APPENDIX E-III
REQUIRED CODE TABLES FOR PILOT AND TEMP CODE FORMS
Code Table |
Page Number |
Indicator |
Descriptor |
0265 |
E-38 |
a4 |
Type of measuring equipment used |
0421 |
E-39 |
101AdfAdf |
Form of Additional Regional Data |
0509 |
E-43 |
CH |
Clouds of the genera Cirrus, Cirrocumulus and Cirrostratus |
0513 |
E-44 |
CL |
Clouds of the genera Stratocumulus, Stratus, Cumulus, and Cumulonimbus |
0515 |
E-45 |
CM |
Clouds of the genera Altocumulus, Altostratus, and Nimbostratus |
0777 |
E-46 |
DtDt--DnDn |
Dew-point depression in two figures |
1600 |
E-47 |
h |
Height above the surface at the base of the lowest cloud |
1734 |
E-48 |
Id |
Indicator used to specify the hundreds of hectopascals figure |
1845 |
E-49 |
im |
Indicator for units of elevation, and confidence factor for accuracy of elevation |
2582 |
E-49 |
MiMi MjMj |
Identification letters of the report; identification letters of the part of the report or the version of the code form |
2590 |
E-50 |
MMM |
Number of Marsden square in which the station is situated at the time of observation |
2700 |
E-54 |
N |
Total cloud cover |
3333 |
E-55 |
Qc |
Quadrant of the globe |
3685 |
E-56 |
rara |
Radiosonde/sounding system used |
3845 |
E-58 |
Sn |
Sign of the data, exponent, and reference value |
3849 |
E-58 |
sr |
Solar and infrared radiation correction |
3872 |
E-59 |
sasa |
Tracking technique/status of system used |
3931 |
E-61 |
Ta-Tc |
Encoding/Decoding the sign and Tenths value of the air temperature |
5300 |
E-62 |
PnPnhnhnhn |
Standard heights of isobaric surfaces |
Table 0265 (WMO-No. 306, Vol I.1)
a4
Type of measuring equipment used
Code | Figure |
0 | Pressure instrument associated with wind-measuring equipment |
1 | Optical theodolite |
2 | Radiotheodolite |
3 | Radar |
4 | Pressure instrument associated with wind-measuring equipment but pressure element failed during ascent |
5 | VLF-Omega |
6 | Loran-C |
7 | Wind profiler |
8 | Satellite navigation |
9 | Reserved |
Table 0421 (WMO-No. 306, Vol II)
101AdfAdf-
Form of Additional Regional Data Reported
Code Figure |
Definition |
00-31 |
|
00 |
Not to be allocated |
01 |
First day of month (UTC) |
02 |
Second day of month (UTC) |
03 |
Third day of month (UTC) |
04 |
Fourth day of month (UTC) |
05 |
Fifth day of month (UTC) |
06 |
Sixth day of month (UTC) |
07 |
Seventh day of month (UTC) |
08 |
Eighth day of month (UTC) |
09 |
Ninth day of month (UTC) |
10 |
Tenth day of month (UTC) |
11 |
Eleventh day of month (UTC) |
12 |
Twelfth day of month (UTC) |
13 |
Thirteenth day of month (UTC) |
14 |
Fourteenth day of month (UTC) |
15 |
Fifteenth day of month (UTC) |
16 |
Sixteenth day of month (UTC) |
17 |
Seventeenth day of month (UTC) |
18 |
Eighteenth day of month (UTC) |
19 |
Nineteenth day of month (UTC) |
20 |
Twentieth day of month (UTC) |
21 |
Twenty-first day of month (UTC) |
22 |
Twenty-second day of month (UTC) |
23 |
Twenty-third day of month (UTC) |
24 |
Twenty-fourth day of month (UTC) |
25 |
Twenty-fifth day of month (UTC) |
26 |
Twenty-sixth day of month (UTC) |
27 |
Twenty-seventh day of month (UTC) |
28 |
Twenty-eighth day of month (UTC) |
29 |
Twenty-ninth day of month (UTC) |
30 |
Thirtieth day of month (UTC) |
31 |
Thirty-first day of month (UTC) |
32-39 |
Not allocated |
40-59 |
Reason for no report or an incomplete report |
40 |
Report not filed |
41 |
Incomplete report; full report to follow |
42 |
Ground equipment failure |
43 |
Observation delayed |
44 |
Power failure |
Table 0421 (WMO-No. 306, Vol II) (Continued)
101AdfAdf-
Form of Additional Regional Data Reported
Code Figure |
Definition |
45 |
Unfavorable weather conditions |
46 |
Low maximum altitude (less than 1500 ft above ground) |
47 |
Leaking balloon |
48 |
Ascent not authorized for this period |
49 |
Alert |
50 |
Ascent did not extend above 400 hPa level |
51 |
Balloon forced down by icing conditions |
52 |
Balloon forced down by precipitation |
53 |
Atmospheric interference |
54 |
Local interference |
55 |
Fading signal* |
56 |
Weak signal* |
57 |
Preventive maintenance |
58 |
Flight equipment failure (transmitter, balloon, attachments, etc.) |
59 |
Any reason not listed above |
* Fading signals differ from weak signals in that "fading signals" are first received satisfactorily, then become increasingly weaker, and finally become too weak for reception, while "weak signals" are weak from the beginning of the ascent.
