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METADATA TO DOCUMENT SURFACE OBSERVATION

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Title: METADATA TO DOCUMENT SURFACE OBSERVATION


1
METADATA TO DOCUMENT SURFACE OBSERVATION
  • Michel Leroy, Météo-France

2
METADATA
  • Metadata is necessary to use efficiently observed
    data.
  • Latitude, longitude, altitude, station Id., date
    and time are obvious metadata.
  • A detailed description of the site and the
    instruments used, their characteristics, the
    historic of any instrument and site change, etc.
    is highly recommended and wished by
    climatologists. But the way to document this
    information is not yet standardized, this
    information is often missing and when available,
    the information is not easy to use by automatic
    means, due to its complexity.
  • The site environment is one of the important
    factor affecting a field measurement and its
    representativeness for various applications.
  • Though quite well known by the meteorological
    services, WMO siting recommendations are not
    always followed in the real world (or cannot be
    followed).
  • It is the same thing for the measurement
    uncertainty when compared to recommended and
    achievable measurement uncertainty stated in WMO
    doc n8 (CIMO Guide),

3
Some condensed metadata
  • In order to document the site environment and the
    sustained characteristics of the measurement
    system in an easy to handle way, Météo-France has
    defined two classifications
  • A siting classification, ranging from 1 to 5, for
    each basic parameter.
  • A maintained performance classification,
    ranging from A to E, for each basic measurement.
  • Reducing the site characteristics and the
    equipments performances to single numbers or
    letters hide many interesting details, but a
    major advantage is to let the results easy to
    use. And these single numbers dont restrict an
    additional detailed documentation (such as
    photos).
  • The definition of these classifications is coming
    from an initial analysis of quality factors
    influencing a measurement

4
Drawbacks
  • These classifications dont allow any corrections
    of the data. They are not developed for that.
  • Especially for wind, may be for precipitation,
    some correction methods exist and could be
    applied. These methods need a detailed knowledge
    of the site environment and sometimes additional
    parameters. There would be a great interest in
    applying standardized methods to correct raw
    measurements using the available metadata of a
    site. But the set of metadata needed to apply
    corrections is not clearly defined or
    standardized (except for wind for the reduction
    of the measured wind to a standard wind at 10
    meters with a roughness length of 0.03 m). It
    would be ideal to have them, but this approach
    may be impracticable in the real world.
  • The advantage of the proposed classification is
    its practicability in the real world, therefore
    adding a practicable value to the information.

5
Quality factors of a measurement
  • The intrinsic characteristics of sensors or
    measurement methods
  • The maintenance and calibration needed to
    maintain the system in nominal conditions.
  • The site representativeness

6
Site representativeness
  • Exposure rules from CIMO recommendations.
  • But not always followed and not always possible
    to follow, depending on the geographical
    situation.
  • In 1997, Météo-France defined a site
    classification for some basic surface variables.
  • Class 1 is for a site following WMO
    recommendations
  • Class 5 is for a site which should be absolutely
    avoided for large scale or meso-scale
    applications.
  • Class 2, 3 and 4 are intermediate
  • This classification has been presented during
    TECO98 in Casablanca.

7
Classification for wind measurements
  •  Roughness classification Davenport, see CIMO
    Guide, WMO Doc n8
  • Siting classification
  • The existence of obstacles nearly always lead to
    a decrease of the mean wind speed. Extreme values
    are generally also decreased, but not always.
    Obstacles increase turbulence and may lead to
    (random) temporary increase of instantaneous wind
    speed.
  • The following classes are considering a
    conventional 10 m measurement.

8
  • Class 1
  • -      The wind tower must be erected at a
    distance of at least 10 times the height of the
    nearby obstacles (therefore seen under an
    elevation angle below 5.7)
  • -      An object is considered as an obstacle if
    it is seen under an angular width greater than
    10.
  • -      The obstacles must be below 5.5 m within a
    150 m distance around the tower (and if possible
    be below 7 m within a 300 m distance).
  • -      The wind sensors must be located at a
    minimum distance of 15 times the width of thin
    nearby obstacles (mast, thin tree with angular
    width lt 10).
  • -      The surrounding country must not present
    any relief change within a 300 m radius. A relief
    change is a 5 m height change.

