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Issued by: DWD/Bobryshev Oleksandr
Dateproduced inDate: 09/06/2021
Ref: C3S_D312b_Lot1.2.2.3-v2.1_202010_PQAR_ECVSurfaceRadiationBudget_v1.0
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General definitions
In the scope of the Copernicus Climate Change Service (C3S), two Surface Radiation Budget datasets are combined into one Climate Data Record (CDR) called "CLARA product family".
The first dataset, EUMETSAT's CM SAF CLARA-A2.1, is the core of this CDR. The second dataset includes extra data products that are not included in the CLARA-A2.1 dataset. The core data products are brokered from CM SAF. The extra net fluxes are not included in the brokered CLARA-A2.1 dataset and are calculated specifically within the C3S project as complimentary data for the convenience of users. Their format is as close as possible to the CLARA-A2.1 and the datasets are meant to be used together. Both datasets are frequently updated with Interim Climate Data Records (ICDRs) or simply extensions, generated using the same software and algorithms to cover more recent periods. The ICDR part for all products covers period from 2019 to 2020.
This separation into two datasets is necessary to keep the origin of the data, e.g. licence affiliations: "EUMETSAT's CM SAF" and "C3S", clear for individual products (Table 1)
Table 1: Licence overview of the CLARA product family Surface Radiation Products available through the CDS
Year
CDR Type
...
CLARA Product Family
...
SIS
...
SDL, SOL
...
SRS
...
Net Fluxes
...
...
Longwave fluxes
...
Extra data products
...
1982 – 2018
...
TCDR
...
CM SAF (CLARA-A2.1)
...
CM SAF
(CLARA-A2.1)
...
C3S
...
C3S
...
2019 – 2020
...
ICDR
...
CM SAF
(CLARA-A2.1 ICDR)
...
C3S
...
C3S
...
C3S
The longwave fluxes are not included in the CM SAF ICDR plans for the current phase. To ensure the dataset integrity and continuity, they are calculated within the C3S for the ICDR part. As such, the longwave fluxes change their licence affiliation, namely they are provided within the C3S project for the ICDR part (2019-2020) and are brokered from EUMETSAT’s CM SAF for the TCDR part (1982 to 2018).
Furthermore the CM SAF CLARA-A2.1 dataset has a temporal coverage of January 1982 to June 2019 (as described in [D2]), but TCDR data are only being brokered to the CDS up to December 2018. Data available from the CDS for January 2019 to December 2020 are brokered/derived from the CLARA A2.1 ICDR1.
In contrast to the original CM SAF CLARA-A2.1 dataset, the brokered service within Copernicus solely provides:
- Level-3 data – excluding the level-2b data format.
- Data on a global equal angle grid – excluding the polar grid format.
- An aggregated version of all satellite data – excluding the provision of the individual satellite datasets.
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List of Figures
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Figure 1-1: Spatial distribution of the propagated SRS accuracies for 1982-2018 (left) and 2019-2020 (right) years Figure 1-2: Spatial distribution of the propagated SNS accuracies for 1982-2018 (left) and 2019-2020 (right) years |
List of Tables
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Table 2-1: Summary of validation results for SDL and SOL ICDR datasets (2019-2020) Table 3-1: Summary of KPI results with 2.5 and 97.5 percentiles and number of ICDR months within the range Table 4-1: Summary of the requirements and achieved accuracies of the brokered CLARA-A2.1 data products], Section 1 [D1 for SIS, SOL, SDL TCDR, D8 for SIS ICDR] |
General definitions
In the scope of the Copernicus Climate Change Service (C3S), two Surface Radiation Budget datasets are combined into one Climate Data Record (CDR) called "CLARA product family".
The first dataset, EUMETSAT's CM SAF CLARA-A2.1, is the core of this CDR. The second dataset includes extra data products that are not included in the CLARA-A2.1 dataset. The core data products are brokered from CM SAF. The extra net fluxes are not included in the brokered CLARA-A2.1 dataset and are calculated specifically within the C3S project as complimentary data for the convenience of users. Their format is as close as possible to the CLARA-A2.1 and the datasets are meant to be used together. Both datasets are frequently updated with Interim Climate Data Records (ICDRs) or simply extensions, generated using the same software and algorithms to cover more recent periods. The ICDR part for all products covers period from 2019 to 2020.