60-64: Miscellaneous |
|
60 |
Unassigned |
61 |
Unassigned |
62 |
Radiosonde report precedes |
63 |
Unassigned |
64 |
Unassigned |
65-69: Doubtful Data |
|
65 |
Geopotential and temperature data are doubtful between following levels: 0PnPnP'nP'n |
66 |
Geopotential data are doubtful between the following levels: 0PnPnP'nP'n |
67 |
Temperature data are doubtful between the following levels: 0PnPnP'nP'n |
68 |
Dew point depression is missing for reasons other than "motor-boating" between the following levels: 0PnPnP'nP'n (not used when TnTn is also missing) |
69 |
Unassigned |
70-74 Not allocated |
Table 0421 (WMO-No. 306, Vol II) (Continued)
101AdfAdf
- Form of Additional Regional Data Reported
Code Figure | Definition |
75 - 89 | Corrected Data |
75 |
Unassigned |
76 |
Unassigned |
77 |
Unassigned |
78 |
Corrected tropopause data section follows |
79 |
Corrected maximum wind section follows |
80 |
Corrected report for the entire report (first* and second* transmissions) precedes |
81 |
Corrected report of the entire first transmission precedes |
82 |
Corrected report of the entire second transmission precedes |
83 |
Corrected data for mandatory levels** follow |
84 |
Corrected data for significant levels** follow |
85 |
Minor error(s) in this report; correction follows |
86 |
Significant level(s) not included in original report follow: //PnPnPn TnTnTanDnDn or PnPnPnTnTn |
87 |
Corrected data for surface follow |
88 |
Corrected additional data groups follow: 101AdfAdf .... etc. |
89 |
Unassigned |
|
|
90-99 |
|
90 |
Extrapolated geopotential data follow: PnPnhnhnhn (dndndnfnfn) |
91 |
Extrapolated data precede * |
92 |
Unassigned |
93 |
Unassigned |
94 |
Averaged wind for the surface to 5000 foot MSL layer and the 5000 to 10000 foot MSL layer follow: ddfff ddfff (can be used in the PART A message) |
95 |
Early transmission of 850 and 500 hPa data and stability index follows: 85hhh TTTaDD ddfff 50hhh TTTaDD ddfff isis |
96 |
Early transmission of 850, 700, and 500 hPa data and stability index follow: 85hhh TTTaDD ddfff 70hhh TTTaDD ddfff 50hhh TTTaDD ddfff isis |
Table 0421 (WMO-No. 306, Vol II) (Continued)
101AdfAdf-
Form of Additional Regional Data Reported
Code Figure | Definition |
97 | Early transmission of 500 hPa data and stability index follows: 50hhh TTTaDD ddfff isis |
98 | Early transmission of 700 hPa data and stability index follows: 70hhh TTTaDD ddfff isis |
99 | Not to be allocated |
* Code figure 91 is used only in reports of dropsonde observations.
Unless both the stability index and the mean winds are missing, the Part A message always contains two special 101 groups as follows:
10164 |
Group that identifies stability index. |
10194 | Group that identifies the mean winds. |
A 5-character group follows the 10164 which contains the encoded stability index. The value that appears in the coded message for the stability index is interpreted as follows:
Coding Stability Index
Code Value |
Meaning |
00 to 40 | Stability index is 0 to 40 |
51 to 90 | Stability index is -1 to -40 |
91 | RH < 20% at either base or 500 hPa level or calculation failed. |
92 | RH is missing at the base level. |
Table 0509 (WMO-No. 306, Vol I.1)
CHClouds
of the genera Cirrus, Cirrocumulus and Cirrostratus
Code figure |
Technical specifications |
|
Code figure |
Non technical specifications |
0 |
No CH clouds |
|
0 |
No Cirrus, Cirrocumulus or Cirrostratus |
1 |
Cirrus fibratus, sometimes uncinus, not progressively invading the sky |
1 |
Cirrus in the form of filaments, strands or hooks, not progressively invading the sky | |
2 |
Cirrus spissatus, in patches or entangled sheaves, which usually do not increase and sometimes seem to be the remains of the upper part of a Cumulonimbus; or Cirrus castellanus or floccus |
2 |
Dense Cirrus, in patches or entangled sheaves, which usually do not increase and sometimes seem to be the remains of the upper part of a Cumulonimbus; or Cirrus with sproutings in the form of small turrets or battlements, or Cirrus having the appearance of cumuliform tufts | |
3 |
Cirrus spissatus cumulonimbogenitus |
3 |
Dense Cirrus, often in the form of an anvil, being the remains of the upper parts of Cumulonimbus | |
4 |
Cirrus uncinus or fibratus, or both, progressively invading the sky; they generally thicken as a whole |
4 |
Cirrus in the form of hooks or of filaments, or both, progressively invading the sky; they generally become denser as a whole | |
5 |
Cirrus (often in bands) and Cirrostratus, or Cirrostratus alone, progressively invading the sky; they generally thicken as a whole, but the continuous veil does not reach 45 degrees above the horizon |
