author_facet Zhao, Y.
Strong, K.
Kondo, Y.
Koike, M.
Matsumi, Y.
Irie, H.
Rinsland, C. P.
Jones, N. B.
Suzuki, K.
Nakajima, H.
Nakane, H.
Murata, I.
Zhao, Y.
Strong, K.
Kondo, Y.
Koike, M.
Matsumi, Y.
Irie, H.
Rinsland, C. P.
Jones, N. B.
Suzuki, K.
Nakajima, H.
Nakane, H.
Murata, I.
author Zhao, Y.
Strong, K.
Kondo, Y.
Koike, M.
Matsumi, Y.
Irie, H.
Rinsland, C. P.
Jones, N. B.
Suzuki, K.
Nakajima, H.
Nakane, H.
Murata, I.
spellingShingle Zhao, Y.
Strong, K.
Kondo, Y.
Koike, M.
Matsumi, Y.
Irie, H.
Rinsland, C. P.
Jones, N. B.
Suzuki, K.
Nakajima, H.
Nakane, H.
Murata, I.
Journal of Geophysical Research: Atmospheres
Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
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 zhao, y.
spelling Zhao, Y. Strong, K. Kondo, Y. Koike, M. Matsumi, Y. Irie, H. Rinsland, C. P. Jones, N. B. Suzuki, K. Nakajima, H. Nakane, H. Murata, I. 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/10.1029/2001jd000748 <jats:p>Tropospheric column amounts and mixing ratios of CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub>, and HCN were retrieved from ground‐based infrared solar spectra using a vertical profile retrieval algorithm (SFIT2). The spectra were recorded with high spectral resolution Fourier transform infrared (FTIR) spectrometers at Moshiri (44.4°N) and Rikubetsu (43.5°N) in northern Japan from May 1995 to June 2000. The retrievals show significant seasonal variations in the tropospheric content of the four molecules over northern Japan with maxima in winter‐spring (February–April) for CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> and in summer (May–July) for HCN. Good correlations between CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> indicated that they had similar sources and underwent similar dilution processes. Deviation of HCN relative to its seasonal mean value (ΔHCN) is correlated with the similar deviation of CO (ΔCO), indicating that enhancements of CO and HCN above the mean levels were probably due to the same sources. Linear trends in tropospheric CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> from May 1995 to June 2000 (excluding 1998) were (−2.10 ± 0.30), (−2.53 ± 0.30), and (−3.99 ± 0.57)%/yr, respectively, while the trend of (−0.93 ± 0.49)%/yr in HCN was relatively small. Abnormally high tropospheric amounts of the four molecules were recorded in 1998. HCN amounts were found to be much higher than its seasonal mean value throughout 1998 with a 65% maximum increase in August 1998. Significant increases of CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> took place in August–October 1998. Trajectory calculations, global fire maps, and satellite smoke images revealed that biomass burning in eastern Siberia from mid‐July to early October 1998 was the major cause of the elevated levels in tropospheric CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub>, and HCN observed in northern Japan in 1998.</jats:p> Spectroscopic measurements of tropospheric CO, C<sub>2</sub>H<sub>6</sub>, C<sub>2</sub>H<sub>2</sub>, and HCN in northern Japan Journal of Geophysical Research: Atmospheres
doi_str_mv 10.1029/2001jd000748
facet_avail Online
Free
finc_class_facet Technik
Geologie und Paläontologie
Geographie
Chemie und Pharmazie
Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft
Biologie
Allgemeine Naturwissenschaft
Physik
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id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDAxamQwMDA3NDg
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DE-Bn3
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imprint American Geophysical Union (AGU), 2002
imprint_str_mv American Geophysical Union (AGU), 2002
issn 0148-0227
issn_str_mv 0148-0227
language English
mega_collection American Geophysical Union (AGU) (CrossRef)
match_str zhao2002spectroscopicmeasurementsoftroposphericcoc2h6c2h2andhcninnorthernjapan
publishDateSort 2002
publisher American Geophysical Union (AGU)
recordtype ai
record_format ai
series Journal of Geophysical Research: Atmospheres
source_id 49
title Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_unstemmed Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_full Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_fullStr Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_full_unstemmed Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_short Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_sort spectroscopic measurements of tropospheric co, c<sub>2</sub>h<sub>6</sub>, c<sub>2</sub>h<sub>2</sub>, and hcn in northern japan
