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Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function: Correcting orbital drift signal in the ti...

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Personen und Körperschaften: Devasthale, Abhay, Karlsson, Karl-Göran, Quaas, Johannes, Graßl, Hartmut
Titel: Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function: Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function
Format: E-Artikel
Sprache: Englisch
veröffentlicht:
Göttingen Copernicus Publications 2012
Online-Ausg.. 2015
Gesamtaufnahme: , Atmospheric measurement techniques (2012) 5, S. 267-273
Schlagwörter:
Quelle: Qucosa
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245 |a Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function  |b Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function 
264 |a Göttingen  |b Copernicus Publications  |c 2012 
533 |a Online-Ausg.  |d 2015  |e Online-Ressource (Text)  |f Universitätsbibliothek Leipzig 
520 |a The Advanced Very High Resolution Radiometer (AVHRR) instruments onboard the series of National Oceanic and Atmospheric Administration (NOAA) satellites offer the longest available meteorological data records from space. These satellites have drifted in orbit resulting in shifts in the local time sampling during the life span of the sensors onboard. Depending upon the amplitude of the diurnal cycle of the geophysical parameters derived, orbital drift may cause spurious trends in their time series. We investigate tropical deep convective clouds, which show pronounced diurnal cycle amplitude, to estimate an upper bound of the impact of orbital drift on their time series. We carry out a rotated empirical orthogonal function analysis (REOF) and show that the REOFs are useful in delineating orbital drift signal and, more importantly, in subtracting this signal in the time series of convective cloud amount. These results will help facilitate the derivation of homogenized data series of cloud amount from NOAA satellite sensors and ultimately analyzing trends from them. However, we suggest detailed comparison of various methods and rigorous testing thereof applying final orbital drift corrections. 
650 |a Wolken 
650 |a Satelliten 
650 |a Atmosphäre 
650 |a Clouds 
650 |a Satellites 
650 |a Atmosphere 
700 |a Karlsson, Karl-Göran 
700 |a Quaas, Johannes 
700 |a Graßl, Hartmut 
773 |g Atmospheric measurement techniques (2012) 5, S. 267-273 
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contents The Advanced Very High Resolution Radiometer (AVHRR) instruments onboard the series of National Oceanic and Atmospheric Administration (NOAA) satellites offer the longest available meteorological data records from space. These satellites have drifted in orbit resulting in shifts in the local time sampling during the life span of the sensors onboard. Depending upon the amplitude of the diurnal cycle of the geophysical parameters derived, orbital drift may cause spurious trends in their time series. We investigate tropical deep convective clouds, which show pronounced diurnal cycle amplitude, to estimate an upper bound of the impact of orbital drift on their time series. We carry out a rotated empirical orthogonal function analysis (REOF) and show that the REOFs are useful in delineating orbital drift signal and, more importantly, in subtracting this signal in the time series of convective cloud amount. These results will help facilitate the derivation of homogenized data series of cloud amount from NOAA satellite sensors and ultimately analyzing trends from them. However, we suggest detailed comparison of various methods and rigorous testing thereof applying final orbital drift corrections.
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spelling Devasthale, Abhay, Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function, Göttingen Copernicus Publications 2012, Online-Ausg. 2015 Online-Ressource (Text) Universitätsbibliothek Leipzig, The Advanced Very High Resolution Radiometer (AVHRR) instruments onboard the series of National Oceanic and Atmospheric Administration (NOAA) satellites offer the longest available meteorological data records from space. These satellites have drifted in orbit resulting in shifts in the local time sampling during the life span of the sensors onboard. Depending upon the amplitude of the diurnal cycle of the geophysical parameters derived, orbital drift may cause spurious trends in their time series. We investigate tropical deep convective clouds, which show pronounced diurnal cycle amplitude, to estimate an upper bound of the impact of orbital drift on their time series. We carry out a rotated empirical orthogonal function analysis (REOF) and show that the REOFs are useful in delineating orbital drift signal and, more importantly, in subtracting this signal in the time series of convective cloud amount. These results will help facilitate the derivation of homogenized data series of cloud amount from NOAA satellite sensors and ultimately analyzing trends from them. However, we suggest detailed comparison of various methods and rigorous testing thereof applying final orbital drift corrections., Wolken, Satelliten, Atmosphäre, Clouds, Satellites, Atmosphere, Karlsson, Karl-Göran, Quaas, Johannes, Graßl, Hartmut, Atmospheric measurement techniques (2012) 5, S. 267-273, text/html https://nbn-resolving.org/urn:nbn:de:bsz:15-qucosa-177609 Online-Zugriff
spellingShingle Devasthale, Abhay, Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function: Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function, The Advanced Very High Resolution Radiometer (AVHRR) instruments onboard the series of National Oceanic and Atmospheric Administration (NOAA) satellites offer the longest available meteorological data records from space. These satellites have drifted in orbit resulting in shifts in the local time sampling during the life span of the sensors onboard. Depending upon the amplitude of the diurnal cycle of the geophysical parameters derived, orbital drift may cause spurious trends in their time series. We investigate tropical deep convective clouds, which show pronounced diurnal cycle amplitude, to estimate an upper bound of the impact of orbital drift on their time series. We carry out a rotated empirical orthogonal function analysis (REOF) and show that the REOFs are useful in delineating orbital drift signal and, more importantly, in subtracting this signal in the time series of convective cloud amount. These results will help facilitate the derivation of homogenized data series of cloud amount from NOAA satellite sensors and ultimately analyzing trends from them. However, we suggest detailed comparison of various methods and rigorous testing thereof applying final orbital drift corrections., Wolken, Satelliten, Atmosphäre, Clouds, Satellites, Atmosphere
title Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function: Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function
title_auth Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function
title_full Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function
title_fullStr Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function
title_full_unstemmed Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function
title_in_hierarchy
title_short Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function
title_sort correcting orbital drift signal in the time series of avhrr derived convective cloud fraction using rotated empirical orthogonal function correcting orbital drift signal in the time series of avhrr derivedconvective cloud fraction using rotated empirical orthogonal function
title_sub Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function
title_unstemmed Correcting orbital drift signal in the time series of AVHRR derived convective cloud fraction using rotated empirical orthogonal function: Correcting orbital drift signal in the time series of AVHRR derivedconvective cloud fraction using rotated empirical orthogonal function
topic Wolken, Satelliten, Atmosphäre, Clouds, Satellites, Atmosphere
topic_facet Wolken, Satelliten, Atmosphäre, Clouds, Satellites, Atmosphere
url https://nbn-resolving.org/urn:nbn:de:bsz:15-qucosa-177609
urn urn:nbn:de:bsz:15-qucosa-177609
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