2018
DOI: 10.1109/tgrs.2017.2758804
|View full text |Cite
|
Sign up to set email alerts
|

Improving Land Surface Temperature and Emissivity Retrieval From the Chinese Gaofen-5 Satellite Using a Hybrid Algorithm

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
34
0

Year Published

2019
2019
2024
2024

Publication Types

Select...
6
1

Relationship

0
7

Authors

Journals

citations
Cited by 60 publications
(37 citation statements)
references
References 48 publications
0
34
0
Order By: Relevance
“…For OI system, the best horizontal correlation length was found to be 50 km [58]. For Nudging data assimilation system, the best depth of influence and time scale were found to be 4.0 m and 1800 s, respectively [54]. For indirect data assimilation via correcting wind stress, the best assimilation coefficient is −1 [41].…”
Section: Resultsmentioning
confidence: 94%
See 3 more Smart Citations
“…For OI system, the best horizontal correlation length was found to be 50 km [58]. For Nudging data assimilation system, the best depth of influence and time scale were found to be 4.0 m and 1800 s, respectively [54]. For indirect data assimilation via correcting wind stress, the best assimilation coefficient is −1 [41].…”
Section: Resultsmentioning
confidence: 94%
“…Other data assimilation cycle lengths less than 1 h were examined as well, but the differences were not significant. The main reasons for assimilating data over shorter temporal intervals into models are presented by Ren and Hartnett [54]. The best data assimilation cycle length was found to be at each model computational time step for DI, OI and Nudging; the best data assimilation cycle length was one minute for indirect data assimilation via correcting wind stress.…”
Section: Resultsmentioning
confidence: 99%
See 2 more Smart Citations
“…With development of earth observation, satellite remote sensing data have been extensively used for numerous studies [1,2], such as land surface temperature retrieval [3][4][5][6], agro-drought monitoring [7], soil moisture estimation [8], evapotranspiration modelling [9] and radiation flux estimation [10]. Since the first Landsat sensor TM (Thematic Mapper) was launched in 1982, Landsat data are referred to as one of the most widely and frequently used imagery sources in land cover study for their availability, relatively high spatial resolution and wide spectral range [11,12].…”
Section: Introductionmentioning
confidence: 99%