Characteristics of CO2 Concentration and Flux in the Beijing Urban Area
Publication Date: |
2018-01-27
|
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Publisher: |
Wiley-Blackwell
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Print ISSN: |
0148-0227
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Topics: |
Geosciences
Physics
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Published by: |
_version_ | 1836398765684031488 |
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autor | X. L. Cheng, X. M. Liu, Y. J. Liu, F. Hu |
beschreibung | Since February 2012, CO 2 , H 2 O, and wind data at 10 Hz have been measured by the open-path eddy covariance systems at 8, 16, 47, 80, 140, 200, and 280 m above ground level on the 325-m Beijing meteorological tower. Analysis of the data from 2013 to 2016 indicates that the annual averaged CO 2 concentration increased and the local and regional CO 2 emission decreased with the sequestration of background CO 2 concentration. The maximum values occurred during winter and the minimum values occurred during summer. During spring, summer, and autumn, there was a constant CO 2 flux layer from 47 m to 140 m. However, during winter, CO 2 flux increased with height, and the maximum appeared at approximately 140 m and then decreased with height. Above 47 m, the CO 2 fluxes were represented as the net efflux; and below 16 m, the fluxes were near zero or a net uptake. At all observed heights, the diurnal variation in the CO 2 concentration displayed a clear cycle with a peak corresponding to the morning transportation rush hour. The local wavelet power spectra of the CO 2 concentration, CO 2 flux and other meteorological elements identified significant cross wavelet powers near the 24-h and 365-day bands for the CO 2 concentration and flux with temperature, wind speed, friction velocity, and turbulent kinetic energy. |
citation_standardnr | 6147600 |
datenlieferant | ipn_articles |
feed_copyright | American Geophysical Union (AGU) |
feed_copyright_url | http://www.agu.org/ |
feed_id | 7528 |
feed_publisher | Wiley-Blackwell |
feed_publisher_url | http://www.wiley.com/wiley-blackwell |
insertion_date | 2018-01-27 |
journalissn | 0148-0227 |
publikationsjahr_anzeige | 2018 |
publikationsjahr_facette | 2018 |
publikationsjahr_intervall | 7984:2015-2019 |
publikationsjahr_sort | 2018 |
publisher | Wiley-Blackwell |
quelle | Journal of Geophysical Research JGR - Atmospheres |
relation | http://onlinelibrary.wiley.com/resolve/doi?DOI=10.1002%2F2017JD027409 |
search_space | articles |
shingle_author_1 | X. L. Cheng, X. M. Liu, Y. J. Liu, F. Hu |
shingle_author_2 | X. L. Cheng, X. M. Liu, Y. J. Liu, F. Hu |
shingle_author_3 | X. L. Cheng, X. M. Liu, Y. J. Liu, F. Hu |
shingle_author_4 | X. L. Cheng, X. M. Liu, Y. J. Liu, F. Hu |
shingle_catch_all_1 | Characteristics of CO2 Concentration and Flux in the Beijing Urban Area Since February 2012, CO 2 , H 2 O, and wind data at 10 Hz have been measured by the open-path eddy covariance systems at 8, 16, 47, 80, 140, 200, and 280 m above ground level on the 325-m Beijing meteorological tower. Analysis of the data from 2013 to 2016 indicates that the annual averaged CO 2 concentration increased and the local and regional CO 2 emission decreased with the sequestration of background CO 2 concentration. The maximum values occurred during winter and the minimum values occurred during summer. During spring, summer, and autumn, there was a constant CO 2 flux layer from 47 m to 140 m. However, during winter, CO 2 flux increased with height, and the maximum appeared at approximately 140 m and then decreased with height. Above 47 m, the CO 2 fluxes were represented as the net efflux; and below 16 m, the fluxes were near zero or a net uptake. At all observed heights, the diurnal variation in the CO 2 concentration displayed a clear cycle with a peak corresponding to the morning transportation rush hour. The local wavelet power spectra of the CO 2 concentration, CO 2 flux and other meteorological elements identified significant cross wavelet powers near the 24-h and 365-day bands for the CO 2 concentration and flux with temperature, wind speed, friction velocity, and turbulent kinetic energy. X. L. Cheng, X. M. Liu, Y. J. Liu, F. Hu Wiley-Blackwell 0148-0227 01480227 |
