TY - CHAP A1 - Gupana, Remika A1 - Ziemba, Alexander A1 - El Serafy, Ghada T1 - Quantification of Benthic Phytoplankton using Remote Sensing and Machine Learning in the Wadden Sea T2 - European Geosciences Union, General Assembly 2018, Vienna, Austria N2 - One of the main indicators of ecosystem stability in coastal regions is the occurrence and distribution of primary producers. In the intertidal flats of the Wadden Sea, benthic phytoplankton such as microphytobenthos are significant primary providers of energy. However, the Wadden Sea monitoring data inventory states that there is low availability of microphytobenthos data despite its high demand. To address this gap, a remote sensing approach coupled with data fusion through machine learning using the Random Forest algorithm was adopted and developed. This study also maximized existing datasets to demonstrate other possible applications of such data and subsequently, the added practical value these datasets offer. Microphytobenthos thrive in areas where the sediments have high mud and nutrient content. These organisms are also known to aid in sediment stability due to excreted extracellular polymeric substances. Following this rationale, it was assumed that sediment grain size, Total Suspended Matter (TSM), Chlorophyll-a (Chl-a) and Photosynthetically Active Radiation (PAR) can be combined in determining microphytobenthos occurrence. The microphytobenthos model derived using Random Forest algorithm has the following input parameters: sediment grain size map derived from Landsat images, MERIS Products TSM, Chl-a and PAR. The benthic diatom model from Het Koninklijk Nederlands Instituut voor Onderzoek der Zee (NIOZ) was used as baseline data for the training model. Another scenario was considered using TSM and Chl-a modelling output from the Generic Ecological Model-Algal Bloom (GEM/BLOOM) model. Two main training models were derived from the microphytobenthos prediction algorithm. These models were distinct from each other; in that the first model had a higher and wider microphytobenthos concentration range (0 – 7000 mg C m-2) and the second model had a lower and narrower range (0 —- 1000 mg C m-2) suitable for warmer and colder time periods, respectively. Although more extensive data is required to further validate this procedure, this alternative method has proven to be a feasible non-invasive technique to quantify microphytobenthos while utilizing existing datasets. Y1 - 2018 UR - https://meetingorganizer.copernicus.org/EGU2018/EGU2018-16069.pdf N1 - EGU2018-16069-1 N1 - This work has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No 641762. PB - European Geophysical Society CY - Katlenburg-Lindau ER - TY - GEN A1 - Varrani, Arianna A1 - Nones, Michael A1 - Gupana, Remika T1 - Long-term modelling of fluvial systems at the watershed scale: Examples from three case studies T2 - Journal of Hydrology N2 - To date, many numerical approaches are available in studying water flow and sediment dynamics along rivers from the reach to the watershed scale, based on various simplifications. The aim of the present research is to demonstrate how the so-called “morphodynamic quasi-equilibrium hypothesis” is effective in modelling riverine landscape morphodynamics evolution at the watershed scale, focussing on the long-term changes of longitudinal profile and bed grainsize composition of large alluvial rivers. A lumped 0-D, two-reach, two-grainsize model based on the Local Uniform Flow hypothesis and originally developed for reproducing fluvial changes at the historical time-scale, has been applied to three large watercourses to reproduce their long-term evolution, performing a sensitivity analysis based on the present conditions. Three morphometric parameters were analysed, aiming to describe the evolution of the longitudinal profile (concavity and aggrading) and the grainsize composition of the river bed (fining). Though the 0-D approach does not allow for a spatial distribution of the input parameters, namely the liquid and solid discharge, the modelling outcomes show reasonably good qualitative trends. At the scale of analysis (centuries to millennia) and for the chosen large sedimentary systems (thousands of kilometres long), which show high inertia to geomorphological changes likely owing to their longitudinal scale, the model can be helpful in detecting where the present conditions reflect a big disturbance to the “natural” trend. This initial detection method can provide additional insights in evaluating the capability of actual rivers to respond to the present external forcing, eventually reaching a quasi-stable configuration. KW - 0-D model KW - Riverbed aggrading KW - Riverbed fining KW - Congo River KW - Large rivers KW - Mississippi River KW - Morphodynamic equilibrium KW - Orinoco River KW - River concavity Y1 - 2019 U6 - https://doi.org/10.1016/j.jhydrol.2019.05.012 SN - 0022-1694 VL - 574 SP - 1042 EP - 1052 ER -