EUMETSAT OSI SAF 25-km, 12.5-km, coastal, EARS 25-km, coastal Wind product User Manual
Oglas
Oglas
Ocean and Sea Ice SAF
EUMETSAT Advanced Retransmission Service
ASCAT Wind Product User Manual
Global OSI SAF 25-km wind product (OSI-102 and OSI-102b)
Global OSI SAF 12.5-km wind product (OSI-103 - discontinued)
Global OSI SAF coastal wind product (OSI-104 and OSI-104b)
Regional EARS 25-km wind product
Regional EARS coastal wind product
Version 1.14, March 2016
SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual
DOCUMENT SIGNATURE TABLE
Prepared by :
Approved by :
Name
O&SI SAF Project
Team
O&SI SAF Project
Manager
Date
Mar 2016
Mar 2016
Signature
DOCUMENTATION CHANGE RECORD
Issue / Revision
Version 0.1
Version 1.0
Version 1.1
Version 1.2
Version 1.3
Version 1.4
Date :
Feb 2007
Mar 2007
Sep 2007
Oct 2007
Oct 2007
Mar 2008
Version 1.5
Version 1.6
Version 1.7
Version 1.8
Version 1.9
Version 1.10
Version 1.11
Version 1.12
Version 1.13
Nov 2008
Jan 2009
Aug 2009
Jan 2010
Feb 2011
Aug 2011
Feb 2012
Aug 2012
May 2013
Minor
Minor
Minor
Minor
Major
Minor
Minor
Minor
Major
Change :
Minor
Minor
Minor
Minor
Minor
Description :
Draft version
First external version
Added release note (sec. 1.4)
Single transponder calibrated L1 data (version 5.2.1)
Take some comments of ORR-A part 1 into account
Three-transponder calibrated L1 data
(version 5.5.0)
Change to neutral winds
Comments of 12.5-km DRI included
NetCDF product format included
Editorial changes, included section 1.7.
Included coastal product and changes for merging of soil moisture and winds
Some editorial changes
Changes for timeliness and EARS coverage
Implementation of Bayesian ice screening
Removed information which is now in the ATBD; include Metop-B; include comments from Metop-B
ORR
Discontinuation of 12.5 km Hamming filter products Version 1.14 Mar 2016 Minor
KNMI, De Bilt, the Netherlands
Reference: SAF/OSI/CDOP/KNMI/TEC/MA/126
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Cover illustration: ASCAT winds over the Atlantic on 7 February 2007, around 21 hour UTC (red arrows). In this picture, only half of the ASCAT wind vectors, with 25-km cell spacing, are plotted. The blue and purple arrows show a 3-hour forecast of the winds by the KNMI High-Resolution Limited Area
Model (HiRLAM). In the background, a METEOSAT infrared image is shown in black and white.
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Contents
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1. Introduction
1.1. Overview
The EUMETSAT Ocean and Sea Ice Satellite Application Facility (OSI SAF) produces a range of airsea interface products, namely: wind, sea ice characteristics, Sea Surface Temperatures (SST) and radiative fluxes, Surface Solar Irradiance (SSI) and Downward Long wave Irradiance (DLI).
KNMI is involved in the OSI SAF and the EUMETSAT Advanced Retransmission Service (EARS)
ASCAT service as the centre where the Level 1b to Level 2 wind processing is carried out. This document is the Product User Manual to the ASCAT wind products. Quality monitoring information on this product and more general information on the whole OSI SAF project, is available on the OSI SAF web site: http://www.osi-saf.org/ . The user is strongly encouraged to register on this web site in order to receive the service messages and the latest information about the OSI SAF products.
The wind products are distributed in two resolutions: a 50-km resolution product with 25-km cell spacing and a 25-km resolution coastal product with 12.5-km cell spacing. In the coastal products the individual backscatter observations are not averaged using a Hamming spatial filtering (like in the
25 km grid spacing product) but using a boxcar filtering. The boxcar spatial filtering yields comparable wind characteristics in full sea regions and additionally more wind data closer to the coast. Both resolutions are available as a regional (mainly covering the Northern Hemisphere) EARS product with a timeliness of approximately 25 minutes from sensing time and as a global OSI SAF product with a timeliness of approximately 1.5-2 hours from sensing time. A global 12.5-km Hamming filter product was available for Metop-A only and it was discontinued in April 2015.
The scatterometer is an instrument that provides information on the wind field near the ocean surface, and scatterometry is the knowledge of extracting this information from the instrument’s output. Spacebased scatterometry has become of great benefit to meteorology and climate in the past years. This is
extensively described in the Algorithm Theoretical Basis Document; see [Ref1].
KNMI has a long experience in scatterometer processing and is developing generic software for this purpose. Processing systems have been developed for the ERS, NSCAT, SeaWinds and ASCAT scatterometers. Scatterometer processing software is developed in the EUMETSAT Numerical
Weather Prediction Satellite Application Facility (NWP SAF), whereas wind processing is performed operationally in the Ocean and Sea Ice SAF (OSI SAF) and in the EARS project.
EUMETSAT makes available near real-time Level 1b scatterometer products from the Metop-A and -B satellites through EUMETCast (global data) and through a private network (regional data). These products are used as basis for further processing at KNMI.
The OSI SAF and EARS products are delivered on request through the KNMI FTP server to all users and through the EUMETCast system. See also http://www.knmi.nl/scatterometer/ for real-time graphical examples of the products and up-to-date information and documentation.
This user manual outlines user information for the OSI SAF and EARS products based on the ASCAT
scatterometer. Section 2 presents a brief description of the ASCAT instrument and section 3 gives an
overview of the data processing configuration. Section 4 provides details on how to access the
product quality is elaborated.
This manual covers the following products:
• OSI SAF ASCAT 25-km wind product (OSI-102, acronym ASCAT25.
• OSI SAF ASCAT 12.5-km wind product (OSI-103, acronym ASCAT12), for Metop-A only, discontinued in April 2015, but still available from archive.
