A dataset provided by the European Space Agency

Name IO_566
Title THE COMPOSITION AND TEMPERATURE OF THE SURFACE OF IO
URL

http://nida.esac.esa.int/nida-sl-tap/data?RETRIEVAL_TYPE=OBSERVATION&PRODUCT_LEVEL=ALL&obsno=341006020

DOI https://doi.org/10.5270/esa-4of7jyp
Author SCHMITT, BERNARD
Description during the last 15 years, numerous studies have been devoted to the determination of the surface composition and temperature of io, and their variation with longitude. in the near infrared (2-5 microns) so2 frost is firmly identified, but the identifications of h2s and h2o are only tentative. in the mid-infrared s8, so3, na2so3, nahso4 and na2so4 are tentatively identified with features seen in the voyager iris spectra. sulfur allotropes, alkali sulfides, and polysulfur oxides have also been proposed to explain the uv and visible spectra of io. a clear identification of several of these molecules can be achieved with ir observations covering simultaneously a wide spectral range. concerning the so2 frost coverage, the current studies do not agree on the fractional area covered by so2 and on the amplitude of their variations with io.s longitude. regarding temperature, a better knowledge of the spatial distribution of the different types of regions of io (ranging from large cold (100-130 k) regions to small hot spots (300-650 k)) are necessary for the study of the io volcanism and of the surface-atmosphere exchanges. the goals of this observing program are (1) the positive identification of new molecules with simultaneous observation of absorption and emission features, (2) the determination of their abundances and their longitudinal variations, (3) the study of the surface and subsurface temperatures of the large and cold regions covered by so2, and (4) the determination of the temperature and of the heat flow radiated from thermal anomalies. these issues can be addressed by iso by (i) performing one high resolution spectroscopic observation in the near infrared (2.4-4.55 microns), (ii) measuring the whole mid-infrared spectrum (2.4-45 microns) at degraded spectral resolution, and (iii) repeating the mid-infrared spectral observation to study variations with io.s longitude. the very large spectral coverage of iso is a necessary requirement to achieve all these scientific goals.
Instrument SWS06
Temporal Coverage 1996-10-22T14:41:34Z/1996-10-22T18:35:04Z
Version 1.0
Mission Description The Infrared Space Observatory (ISO) was the worlds first true orbiting infrared observatory. Equipped with four highly-sophisticated and versatile scientific instruments, it was launched by Ariane in November 1995 and provided astronomers world-wide with a facility of unprecedented sensitivity and capabilities for a detailed exploration of the Universe at infrared wavelengths.
Creator Contact https://support.cosmos.esa.int/iso/
Date Published 1999-04-08T00:00:00Z
Keywords ISO, infrared, SWS, LWS, ISOCAM, ISOPHOT
Publisher And Registrant European Space Agency
Credit Guidelines European Space Agency, SCHMITT et al., 1999, 'THE COMPOSITION AND TEMPERATURE OF THE SURFACE OF IO', 1.0, European Space Agency, https://doi.org/10.5270/esa-4of7jyp