2008
DOI: 10.1029/2008jd010176
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Extinction, refraction, and delay in the atmosphere

Abstract: [1] This paper establishes that absolute optical air mass and hydrostatic atmospheric delay of electromagnetic waves are proportional magnitudes, and, consequently, their respective obliquity ratios are identical dimensionless quantities. This means that a potential source for developing new models for relative optical air mass can be found in the formulae for the atmospheric delay in electromagnetic signals (and vice versa). In this respect, for estimating relative optical air mass, we demonstrate that Herrin… Show more

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Cited by 8 publications
(18 citation statements)
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References 34 publications
(104 reference statements)
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“…Introduced by Kasten [1965], this functional form was applied by Kasten and Young [1989], Rapp‐Arrarás and Domingo‐Santos [2008], and Rapp‐Arrarás [2009, chapter 4]. We will refer to it as Ka‐3, and its mathematical expression, as a function of the apparent zenith distance, is fz,a=1cosz+a1/a2za3. Kasten [1965] also provided an obliquity function for the optical mass of atmospheric water vapor following this model.…”
Section: Functional Formsmentioning
confidence: 99%
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“…Introduced by Kasten [1965], this functional form was applied by Kasten and Young [1989], Rapp‐Arrarás and Domingo‐Santos [2008], and Rapp‐Arrarás [2009, chapter 4]. We will refer to it as Ka‐3, and its mathematical expression, as a function of the apparent zenith distance, is fz,a=1cosz+a1/a2za3. Kasten [1965] also provided an obliquity function for the optical mass of atmospheric water vapor following this model.…”
Section: Functional Formsmentioning
confidence: 99%
“…Adopted by Ifadis [1986, 2000] for modeling the atmospheric delay of radio signals, the triparametric version of the truncated continued fraction by Marini [1972] was applied by Rapp‐Arrarás and Domingo‐Santos [2008]to approximate air mass. We will refer to it as Ma‐3, and its mathematical expression, as a function of the apparent zenith distance, is fz,a=1cosz+a1/cosz+a2/cosz+a3. …”
Section: Functional Formsmentioning
confidence: 99%
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“…is the original light beam intensity β e is the extinction coefficient over the medium thickness h. To calculate transmissivity, β e ∆h for each distinctive layer of the atmosphere Liou [27], Rapp-Arraras [28] need to be determined to give the total extinction, as in Equation (2). Alternatively, Aglietti [29] shows that a global extinction coefficient of 0.32 can be derived using standard test conditions since the SPP is known at the TOA, 1366 Wm −2 , and the AM1.5 direct beam component at MSL; 850 Wm −2 is specified for testing PV panels.…”
Section: Harvesting Of Direct Insolationmentioning
confidence: 99%