This separation into two datasets is necessary to keep the origin of the data, e.g. licence affiliations: "EUMETSAT's CM SAF" and "C3S", clear for individual products (Table 1)
Table 1: Licence overview of the CLARA product family Surface Radiation Products available through the CDS
Year | CDR Type | CLARA Product Family | |||
SIS | SDL, SOL | SRS | Net Fluxes | ||
| Longwave fluxes | Extra data products | |||
1982 – 2018 | TCDR | CM SAF (CLARA-A2.1) | CM SAF (CLARA-A2.1) | C3S | C3S |
2019 – 2020 | ICDR | CM SAF (CLARA-A2.1 ICDR) | C3S | C3S | C3S |
The longwave fluxes are not included in the CM SAF ICDR plans for the current phase. To ensure the dataset integrity and continuity, they are calculated within the C3S for the ICDR part. As such, the longwave fluxes change their licence affiliation, namely they are provided within the C3S project for the ICDR part (2019-2020) and are brokered from EUMETSAT’s CM SAF for the TCDR part (1982 to 2018).
Furthermore the CM SAF CLARA-A2.1 dataset has a temporal coverage of January 1982 to June 2019 (as described in [D2]), but TCDR data are only being brokered to the CDS up to December 2018. Data available from the CDS for January 2019 to December 2020 are brokered/derived from the CLARA A2.1 ICDR1.
In contrast to the original CM SAF CLARA-A2.1 dataset, the brokered service within Copernicus solely provides:
- Level-3 data – excluding the level-2b data format.
- Data on a global equal angle grid – excluding the polar grid format.
- An aggregated version of all satellite data – excluding the provision of the individual satellite datasets.
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Scope of the document
This document is the Product Quality Assessment Report (PQAR) for CLARA Product family CDR. This document provides validation results for the Climate Data Record (CDR) of the Surface Radiation Budget.
Executive summary
The brokering service of the CLARA-A2.1 data products includes 37 years (1982-2018) of level-3 data (monthly means) on a regular global latitude-longitude grid (with 0.25° x 0.25° resolution), merged from various polar orbiting satellites. It includes three products: the Surface Incoming Shortwave radiation (SIS), the Surface Outgoing Longwave radiation (SOL), and the Surface Downwelling Longwave radiation (SDL). SIS daily averages are also available within C3S. This CDR is brokered from EUMETSAT’s CM SAF. Therefore, this document refers to the original EUMETSAT CM SAF Validation Report [D1, D8]. It describes the validation methodology and the validation results.
The extra data products (produced specifically within the C3S project) are: the Surface Reflected Shortwave radiation (SRS), the Surface Net Shortwave radiation (SNS), the Surface Net Longwave radiation (SNL), and the Surface Radiation Budget (SRB). Validation results for these extra data products are described within this document.
The CLARA based ICDR data record is a continuation of the products of the CLARA-A2.1 and the extra data products. It extends both products by 2 years (2019-2020). The longwave fluxes are not included in the CM SAF ICDR plans for the current phase. Therefore SOL and SDL change their license affiliation, namely they are provided within the C3S project for the ICDR part (2019-2020) and are brokered from EUMETSAT’s CM SAF for the TCDR part (1982 to 2018). Table 1 provides an overview of the licenses for all data CLARA family products. Validation results for SDL and SOL ICDR data products are described within this document.
An executive summary of the evaluation of the CLARA-A2.1 and CLARA-based ICDR surface radiation dataset can be found in CM SAF Validation Report, Section 1 [D1, D8]
Table 2: Summary of the accuracy of the brokered CLARA-A2.1 data products, [D1] Section 1 for SIS, SOL, SDL TCDR, [D8] Section 1 for SIS ICDR. The accuracy estimation of SOL and SDL ICDR extensions is performed within the C3S using the algorithms developed by CM SAF Anchor table2 table2
Product Name | Dataset accuracy [W/m2] | |
TCDR | ICDR | |
SIS monthly means | 9.5 | 9.6 |
SIS daily means | 18.6 | 22.9 |
SDL | 8.1 | 15.8 |
SOL | 13.8 | 9.2 |
Table 3: Summary of the accuracy of the extra data products Anchor table3 table3
Product Name | Propagated accuracy [W/m2] | |
TCDR | ICDR | |
SRS | 7.8 | 6.5 |
SNS | 13.0 | 14.2 |
SNL | 21.9 | 25.0 |
SRB | 34.9 | 39.2 |
1. Product validation methodology
In the scope of the Copernicus Climate Change Service (C3S), two Surface Radiation Budget datasets are combined into one Climate Data Record (CDR) called the "CLARA product family".