5 |
Cirrus (often in bands converging towards one point or two opposite points of the horizon) and Cirrostratus, or Cirrostratus alone; in either case, they are progressively invading the sky, and generally growing denser as a whole, but the continuous veil does not reach 45 degrees above the horizon | |
6 |
Cirrus (often in bands) and Cirrostratus, or Cirrostratus alone, progressively invading the sky; they generally thicken as a whole; the continuous veil extends more than 45 degrees above the horizon, without the sky being totally covered |
6 |
Cirrus (often in bands converging towards one point or two opposite points of the horizon) and Cirrostratus, or Cirrostratus alone; in either case, they are progressively invading the sky, and generally growing denser as a whole; the continuous veil extends more than 45 degrees above the horizon, without the sky being totally covered | |
7 |
Cirrostratus covering the whole sky |
7 |
Veil of Cirrostratus covering the celestial dome | |
8 |
Cirrostratus not progressively invading the sky and not entirely covering it |
8 |
Cirrostratus not progressively invading the sky and not completely covering the celestial dome | |
9 |
Cirrocumulus alone, or Cirrocumulus predominant among the CH clouds |
9 |
Cirrocumulus alone, or Cirrocumulus accompanied by Cirrus or Cirrostratus, or both, but Cirrocumulus is predominant | |
/ |
CH clouds invisible owing to darkness, fog, blowing dust or sand, or other similar phenomena, or because of a continuous layer of lower clouds |
/ |
Cirrus, Cirrocumulus and Cirrostratus invisible owing to darkness, fog, blowing dust or sand, or other similar phenomena, or more often because of the presence of a continuous layer of lower clouds |
Table 0513 (WMO-No. 306, Vol I.1)
CL
Clouds of the genera Stratocumulus, Stratus, Cumulus and Cumulonimbus
Code figure |
Technical specifications |
|
Code figure |
Non-technical specifications |
0 |
No CL clouds |
0 |
No Stratocumulus, Stratus, Cumulus or Cumulonimbus | |
1 |
Cumulus humilis or Cumulus fractus other than of bad weather,* or both |
1 |
Cumulus with little vertical extent and seemingly flattened, or ragged Cumulus other than of bad weather,* or both | |
2 |
Cumulus mediocris or congestus, with or without Cumulus of species fractus or humilis or Stratocumulus, all having their bases at the same level |
2 |
Cumulus of moderate or strong vertical extent, generally with protuberances in the form of domes or towers, either accompanied or not by other Cumulus or by Stratocumulus, all having their bases at the same level | |
3 |
Cumulonimbus calvus, with or without Cumulus. Stratocumulus or Stratus |
3 |
Cumulonimbus the summits of which, at least partially, lack sharp outlines, but are neither clearly fibrous (cirriform) nor in the form of an anvil; Cumulus, Stratocumulus or Stratus may also be present | |
4 |
Stratocumulus cumulogenitus |
4 |
Stratocumulus formed by the spreading out of Cumulus; Cumulus may also be present | |
5 |
Stratocumulus other than Stratocumulus cumulogenitus |
5 |
Stratocumulus not resulting from the spreading out of Cumulus | |
6 |
Stratus nebulosus or Stratus fractus other than of bad weather,* or both |
6 |
Stratus in a more or less continuous sheet or layer, or in ragged shreds, or both, but no Stratus fractus of bad weather* | |
7 |
Stratus fractus or Cumulus fractus of bad weather,* or both (pannus), usually below Altostratus or Nimbostratus |
7 |
Stratus fractus of bad weather* or Cumulus fractus of bad weather,* or both (pannus), usually below Altostratus or Nimbostratus | |
8 |
Cumulus and Stratocumulus other than Stratocumulus cumulogenitus, with bases at different levels |
8 |
Cumulus and Stratocumulus other than that formed from the spreading out of Cumulus; the base of the Cumulus is at a different level from that of the Stratocumulus | |
9 |
Cumulonimbus capillatus (often with an anvil), with or without Cumulonimbus calvus, Cumulus, Stratocumulus, Stratus or pannus |
9 |
Cumulonimbus, the upper part of which is clearly fibrous (cirriform), often in the form of an anvil; either accompanied or not by Cumulonimbus without anvil or fibrous upper part, by Cumulus, Stratocumulus, Stratus or pannus | |
/ |
CL clouds invisible owing to darkness, fog, blowing dust or sand, or other similar phenomena |
/ |
Stratocumulus, Stratus, Cumulus and Cumulonimbus invisible owing to darkness, fog, blowing dust or sand, or other similar phenomena |
* 'Bad weather' denotes the conditions which generally exist during precipitation and a short time before and after.
