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The Ice-ClimaLizer research investigates the role of two Antarctic bioconstructional and bioindicator organisms (bryozoan and coralline algae), responsible of promoting marine biodiversity, as proxies of environmental conditions (temperature, light intensity, pressure, oxygen, conductibility and pH). An experimental laboratory has been placed in Tethys Bay (Ross Sea) at 25.5 m deep. The project will compare 1 year of environmental data obtained via continuous recording (every hour) by CTD probe with reconstructed data obtained via geochemical proxies of skeletons/thalli of the investigated species. Data are collected from November 2018 to November 2019.
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Since 1998, ENEA (Italian National Agency for New Technology, Energy and the Environment) has been carrying on researches to develop a plant based greenhouse facility for producing plant fresh food at the Italian bases of TNB (Terra Nova Bay) and Dome C (Concordia base) in Antarctica. Accordingly, at the base TNB “Mario Zucchelli” was installed a sustainable closed greenhouse facility PULSA (Plant-based Unit for Life Support in Antarctica). PULSA has been in operation during four campaigns in Antarctica. 1) A complete automatic hydroponics system for plant cultivation in artificial environmental (C.H.G.S., Closed Hydroponic Greenhouse System); 2. A closed module PULSA Unit. A prototype greenhouse module has been conceived and designed as a transportable unit made of a standard container, dimensions of 6055 (l)*2435(w)*2585(h) mm. The installed microclimate conditioning unit included an air heater of about 6.0 kW which can also act as inside air cooling as well as dehumidifier for removing the internal humidity (up to 2.5 kg/h of water) by forcing the air into a drying service. An air ventilation device composed of two fans each of 400 W and air capacity exchanging of 1200 m3/h was also installed to keep necessary air exchange and CO2 concentration. 3) A treating and recycling wastes unit for the purification of water and for the recycling of residual biomass wastes from the hydroponic cycles, 4) A complete automated and remote-controlling system for the germination and the production of the plantlets (Box-Nursery); 5) A simulator for the growth and the yield production of lettuce (SLS) in function of the temperature and the light applied to the crops. Other prototypes still under developing are: a) the multilevel hydroponics design; b) the solar photovoltaic system of 1.1 kWp, to optimize the yield and the autonomy of the enclosed growing volume using artificial and/or Light Emitting Diodes (LEDs) as light sources for plant crop growth. Considerations and comments are reported on the on-going challenge to use PULSA as scientific platform for implementing activities of research and demonstration on plant growth technologies for Space.
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The Observatory main purpose is to contribute to the monitoring of global climate change monitoring standard meteorological parameters. The automatic weather station AWS Paola is located at Talos Dome (72° 49′ 45″ S - 159° 11′ 36″ E) at 2370 m a.s.l., and has been installed on the 26 january 2003. It acquired, every hour, all year round, the meteorological vaiables of wind velocity, wind direction, temperature, pressure and relative humidity, plus snow height acquired as daily averages.
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The Observatory main purpose is to contribute to the monitoring of global climate change monitoring standard meteorological parameters. The automatic weather station AWS Lola is located at th Sarao Point (74° 8′ 6″ S - 163° 25′ 50″ E) at 1920 m a.s.l., and has been installed on the 9 January 1991. It acquired, all year round, the meteorological variables of wind velocity, wind direction, temperature, pressure and relative humidity.
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The Observatory main purpose is to contribute to the monitoring of global climate change. Standard meteorological parameters are monitored and additional data are obtained by measures of snow transport and accumulation in localities of scientific interest.The monitoring network consists of 16 automatic weather stations (AWS) operating all the year, round.They are setted in the area between 'Mario Zucchelli Station' (MZS, 74 ° 41 ‘S - 164° 05’ E), the French-Italian 'Concordia' base (DC, 75 ° S, 123 ° E) on the Antarctic Plateau and the French base Dumont’Urville (DDU, 66 ° 40’S - 140 ° 01’E) towards Wilkes Land. At OASI laboratories a laser rain gauge, an all sky camera and a Micro-Rain-Radar were maintained and left working during winter season. In OASI surroundings were installed a new ceilometer (VAISALA CL51) for cloud base measurement up to 15 km and a Total Rain weighing Sensor TRwS for snow precipitations.
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The Observatory main purpose is to contribute to the monitoring of global climate change monitoring standard meteorological parameters. The automatic weather station AWS Arelis is located in Cape Ross (76° 42′ 54″ S - 162° 58′ 12″ E) at 150 m of altitude, and has been installed on the 21 January 1990. It acquired, all year round, the meteorological vaiables of wind velocity, wind direction, temperature, pressure and relative humidity.
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The Observatory main purpose is to contribute to the monitoring of global climate change monitoring standard meteorological parameters. The automatic weather station AWS Sofiab is located at David Glacier (75° 36′ 42″ S - 158° 35′ 26″ E) at 1552 m a.s.l., and has been installed on the 28 november 2002. It acquired, every hour, all year round, the meteorological vaiables of wind velocity, wind direction, temperature, pressure and relative humidity.
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The project aims to determine the mass balance components in the Dome C drainage area and to study and monitor local glaciers in Victoria Land. The goal is to define the mass balance of the ice cap through the analysis of its altimetric variation with satellite systems and through the determination of the values of the positive (snow accumulation) and negative (flow of glaciers to the anchor line) components of the balance mass. Trought the study of the snow cores (collected as part of the ITASE project (XVII/XVIII expedition)), was determined the annual stratigraphy and evaluated the snow accumulation, the isotopic temperature and the chemical composition of the snow cores. Moreover analysis of geophysical data (GPR, GPS, RES, spectroradiometry) and remote sensing data were carried out for the study of the variability of snow accumulation, of the dynamics of the ice cap and of the flow of glaciers to the anchor line.
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The IPICS-2kyr-Italia project, through multiple perforations in the Antarctic ice sheet, aims to provide new data on climatic variability over the last 2000 years. The ice caps of the polar caps are valuable natural archives of the Earth's climatic and environmental history. The extraction of the snow and ice cores have taken place during the summer campaign of the Italian expedition to Antarctica 2013/2014. The drilling site GV7 (70°41'S, 158°52'E; 1950 m), chosen for the high snow accumulation, is about 500 km from Mario Zucchelli Station. Drill up to 250 - 500m. Core samples will be studied by chemical, isotopic and physical analyses of the dust and gases contained in the ice. It will thus be possible to reconstruct the evolution of temperatures, the composition of the atmosphere and atmospheric circulation, the frequency of volcanic eruptions and the air pollution produced by human activities over the last millennium with considerable temporal detail.
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Collection of 451 temperature profiles with XBT and 35 profiles of temperature and salinity with XCTD probes in the Drake Strait, the Weddell Sea and between the northern tip of the Antarctica Paeninsula and the Orcadas Islands, to study of the variability of the Mixed Layer and the estimate of the heat content on the first 700 m of the water column, and the large scale representation of the surace and subsurface structure of the ACC. Three oceanographic cruises were performed on board of the Argentinean ice breaker “Almirante Irizar” in the three austral winters 2004-2005, 2005-2006 e 2006-2007. Data are acquired from the 7th of february and the sond were launched with a resolution of 20' of latitude to 70° ad 15' for higher latitudes, to better define the thermal southern front.