Monitoring Lake Primary Production using the PACE satellite (Lake3P)PI: Daniel Odermatt - Swiss Federal Institute of Aquatic Science and Technology
Co-Is: Mortimer Werther (Eawag - Swiss Federal Institute of Aquatic Science and Technology); Abolfazl Irani Rahaghi (Eawag - Swiss Federal Institute of Aquatic Science and Technology); Alexander Damm (University of Zurich); Natacha Pasche (Swiss Federal Institute of Technology Lausanne); Camille Minaudo (University of Barcelona); Evangelos Spyrakos (University of Stirling); Krista Alikas (University of Tartu); Tuuli Soomets (University of Tartu)
Re-oligotrophication is the process to reverse the effects of eutrophication. In order to facilitate the recovery of lakes, a measure of primary production (PP) is essential to identify and monitor the sources that cause phytoplankton growth. Commonly, the concentration of the phytoplankton pigment chlorophyll-a (Chla) is used to estimate PP indirectly. However, the relation of Chla to PP is prone to large uncertainty. Bio-optical models that use inherent optical properties (IOPs) to estimate PP are thus favoured but require an accurate characterisation of the target water conditions. An IOP-based approach to estimate PP was successfully demonstrated using Envisat-MERIS data of Lake Geneva (Switzerland), and it is currently adopted for Sentinel-3 OLCI data over the entirety of Switzerland. The PACE-OCI sensor marks an unprecedented opportunity in terms of its spectro-radiometric sampling properties, and it unlocks a huge potential for improved PP monitoring in large lakes.
Our PACE contribution is to develop and provide a hyperspectral PP model for lakes based on pigment absorption, diffuse attenuation and photosynthetically available radiation. For the model development we investigate the detailed optical-biogeochemical conditions driving model performance. PP model development sites are Lake Geneva on the border of France and Switzerland, the largest lake in Western Europe, and Lake Greifensee close to Zurich. Lake Geneva and Greifensee are characterised by meso-eutrophic states and thus strongly benefit from active re-oligotrophication programmes. Visibility in Lake Geneva varies between 5 and 20 meters and is often larger than the stratification depth. It therefore constitutes an appropriate target for investigating vertical variations as seen by optical satellite sensors like OCI.
In order to develop a novel retrieval method in time for the launch of PACE, we use several data sources:
- OCI-simulated data distributed by NASA
- OCI-analog data acquired through own airborne campaigns using the imaging spectrometer AVIRIS NG
- Automated in situ measurements taken on the LÃ©XPLORE (https://lexplore.info/) research platform using a SeaBird Thetis profiler
- An underwater flow-through system installed on LÃ©XPLORE
- Field campaigns in both Lake Geneva and Greifensee in conjuncture with laboratory analyses