9
  • Class 2 (error 10 ?)
  • -      The wind tower must be erected at a
    distance of at least 10 times the height of the
    nearby obstacles (elevation angle lt 5.7)
  • -      An object is considered as an obstacle if
    it is seen under an angular width greater than
    10.
  • -      A relief change within a 100 m radius is
    also considered as an obstacle.
  • -      The wind sensors must be located at a
    minimum distance of 15 times the width of thin
    nearby obstacles (mast, thin tree with angular
    width lt 10).
  •  Class 3 (error 20 ?)
  • -      The wind tower must be erected at a
    distance of at least 5 times the height of the
    nearby obstacles (elevation angle lt 11.3)
  • -      A relief change within a 50 m radius is
    also considered as an obstacle.
  • -      The wind sensors must be located at a
    minimum distance of 10 times the width of thin
    nearby obstacles.

10
  • Class 4 (error 30 ?)
  • -      The wind tower must be erected at a
    distance of at least 2.5 times the height of the
    nearby obstacles (elevation angle lt 21.8)
  •  
  • Class 5 (error gt 40 ?)
  • - Obstacles are existing at a distance less than
    2.5 times their height.
  • - Obstacles with a height greater than 8 m, at a
    distance less than 25 m.

11
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12
St-SulpiceNord
Est
13
St-SulpiceSud
Ouest
14
St-Sulpice. Relevé de masques
  • Class 4 for wind.
  • New Radome AWS settled at a distance of 60 m,
    away from the woods ? class 3

15
Saint Sulpice, DIRCERatio of mean wind speed (10
min.) between Patac et XariaSouth winds
North winds
16
Classification of stations
  • Between 2000 and 2006, 400 AWS have been
    installed for the Radome network.
  • The objective was class 1 for each parameter
    (Temp, RH, wind, precip., solar radiation).
  • But class 2 or class 3 were accepted when class 1
    not possible.
  • Météo-France is now classifying al the surface
    observing stations, including the climatological
    cooperative network 4300 sites, before the end
    of 2008.
  • Update at least every 5 years.

17
Where are we ?
18
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21
Other quality factors
  • Intrinsic performances
  • Maintenance and calibration
  • Within a homogeneous network, these factors are
    known and generally the same. But Météo-France is
    using data from various networks
  • Radome (554)
  • Non-proprietary AWS (800)
  • Climatological cooperative network (gt 3000)
  • The intrinsic performances, maintenance and
    calibration procedures are not the same.

22
Several reasons
  • The objectives may be different.
  • But some uncertainty objectives are sometimes
    (often) unknown !
  • To get cheap measurements ?
  • The maintenance and/or the calibration are not
    always organized !
  • Within the ISO 9001-2000 certification process,
    Météo-France was forced to increase his knowledge
    of the various networks characteristics.

23
Another classification !
  • After site classification (1 to 5), definition of
    an additional classification, to cover the two
    quality factors
  • Intrinsic performances
  • Maintenance and calibration
  • 5 levels were defined
  • Class A WMO/CIMO recommendations (Annex 1B of
    CIMO guide)
  • Class B Lower specs, but more realistic or
    affordable good performances and good
    maintenance and calibration. RADOME specs.
  • Class C Lower performances and maintenance, but
    maintenance/calibration organized.
  • Class D No maintenance/calibration organized.
  • Class E Unknown performances and/or maintenance
  • This classification is called Maintained
    performance classification

24
Air temperature
  • Class A Overall uncertainty of 0.1C. Therefore,
    the uncertainty of the temperature probe lower
    than 0.1C and use of a perfect artificially
    ventilated screen. Achievable measurement
    uncertainty is 0.2C.
  • Class B Pt100 (or Pt1000) temperature probe of
    class A (? 0.25C). Acquisition uncertainty lt
    0.15C. Radiation screen with known
    characteristics and over-estimation of Tx (daily
    max. temperature) lt 0.15C in 95 of cases.
    Laboratory calibration of the temperature probe
    every 5 years.
  • Class C Temperature probe with uncertainty lt
    0.4C. Acquisition uncertainty lt 0.3C. Radiation
    screen with known characteristics and
    over-estimation of Tx lt 0.3C in 95 of cases.
  • Class D Temperature probe and/or acquisition
    system uncertainty lower than for class C.
    Radiation screen or with unacceptable
    characteristics (for example, over-estimation of
    Tx gt 0.7C in 5 of cases).

