author_facet Harder, J. W.
Jakoubek, R. O.
Mount, G. H.
Harder, J. W.
Jakoubek, R. O.
Mount, G. H.
author Harder, J. W.
Jakoubek, R. O.
Mount, G. H.
spellingShingle Harder, J. W.
Jakoubek, R. O.
Mount, G. H.
Journal of Geophysical Research: Atmospheres
Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
Paleontology
Space and Planetary Science
Earth and Planetary Sciences (miscellaneous)
Atmospheric Science
Earth-Surface Processes
Geochemistry and Petrology
Soil Science
Water Science and Technology
Ecology
Aquatic Science
Forestry
Oceanography
Geophysics
author_sort harder, j. w.
spelling Harder, J. W. Jakoubek, R. O. Mount, G. H. 0148-0227 American Geophysical Union (AGU) Paleontology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Atmospheric Science Earth-Surface Processes Geochemistry and Petrology Soil Science Water Science and Technology Ecology Aquatic Science Forestry Oceanography Geophysics http://dx.doi.org/10.1029/96jd03608 <jats:p>In August and September 1993 a comparative study of tropospheric long‐path absorption techniques with in situ methods was performed for both the hydroxyl radical and the other important trace species. Long‐path measurements were made over the 10.3 km path between Fritz Peak Observatory and Caribou Mine in the mountains 17 km west of Boulder, Colorado. At Caribou Mine, a 121 element, 1 m<jats:sup>2</jats:sup> retroreflector array folds the optical path to give a total path of 20.6 km. The in situ instruments were located at Idaho Hill 0.5 km northwest of Caribou Mine. The optical design and analysis techniques used to obtain the path‐integrated concentrations of O<jats:sub>3</jats:sub>, CH<jats:sub>2</jats:sub>O, SO<jats:sub>2</jats:sub>, and NO<jats:sub>2</jats:sub> will be presented. The spectrograph used in this study is a 1/4 m double, crossed Czerny‐Turner that employs a diode array detector allowing the acquisition of 40 nm spectral bands in the near UV and visible spectral regions. This system also utilizes automatic alignment and self‐adjusting time integration so the system will acquire data in an unattended mode. The spectral bands selected for this study permit the simultaneous measurement of O<jats:sub>3</jats:sub>, NO<jats:sub>2</jats:sub>, CH<jats:sub>2</jats:sub>O, and SO<jats:sub>2</jats:sub>; NO<jats:sub>2</jats:sub> and H<jats:sub>2</jats:sub>O; and NO<jats:sub>3</jats:sub> and H<jats:sub>2</jats:sub>O. The data analysis uses a nonlinear least squares regression procedure to deduce the concentration of each of the species present in the atmosphere and also provides an effective method for removing the influence of scattered solar light for daytime measurements. An estimate of the measurement precision can be found by comparing atmospheric spectra analyzed with two different <jats:italic>I<jats:sub>O</jats:sub></jats:italic> spectra; one measured through the atmosphere and the other a direct arc lamp spectrum.</jats:p> Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment Journal of Geophysical Research: Atmospheres
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Geographie
Chemie und Pharmazie
Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft
Biologie
Allgemeine Naturwissenschaft
Physik
Technik
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series Journal of Geophysical Research: Atmospheres
source_id 49
title Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_unstemmed Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_full Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_fullStr Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_full_unstemmed Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_short Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_sort measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 oh photochemistry experiment
topic Paleontology
Space and Planetary Science
Earth and Planetary Sciences (miscellaneous)
Atmospheric Science
Earth-Surface Processes
Geochemistry and Petrology
Soil Science
Water Science and Technology
Ecology
Aquatic Science
Forestry
Oceanography
Geophysics
url http://dx.doi.org/10.1029/96jd03608
publishDate 1997
physical 6215-6226
description <jats:p>In August and September 1993 a comparative study of tropospheric long‐path absorption techniques with in situ methods was performed for both the hydroxyl radical and the other important trace species. Long‐path measurements were made over the 10.3 km path between Fritz Peak Observatory and Caribou Mine in the mountains 17 km west of Boulder, Colorado. At Caribou Mine, a 121 element, 1 m<jats:sup>2</jats:sup> retroreflector array folds the optical path to give a total path of 20.6 km. The in situ instruments were located at Idaho Hill 0.5 km northwest of Caribou Mine. The optical design and analysis techniques used to obtain the path‐integrated concentrations of O<jats:sub>3</jats:sub>, CH<jats:sub>2</jats:sub>O, SO<jats:sub>2</jats:sub>, and NO<jats:sub>2</jats:sub> will be presented. The spectrograph used in this study is a 1/4 m double, crossed Czerny‐Turner that employs a diode array detector allowing the acquisition of 40 nm spectral bands in the near UV and visible spectral regions. This system also utilizes automatic alignment and self‐adjusting time integration so the system will acquire data in an unattended mode. The spectral bands selected for this study permit the simultaneous measurement of O<jats:sub>3</jats:sub>, NO<jats:sub>2</jats:sub>, CH<jats:sub>2</jats:sub>O, and SO<jats:sub>2</jats:sub>; NO<jats:sub>2</jats:sub> and H<jats:sub>2</jats:sub>O; and NO<jats:sub>3</jats:sub> and H<jats:sub>2</jats:sub>O. The data analysis uses a nonlinear least squares regression procedure to deduce the concentration of each of the species present in the atmosphere and also provides an effective method for removing the influence of scattered solar light for daytime measurements. An estimate of the measurement precision can be found by comparing atmospheric spectra analyzed with two different <jats:italic>I<jats:sub>O</jats:sub></jats:italic> spectra; one measured through the atmosphere and the other a direct arc lamp spectrum.</jats:p>
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author Harder, J. W., Jakoubek, R. O., Mount, G. H.
author_facet Harder, J. W., Jakoubek, R. O., Mount, G. H., Harder, J. W., Jakoubek, R. O., Mount, G. H.
author_sort harder, j. w.