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/10.1029/2001jd000748
publishDate 2002
physical
description <jats:p>Tropospheric column amounts and mixing ratios of CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub>, and HCN were retrieved from ground‐based infrared solar spectra using a vertical profile retrieval algorithm (SFIT2). The spectra were recorded with high spectral resolution Fourier transform infrared (FTIR) spectrometers at Moshiri (44.4°N) and Rikubetsu (43.5°N) in northern Japan from May 1995 to June 2000. The retrievals show significant seasonal variations in the tropospheric content of the four molecules over northern Japan with maxima in winter‐spring (February–April) for CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> and in summer (May–July) for HCN. Good correlations between CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> indicated that they had similar sources and underwent similar dilution processes. Deviation of HCN relative to its seasonal mean value (ΔHCN) is correlated with the similar deviation of CO (ΔCO), indicating that enhancements of CO and HCN above the mean levels were probably due to the same sources. Linear trends in tropospheric CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> from May 1995 to June 2000 (excluding 1998) were (−2.10 ± 0.30), (−2.53 ± 0.30), and (−3.99 ± 0.57)%/yr, respectively, while the trend of (−0.93 ± 0.49)%/yr in HCN was relatively small. Abnormally high tropospheric amounts of the four molecules were recorded in 1998. HCN amounts were found to be much higher than its seasonal mean value throughout 1998 with a 65% maximum increase in August 1998. Significant increases of CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> took place in August–October 1998. Trajectory calculations, global fire maps, and satellite smoke images revealed that biomass burning in eastern Siberia from mid‐July to early October 1998 was the major cause of the elevated levels in tropospheric CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub>, and HCN observed in northern Japan in 1998.</jats:p>
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author Zhao, Y., Strong, K., Kondo, Y., Koike, M., Matsumi, Y., Irie, H., Rinsland, C. P., Jones, N. B., Suzuki, K., Nakajima, H., Nakane, H., Murata, I.
author_facet Zhao, Y., Strong, K., Kondo, Y., Koike, M., Matsumi, Y., Irie, H., Rinsland, C. P., Jones, N. B., Suzuki, K., Nakajima, H., Nakane, H., Murata, I., Zhao, Y., Strong, K., Kondo, Y., Koike, M., Matsumi, Y., Irie, H., Rinsland, C. P., Jones, N. B., Suzuki, K., Nakajima, H., Nakane, H., Murata, I.
author_sort zhao, y.
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container_title Journal of Geophysical Research: Atmospheres
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description <jats:p>Tropospheric column amounts and mixing ratios of CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub>, and HCN were retrieved from ground‐based infrared solar spectra using a vertical profile retrieval algorithm (SFIT2). The spectra were recorded with high spectral resolution Fourier transform infrared (FTIR) spectrometers at Moshiri (44.4°N) and Rikubetsu (43.5°N) in northern Japan from May 1995 to June 2000. The retrievals show significant seasonal variations in the tropospheric content of the four molecules over northern Japan with maxima in winter‐spring (February–April) for CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> and in summer (May–July) for HCN. Good correlations between CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> indicated that they had similar sources and underwent similar dilution processes. Deviation of HCN relative to its seasonal mean value (ΔHCN) is correlated with the similar deviation of CO (ΔCO), indicating that enhancements of CO and HCN above the mean levels were probably due to the same sources. Linear trends in tropospheric CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> from May 1995 to June 2000 (excluding 1998) were (−2.10 ± 0.30), (−2.53 ± 0.30), and (−3.99 ± 0.57)%/yr, respectively, while the trend of (−0.93 ± 0.49)%/yr in HCN was relatively small. Abnormally high tropospheric amounts of the four molecules were recorded in 1998. HCN amounts were found to be much higher than its seasonal mean value throughout 1998 with a 65% maximum increase in August 1998. Significant increases of CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> took place in August–October 1998. Trajectory calculations, global fire maps, and satellite smoke images revealed that biomass burning in eastern Siberia from mid‐July to early October 1998 was the major cause of the elevated levels in tropospheric CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub>, and HCN observed in northern Japan in 1998.</jats:p>
