Data Access for 2A23: http://disc.sci.gsfc.nasa.gov/data/datapool/TRMM_DP/01_Data_Products/01_Orbital/07_Rain_Type_2A_23/ Contents of the TRMM Precipitation Radar Rain Characteristics This document provides basic information on 2A23, TRMM PR Rain Characteristics Product. The TRMM Precipitation Radar (PR), the first of its kind in space, is an electronically scanning radar, operating at 13.8 GHz that measures the 3-D rainfall distribution over both land and ocean, and defines the layer depth of the precipitation. The PR qualitative algorithm (2A23) inputs PR reflectivities (1C21) and returns a rain/no rain decision based on echo structure. When rain is present, a storm height is calculated. If a bright band is detected, the height of the bright band is also given. PR Level 1A ==> 1B21 PR Power ==> 1C21 PR Reflectivities ==> 2A23 PR Rain Characteristics The data flow of all products are shown in Satellite Algorithm Flow Diagram. Data Characteristics TRMM 2A23 Data Characteristics | | | Pre-boost (before 2001-08-07) | Post-boost (after 2001-08-24) | | Temporal Coverage | Start Date: 1997-12-08 Stop Date: 2001-08-07 | Start Date: 2001-08-24 Stop Date: - | | Geographic Coverage | Latitude: 38°S - 38°N Longitude:180°W - 180°E | Latitude: 38°S - 38°N Longitude:180°W - 180°E | | Temporal Resolution | About 91.5 minutes per orbit About 16 orbits per day More information about revisit frequency | About 92.5 minutes per orbit About 16 orbits per day More information about revisit frequency | | Horizontal Resolution | 4.3 km | 5.0 km | | Scan Characteristics | Swath Width: 215 km Rays/Scan: nray = 49 Scans/Second (SS): 1/0.6 Seconds/Orbit (SO): 5490 Average Scans/Orbit: nscan = SS*SO = 9150 | Swath Width: 247 km Rays/Scan: nray = 49 Scans/Second (SS): 1/0.6 Seconds/Orbit (SO): 5550 Average Scans/Orbit: nscan = SS*SO = 9250 | | Average File Size | Compressed: ~6.2 MB Original: ~13.6 MB | Compressed: ~6.3 MB Original: ~13.8 MB | | File Type | HDF | HDF | Data Format Structure Further information on the contents and structure of the 2A23 product can be found in Volume 4 of the "File Specifications for TSDIS Products - Level 2 and Level3" . | Data Format Structure for 2A23, PR Rain Characteristics | | Name | Type | Record Size (byte) | Dim Size/ # of Records | Scaled by | Range | Unit | Description | | ECS Core Metadata | Char Attribute | 10,000 | - | - | - | - | ECS Core Metadata | | PS Metadata | Char Attribute | 10,000 | - | - | - | - | Product Specific Metadata | | Swath Structure | Char Attribute | 5,000 | - | - | - | - | The specification of the swath geometry | | Scan Time | Vdata Table | 8 | nscan | - | - | - | The time associated with the scan, expressed as 8-byte float UTC second of the day. | | Geolocation | Float SDS | 4 | 2*nray*nscan | - | - | degree | The earth location of the center of the IFOV at the altitude of the earth ellipsoid. The first dimension is latitude and longitude, in that order. The next dimensions are numbers of pixels and scans. | | Scan Status | Vdata Table | 15 | nscan | - | - | - | The status of each scan. | | Navigation | Vdata Table | 88 | nscan | - | - | - | Spacecraft geocentric information | | Rain Flag | Integer SDS | 1 | nray*nscan | - | - | - | The rain flag is identical to the Minimum Echo Flag of 1C21. 0: no rain 10: rain possible 11: rain possible (echo greater than rain threshold #1 in clutter region) 12: rain possible (echo greater than rain threshold #2 in clutter region) 13: rain possible 15: rain possible 20: rain certain | | Rain Type | Integer SDS | 2 | nray*nscan | - | - | - | The Rain Type Flag. | | Shallow Rain Flag | Integer SDS | 1 | nray*nscan | - | - | - | The Warm Rain Flag is set as follows: = 10: maybe shallow, isolated = 11: shallow isolated (with confidence) = 20: maybe shallow but not isolated = 21: shallow but not isolated (with confidence) = 0: when not shallow < 0: when not rain certain or data missing | | Status Flag | Integer SDS | 1 | nray*nscan | - | - | - | The Status Flag indicates whether the data are obtained over sea or land and the confidence. | | Height of Bright Band | Integer SDS | 2 | nray*nscan | - | - | - | A positive Height of Bright Band is defined in meters above mean sea level. Negative values are defined as follows: -1111: No bright band -8888: No rain -9999: Data missing. | | Bright Band Intensity | Integer SDS | 4 | nray*nscan | - | - | - | The maximum value of the bright band (dBZ) obtained from normal samples. The range is from 0.00 to 100.0 dBZ. Negative values are defined as: -1111: No bright band -8888: No rain -9999: Data missing. | | Bright Band Peak Bin | Integer SDS | 2 | nray*nscan | - | - | - | A positive range bin number that corresponds to the peak of the bright band. This bin number is in the Level-1 bin numbering scheme (125m, see Level-1 PR description). Negative values are defined as: -1111: No bright band -8888: No rain | | Bright Band Boundary | Integer SDS | 2 | 2*nray*nscan | - | - | - | Positive bin number of the boundary of the bright band. The first index indicates the bottom. This bin