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Featured researches published by Tatiana Di Iorio.


Applied Optics | 2015

Empirical correction of multifilter rotating shadowband radiometer (MFRSR) aerosol optical depths for the aerosol forward scattering and development of a long-term integrated MFRSR-Cimel dataset at Lampedusa.

Alcide di Sarra; Damiano Sferlazzo; Daniela Meloni; F. Anello; C. Bommarito; Stefano Corradini; Lorenzo De Silvestri; Tatiana Di Iorio; F. Monteleone; G. Pace; S. Piacentino; S. Pugnaghi

Aerosol optical properties have been measured on the island of Lampedusa (35.5°N, 12.6°E) with seven-band multifilter rotating shadowband radiometers (MFRSRs) and a CE 318 Cimel sunphotometer (part of the AERONET network) since 1999. Four different MFRSRs have operated since 1999. The Cimel sunphotometer has been operational for a short period in 2000 and in 2003-2006 and 2010-present. Simultaneous determinations of the aerosol optical depth (AOD) from the two instruments were compared over a period of almost 4 years at several wavelengths between 415 and 870 nm. This is the first long-term comparison at a site strongly influenced by desert dust and marine aerosols and characterized by frequent cases of elevated AOD. The datasets show a good agreement, with MFRSR underestimating the Cimel AOD in cases with low Ångström exponent; the underestimate decreases for increasing wavelength and increases with AOD. This underestimate is attributed to the effect of aerosol forward scattering on the relatively wide field of view of the MFRSR. An empirical correction of the MFRSR data was implemented. After correction, the mean bias (MB) between MFRSR and Cimel simultaneous AOD determinations is always smaller than 0.004, and the root mean square difference is ≤0.031 at all wavelengths. The MB between MFRSR and Cimel monthly averages (for months with at least 20 days with AOD determinations) is 0.0052. Thus, by combining the MFRSR and Cimel observations, an integrated long-term series is obtained, covering the period 1999-present, with almost continuous measurements since early 2002. The long-term data show a small (nonstatistically significant) decreasing trend over the period 2002-2013, in agreement with independent observations in the Mediterranean. The integrated Lampedusa dataset will be used for aerosol climatological studies and for verification of satellite observations and model analyses.


Review of Scientific Instruments | 2015

The spectral imaging facility: Setup characterization

Simone De Angelis; E. Ammannito; Tatiana Di Iorio; Maria Cristina de Sanctis; Paola Manzari; Fabrizio Liberati; Fabio Tarchi; Michele Dami; Monica Olivieri; Carlo Pompei; Raffaele Mugnuolo

The SPectral IMager (SPIM) facility is a laboratory visible infrared spectrometer developed to support space borne observations of rocky bodies of the solar system. Currently, this laboratory setup is used to support the DAWN mission, which is in its journey towards the asteroid 1-Ceres, and to support the 2018 Exo-Mars mission in the spectral investigation of the Martian subsurface. The main part of this setup is an imaging spectrometer that is a spare of the DAWN visible infrared spectrometer. The spectrometer has been assembled and calibrated at Selex ES and then installed in the facility developed at the INAF-IAPS laboratory in Rome. The goal of SPIM is to collect data to build spectral libraries for the interpretation of the space borne and in situ hyperspectral measurements of planetary materials. Given its very high spatial resolution combined with the imaging capability, this instrument can also help in the detailed study of minerals and rocks. In this paper, the instrument setup is first described, and then a series of test measurements, aimed to the characterization of the main subsystems, are reported. In particular, laboratory tests have been performed concerning (i) the radiation sources, (ii) the reference targets, and (iii) linearity of detector response; the instrumental imaging artifacts have also been investigated.


Bulletin of the American Meteorological Society | 2017

The GLAM Airborne Campaign across the Mediterranean Basin

Philippe Ricaud; Régina Zbinden; Valéry Catoire; Vanessa Brocchi; François Dulac; Eric Hamonou; Jean-Christophe Canonici; Laaziz El Amraoui; S. Massart; Bruno Piguet; Uri Dayan; Pierre Nabat; Jean Sciare; Michel Ramonet; Marc Delmotte; Alcide di Sarra; Damiano Sferlazzo; Tatiana Di Iorio; S. Piacentino; Paolo Cristofanelli; Nikos Mihalopoulos; G. Kouvarakis; Michael Pikridas; Chrysanthos Savvides; Rodanthi-Elisavet Mamouri; Argyro Nisantzi; Diofantos G. Hadjimitsis; Jean-Luc Attié; Hélène Ferré; Yannick Kangah