doi_str_mv 10.1029/2001jd000748
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id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDAxamQwMDA3NDg
imprint American Geophysical Union (AGU), 2002
imprint_str_mv American Geophysical Union (AGU), 2002
institution DE-D275, DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161, DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1, DE-L229
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match_str zhao2002spectroscopicmeasurementsoftroposphericcoc2h6c2h2andhcninnorthernjapan
mega_collection American Geophysical Union (AGU) (CrossRef)
physical
publishDate 2002
publishDateSort 2002
publisher American Geophysical Union (AGU)
record_format ai
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series Journal of Geophysical Research: Atmospheres
source_id 49
spelling Zhao, Y. Strong, K. Kondo, Y. Koike, M. Matsumi, Y. Irie, H. Rinsland, C. P. Jones, N. B. Suzuki, K. Nakajima, H. Nakane, H. Murata, I. 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/10.1029/2001jd000748 <jats:p>Tropospheric column amounts and mixing ratios of CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub>, and HCN were retrieved from ground‐based infrared solar spectra using a vertical profile retrieval algorithm (SFIT2). The spectra were recorded with high spectral resolution Fourier transform infrared (FTIR) spectrometers at Moshiri (44.4°N) and Rikubetsu (43.5°N) in northern Japan from May 1995 to June 2000. The retrievals show significant seasonal variations in the tropospheric content of the four molecules over northern Japan with maxima in winter‐spring (February–April) for CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> and in summer (May–July) for HCN. Good correlations between CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> indicated that they had similar sources and underwent similar dilution processes. Deviation of HCN relative to its seasonal mean value (ΔHCN) is correlated with the similar deviation of CO (ΔCO), indicating that enhancements of CO and HCN above the mean levels were probably due to the same sources. Linear trends in tropospheric CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> from May 1995 to June 2000 (excluding 1998) were (−2.10 ± 0.30), (−2.53 ± 0.30), and (−3.99 ± 0.57)%/yr, respectively, while the trend of (−0.93 ± 0.49)%/yr in HCN was relatively small. Abnormally high tropospheric amounts of the four molecules were recorded in 1998. HCN amounts were found to be much higher than its seasonal mean value throughout 1998 with a 65% maximum increase in August 1998. Significant increases of CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, and C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub> took place in August–October 1998. Trajectory calculations, global fire maps, and satellite smoke images revealed that biomass burning in eastern Siberia from mid‐July to early October 1998 was the major cause of the elevated levels in tropospheric CO, C<jats:sub>2</jats:sub>H<jats:sub>6</jats:sub>, C<jats:sub>2</jats:sub>H<jats:sub>2</jats:sub>, and HCN observed in northern Japan in 1998.</jats:p> Spectroscopic measurements of tropospheric CO, C<sub>2</sub>H<sub>6</sub>, C<sub>2</sub>H<sub>2</sub>, and HCN in northern Japan Journal of Geophysical Research: Atmospheres
spellingShingle Zhao, Y., Strong, K., Kondo, Y., Koike, M., Matsumi, Y., Irie, H., Rinsland, C. P., Jones, N. B., Suzuki, K., Nakajima, H., Nakane, H., Murata, I., Journal of Geophysical Research: Atmospheres, Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan, 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 Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_full Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_fullStr Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_full_unstemmed Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_short Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
title_sort spectroscopic measurements of tropospheric co, c<sub>2</sub>h<sub>6</sub>, c<sub>2</sub>h<sub>2</sub>, and hcn in northern japan
title_unstemmed Spectroscopic measurements of tropospheric CO, C2H6, C2H2, and HCN in northern Japan
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/10.1029/2001jd000748