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titleTable of Contents

Table of Contents
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History of modifications

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Version

Date

Description of modification

Chapters / Sections

1.0

31/03/2021

Initial version

1–6, References

1.1

07/09/2021

Clarification of PNPR-CLIM input data

2.1.2 – Table 10


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table1
table1
Table 1: AMSU-B and MHS radiometers' characteristics. QV = Quasi-vertical; polarization vector is parallel to the scan plane at nadir; QH = Quasi-horizontal; polarization vector is perpendicular to the scan plane at nadir.

AMSU-B

Advanced Microwave Sounding Unit-B

MHS

Microwave Humidity Sounder Unit

Satellites

AMSU-B: NOAA-15, NOAA-16, NOAA-17MHS: NOAA-18, NOAA-19, MetOp-A, MetOp-B

Mission

Humidity sounding in almost all-weather conditions and precipitation rate

Instrument type

Absorption-band MW radiometer/spectrometer - 5-channels

Scanning technique

Cross-track: 90 steps of 16 km at sub satellite point, swath 2180 km (2250 km) for MHS (AMSU-B) Along-track: one 16-km line every 8/3 s

Coverage/cycle

Near-global coverage twice/day

Resources

Mass: 63 kg – Power: 93 W – Data rate: 3.9 kbps

MHS/AMSU-B
Central frequency (GHz)

MHS/AMSU-B channel bandwidth (MHz)

MHS/AMSU-B channel polarisation

MHS/AMSU-B channel radiometric accuracy (NEΔT)

89.0

2800/1000

QV/QV

0.22/0.37 K

157.0/150.0

2800/1000

QV/QV

0.38/0.84 K

183.31 ± 3.0

2000/2000

QH/QV

0.42/0.60 K

183.31 ± 1.0

1000/500

QH/QV

0.57/0.70 K

190.311/183.31 ± 7

2000/1000

QV/QV

0.45/1.06 K


Other datasets used to develop and test the NN algorithm are:

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table2
table2
Table 2: Summary of channel characteristics of SSM/I instruments as described by Wentz (1991)

Centre Frequency [GHz]

Polarization

Pixel Integration Time [ms]

Samples per scan

Inter-Scan Period [s]

Along-track Sample Spacing [km]

3 dB Footprint Size
(Along-track
× Cross-track)
[km]

19.35

v/h

7.95

64

3.8

25

69 × 43

22.235

v

7.95

64

3.8

25

50 × 40

37.0

v

7.95

64

3.8

25

37 × 28

37.0

h

7.95

64

3.8

25

37 × 29

85.5

v/h

3.89

128

1.9

12.5

15 × 13

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table3
table3
Table 3: Summary of spacecraft's and SSM/I instrument's properties

Altitude

860 km

Inclination

98.8 °

Orbit Period

102 min

Swath Width

1394 km

Effective Scan Angle

102.4 °

Local Zenith Angle

53.1 °

Calibration Method

On board; each scan; fixed cold space reflector and reference black body hot load

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section1_2_2
section1_2_2
1.2.2 The SSMIS Instrument

The SSMIS is a 24-channel microwave radiometer using multiple frequencies and therefore is able to replace different former instruments namely SSM/I, Special Sensor Microwave Temperature (SSM/T), and Special Sensor Microwave Humidity Sounder (SSM/T-2). For precipitation retrieval the channels 12–18, with centre frequencies at 19.35, 22.235, 37.0 and 91.655 GHz, are of main interest here. Thus, SSMIS continues the measurements of the SSM/I instrument with a shift of SSM/I highest frequency channel from 85.5 to 91.655 GHz. Further channel characteristics are given in table 4.

Its first usage was aboard the F-16 spacecraft of the DMSP in October 2003. Further missions followed by F-17 (2006), F-18 (2009) and F-19 (2014). Like earlier satellites of the DMSP (see section 1.2.1) these ones are on a near-polar, sun-synchronous, circular orbits with a period of 101.8 minutes. Their local equator crossing occurred during 2–11 a.m./p.m.