AbstractThe Gradient in Longitude of Atmospheric Constituents above the Mediterranean Basin (GLAM) airborne campaign was set up to investigate the summertime variability of gaseous pollutants, greenhouse gases, and aerosols between the western (∼3°E) and eastern (∼35°E) sections of the Mediterranean basin as well as how this connects with the impact of the Asian monsoon anticyclone on the eastern Mediterranean in the mid- to upper troposphere (∼5–10 km). GLAM falls within the framework of the Chemistry–Aerosol Mediterranean Experiment (ChArMEx) program. GLAM used the French Falcon-20 research aircraft to measure aerosols, humidity, and chemical compounds: ozone, carbon monoxide, methane, and carbon dioxide. GLAM took place between 6 and 10 August 2014, following a route from Toulouse (France) to Larnaca (Cyprus) and back again via Minorca (Spain), Lampedusa (Italy), and Heraklion (Crete, Greece). The aircraft flew at an altitude of 5 km on its outbound journey and 10 km on the return leg. GLAM also collec...


Earth and Space Science | 2016

Microimaging VIS-IR spectroscopy of ancient volcanic rocks as Mars analogues

Paola Manzari; Simone De Angelis; Maria Cristina de Sanctis; Tatiana Di Iorio; E. Ammannito; Nicolas Bost; Frédéric Foucher; Frances Westall

The SPectral Imager (SPIM) facility is a laboratory VIS-IR spectrometer developed to support spaceborne observations of rocky bodies of the solar system. Currently, this laboratory setup is used to support the Dawn NASA mission and to support the 2018 ExoMars mission in the spectral investigation of Martian subsurface. Specifically, for this mission, a selection of relevant Mars analogue materials has been characterized and stored in the International Space Analogue Rockstore (ISAR), hosted in Orleans, France. In this investigation, two volcanic rock samples from the ISAR collection were analyzed. These two samples were chosen because of their similarity in mineralogical composition and age with Martian basalts and volcanic sands. Moreover, volcanic sands are particularly interesting because they can contain fossils of primitive life forms. The analysis of data collected by SPIM resulted in good agreement with the mineralogical phases detected in these two samples by mineralogical and petrographical techniques, demonstrating the effectiveness of the high spatial and spectral resolution of SPIM for identifying and for mapping different mineralogical species on cut rock and mineral samples.


Atmospheric Chemistry and Physics | 2016

Long-range transport and mixing of aerosol sources during the 2013 North American biomass burning episode: analysis of multiple lidar observations in the western Mediterranean basin

Gérard Ancellet; Jacques Pelon; Julien Totems; Patrick Chazette; Ariane Bazureau; Michaël Sicard; Tatiana Di Iorio; François Dulac; Marc Mallet


Atmospheric Chemistry and Physics | 2016

Constraining the ship contribution to the aerosol of the central Mediterranean

Silvia Becagli; F. Anello; C. Bommarito; F. Cassola; G. Calzolai; Tatiana Di Iorio; Alcide di Sarra; José-Luis Gómez-Amo; F. Lucarelli; Miriam Marconi; Daniela Meloni; F. Monteleone; S. Nava; G. Pace; Mirko Severi; Damiano Sferlazzo; Rita Traversi; Roberto Udisti


Planetary and Space Science | 2014

The Ma_Miss instrument performance, I: Analysis of rocks powders by Martian VNIR spectrometer

Simone De Angelis; Maria Cristina de Sanctis; E. Ammannito; Cristian Carli; Tatiana Di Iorio; F. Altieri


Elem Sci Anth | 2017

Investigation of reactive gases and methane variability in the coastal boundary layer of the central Mediterranean basin

Paolo Cristofanelli; Maurizio Busetto; F. Calzolari; Ivano Ammoscato; Daniel Gullì; Adelaide Dinoi; Claudia Roberta Calidonna; Daniele Contini; Damiano Sferlazzo; Tatiana Di Iorio; S. Piacentino; Angela Marinoni; Michela Maione; Paolo Bonasoni


Atmospheric Chemistry and Physics | 2017

Determining the infrared radiative effects of Saharan dust: a radiative transfer modelling study based on vertically resolved measurements at Lampedusa

Daniela Meloni; Alcide di Sarra; Gérard Brogniez; Cyrielle Denjean; Lorenzo De Silvestri; Tatiana Di Iorio; P. Formenti; José Luis Gómez-Amo; Julian Gröbner; N. Kouremeti; Giuliano Liuzzi; Marc Mallet; G. Pace; Damiano Sferlazzo


Planetary and Space Science | 2015

The Ma_Miss instrument performance, II: Band parameters of rocks powders spectra by Martian VNIR spectrometer

Simone De Angelis; Maria Cristina de Sanctis; E. Ammannito; Cristian Carli; Tatiana Di Iorio; F. Altieri

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