• OSI SAF ASCAT 12.5-km coastal wind product (OSI-104, acronym ASCAT12+)
• EARS ASCAT 25-km wind product (acronym EARS-ASCAT-25)
• EARS ASCAT 12.5-km coastal wind product (acronym EARS-ASCAT-12).
Products OSI-102 and OSI-103 also contain soil moisture information over land, the coastal and EARS products do not contain soil moisture information.
1.2. Disclaimer
All intellectual property rights of the OSI SAF and EARS products belong to EUMETSAT. The use of these products is granted to every interested user, free of charge. If you wish to use these products,
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SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual
EUMETSAT's copyright credit must be shown by displaying the words "copyright (year) EUMETSAT" on each of the products used.
The OSI SAF and EUMETSAT are much interested in receiving your feedback, would appreciate your acknowledgment in using and publishing about the data, and like to receive a copy of any publication about the application of the data. Your feedback helps us in maintaining the resources for the OSI
SAF wind services.
1.3. Useful links
KNMI scatterometer web site: http://www.knmi.nl/scatterometer/
Information on OSI SAF activities at KNMI: http://www.knmi.nl/scatterometer/osisaf/
Information on EARS activities at KNMI: http://www.knmi.nl/scatterometer/ears/
ASCAT visual products: http://www.knmi.nl/scatterometer/ascat_osi_25_prod/ , http://www.knmi.nl/scatterometer/ascat_osi_co_prod/ , http://www.knmi.nl/scatterometer/ascat_ear_25_prod/ , http://www.knmi.nl/scatterometer/ascat_ear_12_prod/ , http://www.knmi.nl/scatterometer/ascat_b_osi_25_prod/ , http://www.knmi.nl/scatterometer/ascat_b_osi_co_prod/ , http://www.knmi.nl/scatterometer/ascat_b_ear_25_prod/ , http://www.knmi.nl/scatterometer/ascat_b_ear_co_prod/
Information on EARS and EUMETCast: http://www.eumetsat.int/
O&SI SAF wind product documentation on http://www.osi-saf.org/ :
NWP SAF website: http://www.nwpsaf.org/
EUMETSAT ASCAT documentation (including ASCAT product guide): http://www.eumetsat.int/website/home/Satellites/CurrentSatellites/Metop/MetopDesign/ASCAT/index.h
tml
1.4. Limitations of the ASCAT winds
The following restrictions and limitations hold:
1) Although the Level 1 product is fully calibrated now using three transponders on the ground, the backscatter values are corrected using a calibration table, derived from a geophysical wind model. The backscatter values in the Level 2 wind product are however plain copies of those in the Level 1 product. The corrections are very small and expected to be partly incorporated into a new version of the Geophysical Model Function.
2) The backscatter data and noise values (K
p
) in the coastal product are computed as part of the level
2 wind processing and they are not scientifically validated, other than by validation of the wind retrieval properties in the coastal products.
These restrictions and limitations are subject to further study.
1.5. History of product changes
Here is an historical overview of the changes in the ASCAT wind products:
28-Mar-2007 OSI SAF ASCAT 25-km demonstration wind product available on EUMETCast.
ASCAT Wind Data Processor software version is 1_0i.
23-May-2007 Processing transferred to operational KNMI server.
10-Oct-2007 AWDP version 1_0k: adapted to the improved calibration of the Level 1 product. Wind product status is pre-operational now.
12-Dec-2007 AWDP version 1_0l: OSI SAF ASCAT 25-km winds are available on the GTS.
18-Mar-2008 AWDP version 1_0_13: adapted to the three-transponder calibration of the Level 1 product.
20-Nov-2008 AWDP version 1_0_15: change to neutral winds (0.2 m/s added to the wind speeds) and improved calibration of the level 1 product (activated at 2 December).
03-Dec-2008 OSI SAF ASCAT 25-km wind product has the operational status.
11-Dec-2008 EARS ASCAT 25-km and 12.5-km winds are available to all users.
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03-Mar-2009 OSI SAF ASCAT 12.5-km wind product is available with the operational status.
21-Apr-2009 AWDP version 1_0_17: upgrades in BUFR encoding.
01-Sep-2009 AWDP version 1_0_18: wind products are available in NetCDF now on the KNMI FTP server.
08-Sep-2009 EARS ASCAT data are available on the GTS.
12-Jan-2010 AWDP version 1_0_19: products in BUFR Edition 4 and up to four wind solutions present in 25-km BUFR products.
02-Feb-2010 OSI-SAF products disseminated on EUMETCast are also available to users in Africa and the Americas now.
28-Feb-2011 Both wind and soil moisture information are available in a multi-parameter BUFR product.
16-Aug-2011 AWDP version 2_1_00: up to four wind solutions present in the 12.5-km and coastal
BUFR products, use of NWP Ocean Calibration for more uniform wind characteristics across the swath.
23-Aug-2011 AHRPT data from a number of ground stations are now available in addition to the
EARS ASCAT data acquired at Svalbard.
18-Sep-2012 Implementation of Bayesian ice screening.
14-Nov-2012 First development version of ASCAT-B 25-km and coastal global wind products.
AWDP version is 2_1_01.
14-May-2013 AWDP version 2_2_00: preparation for level 1b data format change.
19-Jun-2013 AWDP version 2_2_01: preparation for ASCAT-B backscatter calibration change.
12-Feb-2014 AWDP version 2_3_00: preparation for change of Metop-A level 1 calibration
(activated at 12 March).
28-Apr-2015 The Metop-A global 12.5-km wind product was discontinued.
29-Mar-2016 The EARS 12.5-km wind products have been replaced by 12.5-km coastal wind products. ASCAT-A backscatter data correction to compensate for the instrument anomalies that occurred in autumn 2014.