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table4
table4
Table 4: Summary of SSMIS channel characteristics exploited in the precipitation retrieval

Channel

Centre Frequency [GHz]

Polarization

Pixel Integration Time [ms]

Samples per scan

Inter-Scan Period [s]

Along-track Sample Spacing [km]

3 dB Footprint Size
(Along-track
× Cross-track)
[km]

12

19.35

h

8.44

90

3.8

25

73.6 × 46.5

13

19.35

v

8.44

90

3.8

25

73.6 × 46.5

14

22.235

v

8.44

90

3.8

25

73.6 × 46.5

15

37.0

v

8.44

90

3.8

25

45.0 × 31.2

16

37.0

h

8.44

90

3.8

25

45.0 × 31.2

17

91.655

v

4.22

180

1.9

12.5

15.5 × 13.2

18

91.655

h

4.22

180

1.9

12.5

15.5 × 13.2

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table5
table5
Table 5: Summary of spacecraft's and instrument's properties for SSMIS

Altitude

833 km

Inclination

98.9 °

Orbit Period

101.8 min

Swath Width

1707 km

Effective Scan Angle

143.2 °

Local Zenith Angle

53.1 °

Calibration Method

On board; each scan; fixed cold space reflector and reference black body warm target


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section1_2_3
section1_2_3
1.2.3 The AMSR-E Instrument

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table6
table6
Table 6: Summary of channel characteristics for the AMSR-E instrument

Centre Frequency [GHz]

Bandwidth
[MHz]

Polarization

Pixel Integration Time [ms]

Scan cycle
[s]

Sampling Interval
[km]

IFOV
[km]

6.925

350

h/v

2.6

1.5

10 × 10

74 × 43

10.65

100

h/v

2.6

1.5

10 × 10

51 × 30

18.7

200

h/v

2.6

1.5

10 × 10

27 × 16

23.8

400

h/v

2.6

1.5

10 × 10

31 × 18

36.5

1000

h/v

2.6

1.5

10 × 10

14 × 8

89.0

3000

h/v

1.3

1.5

5 × 5

6 × 4

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table7
table7
Table 7: Summary of spacecraft's and instrument's properties for AMSR-E

Altitude

705 km

Inclination

98.2 °

Orbit Period

98.8 min

Swath Width

1445 km

Effective Scan Angle

122 °

Earth Incidence Angle

55 °

Calibration Method

On board; each scan; fixed cold space reflector and reference black body warm target

The IFOVs of AMSR-E and SSM/I / SSMIS were harmonized by averaging the brightness temperatures of each three neighbouring AMSR-E scan positions.

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table8
table8
Table 8: Summary of channel characteristics for the TMI instrument

Channel

Centre Frequency [GHz]

Polarization

Pixel Integration Time [ms]

EFOVs per scan

EFOV
(Along-track
× Cross-track)
[km]

Inter-Scan Period [s]

IFOV
(Along-track
× Cross-track)
[km]

1

10.65

v

6.6

104

63.2 × 9.1

6.6

59.0 × 35.7

2

10.65

h

6.6

104

63.2 × 9.1

6.6

60.1 × 36.4

3

19.35

v

6.6

104

30.4 × 9.1

6.6

30.5 × 18.4

4

19.35

h

6.6

104

30.4 × 9.1

6.6

30.1 × 18.2

5

21.3

v

6.6

104

22.6 × 9.1

6.6

27.2 × 16.5

6

37.0

v

6.6

104

16.0 × 9.1

6.6

16.0 × 9.7

7

37.0

h

6.6

104

16.0 × 9.1

6.6

16.0 × 9.7

8

85.5

v

3.3

108

7.2 × 4.6

3.3

6.7 × 4.1

9

85.5

h

3.3

108

7.2 × 4.6

3.3

6.9 × 4.2

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table9
table9
Table 9: Summary of spacecraft's and instrument's properties for TMI

Altitude

402 km

Inclination

35 °

Swath Width

758.5 km

Effective Scan Angle

130 °

Earth Incidence Angle

 52.8 °

Calibration Method

On board; each scan; fixed cold space reflector and reference black body warm target

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section2
section2
2 Input and Auxiliary Data

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section2_1
section2_1
2.1 PNPR-CLIM

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table10
table10
Table 10: Additional algorithm input variables. Sea ice information and snow cover information are Boolean masks derived from daily sea ice cover and snow depth variables, respectively.