Table 0515 (WMO-No. 306, Vol I.1)
CM
Clouds of the genera Altocumulus, Altostratus and Nimbostratus
Code figure |
Technical specifications |
|
Code figure |
Non-technical specifications |
0 |
No CM clouds |
0 |
No Altocumulus, Altostratus or Nimbostratus | |
1 |
Altostratus translucidus |
1 |
Altostratus, the greater part of which is semitransparent; through this part the sun or moon may be weakly visible, as through ground glass | |
2 |
Altostratus opacus or Nimbostratus |
2 |
Altostratus, the greater part of which is sufficiently dense to hide the sun or moon, or Nimbostratus | |
3 |
Altocumulus translucidus at a single level |
3 |
Altocumulus, the greater part of which is semitransparent; the various elements of the cloud change only slowly and are all at a single level | |
4 |
Patches (often lenticular) of Altocumulus translucidus, continually changing and occurring at one or more levels |
4 |
Patches (often in the form of almonds or fish) of Altocumulus, the greater part of which is semitransparent; the clouds occur at one or more levels and the elements are continually changing in appearance | |
5 |
Altocumulus translucidus in bands, or one or more layers of Altocumulus translucidus or opacus, progressively invading the sky; these Altocumulus clouds generally thicken as a whole |
5 |
Semi-transparent Altocumulus in bands, or Altocumulus, in one or more fairly continuous layer (semi-transparent or opaque), progressively invading the sky; these Altocumulus clouds generally thicken as a whole | |
6 |
Altocumulus cumulogenitus (or cumulonimbogenitus) |
6 |
Altocumulus resulting from the spreading out of Cumulus (or Cumulonimbus) | |
7 |
Altocumulus translucidus or opacus in two or more layers, or Altocumulus opacus in a single layer, not progressively invading the sky, or Altocumulus with Altostratus or Nimbostratus |
7 |
Altocumulus in two or more layers, usually opaque in places, and not progressively invading the sky; or opaque layer of Aftocumulus, not progressively invading the sky; or Altocumulus together with Altostratus or Nimbostratus | |
8 |
Altocumulus castellanus or floccus |
8 |
Altocumulus with sproutings in the form of small towers or battlements, or Altocumulus having the appearance of cumuliform tufts | |
9 |
Altocumulus of a chaotic sky, generally at several levels |
9 |
Altocumulus of a chaotic sky, generally at several levels | |
/ |
Cm clouds invisible owing to darkness, fog, blowing dust or sand, or other similar phenomena, or because of continuous layer of lower clouds |
/ |
Altocumulus, Altostratus and Nimbostratus invisible owing to darkness, fog, blowing dust or sand, or other similar phenomena, or more often because of the presence of a continuous layer of lower clouds |
Table 0777 (WMO-No. 306, Vol I.1)
DtDt--DnDn
Dew-point depression in two figures
DtDt D0D0 D1D1 DnDn |
Dew-point depression at the tropopause level Dew-point depression at standard isobaric surfaces or at significant ... levels, starting with station level |
Code |
Degrees |
Code |
Degrees |
Code |
Degrees |
Code |
Degrees |
00 |
0.0 |
25 |
2.5 |
50 |
5 |
75 |
25 |
01 |
0.1 |
26 |
2.6 |
51 |
not used |
76 |
26 |
02 |
0.2 |
27 |
2.7 |
52 |
not used |
77 |
27 |
03 |
0.3 |
28 |
2.8 |
53 |
not used |
78 |
28 |
04 |
0.4 |
29 |
2.9 |
54 |
not used |
79 |
29 |
05 |
0.5 |
30 |
3.0 |
55 |
not used |
80 |
30 |
06 |
0.6 |
31 |
3.1 |
56 |
6 |
81 |
31 |
07 |
0.7 |
32 |
3.2 |
57 |
7 |
82 |
32 |
08 |
0.8 |
33 |
3.3 |
58 |
8 |
83 |
33 |
09 |
0.9 |
34 |
3.4 |
59 |
9 |
84 |
34 |
10 |
1.0 |
35 |
3.5 |
60 |
10 |
85 |
35 |
11 |
1.1 |
36 |
3.6 |
61 |
11 |
86 |
36 |
12 |
1.2 |
37 |
3.7 |
62 |
12 |
87 |
37 |
13 |
1.3 |
38 |
3.8 |
63 |
13 |
88 |
38 |
14 |
1.4 |
39 |
3.9 |
64 |
14 |
89 |
39 |
15 |
1.5 |
40 |
4.0 |
65 |
15 |
90 |
40 |
16 |
1.6 |
41 |
4.1 |
66 |
16 |
91 |
41 |
17 |
1.7 |
42 |
4.2 |
67 |
17 |
92 |
42 |
18 |
1.8 |
43 |
4.3 |
68 |
18 |
93 |
43 |
19 |
1.9 |
44 |
4.4 |
69 |
19 |
94 |
44 |
20 |
2.0 |
45 |
4.5 |
70 |
20 |
95 |
45 |
21 |
2.1 |
46 |
4.6 |
71 |
21 |
96 |
46 |
22 |
2.2 |
47 |
4.7 |
72 |
22 |
97 |
47 |
23 |
2.3 |
48 |
4.8 |
73 |
23 |
98 |
48 |
24 |
2.4 |
49 |
4.9 |
74 |
24 |
99 |
49 |
// No humidity data available
Table 1600 (WMO-No. 306, Vol I.1)
h
- Height above surface of the base of the lowest cloud seen
Code Figure |
|
0 | 0 to 50 m |
1 | 50 to 100 m |
2 | 100 to 200 m |
3 | 200 to 300 m |
4 | 300 to 600 m |
5 | 600 to 1000 m |
6 | 1000 to 1500 m |
7 | 1500 to 2000 m |
8 | 2000 to 2500 m |
9 | 2500 m or more, or no clouds |
/ | Height of base of cloud not known or base of clouds at a level lower and tops at a level higher than that of the station. |
Notes:
(1) A height of exactly equal to one of the values at the ends of the ranges shall be coded in the higher range, e.g., a height of 600 m shall be reported by code Figure 5.