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description <jats:p>In August and September 1993 a comparative study of tropospheric long‐path absorption techniques with in situ methods was performed for both the hydroxyl radical and the other important trace species. Long‐path measurements were made over the 10.3 km path between Fritz Peak Observatory and Caribou Mine in the mountains 17 km west of Boulder, Colorado. At Caribou Mine, a 121 element, 1 m<jats:sup>2</jats:sup> retroreflector array folds the optical path to give a total path of 20.6 km. The in situ instruments were located at Idaho Hill 0.5 km northwest of Caribou Mine. The optical design and analysis techniques used to obtain the path‐integrated concentrations of O<jats:sub>3</jats:sub>, CH<jats:sub>2</jats:sub>O, SO<jats:sub>2</jats:sub>, and NO<jats:sub>2</jats:sub> will be presented. The spectrograph used in this study is a 1/4 m double, crossed Czerny‐Turner that employs a diode array detector allowing the acquisition of 40 nm spectral bands in the near UV and visible spectral regions. This system also utilizes automatic alignment and self‐adjusting time integration so the system will acquire data in an unattended mode. The spectral bands selected for this study permit the simultaneous measurement of O<jats:sub>3</jats:sub>, NO<jats:sub>2</jats:sub>, CH<jats:sub>2</jats:sub>O, and SO<jats:sub>2</jats:sub>; NO<jats:sub>2</jats:sub> and H<jats:sub>2</jats:sub>O; and NO<jats:sub>3</jats:sub> and H<jats:sub>2</jats:sub>O. The data analysis uses a nonlinear least squares regression procedure to deduce the concentration of each of the species present in the atmosphere and also provides an effective method for removing the influence of scattered solar light for daytime measurements. An estimate of the measurement precision can be found by comparing atmospheric spectra analyzed with two different <jats:italic>I<jats:sub>O</jats:sub></jats:italic> spectra; one measured through the atmosphere and the other a direct arc lamp spectrum.</jats:p>
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spelling Harder, J. W. Jakoubek, R. O. Mount, G. H. 0148-0227 American Geophysical Union (AGU) Paleontology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Atmospheric Science Earth-Surface Processes Geochemistry and Petrology Soil Science Water Science and Technology Ecology Aquatic Science Forestry Oceanography Geophysics http://dx.doi.org/10.1029/96jd03608 <jats:p>In August and September 1993 a comparative study of tropospheric long‐path absorption techniques with in situ methods was performed for both the hydroxyl radical and the other important trace species. Long‐path measurements were made over the 10.3 km path between Fritz Peak Observatory and Caribou Mine in the mountains 17 km west of Boulder, Colorado. At Caribou Mine, a 121 element, 1 m<jats:sup>2</jats:sup> retroreflector array folds the optical path to give a total path of 20.6 km. The in situ instruments were located at Idaho Hill 0.5 km northwest of Caribou Mine. The optical design and analysis techniques used to obtain the path‐integrated concentrations of O<jats:sub>3</jats:sub>, CH<jats:sub>2</jats:sub>O, SO<jats:sub>2</jats:sub>, and NO<jats:sub>2</jats:sub> will be presented. The spectrograph used in this study is a 1/4 m double, crossed Czerny‐Turner that employs a diode array detector allowing the acquisition of 40 nm spectral bands in the near UV and visible spectral regions. This system also utilizes automatic alignment and self‐adjusting time integration so the system will acquire data in an unattended mode. The spectral bands selected for this study permit the simultaneous measurement of O<jats:sub>3</jats:sub>, NO<jats:sub>2</jats:sub>, CH<jats:sub>2</jats:sub>O, and SO<jats:sub>2</jats:sub>; NO<jats:sub>2</jats:sub> and H<jats:sub>2</jats:sub>O; and NO<jats:sub>3</jats:sub> and H<jats:sub>2</jats:sub>O. The data analysis uses a nonlinear least squares regression procedure to deduce the concentration of each of the species present in the atmosphere and also provides an effective method for removing the influence of scattered solar light for daytime measurements. An estimate of the measurement precision can be found by comparing atmospheric spectra analyzed with two different <jats:italic>I<jats:sub>O</jats:sub></jats:italic> spectra; one measured through the atmosphere and the other a direct arc lamp spectrum.</jats:p> Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment Journal of Geophysical Research: Atmospheres
spellingShingle Harder, J. W., Jakoubek, R. O., Mount, G. H., Journal of Geophysical Research: Atmospheres, Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment, Paleontology, Space and Planetary Science, Earth and Planetary Sciences (miscellaneous), Atmospheric Science, Earth-Surface Processes, Geochemistry and Petrology, Soil Science, Water Science and Technology, Ecology, Aquatic Science, Forestry, Oceanography, Geophysics
title Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_full Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_fullStr Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_full_unstemmed Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_short Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
title_sort measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 oh photochemistry experiment
title_unstemmed Measurement of tropospheric trace gases by long‐path differential absorption spectroscopy during the 1993 OH Photochemistry Experiment
topic Paleontology, Space and Planetary Science, Earth and Planetary Sciences (miscellaneous), Atmospheric Science, Earth-Surface Processes, Geochemistry and Petrology, Soil Science, Water Science and Technology, Ecology, Aquatic Science, Forestry, Oceanography, Geophysics
url http://dx.doi.org/10.1029/96jd03608