number are in the Level-1 bin numbering scheme (125m, see Level-1 PR description). Negative values are defined as: -1111: No bright band -8888: No rain | | Bright Band Width | Integer SDS | 2 | nray*nscan | - | - | - | The width of the bright band in meters.Negative values are defined as: -1111: No bright band -8888: No rain | | Bright Band Status | Integer SDS | 2 | nray*nscan | - | - | - | Indicates the status of the bright band detection. This flag is a composite of three internal status flags: BB_status[j] = BB_detection_status * 16 + BB_boundary_status[j] * 4 + BB_width_status[j] where each status on the right hand side takes the following values: 1: poor, 2: fair, 3: good. | | Height of Freezing Level | Integer SDS | 2 | nray*nscan | - | - | - | A positive Height of Freezing Level is the height of the 0°C isotherm above mean sea level in meters, estimated from climatological surface temperature data. Negative values are defined as: -5555: When error occurred in the estimation of Height of Freezing Level -8888: No rain -9999: Data missing | | Height of Storm | Integer SDS | 2 | nray*nscan | - | - | m | A positive Height of Storm is the height of the storm top above mean sea level in meters. A positive Height of Storm is given only when rain is present with a high degree of confidence in 1C21 (i.e., the Minimum Echo Flag in 1C21 has the value of 2 [rain certain]). Negative values are defined as: -1111: Height of Storm not calculated because rain is not present with a high level of confidence in 1C21 -8888: No rain -9999: Data missing | | Spare | Float SDS | 2 | nray*nscan | - | - | - | Spare will characterize the width of the bright band. Since this characterization requires much research, the meaning is not disclosed. | TRMM 2A23 can be accessed and ordered using the Goddard DAAC's TRMM Data Search and Order System at http://disc.sci.gsfc.nasa.gov/data/datapool/TRMM_DP/01_Data_Products/01_Orbital/07_Rain_Type_2A_23/ . Appendix TRMM 2A23 Rain Type Flag | | Value | Meaning | Conditions | | 100 | Stratiform certain | When R_type_V = T_stra; (BB exists) and R_type_H = T_stra; | | 110 | Stratiform certain | When R_type_V = T_stra; (BB exists) and R_type_H = T_others; | | 120 | Probably stratiform | When R_type_V = T_others; and R_type_H = T_stra; | | 130 | Maybe stratiform | When R_type_V = T_stra; (BB detection certain) and R_type_H = T_conv; | | 140 | Maybe stratiform or maybe transition or something else | When R_type_V = T_others; (BB hardly expected) and R_type_H = T_stra; | | 152 | Maybe stratiform | Shallow isolated (type of warm rain) is detected When R_type_V = T_others; R_type_H = T_stra; and shallowRain = 20 or 21; | | 160 | Maybe stratiform, but rain hardly expected near surface | BB may exist but is not detected When R_type_V = T_others; R_type_H = T_stra; | | 170 | Maybe stratiform, but rain hardly expected near surface | BB hardly expected. Maybe cloud only When R_type_V = T_others; R_type_H = T_stra; | | 200 | Convective certain | When R_type_V = T_conv; (no BB) and R_type_H = T_conv; | | 210 | Convective certain | When R_type_V = T_others; and R_type_H = T_conv; | | 220 | Convective certain | When R_type_V = T_conv; and R_type_H = T_others; | | 230 | Probably convective | When R_type_V = T_conv; (BB exists) and R_type_H = T_conv; | | 240 | Maybe convective | When R_type_V = T_conv; and R_type_H = T_stra; | | 251 | Convective | Shallow isolated is detected When R_type_V = T_conv, R_type_H = T_conv and shallowRain = 10 or 11; | | 252 | Convective | Shallow rain (non-isolated) is detected When R_type_V = T_conv, R_type_H = T_conv and shallowRain = 20 or 21; | | 261 | Convective | Shallow isolated is detected When R_type_V = T_conv; R_type_H = T_others; and shallowRain = 10 or 11; | | 262 | Convective | Shallow rain (non-isolated) is detected. When R_type_V[i] = T_conv, R_type_H[i] = T_others; and shallowRain[i] = 20 or 21; | | 271 | Convective | Shallow isolated is detected When R_type_V = T_others; R_type_H = T_conv; and shallowRain = 10 or 11; | | 272 | Convective | Shallow isolated is detected When R_type_V = T_others; R_type_H = T_conv; and shallowRain = 20 or 21; | | 281 | Convective | Shallow isolated is detected When R_type_V = T_conv; R_type_H = T_stra; and shallowRain = 10 or 11; | | 282 | Convective | Shallow rain (non-isolated) is detected. When R_type_V[i] = T_conv, R_type_H[i] = T_stra; and shallowRain[i] = 20 or 21; | | 291 | Convective | Shallow isolated is detected When R_type_V = T_others; R_type_H = T_stra; and shallowRain = 10 or 11; | | 300 | Others | When R_type_V = T_others; and R_type_H = T_others; | | 312 | Others | Shallow rain (non-isolated) is detected When R_type_V = T_others, R_type_H = T_others; and shallowRain = 20 or 21; | | 313 | Others | If sidelobe clutter were not rejected, shallow isolated would be detected When R_type_V = T_others, R_type_H = T_others; and shallowRain = 20 or 21; |
where
R_type_V: rain type classified by the V-profile method,
R_type_H: rain type classified by the H-pattern method,
which is based on SHY95 developed by Prof.
