The reflectance spectra were measured with a FieldSpecPro from 350 nm to 2500 nm during a fieldwork in June 2007. The reflectance has been compared with reflectance obtained by multispectral Advanced Space borne Thermal Emission and Reflection Radiometer (ASTER) and by hyper spectral EO1-Hyperion satellites. Prior the comparison, reflectance spectra have been convolved with ASTER and EO1-Hyperion spectral functions. The results show percentage errors in accordance to those present in literature in the ASTER SWIR range. However, some differences have been confirmed for the ASTER reflectance product (ASTER_07) in visible channels. Regarding EO1-Hyperion, a good agreement of reflectance against field measurement has been found resulting...
An empirical comparison of the EO-1 Hyperion, EOS ASTER, and Landsat ETM sensors was performed to ex...
Extraterrestrial solar irradiance spectra detail the solar energy distribution over wavelengths, and...
This work is an evaluation to which degree geological information can be obtained from modern remote...
From 16 to 26 July 2003 a wide field campaign was carried out around Mt. Etna (Sicily) by different ...
Since the advent of LANDSAT I in 1972, many different multispectral satellites have been orbited by ...
In the frame of the Italian Space Agency (ASI) Hyperspectral Mission PRISMA (Precursore IperSpettral...
The aim of this paper is to show the feasibility of evaluating the sulphur dioxide (SO,) flux emitte...
We discussed the possibilities and open questions concerning laboratory refl ectance spectroscopy, s...
From 16 to 26 July 2003 an extensive field campaign was carried out around Mt Etna, Sicily, Italy. D...
Spectral properties of volcanic materials in the optical region (350–2500 nm) of the electromagnetic...
The reflectance values recorded by Earth observing satellite sensors can be different from the surfa...
On May 9, 2000 the Advanced Spaceborne Thermal Emission and Reflection radiometer (ASTER) on the Ter...
The EOS-1 Terra ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) has acquired ...
Abstract—Airborne hyperspectral data have been available to researchers since the early 1980s and th...
The HYPERNETS project (www.hypernets.eu) aims to ensure that high-quality in situ measurements are a...
An empirical comparison of the EO-1 Hyperion, EOS ASTER, and Landsat ETM sensors was performed to ex...
Extraterrestrial solar irradiance spectra detail the solar energy distribution over wavelengths, and...
This work is an evaluation to which degree geological information can be obtained from modern remote...
From 16 to 26 July 2003 a wide field campaign was carried out around Mt. Etna (Sicily) by different ...
Since the advent of LANDSAT I in 1972, many different multispectral satellites have been orbited by ...
In the frame of the Italian Space Agency (ASI) Hyperspectral Mission PRISMA (Precursore IperSpettral...
The aim of this paper is to show the feasibility of evaluating the sulphur dioxide (SO,) flux emitte...
We discussed the possibilities and open questions concerning laboratory refl ectance spectroscopy, s...
From 16 to 26 July 2003 an extensive field campaign was carried out around Mt Etna, Sicily, Italy. D...
Spectral properties of volcanic materials in the optical region (350–2500 nm) of the electromagnetic...
The reflectance values recorded by Earth observing satellite sensors can be different from the surfa...
On May 9, 2000 the Advanced Spaceborne Thermal Emission and Reflection radiometer (ASTER) on the Ter...
The EOS-1 Terra ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) has acquired ...
Abstract—Airborne hyperspectral data have been available to researchers since the early 1980s and th...
The HYPERNETS project (www.hypernets.eu) aims to ensure that high-quality in situ measurements are a...
An empirical comparison of the EO-1 Hyperion, EOS ASTER, and Landsat ETM sensors was performed to ex...
Extraterrestrial solar irradiance spectra detail the solar energy distribution over wavelengths, and...
This work is an evaluation to which degree geological information can be obtained from modern remote...