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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2015-04-01
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Series: | The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences |
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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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AT kzaksek cloudphotogrammetryfromspace AT agerst cloudphotogrammetryfromspace AT jvonderlieth cloudphotogrammetryfromspace AT gganci cloudphotogrammetryfromspace AT mhort cloudphotogrammetryfromspace |
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