Zobrazeno 1 - 10
of 64
pro vyhledávání: '"En-Bo Wei"'
Publikováno v:
Remote Sensing, Vol 6, Iss 11, Pp 10913-10930 (2014)
For a foam-covered sea surface, it is difficult to retrieve sea surface salinity (SSS) with L-band brightness temperature (1.4 GHz) because of the effect of a foam layer with wind speeds stronger than 7 m/s, especially at low sea surface temperature
Externí odkaz:
https://doaj.org/article/21622929d5554449baf6073bafecc4d1
Publikováno v:
International Journal of Remote Sensing. 41:4293-4311
For high wind speeds (7–22 m s−1), a semi-theoretical model for retrieving sea surface salinity (SSS) is derived from the version V3.0 of Aquarius data. In the model, the sea surface bright...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6f72413edd69244ebcac6b3a2e3a67f7
https://doi.org/10.1080/01431161.2020.1714783
https://doi.org/10.1080/01431161.2020.1714783
Publikováno v:
Journal of Ocean University of China. 18:1051-1060
The wind retrieval performance of HY-2A scanning scatterometer operating at Ku-band in HH and VV polarizations has been well evaluated in the wind speed range of 0–25 ms−1. In order to obtain more accurate ocean wind field, a potential extension
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af87ddf9898991ff6fcea88617a1dcdb
https://doi.org/10.1007/s11802-019-4018-z
https://doi.org/10.1007/s11802-019-4018-z
Autor:
Guo-Qing Gu, En-Bo Wei
Publikováno v:
International Journal of Modern Physics B. 35:2150164
In this paper, rotation properties of suspended particles under an external rotating electric field (EREF) are investigated. Based on the re-distribution of surface-induced charges on moving particles, the torque exerting on particles by EREF is deri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c9ce9d9e7d94f3b5c00902745a8a9524
https://doi.org/10.1142/s0217979221501642
https://doi.org/10.1142/s0217979221501642
Publikováno v:
In Physica B: Physics of Condensed Matter 2002 324(1):322-328
The air volume fraction (AVF) of a sea foam layer is a key parameter that affects the microwave emissivity and brightness temperature of the sea surface. To extract AVF of a sea foam layer from the measured emissivity data at microwave frequencies, a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::14b0d7983a996f36a42a7d6cd57c5392
Publikováno v:
Journal of Ocean University of China. 14:38-46
Permittivity of a sea foam layer is very important in investigating ocean brightness temperature model. At microwave frequency, the Rayleigh method is developed to estimate the effective permittivity of the sea foam layer. To simplify the tedious cal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::089c162d01a625a7d8667cc098eff529
https://doi.org/10.1007/s11802-015-2383-9
https://doi.org/10.1007/s11802-015-2383-9
Publikováno v:
Remote Sensing, Vol 6, Iss 11, Pp 10913-10930 (2014)
Remote Sensing; Volume 6; Issue 11; Pages: 10913-10930
Remote Sensing; Volume 6; Issue 11; Pages: 10913-10930
For a foam-covered sea surface, it is difficult to retrieve sea surface salinity (SSS) with L-band brightness temperature (1.4 GHz) because of the effect of a foam layer with wind speeds stronger than 7 m/s, especially at low sea surface temperature
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f9b0faf62f8012c88242a138c2afba17
https://doi.org/10.3390/rs61110913
https://doi.org/10.3390/rs61110913
Publikováno v:
International Journal of Remote Sensing. 35:1511-1525
To investigate the effects of sea foam or whitecaps on the emissivity of sea surface, microwave radiometric experiments of foam-covered sea surface at C-band 6.8 GHz were conducted by artificial foam during September 2012 at Tangdao bay of Qingdao. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c3ce55dcadc4d08d49f97db14b63d20
https://doi.org/10.1080/01431161.2013.878064
https://doi.org/10.1080/01431161.2013.878064
Publikováno v:
Journal of Applied Physics; 3/1/2006, Vol. 99 Issue 5, p054101, 5p, 5 Graphs