Houze and his group.
The above assignment of numbers has the following meaning:
(merged) Rain Type / 100 = 1: stratiform,
2: convective,
3: others.
(merged) Rain Type Flag % 100 = Sub-category,
(merged) Rain Type Flag % 10 = 0: usual,
1: shallow isolated,
2: shallow non-isolated,
3: sidelobe clutter only (once shallow isolated
overwritten as sidelobe clutter only).
rainTytpe % 10 = 3 occurs for type 313 only.
where Rain Type Flag % 10 means MOD (Rain Type, 10) in FORTRAN.
Though rainType is changed to int16, no rain and missing values remain the same, that is
-88: no rain
-99: data missing
| TRMM 2A23 Status Flag | | Value | Meaning | Where | | 0 | good | over ocean | | 10 | BB detection may be good | over ocean | | 20 | R-type classification may be good (BB detection is good or BB does not exist) | over ocean | | 30 | Both BB detection and R-type classification may be good | over ocean | | 50 | not good (because of warnings) | over ocean | | 100 | bad (possible data corruption) | over ocean | | 1 | good | over land | | 11 | BB detection may be good | over land | | 21 | R-type classification may be good (BB detection is good or BB does not exist) | over land | | 31 | Both BB detection and R-type classification may be good | over land | | 51 | not good (because of warnings) | over land | | 101 | bad (possible data corruption) | over land | | 2 | good | over coastline | | 12 | BB detection may be good | over coastline | | 22 | R-type classification may be good (BB detection is good or BB does not exist) | over coastline | | 32 | Both BB detection and R-type classification may be good | over coastline | | 52 | not good (because of warnings) | over coastline | | 102 | bad (possible data corruption) | over coastline | | 4 | good | over inland lake | | 14 | BB detection may be good | over inland lake | | 24 | R-type classification may be good (BB detection is good or BB does not exist) | over inland lake | | 34 | Both BB detection and R-type classification may be good | over inland lake | | 54 | not good (because of warnings) | over inland lake | | 104 | bad (possible data corruption) | over inland lake | | 9 | may be good | land/sea unknown | | 19 | BB detection may be good | land/sea unknown | | 29 | R-type classification may be good (BB detection is good or BB does not exist) | land/sea unknown | | 39 | Both BB detection and R-type classification may be good | land/sea unknown | | 59 | not good (because of warnings) | land/sea unknown | | 109 | bad (possible data corruption) | land/sea unknown |
When it is "no rain" or "data missing", Status Flag contains the following values:
-88: no rain
-99: data missing
Assignment of the above numbers are based on the following rules:
When Status >= 0
Status/100 = 0: good, may be good, or not good
1: doubtful
(Status/10) % 10 = 0: good, may be good when status < 100,
and not good when status >= 100
1: BB detection not so confident
2: R-type classification not so confident
(but BB detection is good, or when BB does not exist)
3: BB detection is not so confident and R-type
classification not so confident
5: Over-all quality of the processed data for the j-th
scan angle is not good (but may not be too bad to be
classified as bad data)
Status % 10 = 0: over ocean
1: over land
2: over coastline
4: over inland lake
9: land/sea unknown
In other words, we can check the confidence level of 2A-23 by the following way:
Status Flag >= 100 : bad (untrustworthy because of possible data corruption)
100 > Status Flag >= 10 : result not so confident (warning)
Status Flag = 9 : may be good
9 > Status Flag >= 0 : good
The last digit of Status Flag indicates over ocean, land, etc.
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