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2. The ASCAT instrument
The Advanced SCATterometer (ASCAT) is one of the instruments carried on-board the Meteorological
Operational (Metop) polar satellites launched by the European Space Agency (ESA) and operated by the EUropean organisation for the exploitation of METeorological SATellites (EUMETSAT). Metop-A, the first in a series of three satellites, was launched on 19 October 2006, Metop-B was launched on 17
September 2012. Metop-C is planned to be launched approximately in 2017.
ASCAT is a real aperture radar using vertically polarised antennas. It transmits a long pulse with
Linear Frequency Modulation (‘chirp’). Ground echoes are received by the instrument and, after dechirping, the backscattered signal is spectrally analysed and detected. In the power spectrum, frequency can be mapped into slant range provided the chirp rate and the Doppler frequency are known. The above processing is in effect a pulse compression, which provides range resolution.
Two sets of three antennas are used to generate radar beams looking 45 degrees forward, sideways, and 45 degrees backwards with respect to the satellite's flight direction, on both sides of the satellite ground track. These beams illuminate approximately 550 km-wide swaths (separated by about 700 km) as the satellite moves along its orbit, and each provide measurements of radar backscatter from the sea surface on a 25 km or 12.5 km grid, i.e. each swath is divided into 21 or 41 so-called Wind
Vector Cells (WVCs). This brings the effective swath width to 525 km (21x25) or 512.5 km (41x12.5) for the 25-km and 12.5-km products, respectively. For each WVC, we obtain three independent backscatter measurements using the three different viewing directions and separated by a short time delay. As the backscatter depends on the sea surface roughness as a function of the wind speed and direction at the ocean surface, it is possible to calculate the surface wind speed and direction by using these 'triplets' within a mathematical model.
The instrument operates at a frequency of 5.255 GHz (C-band), which makes it rather insensitive to rain.
Figure 1: ASCAT wind scatterometer geometry (source: EUMETSAT web site).
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3. Processing scheme
KNMI has a processing chain running in near real-time with ASCAT data, including visualisation on the internet. This processor is based on the NWP SAF software and runs in the KNMI operational environment. The processing includes monitoring and archiving functionalities. A brief overview of the modules of the ASCAT scatterometer processor is given below. General information about the
scatterometer wind processing algorithms can be found in the ATBD [Ref1].
3.1. Backscatter averaging
In this step, which is performed only for the coastal product, the full resolution ASCAT level 1 product is used to re-compute backscatter values (
σ
0 s) in the Wind Vector Cells. The full resolution backscatter data are averaged using a spatial box filter rather than the Hamming filter that is used in the spatial averaging of the
σ
0 s of the nominal level 1 products. All full resolution
σ
0 s within 15 km
from the Wind Vector Cell centre are used in the averaging [Ref2]. Also the time difference between
the Wind Vector Cell time and the full resolution data acquisition time is considered to prevent mixing up of data from different orbits which may be close to the same location. Moreover, in Wind Vector
Cells close to the coast, only those full resolution position of the averaged
σ
0
σ
0 s are used that are entirely over sea. As the
is an averaged value of the positions of the full resolution
σ
0 s, the coastal
Wind Vector Cell is slightly displaced away from the coast. On the other hand, it is possible to compute winds as close as ~15 km from the coast, while in the nominal 12.5-km product, Wind Vector Cells
closer than ~35 km from the coast are flagged because of land contamination. See [Ref2] and [Ref3]
for more information on the coastal product.
3.2. Backscatter calibration
The backscatter values in the Level 1 product are calibrated by adding a WVC and beam dependent bias in dB to the incoming
σ
0 s. The calibration table was obtained by fitting the actual measurements
backscatter values are only available within the wind processing software; the
σ
0
data in the wind product are identical to those in the Level 1 product.
3.3. NWP collocation
KNMI receives NWP model data from ECMWF twice a day through the RMDCN.
NWP model sea surface temperature (SST) data are used to support the Bayesian sea ice
discrimination [Ref1]. The SST values of the four surrounding model grid points around the WVC
location are bilinearly interpolated. Note that the ECMWF model data do not contain SST values over land; if one or more of the four surrounding grid points has missing SST data, the SST value of the grid point closest to the WVC is taken. WVCs with a sea surface temperature above 5 °C are assumed to be always open water. The ice screening procedure may sometimes assign rainy WVCs erroneous as ice; using the extra SST criterion, WVCs in warmer areas will never be labelled as ice. Due to its rather high threshold value, the NWP SST ice screening will only be active in regions far away from the ice extents.
Land presence within each WVC is determined by using the land-sea mask available from the model data. The weighted mean value of the land fractions of all model grid points within 80 km of the WVC centre is calculated. The weight of each grid point scales with 1/r
2
, where r is the distance between the
WVC centre and the model grid point. If this mean land fraction value exceeds a threshold of 0.02, no wind retrieval is performed. Also the land fractions present in the beam information in the level 1b product are considered: if any land fraction in the fore, mid or aft beam exceeds 0.02, no wind retrieval is performed.
NWP forecast wind data are necessary in the ambiguity removal step of the processing. Wind forecasts are available twice a day (00 and 12 GMT analysis time) with forecast time steps of +3h,
+6h, …, +36h. The model wind data are linearly interpolated with respect to time and location and put
into the level 2 information part of each WVC (see section 5.2). Note that the ECMWF winds stored in
the wind products are real winds rather than neutral winds.
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3.4. Quality control and monitoring
In each WVC, the
σ
0
data is checked for quality and completeness and the inversion residual (see
[Ref1]) is checked. Degraded WVCs are flagged; see section 5.2 for more details.
An information file is made for each product. The content of the file is identical for each product and results from a compilation of all the global information concerning this product. From these files, various graphs are produced to visually display the confidence levels of the products and their evolution with time. These graphs are available in near-real time if you click on the ‘Monitoring information’ link on the product visualisation web pages. Data quality is also available to the users
within the products; see section 0 and 0 for a description of quality flags.
