Here, below: Introduction, Mission objectives, Heritage, Instrument description, Atmospheric composition products, List of TROPOMI data products, More information?. This WebPage is mostly based on Veefkind et al. (2012), and ESA & KNMI TROPOMI websites (see below).
The TROPOspheric Monitoring Instrument (TROPOMI) is the single sensor on board of the Copernicus Sentinel-5 Precursor satellite. The Sentinel-5 Precursor (S5p) is the first of the atmospheric composition Sentinels (i.e. long-time series of operational satellite missions supporting the Copernicus programme), launched in 2017, for a nominal lifetime of 7 years. Sentinel-5 Precursor, is a gap-filler and a preparatory programme covering products and applications for Sentinel-5. The S5P mission will fill the gap between the end of the OMI and SCIAMACHY exploitation and the Sentinel-5 mission.
The TROPOMI science objectives (Van Weele et al., 2008) are:
1. To better constrain the strength, evolution, and spatio-temporal variability of the sources of trace gases and aerosols impacting air quality and climate.
2. To improve upon the attribution of climate forcing by a better understanding of the processes controlling the lifetime and distribution of CH4 – Methane, tropospheric O3 – Ozone, and aerosols.
3. To better estimate long-term trends in the troposphere related to air quality and climate from the regional to the global scale.
4. To develop and improve air quality model processes and data assimilation in support of operational services including air quality forecasting and protocol monitoring.
TROPOMI is then expected to provide accurate and timely observations of key atmospheric species, for services on air quality, climate forcing (including non-CO2 – Carbon dioxide emissions), UV and the O3 – Ozone layer. The daily global observations will be used for improving air quality forecasts as well as for monitoring the concentrations of atmospheric constituents. Trend monitoring is very important to verify that policies implemented to control emissions to the atmosphere are effective. In addition, TROPOMI will also contribute to services on volcanic ash for aviation safety, warnings for high levels of UV radiation that can cause skin damage, and to numerical weather prediction.
With its global coverage and open data policy, the mission is an essential contribution for providing critical information to services and decision makers to improve the life and atmospheric composition of European citizens, and our knowledge of important chemical and dynamical processes in the atmosphere.
The Royal Netherlands Meteorological institute (KNMI), via Dr. Pepijn Veefkind as Principal Investigator (PI), & the Netherlands Space institute (SRON) are responsible for processing TROPOMI’s raw data and retrieving geophysical variables. The Dutch space industry has set a new standard for satellite instruments. Without TROPOMI, there would be a gap of several years when it comes to monitoring gasses in the troposphere (the lowest part of the atmosphere and the air that we live in). Dutch climate researchers have signaled this problem, taking the initiative to build TROPOMI. The European Space Agency (ESA) is leading the development of a satellite system encompassing the spacecraft, accommodation of the TROPOMI payload (jointly developed by The Netherlands and ESA), a basic ground segment and the launch and in-orbit commissioning.
The Netherlands has been designing and building satellite atmospheric sensors, such as those carried on ERS and Envisat, since the 1990s. Building on this technical heritage, TROPOMI – the most advanced multi-spectral imaging spectrometer to date (2017) – was developed jointly by ESA and the Netherlands Space Office (NSO).
TROPOMI succeeds the current Ozone Monitoring Instrument (OMI) (Levelt et al., 2006) and past SCanning Imaging Absorption spectroMeter for Atmospheric CartograpHY) (SCIAMACHY) (Bovensmann et al., 1999). It should be then followed by the operational Sentinel-5 mission starting after 2020. In addition, the early afternoon observations of TROPOMI have strong synergy with the morning observations of Global Ozone Monitoring Experiment 2 (GOME-2). Although GOME-2 has a lower spatial resolution and doesn’t have the SWIR spectral range, the combination of TROPOMI and GOME-2 allows observing diurnal variations, as successfully shown with the OMI-SCIAMACHY combination (Boersma et al., 2008).
