First look at Earth reflectance measurements from optical radiometers on Global Positioning System satellites

Earth’s energy budget drives its climate. Many satellite radiometers have provided top of atmosphere radiation measurements to estimate the energy budget. We present a first look at previously unpublished measurements of Earth-reflected sunlight from broadband pixelated radiometers in the visible an...

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Main Authors: Kaczmarowski, A., Dreike, P., Roesler, E., Nelsen, J., DeGraw, C., Mahodaya, A.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018103
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5018103 2023-08-20T03:59:21+02:00 First look at Earth reflectance measurements from optical radiometers on Global Positioning System satellites Kaczmarowski, A. Dreike, P. Roesler, E. Nelsen, J. DeGraw, C. Mahodaya, A. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018103 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1112 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018103 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-1112 2023-07-30T23:40:44Z Earth’s energy budget drives its climate. Many satellite radiometers have provided top of atmosphere radiation measurements to estimate the energy budget. We present a first look at previously unpublished measurements of Earth-reflected sunlight from broadband pixelated radiometers in the visible and near-visible wavelength range operating on satellites in the Global Positioning System (GPS) constellation since 2011.The radiometers collect synoptic measurements of Earth-reflected sunlight, including polar region coverage, due to the 55° inclination and 20,200 km altitude of the GPS orbits. We present an initial comparison of these radiometers with the Spinning Enhanced Visible and InfraRed Imager (SEVIRI) on the Meteosat-11 geostationary satellite. We also demonstrate the ability of these radiometers to detect changes in reflected sunlight over time. Specifically, measurements ±40 days around the polar summer solstices show (1) reflected sunlight from the Antarctic south of 80°S is symmetric around the solstice, implying constant reflectance, and (2) reflection from the Arctic north of 80°N is ~20% dimmer than the Antarctic and decreases 20%-35% over 80 days. The variation in the Arctic region indicates these radiometers observe albedo changes related to sea ice melting. GPS-based radiometers could provide an additional method of validating data collected by other optical sensors. The GPS-based radiometer data could also verify the spatial, temporal, and spectral interpolation and extrapolation to the full earth used for data collected by Low Earth Orbiting satellites and fill in coverage gaps between generations of sensors. Conference Object albedo Antarc* Antarctic Arctic Sea ice GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Antarctic Arctic The Antarctic
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Earth’s energy budget drives its climate. Many satellite radiometers have provided top of atmosphere radiation measurements to estimate the energy budget. We present a first look at previously unpublished measurements of Earth-reflected sunlight from broadband pixelated radiometers in the visible and near-visible wavelength range operating on satellites in the Global Positioning System (GPS) constellation since 2011.The radiometers collect synoptic measurements of Earth-reflected sunlight, including polar region coverage, due to the 55° inclination and 20,200 km altitude of the GPS orbits. We present an initial comparison of these radiometers with the Spinning Enhanced Visible and InfraRed Imager (SEVIRI) on the Meteosat-11 geostationary satellite. We also demonstrate the ability of these radiometers to detect changes in reflected sunlight over time. Specifically, measurements ±40 days around the polar summer solstices show (1) reflected sunlight from the Antarctic south of 80°S is symmetric around the solstice, implying constant reflectance, and (2) reflection from the Arctic north of 80°N is ~20% dimmer than the Antarctic and decreases 20%-35% over 80 days. The variation in the Arctic region indicates these radiometers observe albedo changes related to sea ice melting. GPS-based radiometers could provide an additional method of validating data collected by other optical sensors. The GPS-based radiometer data could also verify the spatial, temporal, and spectral interpolation and extrapolation to the full earth used for data collected by Low Earth Orbiting satellites and fill in coverage gaps between generations of sensors.
format Conference Object
author Kaczmarowski, A.
Dreike, P.
Roesler, E.
Nelsen, J.
DeGraw, C.
Mahodaya, A.
spellingShingle Kaczmarowski, A.
Dreike, P.
Roesler, E.
Nelsen, J.
DeGraw, C.
Mahodaya, A.
First look at Earth reflectance measurements from optical radiometers on Global Positioning System satellites
author_facet Kaczmarowski, A.
Dreike, P.
Roesler, E.
Nelsen, J.
DeGraw, C.
Mahodaya, A.
author_sort Kaczmarowski, A.
title First look at Earth reflectance measurements from optical radiometers on Global Positioning System satellites
title_short First look at Earth reflectance measurements from optical radiometers on Global Positioning System satellites
title_full First look at Earth reflectance measurements from optical radiometers on Global Positioning System satellites
title_fullStr First look at Earth reflectance measurements from optical radiometers on Global Positioning System satellites
title_full_unstemmed First look at Earth reflectance measurements from optical radiometers on Global Positioning System satellites
title_sort first look at earth reflectance measurements from optical radiometers on global positioning system satellites
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018103
geographic Antarctic
Arctic
The Antarctic
geographic_facet Antarctic
Arctic
The Antarctic
genre albedo
Antarc*
Antarctic
Arctic
Sea ice
genre_facet albedo
Antarc*
Antarctic
Arctic
Sea ice
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1112
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018103
op_doi https://doi.org/10.57757/IUGG23-1112
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