1.1 Validation methodology for SIS, SOL, SDL
CLARA-A2.1 data products include the Surface Incoming Shortwave radiation (SIS), the Surface Outgoing Longwave radiation (SOL), and the Surface Downwelling Longwave radiation (SDL) datasets. These datasets were validated against reference data records from surface measurements obtained by the Baseline Surface Radiation Network (BSRN, Ohmura et al., 1998, Driemel et al., 2018). The reference dataset is described in detail in CM SAF Validation Report [D1], Section 4.
Therefore, this document refers to the original EUMETSAT CM SAF Validation Report [D1, D8]. It describes the validation methodology and the validation results. The accuracy estimation of SOL and SDL ICDR extensions is performed within the C3S using the algorithms developed by CM SAF
The validation of the SIS ICDR (2019-2020) product is described in CM SAF Validation Report ICDR, Sections 5.2 [D8]. The validation methodology of SOL and SDL ICDR extensions is performed within the C3S using the algorithms developed by CM SAF.
The validation methodology and definitions of the main metrics are provided in the C3S Product Quality Assurance Document (PQAD) [D4], Section 3, which refers to CM SAF Validation Report [D1], Section 5 and 5.1.
1.2 Validation methodology for CLARA family extra data products
The performed validation approach for extra data products is based on the method of error propagation. These data products are the Surface Reflected Shortwave radiation (SRS), the Surface Net Shortwave radiation (SNS), the Surface Net Longwave radiation (SNL), and the Surface Radiation Budget (SRB).
The ICDR part data are validated in the same way as the TCDR
1.2.1 Surface Reflected Shortwave Radiation (SRS)
The accuracy of the SRS is determined based on the accuracy of the Surface Incoming Shortwave Radiation (SIS) from the Surface Radiation Budget brokered from EUMETSAT’s CM SAF CLARA-A2.1 dataset [D1], and the Surface Albedo (SAL), not provided within the C3S.
The accuracy for the SRS is calculated using the fixed accuracy values for the SIS ( ΔSIS = 10 W/m2 ) and the relative error of the SAL ( ΔSAL = 25% of the SAL value). These values are the target requirements for accuracy from CM SAF Product Requirement Document [D2]. Resulting global mean accuracy for the SRS is 7.8 W/m2 for TCDR and 6.5 W/m2 for ICDR. Figures 1-1 and 1-2 provide the spatial distribution of the propagated SNS accuracies.
Figure 1-1: Spatial distribution of the propagated SRS accuracies for 1982-2018 (left) and 2019-2020 (right) years Anchor figure1_1 figure1_1
1.2.2 Surface Net Shortwave Radiation (SNS)
The accuracy of the SNS is determined based on the accuracy of the SIS and the SAL datasets.
Estimations of the accuracy of the SIS product is given in CM SAF Validation Report [D1] and the accuracy of the SAL product is given in CM SAF Validation Report, Surface Albedo [D6].
The accuracy for the SRS is calculated using the fixed accuracy values for the SIS ( ΔSIS = 10 W/m2 ) and the relative error of the SAL ( ΔSAL = 25% of the SAL value). These values are the target requirements for accuracy from CM SAF Product Requirement Document [D2]. Resulting global mean accuracy for the SNS is 13.0 W/m2. Figure 1-2 provides the spatial distribution of the propagated SNS accuracies.
Figure 1-2: Spatial distribution of the propagated SNS accuracies for 1982-2018 (left) and 2019-2020 (right) years Anchor figure1_2 figure1_2
1.2.3 Surface Net Longwave Radiation (SNL)
The accuracy of the SNL is defined by the accuracy of the Surface Downwelling Longwave Radiation (SDL) and the Surface Outgoing Longwave Radiation (SOL), both datasets are the Surface Radiation Budget brokered from EUMETSAT’s CM SAF CLARA-A2.1 [D1].
Estimations of the accuracy of the SDL and the SOL products are given in CM SAF Validation Report [D1].
The accuracy for the SNL is calculated using the fixed accuracy values for the SDL ( ΔSDL = 8.13 W/m2 ) and the SOL ( ΔSOL = 13.77 W/m2 ). Resulting global mean accuracy for the SNL is 21.9 W/m2.
Global mean accuracy for the SNL ICDR is 25.0 W/m2.
1.2.4 Surface Radiation Budget (SRB)
The accuracy of the SRB is defined by the accuracy of the SNS and the SNL datasets.
The accuracy for the SRB is calculated using the fixed accuracy values for the SNS ( ΔSNS = 13.0 W/m2 ) and the SNL ( ΔSNL = 21.9 W/m2 ).
Resulting global mean accuracy for the SRB is 34.9 W/m2.
