Fluxes of gases and particles above a deciduous forest in wintertime
Abstract Eddy-correlation measurements of the vertical fluxes of ozone, carbon dioxide, fine particles with diameter near 0.1 Μm, and particulate sulfur, as well as of momentum, heat and water vapor, have been taken above a tall leafless deciduous forest in wintertime. During the experimental period...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wesely, M. L. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1983 |
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| Schlagwörter: |
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| Anmerkung: |
© D. Reidel Publishing Company 1983 |
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| Übergeordnetes Werk: |
Enthalten in: Boundary layer meteorology - Kluwer Academic Publishers, 1970, 27(1983), 3 vom: Nov., Seite 237-255 |
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| Übergeordnetes Werk: |
volume:27 ; year:1983 ; number:3 ; month:11 ; pages:237-255 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF00125000 |
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| Katalog-ID: |
OLC2060927447 |
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| 245 | 1 | 0 | |a Fluxes of gases and particles above a deciduous forest in wintertime |
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| 520 | |a Abstract Eddy-correlation measurements of the vertical fluxes of ozone, carbon dioxide, fine particles with diameter near 0.1 Μm, and particulate sulfur, as well as of momentum, heat and water vapor, have been taken above a tall leafless deciduous forest in wintertime. During the experimental period of one week, ozone deposition velocities varied from about 0.1 cm $ s^{−1} $ at night to more than 0.4 cm $ s^{-1} $ during the daytime, with the largest variations associated primarily with changes in solar irradiation. Most of the ozone removal took place in the upper canopy. Carbon dioxide fluxes were directed upward due to respiration and exhibited a strong dependence on air temperature and solar heating. The fluxes were approximately zero at air temperatures less than 5 °C and approached 0.8 mg $ m^{−2} $ $ s^{−1} $ when temperatures exceeded 15 °C during the daytime. Fine-particle deposition rates were large at times, with deposition velocities near 0.8 cm $ s^{−1} $ when turbulence levels were high, but fluxes directed upward were found above the canopy when the surface beneath was covered with snow. Diffusional processes seemed to dominate fine-particle transfer across quasilaminar layers and subsequent deposition to the upper canopy. Deposition velocities for particulate sulfur were highly variable and averaged to a value small in magnitude as compared to similar measurements taken previously over a pine forest in summer. | ||
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| 650 | 4 | |a Ozone | |
| 650 | 4 | |a Respiration | |
| 650 | 4 | |a Water Vapor | |
| 650 | 4 | |a Solar Irradiation | |
| 700 | 1 | |a Cook, D. R. |4 aut | |
| 700 | 1 | |a Hart, R. L. |4 aut | |
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10.1007/BF00125000 doi (DE-627)OLC2060927447 (DE-He213)BF00125000-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Wesely, M. L. verfasserin aut Fluxes of gases and particles above a deciduous forest in wintertime 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1983 Abstract Eddy-correlation measurements of the vertical fluxes of ozone, carbon dioxide, fine particles with diameter near 0.1 Μm, and particulate sulfur, as well as of momentum, heat and water vapor, have been taken above a tall leafless deciduous forest in wintertime. During the experimental period of one week, ozone deposition velocities varied from about 0.1 cm $ s^{−1} $ at night to more than 0.4 cm $ s^{-1} $ during the daytime, with the largest variations associated primarily with changes in solar irradiation. Most of the ozone removal took place in the upper canopy. Carbon dioxide fluxes were directed upward due to respiration and exhibited a strong dependence on air temperature and solar heating. The fluxes were approximately zero at air temperatures less than 5 °C and approached 0.8 mg $ m^{−2} $ $ s^{−1} $ when temperatures exceeded 15 °C during the daytime. Fine-particle deposition rates were large at times, with deposition velocities near 0.8 cm $ s^{−1} $ when turbulence levels were high, but fluxes directed upward were found above the canopy when the surface beneath was covered with snow. Diffusional processes seemed to dominate fine-particle transfer across quasilaminar layers and subsequent deposition to the upper canopy. Deposition velocities for particulate sulfur were highly variable and averaged to a value small in magnitude as compared to similar measurements taken previously over a pine forest in summer. Carbon Dioxide Ozone Respiration Water Vapor Solar Irradiation Cook, D. R. aut Hart, R. L. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 27(1983), 3 vom: Nov., Seite 237-255 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:27 year:1983 number:3 month:11 pages:237-255 https://doi.org/10.1007/BF00125000 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 GBV_ILN_4700 AR 27 1983 3 11 237-255 |