shingle_catch_all_2 | Characteristics of CO2 Concentration and Flux in the Beijing Urban Area Since February 2012, CO 2 , H 2 O, and wind data at 10 Hz have been measured by the open-path eddy covariance systems at 8, 16, 47, 80, 140, 200, and 280 m above ground level on the 325-m Beijing meteorological tower. Analysis of the data from 2013 to 2016 indicates that the annual averaged CO 2 concentration increased and the local and regional CO 2 emission decreased with the sequestration of background CO 2 concentration. The maximum values occurred during winter and the minimum values occurred during summer. During spring, summer, and autumn, there was a constant CO 2 flux layer from 47 m to 140 m. However, during winter, CO 2 flux increased with height, and the maximum appeared at approximately 140 m and then decreased with height. Above 47 m, the CO 2 fluxes were represented as the net efflux; and below 16 m, the fluxes were near zero or a net uptake. At all observed heights, the diurnal variation in the CO 2 concentration displayed a clear cycle with a peak corresponding to the morning transportation rush hour. The local wavelet power spectra of the CO 2 concentration, CO 2 flux and other meteorological elements identified significant cross wavelet powers near the 24-h and 365-day bands for the CO 2 concentration and flux with temperature, wind speed, friction velocity, and turbulent kinetic energy. X. L. Cheng, X. M. Liu, Y. J. Liu, F. Hu Wiley-Blackwell 0148-0227 01480227 |
shingle_catch_all_3 | Characteristics of CO2 Concentration and Flux in the Beijing Urban Area Since February 2012, CO 2 , H 2 O, and wind data at 10 Hz have been measured by the open-path eddy covariance systems at 8, 16, 47, 80, 140, 200, and 280 m above ground level on the 325-m Beijing meteorological tower. Analysis of the data from 2013 to 2016 indicates that the annual averaged CO 2 concentration increased and the local and regional CO 2 emission decreased with the sequestration of background CO 2 concentration. The maximum values occurred during winter and the minimum values occurred during summer. During spring, summer, and autumn, there was a constant CO 2 flux layer from 47 m to 140 m. However, during winter, CO 2 flux increased with height, and the maximum appeared at approximately 140 m and then decreased with height. Above 47 m, the CO 2 fluxes were represented as the net efflux; and below 16 m, the fluxes were near zero or a net uptake. At all observed heights, the diurnal variation in the CO 2 concentration displayed a clear cycle with a peak corresponding to the morning transportation rush hour. The local wavelet power spectra of the CO 2 concentration, CO 2 flux and other meteorological elements identified significant cross wavelet powers near the 24-h and 365-day bands for the CO 2 concentration and flux with temperature, wind speed, friction velocity, and turbulent kinetic energy. X. L. Cheng, X. M. Liu, Y. J. Liu, F. Hu Wiley-Blackwell 0148-0227 01480227 |
shingle_catch_all_4 | Characteristics of CO2 Concentration and Flux in the Beijing Urban Area Since February 2012, CO 2 , H 2 O, and wind data at 10 Hz have been measured by the open-path eddy covariance systems at 8, 16, 47, 80, 140, 200, and 280 m above ground level on the 325-m Beijing meteorological tower. Analysis of the data from 2013 to 2016 indicates that the annual averaged CO 2 concentration increased and the local and regional CO 2 emission decreased with the sequestration of background CO 2 concentration. The maximum values occurred during winter and the minimum values occurred during summer. During spring, summer, and autumn, there was a constant CO 2 flux layer from 47 m to 140 m. However, during winter, CO 2 flux increased with height, and the maximum appeared at approximately 140 m and then decreased with height. Above 47 m, the CO 2 fluxes were represented as the net efflux; and below 16 m, the fluxes were near zero or a net uptake. At all observed heights, the diurnal variation in the CO 2 concentration displayed a clear cycle with a peak corresponding to the morning transportation rush hour. The local wavelet power spectra of the CO 2 concentration, CO 2 flux and other meteorological elements identified significant cross wavelet powers near the 24-h and 365-day bands for the CO 2 concentration and flux with temperature, wind speed, friction velocity, and turbulent kinetic energy. X. L. Cheng, X. M. Liu, Y. J. Liu, F. Hu Wiley-Blackwell 0148-0227 01480227 |
shingle_title_1 | Characteristics of CO2 Concentration and Flux in the Beijing Urban Area |
shingle_title_2 | Characteristics of CO2 Concentration and Flux in the Beijing Urban Area |
shingle_title_3 | Characteristics of CO2 Concentration and Flux in the Beijing Urban Area |
shingle_title_4 | Characteristics of CO2 Concentration and Flux in the Beijing Urban Area |
timestamp | 2025-06-30T23:32:17.216Z |
titel | Characteristics of CO2 Concentration and Flux in the Beijing Urban Area |
titel_suche | Characteristics of CO2 Concentration and Flux in the Beijing Urban Area |
topic | TE-TZ U |
uid | ipn_articles_6147600 |