© Crown copyright Met Office Forecasting Runway Visual Range Lauren Reid, Met Office, 12 September 2013 ECAM
© Crown copyright Met Office
Forecasting Runway Visual RangeLauren Reid, Met Office, 12 September 2013
ECAM
© Crown copyright Met Office
Contents
This presentation covers the following areas
• Introduction
• Definition of RVR
• Methodology
• Models (UKV, MONIM, HT-FRTC)
• Case studies
• Conclusions
• Questions and answers
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Introduction
• Runway Visual Range (RVR) is used at airports to help determine if Low Visibility Procedures (LVP) are necessary.
• LVPs affect airport operations by requiring a reduction in the number of aircraft landing and taking-off depending on the cloud base height, visibility and/or RVR
• The purpose of this study was to determine if it may be possible to generate an RVR forecast to aid airport operations mitigating against the worst impacts of LVP
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RVR ≠ Visibility
The view from the cockpit along runway 22R at Copenhagen during a fog event. The RVR in this photo is 500m [1]
[1] http://picsfromtheoffice.blogspot.co.uk/2011_11_01_archive.html - Mathieu Neuforge
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Definitions
Runway Visual Range is defined by ICAO Annex 3 as:
The range over which the pilot of an aircraft on the centre line of a runway can see the runway surface markings or the lights delineating the runway or identifying its centre line.
Visibility - Visibility for aeronautical purposes is the greater of:
a) the greatest distance at which a black object of suitable dimensions, situated near the ground, can be seen and recognized when observed against a bright background;
b) the greatest distance at which lights in the vicinity of 1 000 candelas can be seen and identified against an unlit background.
Note — The two distances have different values in air of a given extinction coefficient, and the latter b) varies with the background illumination. The former a) is represented by the meteorological optical range (MOR). (ICAO Document 9328 2005):
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Relationships
• Koschmieder's Law. A relationship between the apparent luminance contrast of an object, seen against the horizon sky by a distant observer, where σ = extinction coefficient (m-1)
• Allard's Law. An equation relating illuminance (E) produced by a point source of light of intensity (I) on a plane normal to the line of sight, at distance (R) from the source, in an atmosphere having a transmissivity (T).
E=(Ie-σR)/R2
ln(0.05)MOR
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An illustration of the variation of RVR with MOR for a fixed illumination threshold (Et=10-5) derived from the equation on previous
page. Results are displayed for a range of runway lighting intensity (I) from 10 cd to 10000 cd (shown as different colours).
ln(0.05)
ln( ) 2 ln( )LL
LL
RVRMOR
I RVREt
• The equations from Koschmieder and Allard’s Law can be rearranged to form:
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Data
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MONIM (Met Office Might Illumination Model)
• MONIM is used by defence as a tactical decision aide for use with night vision goggles.
• Adapted for use in built up areas with additional light sources.
• Results in the illumination value, E.
• Et is required for the RVR calculation, so the ratio of the background light vs the whole hemisphere is utilised - 0.137%
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HT-FRTC (Havemann-Taylor Fast Radiative Transfer Code)
• The Havemann-Taylor Fast Radiative Transfer Code was developed at the Met Office for use in simulating the electromagnetic radiation from a source at a specified observation location some distance away
• As the electromagnetic radiation travels to the observer, the radiation is modified by the atmosphere, which absorbs, emits and scatters the radiation by varying amounts depending on the current state of the atmosphere
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Met Office UKV model
• The ability to accurately forecast fog and the subsequent low visibility is incredibly important for airport operations, it is important to recognise that fog is one of the most difficult meteorological phenomena to forecast with the level of detail required.
Output fields from the UKV model valid at 06z 16 October 2011. Left: Visibility at 1.5m height (m). Right: Fog fraction (percentage).
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Observations
Transmissometer
• The three transmissometers record and store the details of the runway lighting, including the background luminance (cd/m2) and the runway light intensity (cd). If the observed RVR is above 1500m then the system does not record the RVR
METAR (Meteorological Terminal Air Report)
• Is a routine meteorological observation given at all airports. METARs give an indication to incoming pilots of the current weather conditions at the runway and includes: temperature; pressure; cloud height and coverage (in octa); wind speed and direction; visibility; and RVR (if below 1500m).
These two methods used to identify and test case studies at Heathrow and Bournemouth
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Heathrow AP 16-10-2011 METAR and Average IRVR Obsevations
0
200
400
600
800
1000
1200
1400
1600
1800
2000
02:00 04:00 06:00 08:00 10:00Time of day
Dis
tan
ce (
m)
calc MOR
avg I-RVR South
avg I-RVR North
METAR RVRNorth
METAR RVRSouth
METAR VIS
Heathrow AP 16-10-2011METAR and IRVR Obsevations at Touchdown Point
0
200
400
600
800
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1600
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02:00 04:00 06:00 08:00 10:00Time of day
Dis
tan
ce (
m)
RVR Touchdown South
RVR Touchdown North
METAR RVRNorth
METAR RVRSouth
Examples of the output transmissometer RVR for Heathrow
Airport on 16 October 2011.
a) Shows only the first (touch down) value of RVR from the
transmissometer. Note how the METAR values for both the northern and southern runway match with the
IRVR data.
b) There are three reported values for the RVR for the north and south
runways which has been averaged to give the blue and red line, from this the
MOR for the northern runway was calculated (green). The overlaid points
are the METAR RVR (for both runways) and visibility in blue, red and
green respectively.
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Case Studies
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Case Studies
• Dates were chosen for the case studies based on METAR observations of RVR that lasted longer than 3.5 hours and resulted in a significant reduction in visibility at Heathrow or Bournemouth Airports.
