Document in postscript
.This product contains reflectivity data for all the antenna elevations of a full volume scan, updated each 5 minutes. One volume dataset is characterized by 20 image files, one for each elevation. POLAR-Z permits the access to the highest spatial resolution of the data which is accessible to the user (fine spatial resolution at short range, sparse at wide range).
The reflectivity assigned tooneimage pixel is representative for one cell with extension of 1 degree in azimuth and 1 km in range laying over the surface scanned during the given elevations. The range gates (the discrete points in range along a single radial beam) are placed between 1km and a maximum which is elevation dependent, for the lowest elevations being of 230 km. The cells reflectivity is coded in range 0 to 15 corresponding to a linear scale in dBZ .
The figure shows an example of this product for the radar station Monte Lema at the first elevation of the volume scan which is -0.3 degrees below the horizon; the data was taken at 09:32 utc time on 1. March 1994. The maximal measured reflectivity in this image reaches the class 52-55 dBZ which is coded with value 14.
Figure 5.1: POLAR-Z image.
This product contains Doppler velocity data for all the antenna elevations of a full volume scan, updated each 5 minutes. One volume dataset is characterized by 20 image files, one for each elevation.
The Doppler velocity assigned to one image pixel is representative for one cell with extension of 1 degree in azi- muth and 1 km in range laying over the conical surface scanned during the given elevation. The range gates (the discrete points in range along a single radial beam) are placed between 1km and a maximum wich is elevation de- pendent, for the lowest elevations being of 130 km. The cells velocity is coded in range 0 to 15 corresponding to a linear scale in fractions of the Nyquist velocity dependent from the active pulse repetition frequency.
The figure shows an example of this product for the radar station Monte Lema at the first elevation of the volume scan which is -0.3 degrees below the horizon; the data was taken at 09:32 utc time on 1. March 1994 (day 060). The velocities coded 01 to 07 are negatives (against the radar), those coded 09 to 15 are positives (toward the radar), 08 is for zero (perpendicular to the beam) and 00 is for unknown velocity (clutter or shielding or noise).
Figure 5.2: POLAR-U image.
| N | Elevation | DElev | D max R | D max U | RPM | Time[s] | Step[s] | PRF | ||||
| 1 | -0.3 | 1.8 | 230 | 130 | 3 | 20 | 1.4 | 600 | ||||
| 2 | 1.5 | 2.0 | 230 | 130 | 3 | 20 | 1.4 | 600 | ||||
| 3 | 3.5 | 2.0 | 162 | 130 | 4 | 15 | 1.4 | 800 | ||||
| 4 | 5.5 | 2.0 | 112 | 112 | 4 | 15 | 1.4 | 800 | ||||
| 5 | 7.5 | 2.0 | 85 | 85 | 6 | 10 | 1.4 | 1200 | ||||
| 6 | 9.5 | 3.5 | 68 | 68 | 6 | 10 | 1.7 | 1200 | ||||
| 7 | *13.0 | 5.3 | 51 | 51 | 6 | 10 | 2.0 | 1200 | ||||
| 8 | *18.3 | 7.0 | 37 | 37 | 6 | 10 | 2.2 | 1200 | ||||
| 9 | *25.3 | 9.2 | 27 | 27 | 6 | 10 | 2.4 | 1200 | ||||
| 10 | +34.5 | -34.0 | 20 | 20 | 6 | 10 | 4.2 | 1200 | ||||
| 11 | 0.5 | 2.0 | 230 | 130 | 3 | 20 | 1.4 | 600 | ||||
| 12 | 2.5 | 2.0 | 205 | 130 | 3 | 20 | 1.4 | 600 | ||||
| 13 | 4.5 | 2.0 | 133 | 130 | 4 | 15 | 1.4 | 800 | ||||
| 14 | 6.5 | 2.0 | 97 | 97 | 4 | 15 | 1.4 | 800 | ||||
| 15 | 8.5 | 2.5 | 76 | 76 | 6 | 10 | 1.5 | 1200 | ||||
| 16 | 11.0 | 4.5 | 59 | 59 | 6 | 10 | 1.9 | 1200 | ||||
| 17 | *15.5 | 6.1 | 43 | 43 | 6 | 10 | 2.1 | 1200 | ||||
| 18 | *21.6 | 8.0 | 31 | 31 | 6 | 10 | 2.3 | 1200 | ||||
| 19 | *29.6 | 10.4 | 23 | 23 | 6 | 10 | 2.6 | 1200 | ||||
| 20 | +40.0 | -40.3 | 18 | 18 | 6 | 10 | 4.5 | 1200 |
