Cloud Photogrammetry from Space

The most commonly used method for satellite cloud top height (CTH) compares brightness temperature of the cloud with the atmospheric temperature profile. Because of the uncertainties of this method, we propose a photogrammetric approach. As clouds can move with high velocities, even instruments with...

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Main Authors: K. Zakšek, A. Gerst, J. von der Lieth, G. Ganci, M. Hort
Format: Article
Language:English
Published: Copernicus Publications 2015-04-01
Series:The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Online Access:http://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XL-7-W3/247/2015/isprsarchives-XL-7-W3-247-2015.pdf
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spelling doaj-27963134a579471b920ddb29515ff4522020-11-24T21:54:20ZengCopernicus PublicationsThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences1682-17502194-90342015-04-01XL-7/W324725410.5194/isprsarchives-XL-7-W3-247-2015Cloud Photogrammetry from SpaceK. Zakšek0A. Gerst1J. von der Lieth2G. Ganci3M. Hort4University of Hamburg, CEN, Institute of Geophysics, Bundesstr. 55, 20146 Hamburg, GermanyESA, European Astronaut Centre, Linder Höhe, 51147 Köln, GermanyUniversity of Hamburg, CEN, Institute of Geophysics, Bundesstr. 55, 20146 Hamburg, GermanyINGV, Sezione di Catania, Piazza Roma, 2, 95125 Catania, ItalyUniversity of Hamburg, CEN, Institute of Geophysics, Bundesstr. 55, 20146 Hamburg, GermanyThe most commonly used method for satellite cloud top height (CTH) compares brightness temperature of the cloud with the atmospheric temperature profile. Because of the uncertainties of this method, we propose a photogrammetric approach. As clouds can move with high velocities, even instruments with multiple cameras are not appropriate for accurate CTH estimation. Here we present two solutions. The first is based on the parallax between data retrieved from geostationary (SEVIRI, HRV band; 1000 m spatial resolution) and polar orbiting satellites (MODIS, band 1; 250 m spatial resolution). The procedure works well if the data from both satellites are retrieved nearly simultaneously. However, MODIS does not retrieve the data at exactly the same time as SEVIRI. To compensate for advection in the atmosphere we use two sequential SEVIRI images (one before and one after the MODIS retrieval) and interpolate the cloud position from SEVIRI data to the time of MODIS retrieval. CTH is then estimated by intersection of corresponding lines-of-view from MODIS and interpolated SEVIRI data. The second method is based on NASA program Crew Earth observations from the International Space Station (ISS). The ISS has a lower orbit than most operational satellites, resulting in a shorter minimal time between two images, which is needed to produce a suitable parallax. In addition, images made by the ISS crew are taken by a full frame sensor and not a push broom scanner that most operational satellites use. Such data make it possible to observe also short time evolution of clouds.http://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XL-7-W3/247/2015/isprsarchives-XL-7-W3-247-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author K. Zakšek
A. Gerst
J. von der Lieth
G. Ganci
M. Hort
spellingShingle K. Zakšek
A. Gerst
J. von der Lieth
G. Ganci
M. Hort
Cloud Photogrammetry from Space
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
author_facet K. Zakšek
A. Gerst
J. von der Lieth
G. Ganci
M. Hort
author_sort K. Zakšek
title Cloud Photogrammetry from Space
title_short Cloud Photogrammetry from Space
title_full Cloud Photogrammetry from Space
title_fullStr Cloud Photogrammetry from Space
title_full_unstemmed Cloud Photogrammetry from Space
title_sort cloud photogrammetry from space
publisher Copernicus Publications
series The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
issn 1682-1750
2194-9034
publishDate 2015-04-01
description The most commonly used method for satellite cloud top height (CTH) compares brightness temperature of the cloud with the atmospheric temperature profile. Because of the uncertainties of this method, we propose a photogrammetric approach. As clouds can move with high velocities, even instruments with multiple cameras are not appropriate for accurate CTH estimation. Here we present two solutions. The first is based on the parallax between data retrieved from geostationary (SEVIRI, HRV band; 1000 m spatial resolution) and polar orbiting satellites (MODIS, band 1; 250 m spatial resolution). The procedure works well if the data from both satellites are retrieved nearly simultaneously. However, MODIS does not retrieve the data at exactly the same time as SEVIRI. To compensate for advection in the atmosphere we use two sequential SEVIRI images (one before and one after the MODIS retrieval) and interpolate the cloud position from SEVIRI data to the time of MODIS retrieval. CTH is then estimated by intersection of corresponding lines-of-view from MODIS and interpolated SEVIRI data. The second method is based on NASA program Crew Earth observations from the International Space Station (ISS). The ISS has a lower orbit than most operational satellites, resulting in a shorter minimal time between two images, which is needed to produce a suitable parallax. In addition, images made by the ISS crew are taken by a full frame sensor and not a push broom scanner that most operational satellites use. Such data make it possible to observe also short time evolution of clouds.
url http://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XL-7-W3/247/2015/isprsarchives-XL-7-W3-247-2015.pdf
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