Global mean accuracy for the SNL ICDR is 39.2 W/m2.
Anchor validation validation
2. Validation results
validation | |
validation |
2.1 Validation results for SIS, SOL, SDL
The TCDR (1982-2018) validation results are fully described in CM SAF Validation Report [D1], Section 5. The validation results for the SIS are provided in CM SAF Validation Report [D1], Section 5.2 and 5.2. The validation results for the SOL are provided in CM SAF Validation Report [D1], Section 5.3. The validation results for the SDL are provided in CM SAF Validation Report [D1], Section 5.4. Considerations for climate applications are provided in CM SAF Data Set Description [D3], Section 6. Conclusions for the validation results are provided
Scope of the document
This document is the Product Quality Assessment Report (PQAR) for CLARA Product family CDR. This document provides validation results for the Climate Data Record (CDR) of the Surface Radiation Budget.
Executive summary
The brokering service of the CLARA-A2.1 data products includes 37 years (1982-2018) of level-3 data (monthly means) on a regular global latitude-longitude grid (with 0.25° x 0.25° resolution), merged from various polar orbiting satellites. It includes three products: the Surface Incoming Shortwave radiation (SIS), the Surface Outgoing Longwave radiation (SOL), and the Surface Downwelling Longwave radiation (SDL). SIS daily averages are also available within C3S. This CDR is brokered from EUMETSAT’s CM SAF. Therefore, this document refers to the original EUMETSAT CM SAF Validation Report [D1, D8]. It describes the validation methodology and the validation results.
The extra data products (produced specifically within the C3S project) are: the Surface Reflected Shortwave radiation (SRS), the Surface Net Shortwave radiation (SNS), the Surface Net Longwave radiation (SNL), and the Surface Radiation Budget (SRB). Validation results for these extra data products are described within this document.
The CLARA based ICDR data record is a continuation of the products of the CLARA-A2.1 and the extra data products. It extends both products by 2 years (2019-2020). The longwave fluxes are not included in the CM SAF ICDR plans for the current phase. Therefore SOL and SDL change their license affiliation, namely they are provided within the C3S project for the ICDR part (2019-2020) and are brokered from EUMETSAT’s CM SAF for the TCDR part (1982 to 2018). Table 1 provides an overview of the licenses for all data CLARA family products. Validation results for SDL and SOL ICDR data products are described within this document.
An executive summary of the evaluation of the CLARA-A2.1 and CLARA-based ICDR surface radiation dataset can be found in CM SAF Validation Report, Section 1 [D1, D8]
Table 2: Summary of the accuracy of the brokered CLARA-A2.1 data products, [D1] Section 1 for SIS, SOL, SDL TCDR, [D8] Section 1 for SIS ICDR. The accuracy estimation of SOL and SDL ICDR extensions is performed within the C3S using the algorithms developed by CM SAF
...
Product Name
...
Dataset accuracy [W/m2]
...
TCDR
...
ICDR
...
SIS monthly means
...
9.5
...
9.6
...
SIS daily means
...
18.6
...
22.9
...
SDL
...
8.1
...
15.8
...
SOL
...
13.8
...
9.2
Table 3: Summary of the accuracy of the extra data products
...
Product Name
...
Propagated accuracy [W/m2]
...
TCDR
...
ICDR
...
SRS
...
7.8
...
6.5
...
SNS
...
13.0
...
14.2
...
SNL
...
21.9
...
25.0
...
SRB
...
34.9
...
39.2
1. Product validation methodology
In the scope of the Copernicus Climate Change Service (C3S), two Surface Radiation Budget datasets are combined into one Climate Data Record (CDR) called the "CLARA product family".
1.1 Validation methodology for SIS, SOL, SDL
CLARA-A2.1 data products include the Surface Incoming Shortwave radiation (SIS), the Surface Outgoing Longwave radiation (SOL), and the Surface Downwelling Longwave radiation (SDL) datasets. These datasets were validated against reference data records from surface measurements obtained by the Baseline Surface Radiation Network (BSRN, Ohmura et al., 1998, Driemel et al., 2018). The reference dataset is described in detail in CM SAF Validation Report [D1], Section 46.
Therefore, this document refers to the original EUMETSAT CM SAF Validation Report [D1, D8]. It describes the validation methodology and the validation results. The accuracy estimation of SOL and SDL ICDR extensions is performed within the C3S using the algorithms developed by CM SAF
Results are summarised in Table 1 in the Executive Summary.
The validation results for SIS ICDR monthly and daily are fully The validation of the SIS ICDR (2019-2020) product is described in CM SAF Validation Report ICDR [D8], Sections Section 5.2 [D8].