| spelling |
10.1007/BF00125000 doi (DE-627)OLC2060927447 (DE-He213)BF00125000-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Wesely, M. L. verfasserin aut Fluxes of gases and particles above a deciduous forest in wintertime 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1983 Abstract Eddy-correlation measurements of the vertical fluxes of ozone, carbon dioxide, fine particles with diameter near 0.1 Μm, and particulate sulfur, as well as of momentum, heat and water vapor, have been taken above a tall leafless deciduous forest in wintertime. During the experimental period of one week, ozone deposition velocities varied from about 0.1 cm $ s^{−1} $ at night to more than 0.4 cm $ s^{-1} $ during the daytime, with the largest variations associated primarily with changes in solar irradiation. Most of the ozone removal took place in the upper canopy. Carbon dioxide fluxes were directed upward due to respiration and exhibited a strong dependence on air temperature and solar heating. The fluxes were approximately zero at air temperatures less than 5 °C and approached 0.8 mg $ m^{−2} $ $ s^{−1} $ when temperatures exceeded 15 °C during the daytime. Fine-particle deposition rates were large at times, with deposition velocities near 0.8 cm $ s^{−1} $ when turbulence levels were high, but fluxes directed upward were found above the canopy when the surface beneath was covered with snow. Diffusional processes seemed to dominate fine-particle transfer across quasilaminar layers and subsequent deposition to the upper canopy. Deposition velocities for particulate sulfur were highly variable and averaged to a value small in magnitude as compared to similar measurements taken previously over a pine forest in summer. Carbon Dioxide Ozone Respiration Water Vapor Solar Irradiation Cook, D. R. aut Hart, R. L. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 27(1983), 3 vom: Nov., Seite 237-255 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:27 year:1983 number:3 month:11 pages:237-255 https://doi.org/10.1007/BF00125000 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 GBV_ILN_4700 AR 27 1983 3 11 237-255 |
| allfields_unstemmed |
10.1007/BF00125000 doi (DE-627)OLC2060927447 (DE-He213)BF00125000-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Wesely, M. L. verfasserin aut Fluxes of gases and particles above a deciduous forest in wintertime 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1983 Abstract Eddy-correlation measurements of the vertical fluxes of ozone, carbon dioxide, fine particles with diameter near 0.1 Μm, and particulate sulfur, as well as of momentum, heat and water vapor, have been taken above a tall leafless deciduous forest in wintertime. During the experimental period of one week, ozone deposition velocities varied from about 0.1 cm $ s^{−1} $ at night to more than 0.4 cm $ s^{-1} $ during the daytime, with the largest variations associated primarily with changes in solar irradiation. Most of the ozone removal took place in the upper canopy. Carbon dioxide fluxes were directed upward due to respiration and exhibited a strong dependence on air temperature and solar heating. The fluxes were approximately zero at air temperatures less than 5 °C and approached 0.8 mg $ m^{−2} $ $ s^{−1} $ when temperatures exceeded 15 °C during the daytime. Fine-particle deposition rates were large at times, with deposition velocities near 0.8 cm $ s^{−1} $ when turbulence levels were high, but fluxes directed upward were found above the canopy when the surface beneath was covered with snow. Diffusional processes seemed to dominate fine-particle transfer across quasilaminar layers and subsequent deposition to the upper canopy. Deposition velocities for particulate sulfur were highly variable and averaged to a value small in magnitude as compared to similar measurements taken previously over a pine forest in summer. Carbon Dioxide Ozone Respiration Water Vapor Solar Irradiation Cook, D. R. aut Hart, R. L. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 27(1983), 3 vom: Nov., Seite 237-255 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:27 year:1983 number:3 month:11 pages:237-255 https://doi.org/10.1007/BF00125000 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 GBV_ILN_4700 AR 27 1983 3 11 237-255 |
| allfieldsGer |