25
Relative humidity
  • Class A Overall uncertainty of 1! Achievable
    2.
  • Class B Sensor specified for ? 6, over a
    temperature range of 20C to 40C. Acquisition
    uncertainty lt 1. Calibration every year, in an
    accredited laboratory.
  • Class C Sensor specified for ? 10, over a
    temperature range of 20C to 40C. Acquisition
    uncertainty lt 1. Calibration every two years in
    an accredited laboratory, or calibration every
    year in a non-accredited laboratory.
  • Class D Sensor with specifications worst than ?
    10 over the common temperature conditions.
    Calibration not organized.

26
Global solar radiation
  • Class A Pyranometer of ISO class 1. Uncertainty
    of 5 for daily total. Ventilated sensor.
    Calibration every two years. Regular cleaning of
    the sensor (at least weekly).
  • Class B Pyranometer of ISO class 1. No
    ventilation. Calibration every two years. No
    regular cleaning of the sensor.
  • Class C Pyranometer of ISO class 2. No
    ventilation. Calibration every five years. No
    regular cleaning of the sensor.
  • Class D Sensor not using a thermopile.
    Calibration not organized.

27
Other parameters
  • Pressure
  • Amount of precipitation
  • Wind
  • Visibility
  • Temperature above ground
  • Soil temperature

28
Status of the RADOME network
  • Air temperature Class B
  • RH Class B
  • Amount of precipitation Class B or Class C,
    depending on the rain gauge used.
  • Wind Class A
  • Global solar radiation Class A for manned
    station, class B for isolated sites.
  • Ground temperatures Class B
  • Pressure Class B
  • Visibility (automatic) Class B

29
Status of the cooperative network
  • Air temperature (liquid in glass thermometers)
    Class C
  • Amount of precipitation Class B

30
Status of non-Météo-France additional networks
  • Air temperature Class B to D
  • RH Class B to D
  • Amount of precipitation Class B to C
  • Wind Class B to D
  • Global solar radiation Class B to D
  • Ground temperature Class B to C
  • Pressure Class B to D

31
Metadata
  • These classification for each site are meta data,
    part of the climatological database.
  • Site classification is on going.
  • Maintained performance classification has been
    defined this year and is being applied is it
    possible to easily classify the additional
    networks.
  • With these two classifications, a measurement on
    a site can be given a short description.
  • Example C3 for global solar radiation is for a
    class 2 pyranometer without ventilation,
    calibrated every 2 years, installed on a site
    with direct obstructions, but below 7.

32
An image of a network
33
An image of the RADOME network
34
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35
Conclusion
  • These classifications are intended to describe
    the real world of measuring networks, which is
    sometimes far form the WMO/CIMO recommendations.
  • WMO (CIMO, CBS) has decided to develop a site
    classification, on the example of this
    classification. Such a standard would be further
    recognized by ISO.
  • This topic has been recently discussed by the
    CIMO Expert Team on Surface Technology and
    Measurement Techniques.
  • Any suggestions or comments are welcomed. To be
    addressed to Michel Leroy

36
Proposed change for precipitation
  • Change class 1 for having in class 1 a well
    protected site homogeneous obstacles around the
    rain gauge which can reduce the wind speed at the
    gauge level.
  • Class 2 unchanged no obstacles closer than 2
    times their height.

37
Proposed change for temperature/humidity
  • To use the climatology of wind for temperature
    classification.
  • of low wind speed ( lt 1.5 or 2 m/s) ?

  • Trappes

  • St Denis, La Réunion

38
Proposed change for temperature/humidity
  • The perturbation from artificial surface is
    greatly reduce with wind. With a 1 m/s wind, the
    air moves by 60 m in one minute. The frequency of
    mean wind speed (at 10 m) below 1.5 m/s could be
    used to reduce the influence of artificial
    surface in the classification.
  • The shading conditions currently used are a big
    constraint. It could be partly replaced by the
    global angle of view of obstacles
  • No obstacles, angle of view is 0
  • Obstacles everywhere angle of view is 2P
    (100).
  • Screen along a wall angle of view is P (50).
  • Angle of view thresholds could be 5, 10, 20
  • But more difficult to evaluate.
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