The validation methodology results of SOL and SDL ICDR extensions is performed within the C3S using the algorithms developed by CM SAF. The validation methodology and definitions of the main metrics are provided in the C3S Product Quality Assurance Document (PQAD) [D4], Section 3, which refers to CM SAF Validation Report [D1], Section 5 and 5.1.
1.2 Validation methodology for CLARA family extra data products
The performed validation approach for extra data products is based on the method of error propagation. These data products are the Surface Reflected Shortwave radiation (SRS), the Surface Net Shortwave radiation (SNS), the Surface Net Longwave radiation (SNL), and the Surface Radiation Budget (SRB).
The ICDR part data are validated in the same way as the TCDR
1.2.1 Surface Reflected Shortwave Radiation (SRS)
The accuracy of the SRS is determined based on the accuracy of the Surface Incoming Shortwave Radiation (SIS) from the Surface Radiation Budget brokered from EUMETSAT’s CM SAF CLARA-A2.1 dataset [D1], and the Surface Albedo (SAL), not provided within the C3S.
The accuracy for the SRS is calculated using the fixed accuracy values for the SIS ( ΔSIS = 10 W/m2 ) and the relative error of the SAL ( ΔSAL = 25% of the SAL value). These values are the target requirements for accuracy from CM SAF Product Requirement Document [D2]. Resulting global mean accuracy for the SRS is 7.8 W/m2 for TCDR and 6.5 W/m2 for ICDR. Figures 1 and 2 provide the spatial distribution of the propagated SNS accuracies.
Figure 1: Spatial distribution of the propagated SRS accuracies for 1982-2018 (left) and 2019-2020 (right) years.
1.2.2 Surface Net Shortwave Radiation (SNS)
The accuracy of the SNS is determined based on the accuracy of the SIS and the SAL datasets.
Estimations of the accuracy of the SIS product is given in CM SAF Validation Report [D1] and the accuracy of the SAL product is given in CM SAF Validation Report, Surface Albedo [D6].
The accuracy for the SRS is calculated using the fixed accuracy values for the SIS ( ΔSIS = 10 W/m2 ) and the relative error of the SAL ( ΔSAL = 25% of the SAL value). These values are the target requirements for accuracy from CM SAF Product Requirement Document [D2]. Resulting global mean accuracy for the SNS is 13.0 W/m2. Figure 2 provides the spatial distribution of the propagated SNS accuracies.
Figure 2: Spatial distribution of the propagated SNS accuracies for 1982-2018 (left) and 2019-2020 (right) years
1.2.3 Surface Net Longwave Radiation (SNL)
The accuracy of the SNL is defined by the accuracy of the Surface Downwelling Longwave Radiation (SDL) and the Surface Outgoing Longwave Radiation (SOL), both datasets are the Surface Radiation Budget brokered from EUMETSAT’s CM SAF CLARA-A2.1 [D1].
Estimations of the accuracy of the SDL and the SOL products are given in CM SAF Validation Report [D1].
The accuracy for the SNL is calculated using the fixed accuracy values for the SDL ( ΔSDL = 8.13 W/m2 ) and the SOL ( ΔSOL = 13.77 W/m2 ). Resulting global mean accuracy for the SNL is 21.9 W/m2.
Global mean accuracy for the SNL ICDR is 25.0 W/m2.
1.2.4 Surface Radiation Budget (SRB)
The accuracy of the SRB is defined by the accuracy of the SNS and the SNL datasets.
The accuracy for the SRB is calculated using the fixed accuracy values for the SNS ( ΔSNS = 13.0 W/m2 ) and the SNL ( ΔSNL = 21.9 W/m2 ).
Resulting global mean accuracy for the SRB is 34.9 W/m2.
Global mean accuracy for the SNL ICDR is 39.2 W/m2.
2. Validation results
2.1 Validation results for SIS, SOL, SDL
The TCDR (1982-2018) validation results are fully described in CM SAF Validation Report [D1], Section 5. The validation results for the SIS are provided in CM SAF Validation Report [D1], Section 5.2 and 5.2. The validation results for the SOL are provided in CM SAF Validation Report [D1], Section 5.3. The validation results for the SDL are provided in CM SAF Validation Report [D1], Section 5.4. Considerations for climate applications are provided in CM SAF Data Set Description [D3], Section 6. Conclusions for the validation results are provided in CM SAF Validation Report [D1], Section 6.
Results are summarised in Table 1 in the Executive Summary.