(2) Due to the limitation in range of the cloud-sensing equipment used by an automatic station, the code figures reported for h could have one of the three following meanings:
(a) The actual height of the base of the cloud is within the range indicated by the code figure; or
(b) the height of the base of the cloud is greater than the range indicated by the code figure but cannot be determined due to instrumental limitations; or
(c) There are no clouds vertically above the station.
Table 1734 (WMO-No. 306, Vol I.1)
Id-
Indicator used to specify the hundreds of hectopascals figure (in Part A of
TEMP, TEMP SHIP, TEMP DROP and TEMP MOBIL reports) or tens of hectopascals
figure (in Part C of TEMP, TEMP SHIP, and TEMP MOBIL reports) of the pressure
relative to the last standard isobaric surface for which the wind is reported.
Code Figure |
Wind group included up to and including the following standard isobaric surfaces: |
Part A | Part C | |
1 | 100 hPa or 150 hPa* | 10 hPa |
2 | 200 hPa or 250 hPa** | 20 hPa |
3 | 300 hPa | 30 hPa |
4 | 400 hPa | --- |
5 | 500 hPa | 50 hPa |
6 | --- | --- |
7 | 700 hPa | 70 hPa |
8 | 850 hPa | --- |
9 | 925 hPa | --- |
0 | 1000 hPa | --- |
/ | No wind group is included for any standard isobaric surface |
_____________
* In this case (150 hPa), the wind group relating to the
100-hPa level shall also be included and coded as ///// except when 150 hPa is
the highest standard isobaric surface reached by the sounding.
** In this case (250 hPa), the wind group relating to the 200 hPa level shall also be included and coded as ///// except when 250 hPa is the highest standard isobaric surface reached by the sounding.
Table 1845 (WMO-No. 306, Vol I.1
im-
Indicator for Units of Elevation and Confidence Factor for Accuracy of Elevation
Code Figure |
Units | Confidence Factor |
0 | Not Used | |
1 | Meters | Excellent (within 3 meters) |
2 | Meters | Good (within 10 meters) |
3 | Meters | Fair (within 20 meters) |
4 | Meters | Poor (more than 20 meters) |
5 | Feet | Excellent (within 10 feet) |
6 | Feet | Good (within 30 feet) |
7 | Feet | Fair (within 60 feet) |
8 | Feet | Poor (more than 60 feet) |
9 | Not Used |
Table 2582 (WMO-No. 306, Vol I.1)
MiMi--MjMj
MiMi | Identification letters of the report |
MjMj | Identification letters of the part of the report or the version of the code form |
Literal (MiMi/MjMj) Designators for Data Type and Message Part
Code Type | PART A | PART B | PART C | PART D | RADAT |
PILOT |
PP |
PPAA |
PPBB |
PPCC |
PPDD |
PILOT SHIP |
QQ |
QQAA |
QQBB |
QQCC |
QQDD |
PILOT MOBIL |
EE |
EEAA |
EEBB |
EECC |
EEDD |
TEMP |
TT TTXX |
TTAA |
TTBB |
TTCC |
TTDD |
TEMP SHIP |
UU UUXX |
UUAA |
UUBB |
UUCC |
UUDD |
TEMP MOBIL |
II IIXX |
IIAA |
IIBB |
IICC |
IIDD |
Table 2590 (WMO No.-306, Vol I.1)
MMM Number of Marsden square in which the station is
situated at the time of observation
Figure E-1: Assignment of Marsden Square numbers.