Variable

Data source

Sea ice information (daily)

ECMWF ERA5

Snow cover information (daily)

ECMWF ERA5

2 m temperature (monthly)

ECMWF ERA5

Freezing level (monthly)

ECMWF ERA5

Sea ice cover (monthly)

ECMWF ERA5

Snow depth (monthly)

ECMWF ERA5

Total column integrated water vapor (monthly)

ECMWF ERA5

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section2_2
section2_2
2.2 HOAPS-v4

The HOAPS v4 Level-2 data have been generated on the basis of the CM SAF SSM/I / SSMIS FCDR (Fennig et al., 2017; Fennig et al., 2020; CM SAF’s HOAPS v4.0 ATBD [D1], section 2.2). The initial dataset was extended to cover the full period until the end of 2017 for the present merged CDR. It is assumed that the inter-calibration coefficients remain applicable over the period 2015–2017.

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table11
table11
Table 11: Summary of the characteristics of the GMP Dual Precipitation Radar. The GPM KuPR minimum threshold is closer to 12–13 dBZ than the official 18 dBZ in the table (from Tang et al., 2017).

Instrument

GPM DPR

KaPR

KuPR

Launch time

27 Feb 2014

27 Feb 2014

Altitude (km)

407

407

Inclination angle (°)

65

65

Frequency (GHz)

35.547 and 35.553

13.597 and 13.603

Horizon resolution at nadir (km)

5

5

Swath width (km)

120

245

Vertical resolution (m)

250/500

250

Minimum detectable Ze (dBZ)

12 (KaHS)
18 (KaMS)

18

Measurement accuracy (dBZ)

< ±  1

< ± 1

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section3_2_2_2
section3_2_2_2
3.2.2.2 The NN training dataset

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table12
table12
Table 12: Characteristics of the NN training dataset built from MHS-DPR coincidences

Period

1/01/2015 – 31/12/2016

Geographical area

67 °S – 67 °N, 180 °W – 180 °E

Number of MHS orbits

36,856

Number of pixels with precipitation

3,000,000

Horizontal resolution (Km)

16 km × 16 km (nadir) 26 km × 52 km (scan edge)

Reference precipitation product

2B-CMB level-2 GMI/DPR combined V06A on Ku-band radar swath (NS)

MHS BTs

FIDUCEO FCDR v4.1


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table13
table13
Table 13: List of variables in the NN training dataset built from MHS-DPR coincidences.

Variable in the database

Data source

Latitude (MHS pixel)

FIDUCEO FCDR v4.1

Longitude (MHS pixel)

FIDUCEO FCDR v4.1

Mean Time (of DPR pixels within the ATMS pixel)

2B-CMB level-2 GMI/DPR combined V06A

Surface precipitation rate

2B-CMB level-2 GMI/DPR combined V06A

Precipitation liquid fraction information

2B-CMB level-2 GMI/DPR combined V06A

Time of MHS pixel

FIDUCEO FCDR v4.1

MHS Scan position

FIDUCEO FCDR v4.1

Sea ice information

ECMWF ERA5

2 m temperature

ECMWF ERA5

Total column integrated water vapor

ECMWF ERA5

Freezing level

ECMWF ERA5

Snow depth

ECMWF ERA5

Land/Sea Mask

ESA

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section3_2_3
section3_2_3
_headingh.17dp8vu
3.2.3 Algorithm Flowchart

The PNPR-CLIM algorithm high-level flowchart is shown in figure 3.

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table14
table14
Table 14: PNC module input variables.

Input Variable

Variable dimensions

Variable type

BT

5

Instantaneous

monthly T2m

1

Average

monthly FL

1

Average

monthly TPWV

1

Average

daily SD

1

Average

daily SIF

1

Average

ANG

1

Static

OLC

1

Static


The static and average variables determine a sort of a priori status of the atmosphere, allowing the NN to correctly interpret the radiative signal (after applying a zenith correction, if necessary): for example, a depression in the BT around the 157 GHz window channel is commonly due to the scattering of precipitating particles. However, if the atmosphere is sufficiently dry, the emission signature of a radiatively cold surface may lead to the same effect on the measured BT. Through the use of the ancillary data the NN aims to discriminate these different states.

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table15
table15
Table 15: Optimal NN module input variables.