The chosen scan sequence allows an aviation product every 2.5 min (two
Half-Volume-Scans, calculated alternatively from revolutions 1-10 and 11-20) and a full
volume scan every 5 min (revolutions 1-20), without exceeding an acceleration of the
antenna of 10 o /s 2 and a maximum speed of the antenna of 20 o /s in elevation (36 o /s
in azimuth). The table gives for each revolu- tion with index N, the Elevation in degrees
above the horizon, the change of the elevation DElev in degrees at the end of the
revolution, the maximum distance in km D max R and D max U for analysing the data in
reflectivity and Doppler applications, the revolutions per minute (RPM), the Time per
revolution in seconds, the time needed to change the elevation (Step) in seconds and the
pulse repetition frequency (PRF) in number of pulses per second. The calibra- tion takes
place during the indicated elevations(*). The wind-profile over the radar station is
estimated every 2.5 min from the highest elevation of each Half-Volume-Scan (+).
Radar products are identified by 3 characters TFS with T -> Type, F -> Format, S -> Source:
Type Format Source ---------------------------------------------------------------------- C: Calibration A: 200x200x2km A: Albis O: Overview D: 100x5 C: Composite (A+D+L) P: Precipitation (Rain) G: 320x256x2km D: La Dôle R: Rapid H: 400x400x1km E: Composite (A+D) S: Status L: 305x269x2km L: Lema T: Today P: 360xN (see notes) X: (experimental) U: Doppler velocity S: 305x269x1km V: Visibility V: various (see notes) W: Wind Y: (see notes) Z: Reflectivity
Identifier Format Levels(name-of-each) ---------------------------------------------- OYC L (1,2,...,9,A,B,C,M) OYL A (1,2,...,9,A,B,C) VYL H (1,2,...,9,A,B,C) UYL,ZYL P (1,2,..,9,A,B,C,D,E,F,G,H,I,J,K)
Operational products are stored in a directory tree resident on a disk of the local server. This tree is built on a directory with standard name /srn/data/. Each product type is located on one different subdirectory having his own standard name (= the product identifier).
Data files are present under the mentioned subdirectories and have a name following a conven- tion related to the product identification also contained in the file data self in form of a prefix- ing header.
(Example for Composite and Lema; analog for Albis and La Dôle):
CVL, OYC, OYL, PAL, PHL, PLC, PSL, RHL, RLC, RSL, SVC, SVL, TGA, TGC, TGD, TGE, TGL, TGX, UYL, VYL, WDL, ZYL
TFS'YY'DDD'HH'MM'Q'C.prd with:
| TFS: | Product identifier |
| YY: | Year [00-99] |
| DDD: | Day-of-the-year (1-366) |
| HH: | Hour (00-23) |
| MM: | Minute(00-59) |
| Q: | Quality factor (0->poor.. 7->good, >7->bad data) |
| C: | Compression (L -> compressed, U -> uncompressed) |
| prd: | file type |
Example: SVL9332711407L.prd ->
Status Lema on day 327 of 1993 at 11 h 40 min, quality = 7, compressed
NOTE:
The quality factor is expressed in hexadecimal form (0,1,...,9,A,...,F) and takes into
account the completeness of the data set (i.e., the number of used elevations), the con-
dition of the radar transmitter (the radiated power), and the condition of the receiver
(the current estimate of the receiver noise figure).
For products RAIN and VISIB (being composed by different single scan volume data) the quality factor is built as the average of the source data factors. For product TODAY-COMPOSITE the quality factor assumes another meaning: it denotes the presence of the data from the different stations summing up the following codes: 1 for Albis, 2 for La Dôle and 4 for Lema (e.g. the resultant quality code for TGC is 1 when just Lema is up and 7 when data from all 3 stations are present).