WEST |
EAST |
|||||||||||||||||||||
99 | 98 | 97 | 96 | 95 | 94 | 93 | 92 | 91 | 90 | 90 | 91 | 92 | 93 | 94 | 95 | 96 | 97 | 98 | 99 | N O R T H | ||
89 | 80 | 80 | 89 | |||||||||||||||||||
79 | 70 | 70 | 79 | |||||||||||||||||||
69 | 60 | 60 | 69 | |||||||||||||||||||
59 | 50 | 50 | 59 | |||||||||||||||||||
49 | 40 | 40 | 49 | |||||||||||||||||||
39 | 30 | 30 | 39 | |||||||||||||||||||
29 | 20 | 20 | 29 | |||||||||||||||||||
19 | 10 | 10 | 19 | |||||||||||||||||||
09 | 08 | 07 | 06 | 05 | 04 | 03 | 02 | 01 | 00 | 00 | 01 | 02 | 03 | 04 | 05 | 06 | 07 | 08 | 09 | |||
QC = 7 |
QC = 1 |
|||||||||||||||||||||
09 | 08 | 07 | 06 | 05 | 04 | 03 | 02 | 01 | 00 | 00 | 01 | 02 | 03 | 04 | 05 | 06 | 07 | 08 | 09 | S O U T H | ||
19 | 10 | 10 | 19 | |||||||||||||||||||
29 | 20 | 20 | 29 | |||||||||||||||||||
39 | 30 | 30 | 39 | |||||||||||||||||||
49 | 40 | 40 | 49 | |||||||||||||||||||
59 | 50 | 50 | 59 | |||||||||||||||||||
69 | 60 | 60 | 69 | |||||||||||||||||||
79 | 70 | 70 | 79 | |||||||||||||||||||
89 | 80 | 80 | 89 | |||||||||||||||||||
99 | 98 | 97 | 96 | 95 | 94 | 93 | 92 | 91 | 90 | 90 | 91 | 92 | 93 | 94 | 95 | 96 | 97 | 98 | 99 | |||
QC = 5 |
QC = 3 |
Figure E-3: Subdivisions of the Marsden 10-degree
squares into one-degree squares
for the eight octants (Q) of the globe.
Note: The number to be coded for ULAULO in the position verifying group MMMULAULO is obtained by combining the second figure for La and the third figure for Lo in the reported position (LaLaLaQCLoLoLoLo) This number ULAULO is the number of the one-degree subdivision of the Marsden 10-degree square in which the ship is located at the time of observation.
When the ship is on the boundary between two (or four) 10-degree Marsden squares, the number to be coded for MMM is that of the Marsden 10-degree square for which the one-degree subdivision whose number is ULAULO, as defined above, corresponds to the ship's position.
When the ship is on the meridian 0 or 180, as well as on the Equator, the number used for reporting QC shall be taken into account for determining the relevant number of the Marsden 10-degree square.
Examples: | |
(1) |
For a ship located at 42.3N and 30.0W, the position is coded as follows: |
(2) |
For a ship located at 40.0S and 120.0E, the position is coded as follows: |
Table 2700 (WMO-No. 306, Vol I.1)
N Total cloud cover
NhAmount
of all the CLcloud present or,
if no CLcloud is present, the
amount of all the CMcloud
present
NsAmount
of individual cloud layer or mass whose genus is indicated by C
N' Amount of cloud whose base is below the level of the station
Code figure |
||
0 1 2 3 4 5 6 7 8 |
0 1 okta or less, but not zero 2 oktas 3 oktas 4 oktas 5 oktas 6 oktas 7 oktas or more, but not 8 oktas 8 oktas |
0 1/10 or less, but not zero 2/10 - 3/10 4/10 5/10 6/10 7/10 - 8/10 9/10 or more, but not 10/10 10/10 |
9 / |
Sky obscured by fog and/or other meteorological phenomena Cloud cover is indiscernible for reasons other than fog or other meteorological phenomena, or observation is not made |
Note: For use of (/), see WMO Regulation 12.1.4, Ref. 7.
