1952
DOI: 10.1021/ie50508a043
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Ozone in Los Angeles and Surrounding Areas

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Cited by 9 publications
(5 citation statements)
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“…It is typically measured by sampling air between 2 m and 10 m above the surface. Historical observations of surface ozone mixing ratios (mole fractions) range from zero to over 400 nmol mol -1 (Bartel and Temple, 1952;Riveros et al, 1998;Lacasaña-Navarro et al, 1999). As documented in this article, current measurements rarely exceed 200 nmol mol -1 (see Table 5 in section 5).…”
Section: Introductionmentioning
confidence: 77%
“…It is typically measured by sampling air between 2 m and 10 m above the surface. Historical observations of surface ozone mixing ratios (mole fractions) range from zero to over 400 nmol mol -1 (Bartel and Temple, 1952;Riveros et al, 1998;Lacasaña-Navarro et al, 1999). As documented in this article, current measurements rarely exceed 200 nmol mol -1 (see Table 5 in section 5).…”
Section: Introductionmentioning
confidence: 77%
“…The sensor solution composition recipes used by the early ECC ozonesondes originated from the wet chemical, iodometric techniques (Bartel and Temple, 1952;Littman and Benoliel, 1953;Saltzman and Gilbert, 1959;Boyd et al, 1970). The method involves the absorption of ozone and oxidation of iodide ions to iodine (I 2 ) with an overall stoichiometric balance of 1 : 1 (O 3 = I 2 ) as shown in Eq.…”
Section: Sensing Solution Type Changesmentioning
confidence: 99%
“…The sensor solution composition recipes 20 used by the early ECC ozonesondes originated from the wet chemical, iodometric techniques (Bartel and Temple (1952); Littman and Benoliel (1953); Saltzman and Gilbert (1959); Boyd et al (1970)). The method involves the absorption of ozone and oxidation of iodide ions to iodine (I2) with an overall stoichiometric balance of 1:1 (O3 = I2) as shown in Eqn.…”
Section: Sensing Solution Type Changesmentioning
confidence: 99%