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4. Helpdesk, product dissemination and archive
For a swift response management procedure, user requests on the OSI SAF data products should be issued at the Ocean and Sea Ice SAF website ( http://www.osi-saf.org/ ). User requests on the EARS products can be sent to [email protected]
. User requests on the Soil Moisture content in the products can be sent to [email protected]
.
The ASCAT BUFR L2 products are disseminated on EUMETCast. Please consult http://www.eumetsat.int/ , under ‘Access to Data’ for more information on EUMETCast dissemination and how to receive these and other EUMETSAT meteorological satellite products, or contact [email protected]
.
The BUFR and NetCDF products are also made available on a password-protected ftp site (data from the last three days only). The access details are provided to new users by email request. Please send your requests to [email protected]
.
The Metop-A ASCAT 25-km global winds in BUFR format are disseminated on the GTS. The messages are distributed to the Exeter node and can be identified by: header (T1T2A1A2ii) =
ISXX[01-06]; CCCC = EHDB. The coastal winds are available on the GTS with identification header
(T1T2A1A2ii) = ISXX[11-16]; CCCC = EHDB. The EARS Metop-A ASCAT winds are also available on the GTS with identification header (T1T2A1A2ii) = ISXN[01-06]; CCCC = EHDB (25-km winds) and header (T1T2A1A2ii) = ISXN[11-16]; CCCC = EHDB (coastal winds).
A BUFR reader is available at www.knmi.nl/scatterometer/bufr_reader/ .
The OSI SAF ASCAT data are archived in the EUMETSAT Data Centre Archive, see http://www.eumetsat.int/Home/Main/DataAccess/EUMETSATDataCentre/index.htm?l=en (BUFR and
NetCDF). For data not (yet) present in the EUMETSAT Data Centre, KNMI also keeps an off line archive of the global products. You can send a request to [email protected]
.
The OSI SAF ASCAT data in NetCDF are also archived in the NASA Physical Oceanography
Distributed Active Archive Center (PO.DAAC) archive, see http://podaac.jpl.nasa.gov/datasetlist?ids=Sensor&values=ASCAT&search= .
The ASCAT 25-km global winds can be explored through the Enhanced Satellite Archive Dataminer
Naiad: http://www.naiad.fr/
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5. Data description
5.1. Wind product characteristics
Physical definition
Horizontal equivalent neutral wind vector at 10 m height (see [Ref1]).
Units and range
Wind speed is measured in m/s. The wind speed range is from 0-50 m/s, but wind speeds over 25 m/s
convention relative to North: 0 degrees corresponds to a wind flowing to the South with a clockwise increment. In the NetCDF products, the wind direction is in oceanographic convention: 0 degrees corresponds to a wind flowing to the North with a clockwise increment.
Input satellite data
The generation of ASCAT level 1b data by EUMETSAT is described in their technical documentation
[Ref6]. The global ASCAT data are acquired in Svalbard (Norway) and transmitted to the EUMETSAT
central processing facilities in Darmstadt, where they are processed up to level 1b. Regional EARS data are acquired at Svalbard and other ground stations, processed up to level 1b and then transmitted to KNMI via a dedicated private network. The product contains geo-located measurement triplets on a satellite swath WVC grid of 25 km or 12.5 km size.
Geographical definition
The Metop satellite flies in a near-polar sun synchronous orbit at 98 degrees inclination at approximately 800 km orbit height. The two satellite swaths are located to the left and to the right of the satellite ground track. The swath width is either 21 25-km size WVCs, corresponding to 525 km or
41 12.5-km size WVCs, corresponding to 512.5 km. Products are organised in rows of 42 or 82 WVCs, respectively.
Coverage
The OSI SAF products have global coverage. For the ascending Metop-A tracks, the EARS data correspond to the last 30 minutes of the X-band data dump when the satellite passes the Svalbard ground station. For the descending tracks, also AHRPT data from several ground stations are used, adding coverage in the European seas and Atlantic and Indian oceans. An up-to-date list of ground stations in use is available on http://www.eumetsat.int/Home/Main/Satellites/GroundNetwork/EARSSystem/EARS-
ASCAT/index.htm?l=en . Actual wind coverage is available on the OSI SAF and EARS ASCAT product visualisation websites (see http://www.knmi.nl/scatterometer/ ).
Output product
The input product in BUFR is processed into a BUFR output product including a unique wind solution
(chosen), its corresponding ambiguous wind solutions and quality information (distance to cone,
descriptors in the BUFR data format. The products are also available in NetCDF format; see section
Delivery time
A wind product is available for distribution within 10 minutes after the input product reception at KNMI.
For the global product, the delivery time between acquisition of the data and availability for the user ranges from 40 to 120 minutes. The regional product is available within 25 minutes after data acquisition. Timeliness statistics are available on the product visualisation websites, after clicking on the ‘Monitoring information’ link.
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Expected accuracy
The expected accuracy is defined as the expected bias and standard deviation of the primary calculations. The accuracy is validated against in situ wind measurements from buoys, platforms, or ship, and against NWP data. Even better, the errors of all NWP model winds, in situ data, and
scatterometer winds are computed in a triple collocation exercise [Ref7]. The performance is pretty
constant over the globe and depends mainly on the sub footprint wind variability. The performance of the products issued by the OSI SAF and EARS is characterised by a wind component standard deviation smaller than 2 m/s and a bias of less than 0.5 m/s in wind speed.
5.2. File formats
Wind products are in BUFR Edition 4 or in NetCDF format. A complete description of BUFR can be found in WMO publication No 306, Manual on Codes. The graphical displays of the wind products are available and explained on the web: see the links on http://www.knmi.nl/scatterometer/ .
