Comparisons between in Situ Anisotropic Reflectance Measurements and Simulations for Vegetation Canopies: Validation and Sensitivity Analysis

Author(s):  
Yen-Ben Cheng ◽  
Lawrence A. Corp ◽  
Elizabeth M. Middleton ◽  
Karl F. Huemmrich ◽  
Qingyuan Zhang ◽  
...  
2007 ◽  
Vol 4 (4) ◽  
pp. 2441-2491 ◽  
Author(s):  
M. S. Twardowski ◽  
H. Claustre ◽  
S. A. Freeman ◽  
D. Stramski ◽  
Y. Huot

Abstract. During the BIOSOPE field campaign October–December 2004, measurements of inherent optical properties from the surface to 500 m depth were made with a ship profiler at stations covering over ~8000 km through the Southeast Pacific Ocean. Data from a ~3000 km section containing the very clearest waters in the central gyre are reported here. The total volume scattering function at 117°, βt(117°), was measured with a WET Labs ECO-BB3 sensor at 462, 532, and 650 nm with estimated uncertainties of 2×10−5, 5×10−6, and 2×10−6 m−1 sr−1, respectively. These values were approximately 6%, 3%, and 3% of the scattering by pure seawater at their respective wavelengths. From a methodological perspective, there were several results: – bbp distributions were resolvable even though some of the values from the central gyre were an order of magnitude lower than the lowest previous measurements in the literature; – Direct in-situ measurements of instrument dark offsets were necessary to accurately resolve backscattering at these low levels; – accurate pure seawater backscattering values are critical in determining particulate backscattering coefficients in the open ocean (not only in these very clear waters); the pure water scattering values determined by Buiteveld et al. (1994) with a [1 + 0.3S/37] adjustment for salinity based on Morel (1974) appear to be the most accurate estimates, with aggregate accuracies as low as a few percent; and – closure was demonstrated with subsurface reflectance measurements reported by Morel et al. (2007) within instrument precisions, a useful factor in validating the backscattering measurements. This methodology enabled several observations with respect to the hydrography and the use of backscattering as a biogeochemical proxy: – The clearest waters sampled were found at depths between 300 and 350 m, from 23.5° S, 118° W to 26° S, 114° W, where total backscattering at 650 nm was not distinguishable from pure seawater; – Distributions of particulate backscattering bbp across the central gyre exhibited a broad particle peak centered ~100 m; – The particulate backscattering ratio typically ranged between 0.4% and 0.6% through the majority of the central gyre from the surface to ~210 m, indicative of "soft" water-filled particles with low bulk refractive index; and – bbp at 532 and 650 nm showed a distinct secondary deeper layer centered ~230 m that was absent in particulate attenuation cp data. The particulate backscattering ratio was significantly higher in this layer than in the rest of the water column, reaching 1.2% in some locations. This high relative backscattering, along with the pigment composition and ecological niche of this layer, appear to be consistent with the coccolithophorid F. profunda. Moreover, results were consistent with several expectations extrapolated from theory and previous work in oceanic and coastal regions, supporting the conclusion that particulate and total backscattering could be resolved in these extremely clear natural waters.


Author(s):  
Jhih-Wei You ◽  
Shi-Yu Huang ◽  
Yu-Hsiang Lin ◽  
Meng-Hsiu Tsai ◽  
Ding-Ming Kwai ◽  
...  

2021 ◽  
Vol 39 (6_suppl) ◽  
pp. 395-395
Author(s):  
Vidit Sharma ◽  
Kevin Wymer ◽  
Christopher Saigal ◽  
Karim Chamie ◽  
Mark S. Litwin ◽  
...  

395 Background: Patients with BCG-unresponsive carcinoma in situ (CIS) are treated with radical cystectomy (RCx) or salvage intravesical chemotherapy (SIC). Recently, the FDA approved pembrolizumab for BCG-unresponsive CIS +/- papillary tumors. Given the costs and toxicities of pembrolizumab, it remains unclear whether its benefits are sufficient to warrant widespread use for BCG-unresponsive CIS. To that end, we conducted a cost-effectiveness analysis comparing pembrolizumab with RCx and SIC (using gemcitabine-docetaxel as the prototypical regimen) for patients with BCG-unresponsive CIS. Methods: A decision-analytic Markov model compared pembrolizumab, SIC (with gemcitabine-docetaxel), and RCx for patients with BCG-unresponsive CIS +/- papillary tumors who are RCx candidates (index patient 1) or are unwilling/unable to undergo RCx (index patient 2). Each treatment option was a Markov node containing distinct variations of the following health states: surveillance, recurrence, progression to MIBC, progression to metastasis, treatment toxicity, and death. Incremental Cost-Effectiveness Ratios (ICERs) were compared using a willingness-to-pay threshold of $100,000/Quality-adjusted life year (QALY). The model used a US Medicare perspective with a 5-year time horizon for the base case. One-way and probabilistic sensitivity analyses were performed for all model parameters. Results: For index patient 1, pembrolizumab was not cost-effective vs. RCx (ICER $1,403,008) or SIC (ICER $2,011,923). One-way sensitivity analysis revealed that pembrolizumab only became cost-effective relative to RCx with a > 93% price reduction. Relative to RCx, SIC was cost-effective for time horizons < 5 years and nearly cost-effective at 5 years (ICER $118,324). One-way sensitivity analysis revealed that SIC became cost-effective relative to RCx if its risk of recurrence or metastasis at 2 years was less than 55% or 5.9%, respectively. For index patient 2, pembrolizumab required > 90% price reduction to be cost-effective vs. RCx (ICER $1,073,240). Probabilistic sensitivity analyses revealed that pembrolizumab was unlikely to be cost-effective even at high willingness-to-pay thresholds. Further sensitivity analyses found that no two-way combination of extrapolated values resulted in pembrolizumab being favored over RCx or SIC for either index patient. Conclusions: Based on decision-analytic Markov modeling of treatment options for patients with BCG-unresponsive CIS, pembrolizumab was unlikely to be cost-effective without a > 90% price reduction. While both RCx and SIC were more cost-effective than pembrolizumab, further studies may validate the cost-effectiveness of gemcitabine-docetaxel relative to RCx if the recurrence and metastasis thresholds are met. Overall, our model supports the preferential use of RCx and SIC over pembrolizumab for BCG-unresponsive CIS.


