Abstract
Sea-ice biophysical properties are characterized by high spatio-temporal variability ranging from the meso- to the millimeter scale. Ice coring is a common yet coarse point sampling technique that struggles to capture such variability in a non-invasive manner. This hinders quantification and understanding of ice algae biomass patchiness and its complex interaction with some of its sea ice physical drivers. In response to these limitations, a novel under-ice sled system was designed to capture proxies of biomass together with 3D models of bottom topography of land-fast sea-ice. This system couples a pushbroom hyperspectral imaging (HI) sensor with a standard digital RGB camera and was trialed at Cape Evans, Antarctica. HI aims to quantify per-pixel chlorophyll-a content and other ice algae biological properties at the ice-water interface based on light transmitted through the ice. RGB imagery processed with digital photogrammetry aims to capture under-ice structure and topography. Results from a 20 m transect capturing a 0.61 m wide swath at sub-mm spatial resolution are presented. We outline the technical and logistical approach taken and provide recommendations for future deployments and developments of similar systems. A preliminary transect subsample was processed using both established and novel under-ice bio-optical indices (e.g., normalized difference indexes and the area normalized by the maximal band depth) and explorative analyses (e.g., principal component analyses) to establish proxies of algal biomass. This first deployment of HI and digital photogrammetry under-ice provides a proof-of-concept of a novel methodology capable of delivering non-invasive and highly resolved estimates of ice algal biomass in-situ, together with some of its environmental drivers. Nonetheless, various challenges and limitations remain before our method can be adopted across a range of sea-ice conditions. Our work concludes with suggested solutions to these challenges and proposes further method and system developments for future research.
Highlights
Sea-ice biophysical properties play a central role in controlling primary production and ecosystem function within the polar oceans [1,2,3]
Ice algal biomass has been linked to sea-ice structure, under-ice roughness, and their complex interplay with the biogeochemical properties of the water column controlled by currents and boundary layer exchange processes [9,10,11,12,13]
normalized difference indices (NDIs) values outputted are observed to match the range of values over the same or similar sea-ice areas [48] and principal component analysis (PCA) loadings shown strong similarities in shape if compared with results from other studies both in real sea ice and in artificial ice tanks [7,27]; the difference being that in this study they were retrieved on a sub-mm per-pixel basis
Summary
Sea-ice biophysical properties play a central role in controlling primary production and ecosystem function within the polar oceans [1,2,3]. Primary physical properties of the sea-ice environment include snow depth, ice thickness, sea-ice texture/structure, and under-ice topography. Ice algal biomass is strongly dependent on sea-ice physical properties, and both show variability at multiple spatial and temporal scales [4,5,6]. The spatio-temporal variability of ice biological properties is determined by some of the sea ice physical properties such as snow depth and ice thickness, governing light availability for the organisms. Ice algal biomass has been linked to sea-ice structure, under-ice roughness, and their complex interplay with the biogeochemical properties of the water column controlled by currents and boundary layer exchange processes [9,10,11,12,13]
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