The time indication is related to the termination time of the full respectively half scan.
CH'TFS'YY'DDD'HH'MM'Q'C'bb.bb.bbbb.bbbb.ss.bb (32 bytes) where:
| CH: | prefix |
| TFS...: | file name without ".prd" |
| bb.b.: | binary data (record length, product size, counts, etc.) |
NOTE 1: For the products RAIN and VISIB a "count" of the cumulated images is available in the header information.
NOTE 2: For the product TODAY the first 4 lines of the file contain a string (called DIGITAL ANNOTATION) with information on the product identification:
Digital annotation string: MRDDMOYYHHMMXX with:
| M: | "W" for radar-site products, "C" for composite products |
| R: | "Z" for Albis, "G" for Dole, "T" for Lema, "C" for Composite |
| DD: | day-of-the-month (01..31) |
| MO: | month-of-the-year (01..12) |
| YY: | last two digits of the year |
| HH: | hour (00..23) |
| MM: | minute (00..59) |
| XX: | "GO" for operational weather measurements |
The product data is not present in physical units (for example in floating point format) but a discretization and coding operation is applied to the measured data. This has the drawback to reduce the data granularity but it was made for reasons of efficiency (transmission time, storage size).
The reflectivity data having a large range of possible values is coded following a
logarithmic scale and use 4bit/pixel; the velocities are coded with a linear scale taking
in consideration the maximum permitted value (dependent from the pulse repetition
frequency) and use either a 4bit/pixel or a 8bit/pixel scheme.
For reasons of compatibility with the past product TG uses 3 bit/pixel.
| Code: | 0 | 1 | 2 | 3 | 4 | 5 | 6 | 7 |
| Rain-rate [mm/h]: | <.16 | .16-.25 | .25-.40 | .40-.63 | .63-1.0 | 1.0-1.6 | 1.6-2.5 | 2.5-4.0 |
| dBZ: | <13 | 13-16 | 16-19 | 19-22 | 22-25 | 25-28 | 28-31 | 31-34 |
| Code: | 8 | 9 | 10 | 11 | 12 | 13 | 14 | 15 |
| Rain-rate [mm/h]: | 4.0-6.3 | 6.3-10 | 10-16 | 16-25 | 25-40 | 40-63 | 63-100 | >100 |
| dBZ: | 34-37 | 37-40 | 40-43 | 43-46 | 46-49 | 49-52 | 52-55 | >55 |
| Code: | 0 | 1 | 2 | 3 | 4 | 5 | 6 |
| Rain-rate [mm/h]: | <0.3 | 0.3-1.0 | 1.0-3.0 | 3.0-10 | 10-30 | 30-100 | >100 |
...............................(code 7 is reserved for graphics overlay)
Velocity for a coded value = k ® (Vn/16)*(2*k-15± 1) for
k=0..15
Example: k = 10 -> the velocity interval is Vn*[4/16,6/16].
Vn is the Nyquist velocity in [m/s] for the current PRF (Pulse Repetition Frequency) in
[Herz]
by a wavelength (l) in [m] given by the relationship:
Vn = l*PRF/4.
Considering a l of 5.5 cm and taking the appropriate PRF
(see "Antenna scan table" )we
have:
| Elevation index: | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 |
| Vn [m/s]: | 8.25 | 8.25 | 11.0 | 11.0 | 16.5 | 16.5 | 16.5 | 16.5 |
| Elevation index: | 9 | 10 | 11 | 12 | 13 | 14 | 15 | 16 |
| Vn [m/s]: | 16.5 | 16.5 | 8.25 | 8.25 | 11.0 | 11.0 | 16.5 | 16.5 |
| Elevation index: | 17 | 18 | 19 | 20 | ||||
| Vn[m/s]: | 16.5 | 16.5 | 16.5 | 16.5 |
N.B.: - a frequency shift of 40Hz corresponds to a radial speed of 1 m/s.