Table 3333 (WMO-No. 306, Vol I.1)
Qc
Quadrant of the globe
Code figure |
Latitude | Longitude |
1 3 5 7 |
North South South North |
East East West West |
Note : -- |
The choice is left to the observer in the
following cases: When the ship is on the Greenwich meridian or the 180th meridian (LOLOLOLO = 0000 or 1800 respectively): QC = 1 or 7 (northern hemisphere) or QC = 3 or 5 (southern hemisphere); |
|
-- | When the ship is on the Equator (LaLaLa.,
= 000): Qc = 1 or 3 (eastern longitude) or Qc = 5 or 7 (western longitude) |
Table 3685 (WMO-No. 306, Vol I.1)
(Table
0 02 011 WMO-No. 306, Vol I Part B)
rara
- Radiosonde/sounding system used
Code |
Meaning |
00 |
Reserved |
01 |
Reserved |
02 |
No radiosonde/Passive target (e.g. reflector) |
03 |
No radiosonde/Active target (e.g. transponder) |
04 |
No radiosonde/Passive temperature-humidity profiler |
05 |
No radiosonde/Active temperature-humidity profiler |
06 |
No radiosonde/Radio-acoustic sounder |
07 |
No radiosonde/...)reserved |
08 |
No radiosonde/...)reserved |
09 |
No radiosonde/Sounding system unknown or not specified |
10 |
RS VIZ type A pressure-commutated (USA) |
11 |
RS VIZ type B time-commutated |
12 |
RS SDC (Space Data Corporation - USA) |
13 |
Astor (no longer made - Australia) |
14 |
VIZ MARK I MICROSONDE (USA) |
15 |
EEC Company Type 23 (USA) |
16 |
Elin (Austria) |
17 |
Graw G. (Germany) |
18 |
Reserved for allocation of radiosondes |
19 |
Graw M60 (Germany) |
20 |
Indian Meteorological Service MK3 (India) |
21 |
VIZ/Jin Yang Mark I MICROSONDE (South Korea) |
22 |
Meisei RS2-80 (Japan) |
23 |
Mesural FMO 1950A (France) |
24 |
Mesural FMO 1945A (France) |
25 |
Mesural MH73A (France) |
26 |
Meteolabor Basora (Switzerland) |
27 |
AVK-MRZ (Russian Federation) |
28 |
Meteorite Marz2-1 (Russian Federation) |
29 |
Meteorite Marz2-2 (Russian Federation) |
30 |
Oki RS2-80 (Japan) |
31 |
VIZ/Valcom type A pressure-commutated (Canada)Sangamo |
32 |
Shanghai Radio (China) |
33 |
UK Met Office MK3 (UK) |
34 |
Vinohrady (Czechoslovakia) |
35 |
Vaisala RS18 (Finland) |
36 |
Vaisala RS21 (Finland) |
37 |
Vaisala RS80 (Finland) |
38 |
VIZ LOCATE Loran-C (USA) |
39 |
Sprenger E076 (Germany) |
40 |
Sprenger E084 (Germany) |
41 |
Sprenger E085 (Germany) |
42 |
Sprenger E086 (Germany) |
43 |
AIR IS-4A-1680 (USA) |
44 |
AIR IS-4A-1680 X (USA) |
45 |
RS MSS (USA) |
Table 3685 (WMO-No. 306, Vol I.1)
(Table
0 02 011 WMO-No. 306, Vol I Part B) (Continued)
rara
- Radiosonde/sounding system used
46 |
Air IS-4A-403 (USA) |
|
47 |
Meisei RS2-91 (Japan) |
|
48 |
VALCOM (Canada) |
|
49 |
VIZ MARK II (USA) |
|
50 |
GRAW DFM-90 (Germany) |
|
51 |
VIZ B2 |
|
52 |
Vaisala RS80-57 |
|
53 |
Reserved for allocation of radiosondes |
|
54 |
Reserved for allocation of radiosondes |
|
55 |
Reserved for allocation of radiosondes |
|
56 |
Reserved for allocation of radiosondes |
|
57 |
Reserved for allocation of radiosondes |
|
58 |
Reserved for allocation of radiosondes |
|
59 |
Reserved for allocation of radiosondes |
|
60 |
Vaisala RS80/MicroCora (Finland) |
|
61 |
Vaisala RS80/DigiCora or Marwin (Finland) |
|
62 |
Vaisala RS80/PCCora (Finland) |
|
63 |
Vaisala RS80/Star (Finland) |
|
64 |
Orbital Sciences Corporation, Space Data Division, transponder radiosonde, type 909-11-XX, where XX correspondes to the model of the instrument (USA) |
|
65 |
VIZ transponder radiosonde, model number 1499-520 (USA) |
|
|
|
|
66-89 |
Reserved for additional automated soundings systems |
|
|
|
|
90 |
Radiosonde not specified or unknown |
|
91 |
Pressure-only radiosonde |
|
92 |
Pressure-only radiosonde plus transponder |
|
93 |
Pressure-only radiosonde plus radar reflector |
|
94 |
No-pressure radiosonde plus transponder |
|
95 |
No-pressure radiosonde plus radar reflector |
|
96 |
Descending radiosonde |
|
|
|
|
97-99 |
Reserved for allocation of sounding systems with incomplete sondes |
|
|
|
|
100 |
|
|
... |
Reserved |
BUFR Table 002011 only |
... |
|
|
254 |
|
|
255 |
Missing value |
|
NOTES:
(1) References to countries in brackets indicate the manufacturing location rather than the country using the instrument.
(2) Some of the radiosondes listed are no longer in use but are retained for archiving purposes.
Table 3845 (WMO-No. 306 Vol I.1)
sn |
Sign of the data, and relative humidity indicator |
sn |
Sign of the exponent |
sn |
Sign of the reference value indicated by rrrrrrr |
Code
figure
0 | Positive or zero |
1 | Negative |
2 | Relative humidity follows |
Notes:
(1) Code figures 3 to 8 are not used.
