Applying double-difference methods for fine-scale acoustic tracking using a short aperture vertical array

2016 ◽  
Vol 140 (4) ◽  
pp. 2950-2950
Author(s):  
Ludovic Tenorio-Hallé ◽  
Aaron M. Thode ◽  
Jit Sarkar ◽  
Chris Verlinden ◽  
Jeffrey Tippmann ◽  
...  
2016 ◽  
Vol 139 (4) ◽  
pp. 2172-2172
Author(s):  
Ludovic Tenorio-Hallé ◽  
Aaron M. Thode ◽  
Jit Sarkar ◽  
Chris Verlinden ◽  
Jeffrey D. Tippmann ◽  
...  

2017 ◽  
Vol 142 (6) ◽  
pp. 3474-3485
Author(s):  
Ludovic Tenorio-Hallé ◽  
Aaron M. Thode ◽  
Jit Sarkar ◽  
Christopher Verlinden ◽  
Jeffrey Tippmann ◽  
...  

2013 ◽  
Vol 134 (3) ◽  
pp. 2446-2461 ◽  
Author(s):  
Delphine Mathias ◽  
Aaron M. Thode ◽  
Jan Straley ◽  
Russel D. Andrews

2020 ◽  
Vol 12 (16) ◽  
pp. 2590 ◽  
Author(s):  
Marie-Laure Frery ◽  
Mathilde Siméon ◽  
Christophe Goldstein ◽  
Pierre Féménias ◽  
Franck Borde ◽  
...  

Copernicus Sentinel-3 Surface Topography Mission embarks a two-channel microwave radiometer combined with the altimeter in order to correct the altimeter range for the excess path delay resulting from the presence of water vapour in the troposphere. The in-flight calibration of a single instrument is the critical point to achieve the expected performances. In the context of a constellation, the inter-calibration is even more important. After a presentation of the instrument design, we present the diagnoses used for the calibration of Sentinel-3A, using vicarious calibration over specific areas and double difference methods. The inter-calibration of Sentinel-3B with Sentinel-3A is performed during the tandem phase, using the residual differences of co-located measurements. Finally performances are assessed at crossover points with two parameters, first the wet troposphere correction by comparison with Jason-3; secondly on the Sea Surface Height by difference of variance. Analysis results have shown that Sentinel-3A is well calibrated, consistent with other instruments, and that Sentinel-3B is calibrated within 0.4 K with Sentinel-3A as a reference. Performances and stability fulfill the requirements for both missions.


2011 ◽  
Vol 82 (6) ◽  
pp. 839-845 ◽  
Author(s):  
S. Bannister ◽  
B. Fry ◽  
M. Reyners ◽  
J. Ristau ◽  
H. Zhang
Keyword(s):  

2018 ◽  
Vol 606 ◽  
pp. 133-150 ◽  
Author(s):  
NM Bacheler ◽  
KW Shertzer ◽  
JA Buckel ◽  
PJ Rudershausen ◽  
BJ Runde

Author(s):  
Russell L. Steere

Complementary replicas have revealed the fact that the two common faces observed in electron micrographs of freeze-fracture and freeze-etch specimens are complementary to each other and are thus the new faces of a split membrane rather than the original inner and outer surfaces (1, 2 and personal observations). The big question raised by published electron micrographs is why do we not see depressions in the complementary face opposite membrane-associated particles? Reports have appeared indicating that some depressions do appear but complementarity on such a fine scale has yet to be shown.Dog cardiac muscle was perfused with glutaraldehyde, washed in distilled water, then transferred to 30% glycerol (material furnished by Dr. Joaquim Sommer, Duke Univ., and VA Hospital, Durham, N.C.). Small strips were freeze-fractured in a Denton Vacuum DFE-2 Freeze-Etch Unit with complementary replica tooling. Replicas were cleaned in chromic acid cleaning solution, then washed in 4 changes of distilled water and mounted on opposite sides of the center wire of a Formvar-coated grid.


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