The validation results for SIS ICDR monthly and daily are fully described in CM SAF Validation Report ICDR [D8], Section 5.2.
The validation results of SOL and SDL ICDR extensions is performed within the C3S using the algorithms developed by CM SAF. The summary of validation results for the monthly ICDR SDL and ICDR SOL datasets are shown in Table 4.
At the time of writing (May 2021) only 34 out of 60 BSRN stations have submitted data for years 2019-2020. 12 stations had less than 4 month worth of data and they were discarded. A full list of BSRN stations used in the validation and stationwise results are presented in Tables 5 and 6, Section 5 Appendix of this document. The outgoing longwave measurements are performed not on all BSRN stations. Only 9 stations have submitted data for years 2019-2020. A full list of BSRN stations used in the validation and stationwise results are presented in Table 5 and 6, Section 5 Appendix of this document.
Table 4: Summary of validation results for SDL and SOL ICDR datasets (2019-2020)
...
Dataset
...
Number of months analysed
...
BSRB Stations
...
Abs.bias, W/m2
...
Std.Dev, W/m2
...
SDL, ICDR
...
404
...
24
...
15.8
...
25.16
...
SOL, ICDR
...
188
...
9
...
9.19
...
12.87
summary of validation results for the monthly ICDR SDL and ICDR SOL datasets are shown in Table 2-1.
At the time of writing (May 2021) only 34 out of 60 BSRN stations have submitted data for years 2019-2020. 12 stations had less than 4 month worth of data and they were discarded. A full list of BSRN stations used in the validation and stationwise results are presented in Tables 6 and 7, Section 5 Appendix of this document. The outgoing longwave measurements are performed not on all BSRN stations. Only 9 stations have submitted data for years 2019-2020. A full list of BSRN stations used in the validation and stationwise results are presented in Table 6 and 7, Section 5 Appendix of this document.
Table 2-1: Summary of validation results for SDL and SOL ICDR datasets (2019-2020) Anchor table2_1 table2_1
Dataset | Number of months analysed | BSRB Stations | Abs.bias, W/m2 | Std.Dev, W/m2 |
SDL, ICDR | 404 | 24 | 15.8 | 25.16 |
SOL, ICDR | 188 | 9 | 9.19 | 12.87 |
2.2 Validation results for CLARA family extra data products (SRS, SNS, SNL, SRB)
The validation methodology for the extra data products is selected in a way to provide the most conservative accuracy estimation, i.e. by assuming that the uncertainties in the input datasets align perfectly and contribute fully to the overall uncertainty. Table 2 in the Executive summary provides a summary of the accuracies for the SRS, the SNS, the SNL, and the SRB. The SRS accuracy is 7.8 (6.5) W/m2, the SNS accuracy is 13.0 (14.2) W/m2, the SNL accuracy is 21.9 (25.0) W/m2, and the SRB accuracy is 34.9 (39.2) W/m2, ICDR values are in parenthesis.
3. Application(s) specific assessments
In addition to the extensive product validation (see chapter 2 for results and chapter 2/3 in [D10] for validation methodology) a second assessment is introduced to evaluate the Interim Climate Data Record (ICDR) against the Thematic Climate Data Record (TCDR) in terms of consistency. Since frequent ICDR deliveries make detailed validation not feasible, a consistency check against the deeply validated TCDR is used as an indication of quality. This is done by a comparison of the following two evaluations:
- TCDR against a stable, long-term and independent reference dataset
- ICDR against the same stable, long-term and independent reference dataset
The evaluation method is generated to detect differences in the ICDR performance in a quantitative, binary way with so called Key Performance Indicators. The general method is outlined in [D9] chapter 3. The same difference between TCDR/ICDR and the reference dataset would lead to the conclusion that TCDR and ICDR have the same quality (key performance is "good"). Variations or trends in the differences (TCDR/ICDR against reference) would require a further investigation to analyze the reasons. The key performance would be marked as "bad". The binary decision whether the key performance is good or bad is made in a statistical way by a hypotheses test (binomial test). Based on the TCDR/reference comparison (global means, monthly or daily means) a range is defined with 95% of the differences are within. This range (2.5 and 97.5 percentile) is used for the ICDR/reference comparison to check whether the values are in or out of the range. The results could be the following:
- All or a sufficient high number of ICDR/reference differences lies within the range defined by the TCDR/reference comparison: Key performance of the ICDR is "good"
- A smaller number of ICDR/reference differences is within the pre-defined range: Key performance of the ICDR is "bad"
3.1 Results
The results of the KPI test are summarized in Table 3-1.