Variable Type

Input Variable

Variable dimension

Variable type

BT

89.0 GHz
157.0 GHz
183.31 ± 7.0 GHz

3

Instantaneous

BT Differences

183.31 ± 3.0–183.31 ± 1.0 GHz
183.31 ± 3.0–183.31 ± 7.0 GHz
183.31 ± 1.0–183.31 ± 7.0 GHz
183.31 ± 3.0–157 GHz
183.31 ± 7.0–157 GHz

5

Instantaneous

Model Derived Ancillary Variables

monthly T2m (K)
monthly FL (m)
monthly TPWV (kg m-2)
daily SD
daily SIF

5

Average
(from ECMWF ERA5 reanalysis)

Ancillary Variables

ANG
OLC

2

Static Map


The performance analysis of the PRE module was carried out using the 2016 dataset, which is an independent part of the observational MHS-DPR coincidence database, not used in the training and design phase of the algorithm (about 1.5 million points) (see section 3.2.2.2).

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table16
table16
Table 16: PNPR-CLIM precipitation retrieval module statistical indexes.

 

Ocean

Land

BIAS[mm/h]

0.02

0.01

CC

0.75

0.70

RMSE[mm/h]

1.02

1.08

Another result of the verification study is shown in figure 7. It shows the 2D histogram of the surface precipitation rate estimates from the NN and the corresponding values in the 2B-CMB dataset over ocean and land. Only pixels for which both the neural network and the 2B-CMB provided rainfall estimates ≥ 0.1 mm/h (TP pixels) were considered. In the scatterplot, the logarithmic axes represent the precipitation rate (NN vs. GPM 2B-CMB referred to as DPR), while the colour represents the number of points in the dataset for each 2D precipitation rate bin. Most of the points are close to the main diagonal for both ocean and land, with slight overestimation of very low precipitation (precipitation rate < 0.5 mm/h) over land by the NN.

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table17
table17
Table 17: Contribution of the conditions occurred in the BQF index.

BQF

Occurred Condition

0

Precipitation Probability Index

1

Radiometer Scan index

2

Quality of input data

3

Background surface index (Snow)

4

Background surface index (Sea Ice)

5

Orography index

6

High Latitudes Index

7

Calibration Index

8

Invalid Data

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figure11
figure11

Figure 11: Distribution of the QF index (percentage over all the available observations) for the year 2017.

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table18
table18
Table 18: Semi axes in km for the two instrument classes. For AMSU-B / MHS, the semi axes depend on the scan position sp = 1, …, 90 with 45 and 46 being the central positions in the scan line, close to the sub-satellite point. It is nb = sp for sp ≤ 45 and nb = 91 - sp else


AMSU-B / MHS (PNPR-CLIM)

SSM/I / SSMIS (HOAPS v4)

AMSR-E2 (HOAPS v4 extended)

TMI (HOAPS v4 extended)

Along-scan


Mathdisplay
0.5 \cdot 79.08 + 2.84 \cdot nb - 14.78 \cdot nb^{0.666}


15.5

15.5

9

Cross-scan


Mathdisplay
0.5 \cdot 28.72 - 0.90 \cdot nb + 0.094 \cdot nb^{1.5}


22.5

22.5

16


Info
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note2
note2
2 AMSR-E brightness temperatures from three neighbouring scan positions are averaged to match the SSM/I and SSMIS resolutions, see section 1.2

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table19
table19
Table 19: Valid versions of COBRA products

Version

Description

1.0

Precipitation rates are derived from the original algorithm as described in this document. The version number is valid for daily and monthly files.

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section4_1
section4_1
4.1 Daily merged COBRA data

Files containing daily data of accumulated rain rates are named after following syntax:

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table20
table20
Table 20: List of variables used in any file of daily precipitation rates

Variable Name

Dimension(s)

Unit

Description

Coordinates


lat

1

°N (degrees North)

Latitude of grid cell centre

lat_bnds

2

°N (degrees North)

Boundaries of top (northern) and bottom (southern) grid cell edge

lon

1

°E (degrees East)

Longitude of grid cell centre

lon_bnds

2

°E (degrees East)

Boundaries of left (western) and right (eastern) grid cell edge

time

1

Seconds since 1970-01-01

Time stamp of the current day

time_bnds

2

Seconds since 1970-01-01

Boundaries of the time interval covered by time variable

platform_id

1

N/A

An integer used for internal platform assignment

instrument_id

1

N/A

An integer used for internal instrument assignment

Data Variables


precip

3 (time, lat, lon)

mm/d

Daily accumulated precipitation rates that are represented by a single multi-platform composite

precip_stdv

3 (time, lat, lon)

mm/d

Daily mean of intra-platform standard deviation derived from hourly values

Quality Variables


quality_flag

3 (time, lat, lon)