The file name convention for the Level 2 BUFR product is ascat_YYYYMMDD_HHMMSS_SAT_ORBIT_SRV_T_SMPL(_CONT).l2_bufr, where
• ascat denotes the instrument
• YYYYMMDD denotes the date of the first data in the file
• HHMMSS denotes the time (UTC) of the first data in the file
• SAT denotes the satellite name: ‘metopa’ or ‘metopb’
• ORBIT is the orbit number (00000-99999)
• SRV is the service (‘eps’ for global OSI SAF or ‘ear’ for regional EARS)
• T is the processing type (‘o’ for operational, ‘t’ for test)
• SMPL is the WVC sampling (cell spacing): it contains ‘250’ or ‘125’, or ‘coa’ for the coastal product which has a WVC spacing of 12.5 km, as well.
• CONT (optional field) refers to the product contents: it contains ‘ovw’ for a product containing only
Ocean Vector Winds and no soil moisture information, CONT is omitted if the product contains both winds and soil moisture.
• l2_bufr (l is the lowercase L) denotes Level 2 product in BUFR
Examples of file names are ascat_20070213_021503_metopa_01653_eps_t_250.l2_bufr for a global test product containing soil moisture information, or ascat_20070213_021503_metopa_01653_ear_o_coa_ovw.l2_bufr for a regional operational product containing no soil moisture information.
The wind product is stored in the BUFR format as proposed for ASCAT and described in the WMO
Manual on Codes, a list of descriptors (fields) contained in each WVC is provided in section 0.
The NetCDF data have almost the same file name convention as the BUFR data, only the part
‘l2_bufr’ is replaced by ‘.l2.nc’, for example: ascat_20070213_021503_metopa_01653_eps_o_250_ovw.l2.nc
Contrary to the BUFR products, the NetCDF data do not contain backscatter information but only the level 2 wind (selected wind solution only) and sea ice information. They are intended to be an easy to
handle wind-only product, see section 10.
The BUFR data contain three main sections: level 1 information (fields 1-62), level 2 Soil Moisture information (fields 63-82) and level 2 wind information (fields 83 and up). The L1 information is simply copied into the L2 data, except for the coastal product, where the backscatter data are recalculated
can be found in the EUMETSAT ASCAT Product Guide, see the link in section 1.3. The Soil Moisture
data are produced by and under the responsibility of the EUMETSAT central facilities. The coastal product does not contain Soil Moisture information since it contains recalculated backscatter information which is not input to the Soil Moisture computations. In this way, inconsistency between the backscatter data and Soil Moisture in one product is avoided.
Field 2 (‘Identification of originating/generating sub-centre’) is set to 0 for OSI SAF products. For
EARS products, a value of 1 refers to X-band data dumps from Svalbard, whereas other values refer
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.
Field 84 (‘Generating Application’) contains the value 91 which means that first guess model winds are used for ambiguity removal. The interpolated model winds are in the fields 85-86.
The Wind Vector Cell Quality Flag (field 89, table 021155) has the following definitions:
Description
Reserved
BUFR bit Fortran bit
1 23
Not enough good sigma-0 available for wind retrieval
Poor azimuth diversity among sigma-0 for wind retrieval
Any beam noise content above threshold
Product monitoring not used
2
3
4
5
22
21
20
19
Product monitoring flag
KNMI quality control data rejection
Variational quality control data rejection
Some portion of wind vector cell is over land
Some portion of wind vector cell is over ice
Wind inversion not successful for wind vector cell
Reported wind speed is greater than 30 m/s
Reported wind speed is less than or equal to 3 m/s
6
7
8
9
10
11
12
13
18
17
16
15
14
13
12
11
Not used
Not used
No meteorological background used
Data are redundant
14
15
16
17
8
7
10
9
Distance to GMF too large
Reserved
18
19-23
6
5-1
Missing value All 24 set All 24 set
In Fortran, if the Wind Vector Cell Quality is stored in an integer I then use BTEST(I,NDW-NB) to test
BUFR bit NB, where NDW=24 is the width in bits of the data element in BUFR. The BTEST function is equivalent to (I/2^NF) modulo 2 where NF is the Fortran bit number.
If the ‘product monitoring not used’ bit, Fortran bit 19, is set to zero, the product is monitored. If the product is monitored and the ‘product monitoring flag’ bit, Fortran bit 18, is set to zero, the product is
value in all WVCs in one BUFR output file.
If the KNMI QC flag, Fortran bit 17, is set in a WVC this means that the backscatter information is of poor usability for various reasons, such as a too large inversion residual, or a too high noise value in the input product. WVCs in which the KNMI QC flag is set, are not used in the calculation of the analysis field in the ambiguity removal step. However, after the ambiguity removal the wind solution closest to the analysis field is chosen (if wind solutions are present in the WVC). This means that such a WVC may contain a selected wind solution, but it is suspect.
Land presence flag, Fortran bit 15, is set if a land fraction (see section 3.3) larger than zero is
calculated for the WVC. As long as the land fraction is below the limit value, a reliable wind solution may however still be present so there is normally no reason to reject WVCs with the land flag set.
Ice presence flag, Fortran bit 14, is set if the Bayesian sea ice screening algorithm calculates ice for
the WVC (see [Ref1]). Note that the products contain wind solutions also over sea ice regions. These
Page 14 of 23
SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual bogus winds are flagged both by the KNMI quality control flag and by the ice flag. Hence it is important to reject any winds with the KNMI quality control flag set when ingesting the products. Note that WVCs that are rejected due to a large inversion residual (e.g., in case of rain), only have the KNMI quality control flag set. On the other hand, WVCs that are rejected due to sea ice, have both the KNMI quality control flag and the ice flag set.
If the variational QC flag, Fortran bit 16, is set, the wind vector in the WVC is rejected during ambiguity removal due to spatial inconsistency. A wind solution is present, but it may be suspect.