- a positive velocity is toward the radar (in the direction of the beam)
Velocity for a coded value = k ® (Vn/255)*(2*k-256± 1) for k=1..255
Value = 0 ® missing value
| Examples: | k = 001 -> the velocity interval is ~Vn*[-1.000,-0.992] |
| k = 128 -> the velocity interval is ~Vn*[-0.004,+0.004] | |
| k = 255 -> the velocity interval is ~Vn*[+0.992,+1.000] |
NOTES:
For the interpretation of the Doppler data it is important to take note of following
aspects related to the signal processing and data handling procedures of the equipment:
The Swiss National Coordinates result from a conformal mapping (true angles) with skew axis of the earth surface to a cylindrical surface.
The earth surface (approximated by a Bessel's rotation ellipsoid) is first projected onto a sphere with radius the earth radius in Berne (i.e. the distance between Berne and the ellipsoid's rota- tion centre) having as centre the ellipsoid's rotation centre. The sphere surface is successively projected onto a cylindrical surface tangent in Berne having the cross section correspondent to the great circle of the sphere perpendicular to the earth meridian passing across Berne.
Geographic coordinates of Berne: LAT = 46.952, LON = 7.440
The radar products OVERVIEW, RAIN, RAPID, TODAY, VISIB are georeferenced with respect to the Swiss National Coordinates system.
Following formulas are useful in association with the indications of the Swiss National Coordinates given in the various product layouts.
Swiss National (Y,X) to Geographic (LAT,LON) coordinate conversion:
LAT = 45.16 + 0.008967*X - 7.7E-7*(Y-600)**2 [dec.degr.,km]
LON = 07.44 + (0.008967*Y-5.38)/cos(LAT) [dec.degr., km]
precision better than 16 seconds (0.5km) within the Swiss TODAY-Composite (298/405, 862/-31).
Geographic (LAT,LON) to Swiss National (Y,X) coordinateconversion:
X = 111.526*LAT + 0.5*(LON-7.44)**2 - 5036.44 [km,dec.deg.]
Y = 111.526*(LON-7.44)*cos(LAT) + 600 [km, dec.degr.]
with precision better than 1 km within the Swiss TODAY-Composite (298/405, 862/-31).
Table 1: Comparison of the main radar characteristics
| Element | old | new |
| Antenna: half-power beam width | 1.1 degree | 1.0 degree |
| Number of elevations | 19 in 10 min | 20 in 5 min |
| Antenna revolutions/min | 3 | 3, 4 or 6 (depending on elevations) |
| PRF (pulse repetition frequency) | 250 Hz | 600, 800 or 1200 Hz (dep. on el.) |
| Wavelength | 5.5cm | 5.5cm |
| Transmitter type | Magnetron | Magnetron |
| Transmitted power, pulse length | 250 kW, 2µs | 250 kW, 0.5 µs |
| Receiver sensitivity at 230 km | 0.5 mm/h | 0.17 mm/h |
| Receiver: log amplifier | 90 ± 0.5 dB | 90 ± 0.5 dB |
| Samples per degree and per km | 32 x 3 | 32 x 12 |
| Processed Video signals | og-Z: 8 bit | I, Q, log-Z, resolution: 12 bits |
| Clutter suppression | static map | 6 complem. tests, incl. dyn. map |
| Calibration with noise source | - | every 2.5 min |
| Calibration with signal generator | manual 1/month | full automat, 121 points every 24h |
| Profile corrections | range dependent fixed approx | visibility and profile estimated in real time |
Table 2: Location of weather radars in Switzerland
| Radar | Height | Longitude | Latitude | CH-coord E/W | CH-coord S/N |
| Albis | 928 m | 8.513E | 47.285N | 681'193 m | 237'593 m |
| La Dôle | 1680 m | 6.100E | 46.426N | 497'057 m | 142'408 m |
| Lema | 1625 m | 8.834E | 46.042N | 707'957 m | 99'762 m |
Table 3: Dates of radar equipment renewal
| Radar | II generation (end date) | III generation (start date) |
| Albis | 11 July 1994 | 20 October 1994 |
| La Dôle | 01 May 1995 | 07 November 1995 |
| Lema | 13 September 1993 |
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