(2) See
WMO Regulation 12.2.3.3.1 for the use of code figure 9.
Table 3849 (WMO-No. 306, Vol I.1)
(Table
0 02 013 WMO-No. 306, Vol I Part B)
sr- Solar and Infrared Radiation Correction
Code Figure |
Meaning |
0 1 2 3 4 5 6 7 8-14* 15* |
No correction CIMO solar corrected and CIMO infrared corrected CIMO solar corrected and infrared corrected CIMO solar corrected only Solar and infrared corrected automatically by radiosonde system Solar corrected automatically by radiosonde system Solar and infrared corrected as specified by country Solar corrected as specified by country Reserved Missing Value |
* BUFR Table 0 02 012 only
Table 3872 (WMO-No. 306, Vol I.1)
(Table 0 02 014
WMO-No. 306, Vol I Part B)
sasa - Tracking
Technique/Status of System Used
Code |
|
00 |
No windfinding |
01 |
Automatic with auxiliary optical direction finding |
02 |
Automatic with auxiliary radio direction finding |
03 |
Automatic with auxiliary ranging |
04 |
Not used |
05 |
Automatic with multiple VLF-Omega frequencies |
06 |
Automatic cross chain Loran-C |
07 |
Automatic with auxiliary wind profiler |
08 |
Automatic satellite navigation |
09-18 |
Reserved |
19 |
Tracking technique not specified |
Tracking Technique/Status of ASAP System | |
20 |
Vessel stopped |
21 |
Vessel diverted from original destination |
22 |
Vessel's arrival delayed |
23 |
Container damaged |
24 |
Power failure to container |
25-28 |
Reserved for future use |
29 |
Other problems |
Sounding System | |
30 |
Major power problems |
31 |
UPS inoperative |
32 |
Receiver hardware problems |
33 |
Receiver software problems |
34 |
Processor hardware problems |
35 |
Processor software problems |
36 |
NAVAID system damaged |
37 |
Shortage of lifting gas |
38 |
Reserved |
39 |
Other problems |
Launch Facilities | |
40 |
Mechanical defect |
41 |
Material defect (Hand launcher) |
42 |
Power failure |
43 |
Control failure |
44 |
Pneumatic/hydraulic failure |
45 |
Other problems |
46 |
Compressor problems |
47 |
Balloon problems |
48 |
Balloon release problems |
49 |
Launcher damaged |
Table 3872 (WMO-No. 306, Vol I.1) (Continued)
(Table
0 02 014 WMO-No. 306, Vol I Part B)
sasa - Tracking
Technique/Status of System Used
Code |
|
Data Acquisition Systems | |
50 |
R/S receiver antenna defect |
51 |
NAVAID antenna defect |
52 |
R/S receiver cabling (antenna) defect |
53 |
NAVAID antenna cabling defect |
54-58 |
Reserved |
59 |
Other problems |
Communications | |
60 |
ASAP communications defect |
61 |
Communications facility rejected data |
62 |
No power at transmitting antenna |
63 |
Antenna cable broken |
64 |
Antenna cable defect |
65 |
Message transmitted power below normal |
66-68 |
Reserved |
69 |
Other problems |
70 |
All systems in normal operation |
71-98 |
Reserved |
99 |
Status of system and its components not specified |
100-126 |
Reserved |
127 |
Missing value |
Table 3931 (WMO-No. 306, Vol I.1)
Ta -- Tc
Encoding/Decoding the Sign
and Tenths Value of the Air Temperature in
Radiosonde Reports
Code Figures
Tenths Figure |
|
|
|
0 |
} |
0 |
1 |
2 |
} |
2 |
3 |
4 |
} |
4 |
5 |
6 |
} |
6 |
7 |
8 |
} |
8 |
9 |
Table 5300 (WMO-No. 306, Vol. I.1)
Standard Heights of Isobaric Surfaces
(Based on
U.S. Standard Atmosphere - 1976)
Standard |
PnPn |
Approximate |
hnhnhn |
1000 |
00 |
100 |
100 |
925 |
92 |
750 |
750 |
850 |
85 |
1500 |
500 |
700 |
70 |
3000 |
000 |
500 |
50 |
5600 |
560 |
400 |
40 |
7200 |
720 |
300 |
30 |
9200 |
920 |
250 |
25 |
10400 |
040 |
200 |
20 |
11800 |
180 |
150 |
15 |
13600 |
360 |
100 |
10 |
16200 |
620 |
70 |
70 |
18500 |
850 |
50 |
50 |
20600 |
060 |
30 |
30 |
23900 |
390 |
20 |
20 |
26500 |
650 |
10 |
10 |
31100 |
110 |
7 |
07 |
33400 |
340 |
5 |
05 |
35800 |
580 |
3 |
03 |
39400 |
940 |
2 |
02 |
42400 |
240 |
1 |
01 |
47800 |
780 |
Appendix E-II
Appendix F
Table of Contents
Publications List
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