The redundancy flag, Fortran bit 7, is set when a specific WVC has been sent out before. This is the case for WVCs which are present both in the regional EARS data stream and in the global OSI SAF data stream. In most cases, the EARS wind vector cell will be sent out earlier than the corresponding
OSI SAF wind vector cell and in such cases the redundancy flag will be set in the OSI SAF wind vector cell. Note that the OSI SAF global products still have full coverage and users not ingesting EARS-
ASCAT winds can simply ignore the redundancy flag. On the other hand, users who use both data streams can simply filter out any duplicate wind vector cells by evaluating the redundancy flag.
It is recommended not to use WVCs with the product monitoring flag, the KNMI quality control flag or
the variational quality control flag set. See [Ref1] for more information on product reliability.
The ‘likelihood computed for solution’ (descriptor 021104) actually contains the log
10
of the calculated likelihood for the wind solution. This is done since otherwise values close to zero will be rounded to zero in the BUFR encoding. In order to recalculate the probability, the user should compute 10 to the power <value from BUFR>.
Page 15 of 23
SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual
6. Data quality
As introduced in section 5.1, the accuracy should be better than 2 m/s in wind component standard
deviation with a bias of less than 0.5 m/s in wind speed.
Figure 2: Contoured histograms of the 25-km ASCAT wind product from Metop-A (top) and
Metop-B (bottom) vs. ECMWF model forecast winds.
Figure 2 shows two-dimensional histograms of the retrieved winds versus ECMWF 10m wind
data for these plots are from consecutive Metop-A and Metop-B orbits from 1 and 2 November 2012
(28 orbits from both satellites).
The top left plots correspond to wind speed (bins of 0.5 m/s) and the top right plots to wind direction
(bins of 2.5°). The latter are computed for ECMWF winds larger than 4 m/s. The bottom plots show the
u and v wind component statistics (bins of 0.5 m/s).
From these results, it is clear that the spread in the distributions is small. The wind speed biases are quite small, ~0.20 m/s. We obtain wind component standard deviations of 1.44 in u and 1.49 in v
Page 16 of 23
SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual directions, both for Metop-A and Metop-B. Note that the data in the plots do not include WVCs that are quality controlled, i.e. have a too large inversion residual.
Figure 3: Contoured histograms of the 25-km ASCAT wind product from Metop-A (top) and
Metop-B (bottom) vs. in situ buoy winds.
Figure 3 shows the results of collocations of ASCAT winds from Metop-A and Metop-B with buoy winds. These results cover the period of November 2012 to January 2013 (3 months). For more details
Metop-A and 0.05 m/s for Metop-B. Standard deviations of u and v wind components are 1.72 m/s and
1.76 m/s for Metop-A and 1.78 m/s and 1.80 m/s for Metop-B, respectively. These figures are all well within the OSI SAF requirements.
More validation information can be found in [Ref4] and [Ref5].
Page 17 of 23
SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual
7. References
[Ref1] OSI SAF, Algorithm Theoretical Basis Document for the OSI SAF wind products,
SAF/OSI/CDOP2/KNMI/SCI/MA/197 (*)
[Ref2] Verhoef, A., and A. Stoffelen, ASCAT coastal winds validation report, OSI SAF Report,
SAF/OSI/CDOP/KNMI/TEC/RP/176, 2011 (*)
[Ref3] Verhoef, A., M. Portabella and A. Stoffelen, High-resolution ASCAT scatterometer winds near the coast, IEEE Transactions on Geoscience and Remote Sensing, 2012, 50, 7, 2481-
2487, doi:10.1109/TGRS.2011.2175001
[Ref4] Verspeek, J., M. Portabella, A. Stoffelen and A. Verhoef, ASCAT Calibration and Validation,
OSI SAF Technical Report, SAF/OSI/CDOP/KNMI/TEC/TN/163 (*)
[Ref5] Verspeek, J., A. Verhoef and A. Stoffelen, ASCAT-B NWP Ocean Calibration and
Validation, OSI SAF Technical Report, SAF/OSI/CDOP2/KNMI/TEC/RP/199, 2013 (*)
[Ref6] EUMETSAT, ASCAT Level 1 Product Generation Function Specification,
EUM.EPS.SYS.SPE.990009
[Ref7] Thesis “Scatterometry” by Ad Stoffelen, 1998 (*)
References marked with a (*) are available on http://www.knmi.nl/scatterometer/publications/ .
