DIEGO: A Multispectral Thermal Mission for Earth Observation on the International Space Station
Observations in thermal infrared (IR) contribute substantially to the understanding of the global fluxes of energy and matter between Earth’s surface, ocean and atmosphere. Key parameters derived from such observations are Sea Surface Temperature (SST), Land Surface Temperature (LST) and Land Surfac...
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doaj-2243dc409ccd4d49b88cba6573276c842020-11-25T03:21:32ZengTaylor & Francis GroupEuropean Journal of Remote Sensing2279-72542020-07-0153S2283810.1080/22797254.2019.16983181698318DIEGO: A Multispectral Thermal Mission for Earth Observation on the International Space StationJohannes A. Schultz0Maik Hartmann1Sascha Heinemann2Jens Janke3Carsten Jürgens4Dieter Oertel5Gernot Rücker6Frank Thonfeld7Andreas Rienow8Ruhr-University BochumAstro- und Feinwerktechnik Adlershof GmbHInstitute of Bio- and Geosciences, Plant Sciences (IBG-2), Forschungszentrum Jülich GmbHCRN Management GmbHRuhr-University BochumAstro- und Feinwerktechnik Adlershof GmbHZEBRIS GbRGerman Remote Sensing Data Center (DFD), German Aerospace Center (DLR)Ruhr-University BochumObservations in thermal infrared (IR) contribute substantially to the understanding of the global fluxes of energy and matter between Earth’s surface, ocean and atmosphere. Key parameters derived from such observations are Sea Surface Temperature (SST), Land Surface Temperature (LST) and Land Surface Emissivity (LSE). These variables are important for weather forecasting and climate modelling. However, satellite systems currently in orbit provide only a small number of spectral bands in the thermal region, and consequently cannot be used for temperature emissivity separation (TES) to accurately derive LST and LSE. Hence, capacities to investigate processes or phenomena where LST in high temporal and high spatial resolution (<100 m) is required, such as agricultural applications or urban heat island monitoring, are limited. Additionally, the measurement of radiative energy released from active large and small fires, which contribute significantly to greenhouse gas emissions, is still challenging with current IR systems. Here, we introduce the proposed multispectral sensor system DIEGO (Dynamic Infrared Earth Observation on the ISS Orbit) with 11 spectral bands and a ground sampling distance of less than 60 m, which aims to reduce the observation gap in the thermal infrared significantly.http://dx.doi.org/10.1080/22797254.2019.1698318thermal infraredinternational space station (iss)land surface temperatureland surface emissivityevapotranspiration |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Johannes A. Schultz Maik Hartmann Sascha Heinemann Jens Janke Carsten Jürgens Dieter Oertel Gernot Rücker Frank Thonfeld Andreas Rienow |
spellingShingle |
Johannes A. Schultz Maik Hartmann Sascha Heinemann Jens Janke Carsten Jürgens Dieter Oertel Gernot Rücker Frank Thonfeld Andreas Rienow DIEGO: A Multispectral Thermal Mission for Earth Observation on the International Space Station European Journal of Remote Sensing thermal infrared international space station (iss) land surface temperature land surface emissivity evapotranspiration |
author_facet |
Johannes A. Schultz Maik Hartmann Sascha Heinemann Jens Janke Carsten Jürgens Dieter Oertel Gernot Rücker Frank Thonfeld Andreas Rienow |
author_sort |
Johannes A. Schultz |
title |
DIEGO: A Multispectral Thermal Mission for Earth Observation on the International Space Station |
title_short |
DIEGO: A Multispectral Thermal Mission for Earth Observation on the International Space Station |
title_full |
DIEGO: A Multispectral Thermal Mission for Earth Observation on the International Space Station |
title_fullStr |
DIEGO: A Multispectral Thermal Mission for Earth Observation on the International Space Station |
title_full_unstemmed |
DIEGO: A Multispectral Thermal Mission for Earth Observation on the International Space Station |
title_sort |
diego: a multispectral thermal mission for earth observation on the international space station |
publisher |
Taylor & Francis Group |
series |
European Journal of Remote Sensing |
issn |
2279-7254 |
publishDate |
2020-07-01 |
description |
Observations in thermal infrared (IR) contribute substantially to the understanding of the global fluxes of energy and matter between Earth’s surface, ocean and atmosphere. Key parameters derived from such observations are Sea Surface Temperature (SST), Land Surface Temperature (LST) and Land Surface Emissivity (LSE). These variables are important for weather forecasting and climate modelling. However, satellite systems currently in orbit provide only a small number of spectral bands in the thermal region, and consequently cannot be used for temperature emissivity separation (TES) to accurately derive LST and LSE. Hence, capacities to investigate processes or phenomena where LST in high temporal and high spatial resolution (<100 m) is required, such as agricultural applications or urban heat island monitoring, are limited. Additionally, the measurement of radiative energy released from active large and small fires, which contribute significantly to greenhouse gas emissions, is still challenging with current IR systems. Here, we introduce the proposed multispectral sensor system DIEGO (Dynamic Infrared Earth Observation on the ISS Orbit) with 11 spectral bands and a ground sampling distance of less than 60 m, which aims to reduce the observation gap in the thermal infrared significantly. |
topic |
thermal infrared international space station (iss) land surface temperature land surface emissivity evapotranspiration |
url |
http://dx.doi.org/10.1080/22797254.2019.1698318 |
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