10.1007/BF00125000 doi (DE-627)OLC2060927447 (DE-He213)BF00125000-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Wesely, M. L. verfasserin aut Fluxes of gases and particles above a deciduous forest in wintertime 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1983 Abstract Eddy-correlation measurements of the vertical fluxes of ozone, carbon dioxide, fine particles with diameter near 0.1 Μm, and particulate sulfur, as well as of momentum, heat and water vapor, have been taken above a tall leafless deciduous forest in wintertime. During the experimental period of one week, ozone deposition velocities varied from about 0.1 cm $ s^{−1} $ at night to more than 0.4 cm $ s^{-1} $ during the daytime, with the largest variations associated primarily with changes in solar irradiation. Most of the ozone removal took place in the upper canopy. Carbon dioxide fluxes were directed upward due to respiration and exhibited a strong dependence on air temperature and solar heating. The fluxes were approximately zero at air temperatures less than 5 °C and approached 0.8 mg $ m^{−2} $ $ s^{−1} $ when temperatures exceeded 15 °C during the daytime. Fine-particle deposition rates were large at times, with deposition velocities near 0.8 cm $ s^{−1} $ when turbulence levels were high, but fluxes directed upward were found above the canopy when the surface beneath was covered with snow. Diffusional processes seemed to dominate fine-particle transfer across quasilaminar layers and subsequent deposition to the upper canopy. Deposition velocities for particulate sulfur were highly variable and averaged to a value small in magnitude as compared to similar measurements taken previously over a pine forest in summer. Carbon Dioxide Ozone Respiration Water Vapor Solar Irradiation Cook, D. R. aut Hart, R. L. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 27(1983), 3 vom: Nov., Seite 237-255 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:27 year:1983 number:3 month:11 pages:237-255 https://doi.org/10.1007/BF00125000 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 GBV_ILN_4700 AR 27 1983 3 11 237-255 |
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10.1007/BF00125000 doi (DE-627)OLC2060927447 (DE-He213)BF00125000-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Wesely, M. L. verfasserin aut Fluxes of gases and particles above a deciduous forest in wintertime 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1983 Abstract Eddy-correlation measurements of the vertical fluxes of ozone, carbon dioxide, fine particles with diameter near 0.1 Μm, and particulate sulfur, as well as of momentum, heat and water vapor, have been taken above a tall leafless deciduous forest in wintertime. During the experimental period of one week, ozone deposition velocities varied from about 0.1 cm $ s^{−1} $ at night to more than 0.4 cm $ s^{-1} $ during the daytime, with the largest variations associated primarily with changes in solar irradiation. Most of the ozone removal took place in the upper canopy. Carbon dioxide fluxes were directed upward due to respiration and exhibited a strong dependence on air temperature and solar heating. The fluxes were approximately zero at air temperatures less than 5 °C and approached 0.8 mg $ m^{−2} $ $ s^{−1} $ when temperatures exceeded 15 °C during the daytime. Fine-particle deposition rates were large at times, with deposition velocities near 0.8 cm $ s^{−1} $ when turbulence levels were high, but fluxes directed upward were found above the canopy when the surface beneath was covered with snow. Diffusional processes seemed to dominate fine-particle transfer across quasilaminar layers and subsequent deposition to the upper canopy. Deposition velocities for particulate sulfur were highly variable and averaged to a value small in magnitude as compared to similar measurements taken previously over a pine forest in summer. Carbon Dioxide Ozone Respiration Water Vapor Solar Irradiation Cook, D. R. aut Hart, R. L. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 27(1983), 3 vom: Nov., Seite 237-255 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:27 year:1983 number:3 month:11 pages:237-255 https://doi.org/10.1007/BF00125000 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 GBV_ILN_4700 AR 27 1983 3 11 237-255 |
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Enthalten in Boundary layer meteorology 27(1983), 3 vom: Nov., Seite 237-255 volume:27 year:1983 number:3 month:11 pages:237-255 |
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Enthalten in Boundary layer meteorology 27(1983), 3 vom: Nov., Seite 237-255 volume:27 year:1983 number:3 month:11 pages:237-255 |
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Wesely, M. L. @@aut@@ Cook, D. R. @@aut@@ Hart, R. L. @@aut@@ |
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550 VZ 16,13 ssgn Fluxes of gases and particles above a deciduous forest in wintertime Carbon Dioxide Ozone Respiration Water Vapor Solar Irradiation |
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Fluxes of gases and particles above a deciduous forest in wintertime |