Page 18 of 23
SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual
8. Abbreviations and acronyms
NSCAT
NWP
OSI SAF
PO.DAAC
QC
QuikSCAT
RMDCN
SAF
SeaWinds
SM
SOS
SST
AR
ASCAT
BUFR
EARS
EPS
Ambiguity Removal
Advanced Scatterometer
Binary Universal Format Representation
EUMETSAT Advanced Retransmission Service
EUMETSAT Polar System
ERS European Remote-Sensing Satellite
EUMETCast EUMETSAT’s Digital Video Broadcast Data Distribution System
EUMETSAT European Organisation for the Exploitation of Meteorological Satellites
HDF Hierarchical Data Format
JPL
KNMI
Jet Propulsion Laboratory (NASA)
Royal Netherlands Meteorological Institute
Metop
NASA
NetCDF
NOAA
Meteorological operational satellite
National Aeronautics and Space Administration (USA)
Network Common Data Form
National Oceanic and Atmospheric Administration (USA)
NASA Scatterometer
Numerical Weather Prediction
Ocean and Sea Ice SAF
Physical Oceanography Distributed Active Archive Center
Quality Control
USA dedicated scatterometer mission
u
v
WVC
Regional Meteorological Data Communication Network
Satellite Application Facility
Scatterometer on-board QuikSCAT platform (USA)
Soil Moisture
Scatterometer Ocean Stress
Sea Surface Temperature
West-to-east wind component
South-to-north wind component
Wind Vector Cell
Page 19 of 23
SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual
9. ASCAT BUFR data descriptors
Number Descriptor Parameter
40
41
42
43
36
37
38
39
30
31
32
33
34
35
44
45
46
47
48
49
50
51
26
27
28
29
22
23
24
25
16
17
18
19
20
21
12
13
14
15
8
9
10
11
4
5
6
7
1
2
3
021162
021163
021164
021165
021166
008085
002111
002134
021062
021063
021158
021159
021160
021161
021162
021163
021164
021165
021166
008085
002111
002134
005040
006034
010095
021157
021150
008085
002111
002134
021062
021063
021158
021159
021160
021161
001033
001034
025060
001007
002019
001012
004001
004002
004003
004004
004005
004006
005001
006001
005033
Identification Of Originating/Generating Centre
Identification Of Originating/Generating Sub-Centre
Software Identification
Satellite Identifier
Satellite Instruments
Direction Of Motion Of Moving Observing Platform
Year
Month
Day
Hour
Minute
Second
Latitude (High Accuracy)
Longitude (High Accuracy)
Pixel Size On Horizontal-1
Orbit Number
Cross Track Cell Number
Height Of Atmosphere Used
Loss Per Unit Length Of Atmosphere Used
Beam Collocation
Beam Identifier
Radar Incidence Angle
Antenna Beam Azimuth
Backscatter
Radiometric Resolution (Noise Value)
ASCAT Kp Estimate Quality
ASCAT Sigma-0 Usability
ASCAT Use Of Synthetic Data
ASCAT Synthetic Data Quality
ASCAT Satellite Orbit And Attitude Quality
ASCAT Solar Array Reflection Contamination
ASCAT Telemetry Presence And Quality
ASCAT Extrapolated Reference Function
ASCAT Land Fraction
Beam Identifier
Radar Incidence Angle
Antenna Beam Azimuth
Backscatter
Radiometric Resolution (Noise Value)
ASCAT Kp Estimate Quality
ASCAT Sigma-0 Usability
ASCAT Use Of Synthetic Data
ASCAT Synthetic Data Quality
ASCAT Satellite Orbit And Attitude Quality
ASCAT Solar Array Reflection Contamination
ASCAT Telemetry Presence And Quality
ASCAT Extrapolated Reference Function
ASCAT Land Fraction
Beam Identifier
Radar Incidence Angle
Antenna Beam Azimuth
Unit
Numeric
Numeric
Numeric
Numeric
Numeric
Code Table
Degree
Degree dB
%
Code Table
Code Table
Numeric
Numeric
Numeric
Numeric
Numeric
Numeric
Numeric
Code Table
Degree
Degree
Numeric
Numeric m dB/m
Flag Table
Code Table
Degree
Degree dB
%
Code Table
Code Table
Numeric
Numeric
Code Table
Code Table
Numeric
Code Table
Code Table
Degree True
Year
Month
Day
Hour
Minute
Second
Degree
Degree m
Page 20 of 23
SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual
Number Descriptor Parameter
72
73
74
75
76
77
78
79
68
69
70
71
64
65
66
67
56
57
58
59
52
53
54
55
60
61
62
63
92
93
94
95
87
88
89
90
91
80
81
82
83
84
85
86
96
97
98
99
100
025062
040001
040002
021062
021151
021152
021153
021154
021062
021088
040003
040004
040005
040006
040007
020065
021062
021063
021158
021159
021160
021161
021162
021163
021164
021165
021166
025060
040008
040009
040010
025060
001032
011082
011081
020095
020096
021155
021101
021102
031001
011012
011011
021156
021104
011012
011011
021156
021104
Backscatter
Radiometric Resolution (Noise Value)
ASCAT Kp Estimate Quality
ASCAT Sigma-0 Usability
ASCAT Use Of Synthetic Data
ASCAT Synthetic Data Quality
ASCAT Satellite Orbit And Attitude Quality
ASCAT Solar Array Reflection Contamination
ASCAT Telemetry Presence And Quality
ASCAT Extrapolated Reference Function
ASCAT Land Fraction
Software Identification
Database Identification
Surface Soil Moisture (Ms)
Estimated Error In Surface Soil Moisture
Backscatter
Estimated Error In Sigma0 At 40 Deg Incidence Angle
Slope At 40 Deg Incidence Angle
Estimated Error In Slope At 40 Deg Incidence Angle
Soil Moisture Sensitivity
Backscatter
Wet Backscatter
Mean Surface Soil Moisture
Rain Fall Detection
Soil Moisture Correction Flag
Soil Moisture Processing Flag
Soil Moisture Quality
Snow Cover
Frozen Land Surface Fraction
Inundation And Wetland Fraction
Topographic Complexity
Software Identification
Generating Application
Model Wind Speed At 10 m
Model Wind Direction At 10 m
Ice Probability
Ice Age (A-Parameter)
Wind Vector Cell Quality
Number Of Vector Ambiguities
Index Of Selected Wind Vector
Delayed Descriptor Replication Factor
Wind Speed At 10 m
Wind Direction At 10 m
Backscatter Distance
Likelihood Computed For Solution
Wind Speed At 10 m
Wind Direction At 10 m
Backscatter Distance
Likelihood Computed For Solution
Unit
dB
%
Code Table
Code Table
Numeric
Numeric
Numeric
Numeric
Numeric
Numeric
Numeric
Numeric
Numeric
%
% dB dB dB/Degree dB/Degree dB dB dB
Numeric
Numeric
Flag Table
Flag Table
%
%
%
%
%
Numeric
Code Table m/s
Degree True
Numeric dB
Flag Table
Numeric
Numeric
Numeric m/s
Degree True
Numeric
Numeric m/s
Degree True
Numeric
Numeric
Note that descriptor numbers 93-96 can be repeated 1 to 144 times, depending on the value of the
Delayed Descriptor Replication Factor (descriptor number 92)
Page 21 of 23
SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual
10. NetCDF data format
The ASCAT wind products are also available in the NetCDF format, with the following characteristics:
• The data are organised in full orbits rather than in 3-minute granules.
• The data format meets the NetCDF Climate and Forecast Metadata Convention version 1.4
( http://cfconventions.org/ ).