Anchor | ||||
---|---|---|---|---|
|
Surface Incoming Shortwave Radiation (monthly means) | Surface Incoming Shortwave Radiation (daily means) | Surface Downwelling Longwave Radiation | Surface Outgoing Longwave Radiation | |||||
---|---|---|---|---|---|---|---|---|
01/2019 - 06/2021 | p2.5 = 5.28 W/m² p97.5 = 14.66 W/m² | 30/30 | p2.5 = 5.11 W/m² p97.5 = 11.63 W/m² | 29/30 | p2.5 = 8.12 W/m² p97.5 = 25.84 W/m² | 30/30 | ||
01/2019 - 12/2021 | p2.5 = 5.28 W/m² p97.5 = 14.66 W/m² | 36/36 | p2.5 = 8.81 W/m² p97.5 = 40.95 W/m² | 36/36 | p2.5 = 5.11 W/m² p97.5 = 11.63 W/m² | 35/36 | p2.5 = 7.66 W/m² p97.5 = 25.79 W/m² | 35/36 |
01/2019 - 06/2022 | p2.5 = 5.28 W/m² p97.5 = 14.66 W/m² | 41/42 | p2.5 = 8.81 W/m² p97.5 = 40.95 W/m² | 42/42 | p2.5 = 5.11 W/m² p97.5 = 11.63 W/m² | 42/42 | p2.5 = 6.94W/m² p97.5 = 25.72 W/m² | 42/42 |
Percentiles were calculated based on the comparison of the TCDR using the Advanced Very High Resolution Radiometer (AVHRR) instrument against ground-based Baseline Surface Radiation Network (BSRN) measurements for the variables Surface Incoming Shortwave Radiation (monthly means and daily means), Surface Downwelling Longwave Radiation and Surface Outgoing Longwave Radiation from 1992-2018. All products stay within the TCDR-based limits and binomial tests lead to "good" KPI performance. The ICDR is therefore stable in relation to the deeply validated TCDR.
2.2 Validation results for CLARA family extra data products (SRS, SNS, SNL, SRB)
The validation methodology for the extra data products is selected in a way to provide the most conservative accuracy estimation, i.e. by assuming that the uncertainties in the input datasets align perfectly and contribute fully to the overall uncertainty. Table 2 in the Executive summary provides a summary of the accuracies for the SRS, the SNS, the SNL, and the SRB. The SRS accuracy is 7.8 (6.5) W/m2, the SNS accuracy is 13.0 (14.2) W/m2, the SNL accuracy is 21.9 (25.0) W/m2, and the SRB accuracy is 34.9 (39.2) W/m2, ICDR values are in parenthesis.
3. Application(s) specific assessments
N/A
4. Compliance with user requirements
...
The compliance with the user requirements (as defined in the CM SAF PRD document ([D2], Section 5) for the SIS, SDL, and SOL is provided in Table 54-1.
Table 4-1Table 5: Summary of the requirements and achieved accuracies of the brokered CLARA-A2.1 data products], Section 1 [D1 for SIS, SOL, SDL TCDR, D8 for SIS ICDR]. The accuracy estimation of SOL and SDL ICDR extensions is performed within the C3S using the algorithms developed by CM SAF Anchor table4_1 table4_1
Product Name | Threshold/ Target / Optimal accuracies | Dataset accuracy [W/m2] | |
TCDR | ICDR | ||
SIS monthly means | 15 / 10 / 8 | 9.5 | 9.6 |
SIS daily means | 30 / 20 / 15 | 18.6 | 22.9 |
SDL | 15 / 10 / 8 | 8.1 | 15.8 |
SOL | 15 / 10 / 8 | 13.77 | 9.2 |
The validation methodology for the extra data products is selected in a way to provide the most conservative accuracy estimation, i.e. by assuming that the uncertainties in the input datasets align perfectly and contribute fully to the overall uncertainty. The SRS accuracy is 7.8 (6.5) W/m2, the SNS accuracy is 13.0 (14.2) W/m2, the SNL accuracy is 21.9 (25.0) W/m2, and the SRB accuracy is 34.9 (39.2) W/m2, ICDR values are in parenthesis.
