Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn
Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pr...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Tishchenko, P. Ya. [verfasserIn] Lobanov, V. B. [verfasserIn] Gulenko, T. A. [verfasserIn] Nedashkovskii, A. P. [verfasserIn] Popov, O. S. [verfasserIn] Sagalaev, S. G. [verfasserIn] Tishchenko, P. P. [verfasserIn] Chichkin, R. V. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2012 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Russian meteorology and hydrology - New York, NY : Allerton Press, 2007, 37(2012), 11-12 vom: Nov., Seite 775-782 |
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| Übergeordnetes Werk: |
volume:37 ; year:2012 ; number:11-12 ; month:11 ; pages:775-782 |
| Links: |
|---|
| DOI / URN: |
10.3103/S106837391211012X |
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| Katalog-ID: |
SPR023458011 |
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| 100 | 1 | |a Tishchenko, P. Ya. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn |
| 264 | 1 | |c 2012 | |
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| 520 | |a Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pressure of carbon dioxide (p$ CO_{2} $) was computed which was below its atmospheric value and varied from 290 to 360μatm. Thus, during the period under study, the surface water of the bay forms the runoff for the atmospheric carbon dioxide. The minimum values of p$ CO_{2} $ are associated with the warm stream entering the bay from the southwestern part of the open sea. The maximum values of p$ CO_{2} $ are associated with the local upwelling of bottom waters. It is suggested that the horizontal convection caused by the nonuniform cooling of coastal water in the autumn forms the revealed mesoscale dynamic structures. | ||
| 650 | 4 | |a Partial Pressure |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a RUSSIAN Meteorology |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Electromotive Force |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Atmospheric Carbon Dioxide |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Liquid Junction |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Lobanov, V. B. |e verfasserin |4 aut | |
| 700 | 1 | |a Gulenko, T. A. |e verfasserin |4 aut | |
| 700 | 1 | |a Nedashkovskii, A. P. |e verfasserin |4 aut | |
| 700 | 1 | |a Popov, O. S. |e verfasserin |4 aut | |
| 700 | 1 | |a Sagalaev, S. G. |e verfasserin |4 aut | |
| 700 | 1 | |a Tishchenko, P. P. |e verfasserin |4 aut | |
| 700 | 1 | |a Chichkin, R. V. |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Russian meteorology and hydrology |d New York, NY : Allerton Press, 2007 |g 37(2012), 11-12 vom: Nov., Seite 775-782 |w (DE-627)531203581 |w (DE-600)2324879-8 |x 1934-8096 |7 nnns |
| 773 | 1 | 8 | |g volume:37 |g year:2012 |g number:11-12 |g month:11 |g pages:775-782 |
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10.3103/S106837391211012X doi (DE-627)SPR023458011 (SPR)S106837391211012X-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Tishchenko, P. Ya. verfasserin aut Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pressure of carbon dioxide (p$ CO_{2} $) was computed which was below its atmospheric value and varied from 290 to 360μatm. Thus, during the period under study, the surface water of the bay forms the runoff for the atmospheric carbon dioxide. The minimum values of p$ CO_{2} $ are associated with the warm stream entering the bay from the southwestern part of the open sea. The maximum values of p$ CO_{2} $ are associated with the local upwelling of bottom waters. It is suggested that the horizontal convection caused by the nonuniform cooling of coastal water in the autumn forms the revealed mesoscale dynamic structures. Partial Pressure (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Electromotive Force (dpeaa)DE-He213 Atmospheric Carbon Dioxide (dpeaa)DE-He213 Liquid Junction (dpeaa)DE-He213 Lobanov, V. B. verfasserin aut Gulenko, T. A. verfasserin aut Nedashkovskii, A. P. verfasserin aut Popov, O. S. verfasserin aut Sagalaev, S. G. verfasserin aut Tishchenko, P. P. verfasserin aut Chichkin, R. V. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 37(2012), 11-12 vom: Nov., Seite 775-782 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:37 year:2012 number:11-12 month:11 pages:775-782 https://dx.doi.org/10.3103/S106837391211012X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE 38.85 ASE AR 37 2012 11-12 11 775-782 |
| spelling |
10.3103/S106837391211012X doi (DE-627)SPR023458011 (SPR)S106837391211012X-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Tishchenko, P. Ya. verfasserin aut Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pressure of carbon dioxide (p$ CO_{2} $) was computed which was below its atmospheric value and varied from 290 to 360μatm. Thus, during the period under study, the surface water of the bay forms the runoff for the atmospheric carbon dioxide. The minimum values of p$ CO_{2} $ are associated with the warm stream entering the bay from the southwestern part of the open sea. The maximum values of p$ CO_{2} $ are associated with the local upwelling of bottom waters. It is suggested that the horizontal convection caused by the nonuniform cooling of coastal water in the autumn forms the revealed mesoscale dynamic structures. Partial Pressure (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Electromotive Force (dpeaa)DE-He213 Atmospheric Carbon Dioxide (dpeaa)DE-He213 Liquid Junction (dpeaa)DE-He213 Lobanov, V. B. verfasserin aut Gulenko, T. A. verfasserin aut Nedashkovskii, A. P. verfasserin aut Popov, O. S. verfasserin aut Sagalaev, S. G. verfasserin aut Tishchenko, P. P. verfasserin aut Chichkin, R. V. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 37(2012), 11-12 vom: Nov., Seite 775-782 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:37 year:2012 number:11-12 month:11 pages:775-782 https://dx.doi.org/10.3103/S106837391211012X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE 38.85 ASE AR 37 2012 11-12 11 775-782 |