• The data contain, contrary to the BUFR data, only Level 2 wind and sea ice information, no sigma0 nor soil moisture information. The aim was to create a compact and easy to handle product for oceanographic and climatological users.
• The data contain only the selected wind solutions, no ambiguity information.
• The wind directions are in oceanographic rather than meteorological convention (see section 5.1)
• The format is usable for ASCAT, ERS, QuikSCAT and any other scatterometer data.
• The data has file sizes comparable to those of the corresponding BUFR data (e.g., one orbit of
ASCAT 25-km wind data is 2.6 MB in BUFR and 2.2 MB in NetCDF). When compressed with gzip, the size of one orbit in NetCDF reduces to ~820 kB.
• The NetCDF data in near real-time are only available on the KNMI FTP server, but EUMETCast dissemination can be considered on user request.
The file name convention for the gzipped NetCDF product is ascat_YYYYMMDD_HHMMSS_SAT_ORBIT_SRV_T_SMPL_VERS(_CONT).l2.nc.gz where the
meaning of the fields is identical to those in the BUFR file names (see section 5.2). Note that in
NetCDF the SRV is always “eps” (global data) and the CONT is always “ovw” (Ocean Vector Winds).
The VERS part of the file name denotes the software version. A file name example is: ascat_20090826_051502_metopa_14797_eps_o_250_1018_ovw.l2.nc.gz
Below are some meta data contained in the NetCDF data files: dimensions:
NUMROWS = 1581 ;
NUMCELLS = 42 ; variables:
int time(NUMROWS, NUMCELLS) ;
time:long_name = "time" ;
time:units = "seconds since 1990-01-01 00:00:00" ;
int lat(NUMROWS, NUMCELLS) ;
lat:long_name = "latitude" ;
lat:units = "degrees_north" ;
int lon(NUMROWS, NUMCELLS) ;
lon:long_name = "longitude" ;
lon:units = "degrees_east" ;
short wvc_index(NUMROWS, NUMCELLS) ;
wvc_index:long_name = "cross track wind vector cell number" ;
wvc_index:units = "1" ;
short model_speed(NUMROWS, NUMCELLS) ;
model_speed:long_name = "model wind speed at 10 m" ;
model_speed:units = "m s-1" ;
short model_dir(NUMROWS, NUMCELLS) ;
model_dir:long_name = "model wind direction at 10 m" ;
model_dir:units = "degree" ;
short ice_prob(NUMROWS, NUMCELLS) ;
ice_prob:long_name = "ice probability" ;
ice_prob:units = "1" ;
short ice_age(NUMROWS, NUMCELLS) ;
ice_age:long_name = "ice age (a-parameter)" ;
ice_age:units = "dB" ;
Page 22 of 23
SAF/OSI/CDOP/KNMI/TEC/MA/126 OSI SAF/EARS ASCAT Wind Product User Manual
int wvc_quality_flag(NUMROWS, NUMCELLS) ;
wvc_quality_flag:long_name = "wind vector cell quality" ;
wvc_quality_flag:flag_masks = 64, 128, 256, 512, 1024, 2048, 4096,
8192, 16384, 32768, 65536, 131072, 262144, 524288, 1048576, 2097152, 4194304 ;
wvc_quality_flag:flag_meanings = "distance_to_gmf_too_large data_are_redundant no_meteorological_background_used rain_detected rain_flag_not_usable small_wind_less_than_or_equal_to_3_m_s large_wind_greater_than_30_m_s wind_inversion_not_successful some_portion_of_wvc_is_over_ice some_portion_of_wvc_is_over_land variational_quality_control_fails knmi_quality_control_fails product_monitoring_event_flag product_monitoring_not_used any_beam_noise_content_above_threshold poor_azimuth_diversity not_enough_good_sigma0_for_wind_retrieval" ;
short wind_speed(NUMROWS, NUMCELLS) ;
wind_speed:long_name = "wind speed at 10 m" ;
wind_speed:units = "m s-1" ;
short wind_dir(NUMROWS, NUMCELLS) ;
wind_dir:long_name = "wind direction at 10 m" ;
wind_dir:units = "degree" ;
short bs_distance(NUMROWS, NUMCELLS) ;
bs_distance:long_name = "backscatter distance" ;
bs_distance:units = "1" ;
// global attributes:
:title = "MetOp-A ASCAT Level 2 25.0 km Ocean Surface Wind Vector Product" ;
:title_short_name = "ASCAT-L2-25km" ;
:Conventions = "CF-1.4" ;
:institution = "EUMETSAT/OSI SAF/KNMI" ;
:source = "MetOp-A ASCAT" ;
:software_identification_level_1 = 702 ;
:instrument_calibration_version = 0 ;
:software_identification_wind = 1018 ;
:pixel_size_on_horizontal = "25.0 km" ;
:service_type = "eps" ;
:processing_type = "O" ;
:contents = "ovw" ;
:granule_name = "ascat_20090826_051502_metopa_14797_eps_o_250_1018_ovw.l2.nc" ;
:processing_level = "L2" ;
:orbit_number = 14797 ;
:start_date = "2009-08-26" ;
:start_time = "05:15:02" ;
:stop_date = "2009-08-26" ;
:stop_time = "06:53:56" ;
:equator_crossing_longitude = " 244.606" ;
:equator_crossing_date = "2009-08-26" ;
:equator_crossing_time = "05:12:26" ;
:rev_orbit_period = "6081.7" ;
:orbit_inclination = "98.7" ;
:history = "N/A" ;
:references = "ASCAT Wind Product User Manual, http://www.osi-saf.org/, http://www.knmi.nl/scatterometer/" ;
:comment = "Orbit period and inclination are constant values. All wind directions in oceanographic convention (0 deg. flowing North)" ;
:creation_date = "2009-08-26" ;
:creation_time = "08:31:31" ;
Page 23 of 23
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