1999
DOI: 10.1117/12.373198
|View full text |Cite
|
Sign up to set email alerts
|

<title>Development of ADEOS-II/GLI operational algorithm for Earth observation</title>

Abstract: GLI (Global Jmager) is a 36 channel visible and infrared radiometer/imager onboard the NASDA/ADEOS-II satellite. The information carried by GLI for the earth-atmosphere system is huge and difficult to be extracted enough efficiently with an operational satellite data analyzing system. We discuss and overview the algorithm development of the GLI Level-2 products at NASDAIEORC. We have several innovations to make the system unique and efficient. GLI simulator and GLI synthetic data sets are among those, which wi… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

2009
2009
2016
2016

Publication Types

Select...
2
1
1

Relationship

1
3

Authors

Journals

citations
Cited by 4 publications
(2 citation statements)
references
References 2 publications
0
2
0
Order By: Relevance
“…The GLI has 36 channels that can observe the land, ocean, and atmosphere [ Nakajima et al , 1999]. It can retrieve detailed particle optical properties in the atmosphere.…”
Section: Datamentioning
confidence: 99%
See 1 more Smart Citation
“…The GLI has 36 channels that can observe the land, ocean, and atmosphere [ Nakajima et al , 1999]. It can retrieve detailed particle optical properties in the atmosphere.…”
Section: Datamentioning
confidence: 99%
“…We used the Comprehensive Analysis Program for Cloud Optical Measurement (CAPCOM) [ Nakajima and Nakajima , 1995; Kawamoto et al , 2001] to retrieve cloud optical thickness from MTSAT‐1R/JAMI. This algorithm was also adopted as one of the standard algorithms for the Advanced Earth Observing Satellite II/Global Imager (ADEOS‐II/GLI) products [ Nakajima et al , 1999]. The original CAPCOM estimated the cloud optical thickness, effective particle radius, and cloud‐top temperature from visible, near‐infrared, and thermal infrared channels using a LUT calculated from radiative transfer [ Nakajima and Tanaka , 1986, 1988] under a plane‐parallel and single‐layer cloud model.…”
Section: Retrieval Of Cloud Optical Propertiesmentioning
confidence: 99%