MERCATOR OCEAN JOURNA:
SEPTEMBER 2021
1.3 Toward more wave parameters
SAR measurements are processed in a single type of product:
Level-3 SPC. It consists in both along-track and along swell-
oath wave integral parameters, derived from Sentinel-1A and
-1B missions. The dataset parameters include partition SWH,
partition peak period and partition peak or principal direction
given along swell propagation path in space and time at a
3-hour timestep, from source to land.
This product is proposed in two different formats:
öbservations grouped according to the initial storm event
they originate from or grouped in 3-hour files according to
their observation time. This last format was introduced in
2019 as required by numerical wave modelers for data
assimilation.
In 2019, a better characterization of long swell was also
introduced in the Level-3 processing to deal with the
Level-2 inherited inability to properly estimate the swel.
propagation direction for the longest swell systems.
An important work was also initiated to integrate spectral
parameters derived from CFOSAT off-nadir SWIM instrument.
This new Level-3 dataset should become operational to all
users in 2021. This new source of data will complement the
Sentinel-1 mission already existing products by providing
swell observations on all ocean basins, including North
Atlantic, and with different limitations than those of SAR
(especially shortest and azimuth propagating swells). This
will be the first inclusion of measurements from another
mission concept in the L3 SPC products, which will require a
careful intercomparison and inter-calibration.
2. STATUS AT THE END OF COPERNICUS 1
At the end of Copernicus 1, the WAVE-TAC is delivering three
NRT wave products (see Figure 2), including SWH and spectral
parameters, derived from a constellation of nine satellites.
The spatio-temporal coverage of the Level-3 SWH product
was significantly increased with the integration of a total of
7 altimeters, including the Copernicus Sentinel-3A/B
‚nterleaved missions. Only valid measurements are
jisseminated, and the consistency between measurements
ıs guaranteed by the cross-calibration onto the reference
mission (Jason-3) and onto in-situ measurements. NRT
Jata are usually available 3 to 4 hours after the actuaı
acquisition, enabling their assimilation in forecasting
systems. Also, the high number of qualified measurements
and associated wind field directly benefit wave simulations
and ensure an increased resilience of the system when a
mission Is temporarily unavallable.
The gridded Level-4 SWH product also benefited from the
high number of Level-3 measurements and provides user-
friendly maps, containing different daily statistics and an
instantaneous estimate of the mid-day wave height field
The Level-3 SPC product based on Sentinel-1’s constellation
currently delivers partitioned wave spectra at observation
time as well as integral parameters (partition significant
wave height, partition peak period and partition peak or
orincipal direction) given along swell propagation path in
space and time at a 3-hour timestep, from source to land.
Quality flags are also included for each parameter and
indicate the valid time steps along propagation (e.g., no
propagation for SWH close to a storm source or any integraı
parameter when reaching the land). The integral parameters
at observation points are also available together with a
quality flag based on the consistency between each
propagated observation and the overall swell field.
Since the creation of the WAVE-TAC, the quality and quantity
of data has been continuously improved. New fields (quality
flags, uncertainty, wind speed) were added to match evolving
user's needs. The validation approach was reinforced by
zomparing satellite measurements not only with other
satellites, but also with in-situ measurements and simulation
autputs. Facilitating the uptake of Copernicus Marine Service
Wave products is essential for a broader utilization by both
internal and external users. Along-track altimeter and SAR
products are well known In the assimilation community, but
their spatio-temporal sampling requires some expertise for
new users. Therefore, the WAVE-TAC took the opportunity to
zommunicate on the wave products and their evolution and
Juality at international scientific conferences and during a
dedicated Wave Group / TWAPAS (Tailored WAve Products
for Assimilation Systems) meeting