Earth Observing Systems XXVII 2022
DOI: 10.1117/12.2633379
|View full text |Cite
|
Sign up to set email alerts
|

MODIS solar diffuser calibration strategies for the post orbital drift era

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2

Citation Types

0
2
0

Year Published

2023
2023
2023
2023

Publication Types

Select...
2

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(2 citation statements)
references
References 9 publications
0
2
0
Order By: Relevance
“…To characterize over an expanded angle range, late mission yaw maneuvers will be required, however, methods for extrapolation of our current characterization as the new data is acquired are currently being explored. 3,8 For the desert data, IAMs and DMUs kept the satellites in a stable 16-day repeating ground-track cycle, where observations of selected sites at particular scan angles repeated every 16 days throughout the mission. As a result of the drifting orbits, the pattern is now lost for each instrument and the desert sites will now be observed at varying scan angles versus time.…”
Section: Introductionmentioning
confidence: 99%
“…To characterize over an expanded angle range, late mission yaw maneuvers will be required, however, methods for extrapolation of our current characterization as the new data is acquired are currently being explored. 3,8 For the desert data, IAMs and DMUs kept the satellites in a stable 16-day repeating ground-track cycle, where observations of selected sites at particular scan angles repeated every 16 days throughout the mission. As a result of the drifting orbits, the pattern is now lost for each instrument and the desert sites will now be observed at varying scan angles versus time.…”
Section: Introductionmentioning
confidence: 99%
“…This paper focuses on the impact of the satellite orbit drift on the Earth scene data that is used in the calibration of MODIS RSB by the MODIS Characterization Support Team (MCST), particularly for the North African desert sites and the deep convective clouds (DCC). The impacts of the orbit drift on the solar diffuser calibration and lunar calibration are not discussed here but the strategies have been introduced previously 7,8 and will continue to be developed and improved. In Section 2, we review the calibration algorithms used to generate the Collection 6.1 (C6.1) and Collection 7 (C7) Level 1B (L1B) data products, focusing on how the Earth scene data are used.…”
Section: Introductionmentioning
confidence: 99%