• The dates investigated were:
• 30th September 2011 at Bournemouth
• 16th October 2011 at Heathrow
• 20th September 2011 at both sites
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Bournemouth Airport 30 September 2011
Bournemouth AP 30-09-2011 (METAR and IRVR Obsevations)
0
500
1000
1500
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2500
3000
3500
4000
02:00 03:00 04:00 05:00 06:00 07:00 08:00
Time of day
Dis
tan
ce (
m)
calc MOR
avg I-RVR
METARVIS
METARRVR R26
METARRVR R08
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Bournemouth Airport 30 September 2011
Forecast TimeUKV Visibility
(m)
36km box Average (m)
Percentage Fog (0-1)
METAR Visibility (m)
METAR RVR (m)
03z (T+0) 4508 6046 0.125 1000R26/0450R08/0600
04z (T+1) 4668 5488 0.125 900R26/P1500R08/0250
05z (T+2) 5408 5953 0.00 200R26/0250R08/0300
06z (T+3) 5754 6293 0.00 100 R26/0400
07z (T+4) 6376 6685 0.00 600 R26/0175
08z (T+5) 7783 8858 0.00 4000 -
09z (T+6) 11083 11731 0.00 9000 -
10z (T+7) 12254 13414 0.00 CAVOK -
11z (T+8) 12379 13365 0.00 CAVOK -
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HT-FRTC: Obs of visibility and forecast RVRBournemouth 20110930
0
1000
2000
3000
4000
5000
6000
03:00 04:00 05:00 06:00 07:00 08:00 09:00Time
Dis
tan
ce
(m
)
METAR RVRR26
METAR RVRR08
Continental,I=3000
Koschmieder -MOR
The minimum and maximum differences plus RMSE in metres of RVR using the forecast NWP input compared to the average transmissometer observations.
Difference RVR (m)
Minimum 2338
Maximum 4303
RMSE 3514
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Bournemouth Airport30 September 2011
• Poor visibility forecast unrepresentative of the conditions experienced
• The other case study also had a similar situation where the forecast visibility was too large resulting in unrealistic RVR forecast
• As Bournemouth has a costal location this impacts on fog formation in the region
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Heathrow Airport 16 October 2011
Heathrow AP 16-10-2011 METAR and Average IRVR Obsevations
0
200
400
600
800
1000
1200
1400
1600
1800
2000
02:00 04:00 06:00 08:00 10:00Time of day
Dis
tan
ce (
m)
calc MOR
avg I-RVR South
avg I-RVR North
METAR RVRNorth
METAR RVRSouth
METAR VIS
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Heathrow Airport 16 October 2011
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Heathrow Airport 16 October 2011 - sensitivity
Sensitivity study: Obs of visibility and forecast RVRHeathrow 20111016
0
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03:00 04:00 05:00 06:00 07:00 08:00 09:00 10:00
Time
Dis
tan
ce
(m
)
METARRVR R27L
METARRVR R27R
IRVR data
MONIM Et,I=3000
IRVR avg
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HT-FRTC: Obs of visibility and forecast RVRHeathrow 20111016
0
500
1000
1500
2000
2500
3000
3500
03:00 04:00 05:00 06:00 07:00 08:00 09:00 10:00
Time
Dis
tan
ce
(m
)
METAR RVRR27L
METAR RVRR27R
Continental,I=3000
Koschmieder -MOR
The minimum and maximum differences plus RMSE of the RVR using the forecast NWP input compared to the average transmissometer observations.
Difference RVR (m)
Minimum -141
Maximum 2691
RMSE 1722
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Heathrow Airport 16 October 2011
• Fog/visibility forecast was reflective of the observed conditions
• The forecast data used in the RVR forecast did result in a good approximation of the RVR though it did tend to be too large compared to the METARs
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Conclusions
• When using obviations as inputs to the RVR calculation RMS error is in the region of 300-900m.
• When using the forecast visibility the RVR can degrade significantly to be over 2000m larger than the observations.
• It is possible to forecast RVR, but only if the forecast visibility and low level cloud is an accurate representation of the conditions experienced
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Questions & answers
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RVR Definition
• Runway visual range is defined by ICAO Annex 3 as:
The range over which the pilot of an aircraft on the centre line of a runway can see the runway surface markings or the lights delineating the runway or identifying its centre line.
• Further details are given by ICAO Doc 9328 section 2.2:
The definition implies that RVR is not an “observation” or a “measurement” of a meteorological parameter such as surface wind direction and speed, temperature and pressure; it is an assessment, based on calculations that take into account various elements, including atmospheric factors such as extinction coefficient of the atmosphere, physical/biological factors such as visual threshold of illumination, and operational factors such as runway light intensity.
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Visibility Definitions
The definitions of visibility and meteorological optical range are (ICAO Document 9328 2005):
Visibility - Visibility for aeronautical purposes is the greater of:
a) the greatest distance at which a black object of suitable dimensions, situated near the ground, can be seen and recognized when observed against a bright background;
b) the greatest distance at which lights in the vicinity of 1 000 candelas can be seen and identified against an unlit background.
Note — The two distances have different values in air of a given extinction coefficient, and the latter b) varies with the background illumination. The former a) is represented by the meteorological optical range (MOR).
Meteorological Optical Range (MOR) - The length of the path in the atmosphere required to reduce the luminous flux in a collimated beam from an incandescent lamp at a colour temperature of 2,700 K to 0.05 of its original value, the luminous flux being evaluated by means of the photometric luminosity function of the International Commission on Illumination.