2019 ◽  
Vol 46 (16) ◽  
pp. 9439-9447 ◽  
Author(s):  
Xiaoyi Hu ◽  
Pei Ma ◽  
Yazhou Yang ◽  
Meng‐Hua Zhu ◽  
Te Jiang ◽  
...  

2007 ◽  
Vol 4 (6) ◽  
pp. 1041-1058 ◽  
Author(s):  
M. S. Twardowski ◽  
H. Claustre ◽  
S. A. Freeman ◽  
D. Stramski ◽  
Y. Huot

Abstract. During the BIOSOPE field campaign October–December 2004, measurements of inherent optical properties from the surface to 500 m depth were made with a ship profiler at stations covering over 8000 km through the Southeast Pacific Ocean. Data from a ~3000 km section containing the very clearest waters in the central gyre are reported here. The total volume scattering function at 117°, βt(117°), was measured with a WET Labs ECO-BB3 sensor at 462, 532, and 650 nm with estimated uncertainties of 2×10-5, 5×10-6, and 2×10-6 m−1 sr−1, respectively. These values were approximately 6%, 3%, and 3% of the volume scattering by pure seawater at their respective wavelengths. From a methodological perspective, there were several results: – distributions were resolvable even though some of the values from the central gyre were an order of magnitude lower than the lowest previous measurements in the literature; – Direct in-situ measurements of instrument dark offsets were necessary to accurately resolve backscattering at these low levels; – accurate pure seawater backscattering values are critical in determining particulate backscattering coefficients in the open ocean (not only in these very clear waters); the pure water scattering values determined by Buiteveld et al. (1994) with a [1+0.3S/37] adjustment for salinity based on Morel (1974) appear to be the most accurate estimates, with aggregate accuracies as low as a few percent; and – closure was demonstrated with subsurface reflectance measurements reported by Morel et al. (2007) within instrument precisions, a useful factor in validating the backscattering measurements. This methodology enabled several observations with respect to the hydrography and the use of backscattering as a biogeochemical proxy: –The clearest waters sampled were found at depths between 300 and 350 m, from 23.5° S, 118° W to 26° S, 114° W, where total backscattering at 650 nm was not distinguishable from pure seawater; –Distributions of particulate backscattering bbp across the central gyre exhibited a broad particle peak centered ~100 m; –The particulate backscattering ratio typically ranged between 0.4% and 0.6% at 650 nm through the majority of the central gyre from the surface to ~210 m, indicative of "soft" water-filled particles with low bulk refractive index; and – bbp showed a distinct secondary deeper layer centered ~230 m that was absent in particulate attenuation cp data. The particulate backscattering ratio was significantly higher in this layer than in the rest of the water column, reaching 1.2% in some locations. This high relative backscattering, along with the pigment composition and ecological niche of this layer, appear to be consistent with the coccolithophorid Florisphaera profunda. Moreover, results were consistent with several expectations extrapolated from theory and previous work in oceanic and coastal regions, supporting the conclusion that particulate and total backscattering could be resolved in these extremely clear natural waters.


1995 ◽  
Vol 9 (4) ◽  
pp. 471-476 ◽  
Author(s):  
A. Joiner ◽  
N.M. Jones ◽  
S.J. Raven

In order to understand the factors of extrinsic stain formation more fully, we have developed an in situ stain model. This consists of polished bovine enamel blocks attached to partial or full dentures worn by adult volunteers for 24 h per day. The dentures were cleaned twice daily with a commercial dentifrice and toothbrush, with care taken to avoid brushing the inserts. A Minolta CR321 Chroma Meter in the L*a*b* mode was used for taking reflectance measurements of the stain formed on the enamel inserts. From these values, changes in the color of the inserts were calculated and the level of stain determined. In general, the stain formed on the enamel inserts was yellow and increased in intensity and darkness with time. The enamel inserts with the largest stain increases were from smokers rather than non-smokers. No correlation was observed between amount of stain and quantity of tea and coffee consumed. When the effects of surface roughness on in situ stain formation were considered, the major variable in this study was found to be the location of the enamel insert in the denture rather than the surface roughness.


2007 ◽  
Vol 8 (4-5) ◽  
pp. 187-197 ◽  
Author(s):  
Wenjiang Huang ◽  
David W. Lamb ◽  
Zheng Niu ◽  
Yongjiang Zhang ◽  
Liangyun Liu ◽  
...  

1995 ◽  
Vol 20 (12) ◽  
pp. 1450 ◽  
Author(s):  
Claude Montcalm ◽  
Brian T. Sullivan ◽  
Henri Pépin ◽  
M. Chaker ◽  
Sophie Duguay ◽  
...  

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