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fluxes of gases and particles above a deciduous forest in wintertime |
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Fluxes of gases and particles above a deciduous forest in wintertime |
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Abstract Eddy-correlation measurements of the vertical fluxes of ozone, carbon dioxide, fine particles with diameter near 0.1 Μm, and particulate sulfur, as well as of momentum, heat and water vapor, have been taken above a tall leafless deciduous forest in wintertime. During the experimental period of one week, ozone deposition velocities varied from about 0.1 cm $ s^{−1} $ at night to more than 0.4 cm $ s^{-1} $ during the daytime, with the largest variations associated primarily with changes in solar irradiation. Most of the ozone removal took place in the upper canopy. Carbon dioxide fluxes were directed upward due to respiration and exhibited a strong dependence on air temperature and solar heating. The fluxes were approximately zero at air temperatures less than 5 °C and approached 0.8 mg $ m^{−2} $ $ s^{−1} $ when temperatures exceeded 15 °C during the daytime. Fine-particle deposition rates were large at times, with deposition velocities near 0.8 cm $ s^{−1} $ when turbulence levels were high, but fluxes directed upward were found above the canopy when the surface beneath was covered with snow. Diffusional processes seemed to dominate fine-particle transfer across quasilaminar layers and subsequent deposition to the upper canopy. Deposition velocities for particulate sulfur were highly variable and averaged to a value small in magnitude as compared to similar measurements taken previously over a pine forest in summer. © D. Reidel Publishing Company 1983 |
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Abstract Eddy-correlation measurements of the vertical fluxes of ozone, carbon dioxide, fine particles with diameter near 0.1 Μm, and particulate sulfur, as well as of momentum, heat and water vapor, have been taken above a tall leafless deciduous forest in wintertime. During the experimental period of one week, ozone deposition velocities varied from about 0.1 cm $ s^{−1} $ at night to more than 0.4 cm $ s^{-1} $ during the daytime, with the largest variations associated primarily with changes in solar irradiation. Most of the ozone removal took place in the upper canopy. Carbon dioxide fluxes were directed upward due to respiration and exhibited a strong dependence on air temperature and solar heating. The fluxes were approximately zero at air temperatures less than 5 °C and approached 0.8 mg $ m^{−2} $ $ s^{−1} $ when temperatures exceeded 15 °C during the daytime. Fine-particle deposition rates were large at times, with deposition velocities near 0.8 cm $ s^{−1} $ when turbulence levels were high, but fluxes directed upward were found above the canopy when the surface beneath was covered with snow. Diffusional processes seemed to dominate fine-particle transfer across quasilaminar layers and subsequent deposition to the upper canopy. Deposition velocities for particulate sulfur were highly variable and averaged to a value small in magnitude as compared to similar measurements taken previously over a pine forest in summer. © D. Reidel Publishing Company 1983 |
| abstract_unstemmed |
Abstract Eddy-correlation measurements of the vertical fluxes of ozone, carbon dioxide, fine particles with diameter near 0.1 Μm, and particulate sulfur, as well as of momentum, heat and water vapor, have been taken above a tall leafless deciduous forest in wintertime. During the experimental period of one week, ozone deposition velocities varied from about 0.1 cm $ s^{−1} $ at night to more than 0.4 cm $ s^{-1} $ during the daytime, with the largest variations associated primarily with changes in solar irradiation. Most of the ozone removal took place in the upper canopy. Carbon dioxide fluxes were directed upward due to respiration and exhibited a strong dependence on air temperature and solar heating. The fluxes were approximately zero at air temperatures less than 5 °C and approached 0.8 mg $ m^{−2} $ $ s^{−1} $ when temperatures exceeded 15 °C during the daytime. Fine-particle deposition rates were large at times, with deposition velocities near 0.8 cm $ s^{−1} $ when turbulence levels were high, but fluxes directed upward were found above the canopy when the surface beneath was covered with snow. Diffusional processes seemed to dominate fine-particle transfer across quasilaminar layers and subsequent deposition to the upper canopy. Deposition velocities for particulate sulfur were highly variable and averaged to a value small in magnitude as compared to similar measurements taken previously over a pine forest in summer. © D. Reidel Publishing Company 1983 |
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