Unmanned Vehicles for Autonomous Sensing and Sensing

In the global warming process the Arctic region is heating up faster than other places on Earth. This has brought to a rapid environmental change which is increasingly evident in the observations of many geophysical and biological properties. The interactions between atmosphere, ocean, cryosphere and biosphere are responsible for the phenomenon of "Arctic amplification". The complex system of interactions involving heat exchanges and water cycle (vapor and liquid) in the Arctic Ocean that is generated by these climate changes is at the base of the instabilities inducing large uncertainties and errors in climate models. Within this scene extreme and unpredictable events, especially the collapse of the ice sheets, appear to be not so remote. The ARCA project aims to develop a conceptual model on the mechanism(s) behind the release of large volumes of cold and fresh water from melting of ice caps, investigating this complex system from both paleoclimatic and modern air-sea-ice interaction process point of view. Ice process of melting depends on the energy balance at the surface of the glaciers which is controlled by mutual interactions between the atmosphere and the surface of the glacier thus depending on weather conditions (temperature, radiation, turbidity, etc.) and on ice surface properties. Among the others, ARCA project focuses on the analysis of the interface between the melting glaciers fronts and the sea inside the Arctic fjords and studies the actual sedimentary processes by analysing the ice and sediments collected in the inner part of the fjords. The Svalbard Archipelago is considered a suitable region to explore the impacts of possible climate changes, being characterised by Atlantic water influx and melting of tidal glaciers, both linked to climate variability. The retreat of the glacier front has been particularly pronounced in recent decades and has led to the accumulation of sediments in the depressions inter-moraine near the sea-ice interfaces. Particularly interesting is the case of the Kongsfjorden where high sedimentation rates have been recorded. Kongsfjorden is an Arctic glacial fjord located on the west coast of the Svalbard at 79° N, 12° E. In the inner part of the fjord, many glaciers reach the sea and the shape of the glacier front is an almost vertical wall of ice above seawater. For this reason direct measurements in the proximity of the glacier front are very critical due to the possible sudden fall of ice blocks causing extreme conditions which are dangerous for human beings carrying out operations in the surrounding area. Within the ARCA project a first prototype of automatic equipment was designed to perform discrete sampling of waters in the area close to the Kronebreen glacier in the Kongsfjorden. The aim was to obtain in situ data to study the heterotrophic bacterial distribution and functional metabolism near the glacier to better understand the hydrology cycle and its consequences on the climate in the Boreal hemisphere.The Shark USSV (Unmanned Semi-Submersible Vehicle) designed and built by CNR-ISSIA was used for collecting samples in the stretch of sea near the Kronebreen glacier; this was the first time that an autonomous sampling was carried out near the front of the glacier. Shark was used to tow along a transect and via an adequate rope a small catamaran carrying an Automatic Water Multisampler designed on the experience of CNR-IAMC. Using the USSV+Sampling System has unquestionable advantages: possibility of carrying out real-time or near real-time acquisition of physical, chemical and biological data series; avoiding the presence of manifold (small and medium) drifting icebergs obstructing the passage to the glacier; protecting the operators from falling of ice blocks that can be dire