The combination of TROPOMI and GOME-2 is a first step toward higher temporally resolved observations over Europe starting in 2019-2020 with the Sentinel-4 mission on the geostationary Meteosat Third Generation (MTG) sounder platform (Ingmann et al., 2012). In addition to the GOME-2 synergy, there is also a synergy between TROPOMI and the American Soumi National Polar-orbiting Partnership (NPP) satellite. Identified synergies include the use of the Visible/Infrared Imager Radiometer Suite (VIIRS) for high spatially resolved cloud information and Ozone Monitoring and Profiling Suite (OMPS) for high vertically resolved stratospheric O3 – Ozone profiles. It is planned to fly the S5P mission within approximately 5 min of NPP, thus building upon the successes of the “A-Train” constellation of Earth observation satellites (L’Ecuyer & Jiang, 2010).
TROPOMI measures the Solar light in the ultraviolet and visible (270–500 nm), near-infrared (675–775 nm) and shortwave infrared (2305–2385 nm) spectral bands. The spectral resolution lies in the range of 0.25-0.55 nm. With a spatial resolution as high as 7 km × 3.5 km and in a nadir pointing observation mode, it has the potential to detect air pollution over individual mega-cities. The daily-global coverage is ensured by a swath width of 2600 km.
The instrument images a strip of the Earth on a two dimensional detector for a period of 1 s during which the satellite moves by about 7 km. This strip has dimensions of approximately 2600 km in the direction across the track of the satellite and 7 km in the along track direction. After the 1 second measurement a new measurement is started, thus the instrument scans the Earth as the satellite moves. The two dimensions of the detector are used to detect the different ground pixels in the across track direction and for the different wavelengths. The light is separated in the different wavelengths using grating spectrometers. TROPOMI has four different detectors for the different spectral bands.
The payload mass is 200 kg.
As compared to the OMI instrument, TROPOMI has extended the wavelength range with bands in the Near InfraRed (NIR) and in the SHort-Wave InfraRed (SWIR). The primary objective of the NIR band is to perform a better cloud correction of trace gas retrievals. The deeper oxygen A band (758–770 nm) contains significantly more information on clouds, including cloud pressure and cloud fraction, compared to the weak O2–O2 band (460–485 nm) that is used for this purpose in OMI. The SWIR band at 2.3 um has been added for observations of CO – Carbon monoxide and CH4 – Methane. Furthermore, improvements in signal-to-noises are of factor of 2-5 compared to OMI and SCIAMACHY (Veefkind et al., 2012).
Atmospheric composition products
TOPOMI instrument is expected to deliver information about a wide range of pollutants gases such as NO2 – Nitrogen dioxide, O3 – Ozone, HCHO – Formaldehyde, SO2 – Sulphur dioxide, and CO – Carbon monoxide, the important green-house gas CH4 – Methane and aerosol particles. Effective cloud parameters will be also monitored.
List of TROPOMI data products
The TROPOMI Level 2 data products are generated within the Copernicus ground system and are listed in the table below. There are three different data streams: the near-real-time (NRT) stream, the Off-line stream and the Reprocessing stream. NRT data are available within 3 hours after data acquisition and intended for users that need quick access to the data. NRT data may be incomplete and may not have the full data quality. Most data users should use the off-line data, available within a few days after acquisition, or the latest version of reprocessed data. The data products contain information on the data quality for each TROPOMI ground pixel.
- Tropomi.eu website maintained by KNMI R&D Satellite Observations here
- Public TROPOMI website maintained by the Netherlands here
- European Space Agency (ESA) Sentinel-5 Precursor / TROPOMI website here
- ESA Sentinel-5 Precursor launch campaign blog here
- Veefkind et al., 2012: Veefkind, J. P., Aben, E. A. A., McMullan, K., Forster, H., de Vries, J., Otter, G., … Visser, H.: TROPOMI on the ESA Sentinel-5 Precursor: A GMES mission for global observations of the atmospheric composition for climate, air quality and ozone layer applications. Remote Sensing of Environment, 120(SI), 70-83. DOI: 10.1016/j.rse.2011.09.027, 2012.
- Ingmann, P., Veihelmann, B., Langen, J., Lamarre, D., Stark, H., and Courrèges-Lacoste, G. B.: Requirements for the GMES Atmosphere Service and ESA’s implementation concept: Sentinels-4/-5 and -5p, Remote Sens. Environ., 120, 58–69, doi:10.1016/j.rse.2012.01.023, 2012.
- NO2 – Nitrogen dioxide WebPage here
- Aerosols WebPage here
- CO – Carbon monoxide WebPage here
- CH4 – Methane WebPage here