In situ angular measurements of thermal infrared sea surface emissivity—Validation of models

2005 ◽  
Vol 94 (1) ◽  
pp. 83-93 ◽  
Author(s):  
Raquel Niclòs ◽  
Enric Valor ◽  
Vicente Caselles ◽  
César Coll ◽  
Juan Manuel Sánchez
2005 ◽  
Vol 131 (610) ◽  
pp. 2539-2557 ◽  
Author(s):  
S. M. Newman ◽  
J. A. Smith ◽  
M. D. Glew ◽  
S. M. Rogers ◽  
J. P. Taylor

2004 ◽  
Author(s):  
Raquel R. Niclos ◽  
Enric Valor ◽  
Vicente Caselles ◽  
Cesar Coll

Author(s):  
Raquel Niclòs ◽  
Vicente Caselles ◽  
César Coll ◽  
Enric Valor ◽  
Eva Rubio

2013 ◽  
Vol 24 (3) ◽  
pp. 147
Author(s):  
Ming LI ◽  
Qinghua YANG ◽  
Jiechen ZHAO ◽  
Lin ZHANG ◽  
Chunhua LI ◽  
...  

2021 ◽  
Vol 1961 (1) ◽  
pp. 012065
Author(s):  
Yanyan Li ◽  
Zhenzhan Wang ◽  
Yiqiang Hu ◽  
Xiaolin Tong

2021 ◽  
Vol 13 (4) ◽  
pp. 811
Author(s):  
Hao Liu ◽  
Zexun Wei

The variability in sea surface salinity (SSS) on different time scales plays an important role in associated oceanic or climate processes. In this study, we compare the SSS on sub-annual, annual, and interannual time scales among ten datasets, including in situ-based and satellite-based SSS products over 2011–2018. Furthermore, the dominant mode on different time scales is compared using the empirical orthogonal function (EOF). Our results show that the largest spread of ten products occurs on the sub-annual time scale. High correlation coefficients (0.6~0.95) are found in the global mean annual and interannual SSSs between individual products and the ensemble mean. Furthermore, this study shows good agreement among the ten datasets in representing the dominant mode of SSS on the annual and interannual time scales. This analysis provides information on the consistency and discrepancy of datasets to guide future use, such as improvements to ocean data assimilation and the quality of satellite-based data.


2012 ◽  
Vol 433-440 ◽  
pp. 6054-6059
Author(s):  
Gan Nan Yuan ◽  
Rui Cai Jia ◽  
Yun Tao Dai ◽  
Ying Li

In the radar imaging mechanism different phenomena are present, as a result the radar image is not a direct representation of the sea state. In analyzing radar image spectra, it can be realized that all of these phenomena produce distortions in the wave spectrum. The main effects are more energy for very low frequencies. This work investigates the structure of the sea clutter spectrum, and analysis the low wave number energy influence on determining sea surface current. Then the radar measure current is validated by experiments. By comparing with the in situ data, we know that the radar results reversed by image spectrum without low wave number spectrum have high precision. The low wave number energy influent determining current seriously.


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