Appendix
Table 6: Stationwise validation results for SDL, 2019-2020 Anchor table6 table6
Full name | Abbreviation | #of months | Mean BSRN, W/m2 | Mean CLARA, W/m2 | AbsBias | RMSE | Fraction above 15 W/m2 |
Ny Alesund | nya | 24 | 259,3 | 242,9 | 16,4 | 17,0 | 50 |
Cabauw | cab | 24 | 323,1 | 318,3 | 4,8 | 5,5 | 0 |
Palaiseu Cedex | pal | 10 | 323,1 | 318,7 | 4,5 | 5,4 | 0 |
Fort Peck | fpe | 16 | 274,2 | 251,9 | 22,3 | 22,5 | 100 |
Payerne | pay | 14 | 312,3 | 288,3 | 24,1 | 24,2 | 100 |
Sioux Falls | sxf | 11 | 305,5 | 291,9 | 13,6 | 14,1 | 55 |
Sapporo | sap | 22 | 314,9 | 308,9 | 6,4 | 8,2 | 5 |
Cener | cnr | 23 | 322,3 | 305,5 | 16,8 | 17,5 | 65 |
Rock Springs | psu | 11 | 323,7 | 311,5 | 12,2 | 13,0 | 27 |
Boulder | bos | 16 | 280,7 | 229,9 | 50,9 | 50,9 | 100 |
Bondville | bon | 16 | 315,2 | 308,3 | 7,0 | 7,9 | 0 |
Desert Rock | dra | 16 | 311,1 | 272,8 | 38,3 | 40,2 | 100 |
Great Plains | e13 | 7 | 338,1 | 324,5 | 13,6 | 14,0 | 29 |
Tateno | tat | 23 | 346 | 348,5 | 2,6 | 3,0 | 0 |
Goodwin Creek | gcr | 16 | 347,5 | 348,8 | 4,9 | 6,0 | 6 |
Fukuoka | fua | 22 | 354,5 | 353,1 | 2,0 | 2,3 | 0 |
Ishigakijima | ish | 22 | 408,5 | 411,9 | 3,7 | 4,5 | 0 |
Minamitorishima | mnm | 22 | 403,5 | 404,7 | 2,0 | 2,6 | 0 |
Tamanrasset | tam | 24 | 330,6 | 273,8 | 56,8 | 57,0 | 100 |
Gobabeb | gob | 24 | 338,3 | 327,5 | 11,0 | 11,9 | 17 |
Florinopolis | flo | 22 | 383,5 | 374,7 | 8,8 | 9,0 | 0 |
De Aar | daa | 11 | 300,4 | 301,2 | 1,6 | 1,9 | 0 |
Total | 404 | 330,8 | 318,6 | 15,8 | 25,2 | 34 |
Table 7: Stationwise validation results for SOL, 2019-2020 Anchor table7 table7
Full name | Abbreviation | #of months | Mean BSRN, W/m2 | Mean CLARA, W/m2 | AbsBias | RMSE | Fraction above 15 W/m2 |
Cabauw | cab | 24 | 373,1 | 372,1 | 3,3 | 4,7 | 4 |
Concordia Station | dom | 24 | 140,4 | 139,1 | 11,1 | 14,3 | 21 |
Gobabeb | gob | 24 | 442,4 | 447,8 | 7,1 | 8,1 | 0 |
Georg von Neumayer | gvn | 13 | 246,7 | 259,4 | 12,7 | 14,8 | 46 |
Ny Alesund | nya | 24 | 292,6 | 285,8 | 15,8 | 21,2 | 29 |
Payerne | pay | 14 | 363,9 | 341,4 | 22,5 | 22,9 | 100 |
Syowa | syo | 24 | 264,2 | 263,5 | 3,1 | 4,0 | 0 |
Toravere | tor | 17 | 351,4 | 344 | 7,4 | 9,0 | 12 |
Tateno | tat | 24 | 394 | 400,2 | 6,4 | 7,6 | 0 |
Total | 188 | 319,3 | 318,1 | 9,2 | 12,9 | 19 |
References
Ohmura, A., et al. (1998), Baseline Surface Radiation Network (BSRN/WCRP): New precision radiometry for climate research, Bulletin of the American Meteorological Society, 79(10), 2115-2136.
...
Further references are listed in CM SAF Validation Report [D1], Section 7.
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This document has been produced with funding by the European Union in the context of the Copernicus Climate Change Service (C3S) .The activities leading to these results have been contracted, operated by the European Centre for Medium-Range Weather Forecasts , operator of C3Son behalf ofon the European Union ( Delegation agreementContribution Agreement signed on 1122/ 1107/ 20142021). All information in this document is provided "as is" and no guarantee orof warranty is given that the information is fit for any particular purpose. The users thereof use the information at their sole risk and liability. For the avoidance of all doubt, the European Commission and the European Centre for Medium-Range Weather Forecasts have no liability in respect of this document, which is merely representing the author's view. |
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