even more with the POF
  • At the WIGOS February 2009 meeting, it was noted
    that the CANADIAN AMDAR data are less accurate in
    high latitudes due to using magnetic, rather than
    GPS navigation

17
Ascent vs descent is large
18
Ascent vs descent is very large
19
Relative Humidity Bias Comparison
  • The next two slides show counts of moisture
    observations and relative humidity biases
    differences versus the guess for the North
    American area in June 2008 for sonds, ACARS and
    TAMDAR data
  • The TAMDAR data (at this time) are mainly in the
    mid west, yet have higher counts and very good
    stats versus the guess

20
TAMDAR has large counts, but are just in mid-west
only
21
TAMDAR biases may be better than sonds
22
Proposed Aircraft Temperature Bias Corrections
  • Ballish and Kumar BAMS(Nov 2008) studied aircraft
    temperature biases and proposed bias corrections
    shown in the next slide for January 2007 for the
    15 aircraft types with the largest counts
  • In the following slide, the same is shown for non
    US AMDAR types
  • This study did not include TAMDAR or Canadian
    AMDAR types

23
Most corrections are negative
24
(No Transcript)
25
Aircraft vs Sond GSI Draws to Temps between
200-300 hPa
SOND Tdiff (obs-ges)
Aircraft Tdiff (obs-ges)
Aircraft Tdiff (obs-anl)
SOND Tdiff (obs-anl)
Aircraft Sondes, thus warm aircraft data
overwhelms the GSI/GFS system
26
AMDAR Versus Sond Counts 300-200 hPa
Aircraft
Aircraft
Sonds
Sonds
27
Suru Sahas website displays model fits to RAOBS
in North America showing the GFS analysis and
guess maintain a warm bias throughout most of the
troposphere that may be related to large numbers
of aircraft with warm biases
28
Model Climate Impact from Aircraft Warm
Temperatures
  • The next slide courtesy of Dick Dee of ECMWF
    shows the increase in the number of aircraft
    reports versus time in the ECMWF reanalysis
  • The temperature bias of the ECMWF analysis and
    background seem to be affected by the large
    increase in the number of aircraft temperatures
    along with other factors
  • The NCEP GSI may have more bias impact as it does
    not thin aircraft data and its satellite radiance
    bias corrections are anchored to the analysis as
    truth as opposed to radiosondes as truth

29
Model Climate Bias Impact From Warm Aircraft
Temperatures
Global-mean departures of analysis (blue) and
background (red) from radiosonde temperatures (K)
at 200hPa, and number of obs/day (x10-4, green)
Global-mean departures of analysis (blue) and
background (red) from aircraft temperatures (K)
at 200hPa, and number of obs/day (x10-4, green)
30
Summary
  • The standard monthly AMDAR reports are useful but
    do not contain enough information on aircraft
    data quality
  • In part due to the WIGOS project, more frequent
    and complete quality information will be needed
  • Improvements are needed in the aircraft
    track-checking
  • The TAMDAR data appear to be of useful quality,
    especially the moisture
  • The Canadian AMDAR data show considerable bias
    differences with the aircraft phase of flight and
    will need more effort to assimilate them well
  • There is evidence that large numbers of
    relatively warm aircraft temperatures are
    impacting model analysis bias
  • Improvements are needed in the bias correcting
    and or use of aircraft temperatures, winds and
    moisture
  • NCEP and the ECMWF are both planning to perform
    aircraft temperature bias corrections
  • It is likely that 4DVAR assimilation is needed to
    get maximum impact of aircraft data due to their
    reporting at off times
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