N/A

Mean of PNPR-CLIM quality flags, whose assigned data was used in composite creation

num_obs

4 (time, lat, lon, instrument_id)

N/A

Total number of observations separated by instrument type

num_covered_hours

3 (time, lat, lon)

N/A

Accumulated number of hours, for which data of at least one platform is available on the respective day

Ancillary Variables


platform_name

2 (time, platform_id)

N/A

Names of all platforms that are used for composite creation for the respective day. The names are allocated to the platform identifier. Platform names are saved as char array. Thus, there is an additional dimension in the netCDF file describing the length of the longest string.

instrument_name

2 (time, instrument_id)

N/A

Assigned names of the specific instrument identifier. Instrument names are saved as char array. Thus, there is an additional dimension in the netCDF file describing the length of the longest string.

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section4_2
section4_2
4.2 Monthly merged COBRA data

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table21
table21
Table 21: List of variables used in files with monthly precipitation rates

Variable Name

Dimension(s)

Unit

Description

Coordinates


lat

1

°N (degrees north)

Latitude of grid cell centre

lat_bnds

2

°N (degrees north)

Boundaries of top (northern) and bottom (southern) grid cell edge

lon

1

°E (degrees east)

Longitude of grid cell centre

lon_bnds

2

°E (degrees east)

Boundaries of left (western) and right (eastern) grid cell edge

time

1

Seconds since 1970-01-01

Time stamp of the current month

time_bnds

2

Seconds since 1970-01-01

Boundaries of the time interval covered by time variable

platform_id

1

N/A

An integer used for internal platform assignment

instrument_id

1

N/A

An integer used for internal instrument assignment

Data Variables


precip

3 (time, lat, lon)

mm/d

Monthly mean precipitation that is represented by a single multi-platform composite

precip_stdv

3 (time, lat, lon)

mm/d

Monthly mean of intra-platform standard deviation derived from hourly values

Quality Variables


quality_flag

3 (time, lat, lon)

N/A

Mean of PNPR-CLIM quality flags, whose assigned data was used in composite creation

num_obs

4 (time, lat, lon, instrument_id)

N/A

Total number of observations separated by instrument type

num_covered_hours

3 (time, lat, lon)

N/A

Accumulated number of hours, for which data of at least one platform is available in the respective month

Ancillary Variables


platform_name

2 (time, platform_id)

N/A

Names of all platforms that are used for composite creation for the respective month. The names are allocated to the platform identifier. Platform names are saved as char array. Thus, there is an additional dimension in the netCDF file describing the length of the longest string.

instrument_name

2 (time, instrument_id)

N/A

Assigned names of the specific instrument identifier. Instrument names are saved as char array. Thus, there is an additional dimension in the netCDF file describing the length of the longest string.

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annex
annex
Annex

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Intermediate_PNPR-CLIM_output
Intermediate_PNPR-CLIM_output
Intermediate PNPR-CLIM output

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FIDUCEO_FCDR_L1C_<RADIOMETER><SATELLITE><START TIME, YYYYMMDDHHMMSS><END TIME, YYYYMMDDHHMMSS{_}>_EASY_v4.1_fv2.0.1.nc

  1. PNPR-CLIM output:

PNPR-CLIM_<FIDUCEO input filename>.nc

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table22
table22
Table 22: Variables within the PNPR-CLIM output file

Name

Long Name

Type

CHAN

Channel

1D

LAT

Latitude

2D

LON

Longitude

2D

POS

Scan position

1D

PP

Probability of Precipitation

Geo2D

PR

Precipitation Rate

Geo2D

QUALITY_PIXEL_BITMASK

FIDUCEO quality pixel bitmask

Geo2D

SCAN

Scan line

1D

UPR

Unmasked Precipitation Rate

Geo2D

UTIME

Scan time

1D

QF

Quality Flag

Geo2D

BQF

Quality Bit Flag

Geo2D


A list of global attributes of PNPR-CLIM netCDF output files is reported, as an example, in the following paragraph:

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