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10.3103/S106837391211012X doi (DE-627)SPR023458011 (SPR)S106837391211012X-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Tishchenko, P. Ya. verfasserin aut Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pressure of carbon dioxide (p$ CO_{2} $) was computed which was below its atmospheric value and varied from 290 to 360μatm. Thus, during the period under study, the surface water of the bay forms the runoff for the atmospheric carbon dioxide. The minimum values of p$ CO_{2} $ are associated with the warm stream entering the bay from the southwestern part of the open sea. The maximum values of p$ CO_{2} $ are associated with the local upwelling of bottom waters. It is suggested that the horizontal convection caused by the nonuniform cooling of coastal water in the autumn forms the revealed mesoscale dynamic structures. Partial Pressure (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Electromotive Force (dpeaa)DE-He213 Atmospheric Carbon Dioxide (dpeaa)DE-He213 Liquid Junction (dpeaa)DE-He213 Lobanov, V. B. verfasserin aut Gulenko, T. A. verfasserin aut Nedashkovskii, A. P. verfasserin aut Popov, O. S. verfasserin aut Sagalaev, S. G. verfasserin aut Tishchenko, P. P. verfasserin aut Chichkin, R. V. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 37(2012), 11-12 vom: Nov., Seite 775-782 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:37 year:2012 number:11-12 month:11 pages:775-782 https://dx.doi.org/10.3103/S106837391211012X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE 38.85 ASE AR 37 2012 11-12 11 775-782 |
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10.3103/S106837391211012X doi (DE-627)SPR023458011 (SPR)S106837391211012X-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Tishchenko, P. Ya. verfasserin aut Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pressure of carbon dioxide (p$ CO_{2} $) was computed which was below its atmospheric value and varied from 290 to 360μatm. Thus, during the period under study, the surface water of the bay forms the runoff for the atmospheric carbon dioxide. The minimum values of p$ CO_{2} $ are associated with the warm stream entering the bay from the southwestern part of the open sea. The maximum values of p$ CO_{2} $ are associated with the local upwelling of bottom waters. It is suggested that the horizontal convection caused by the nonuniform cooling of coastal water in the autumn forms the revealed mesoscale dynamic structures. Partial Pressure (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Electromotive Force (dpeaa)DE-He213 Atmospheric Carbon Dioxide (dpeaa)DE-He213 Liquid Junction (dpeaa)DE-He213 Lobanov, V. B. verfasserin aut Gulenko, T. A. verfasserin aut Nedashkovskii, A. P. verfasserin aut Popov, O. S. verfasserin aut Sagalaev, S. G. verfasserin aut Tishchenko, P. P. verfasserin aut Chichkin, R. V. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 37(2012), 11-12 vom: Nov., Seite 775-782 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:37 year:2012 number:11-12 month:11 pages:775-782 https://dx.doi.org/10.3103/S106837391211012X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE 38.85 ASE AR 37 2012 11-12 11 775-782 |
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10.3103/S106837391211012X doi (DE-627)SPR023458011 (SPR)S106837391211012X-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Tishchenko, P. Ya. verfasserin aut Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pressure of carbon dioxide (p$ CO_{2} $) was computed which was below its atmospheric value and varied from 290 to 360μatm. Thus, during the period under study, the surface water of the bay forms the runoff for the atmospheric carbon dioxide. The minimum values of p$ CO_{2} $ are associated with the warm stream entering the bay from the southwestern part of the open sea. The maximum values of p$ CO_{2} $ are associated with the local upwelling of bottom waters. It is suggested that the horizontal convection caused by the nonuniform cooling of coastal water in the autumn forms the revealed mesoscale dynamic structures. Partial Pressure (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Electromotive Force (dpeaa)DE-He213 Atmospheric Carbon Dioxide (dpeaa)DE-He213 Liquid Junction (dpeaa)DE-He213 Lobanov, V. B. verfasserin aut Gulenko, T. A. verfasserin aut Nedashkovskii, A. P. verfasserin aut Popov, O. S. verfasserin aut Sagalaev, S. G. verfasserin aut Tishchenko, P. P. verfasserin aut Chichkin, R. V. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 37(2012), 11-12 vom: Nov., Seite 775-782 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:37 year:2012 number:11-12 month:11 pages:775-782 https://dx.doi.org/10.3103/S106837391211012X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE 38.85 ASE AR 37 2012 11-12 11 775-782 |
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Enthalten in Russian meteorology and hydrology 37(2012), 11-12 vom: Nov., Seite 775-782 volume:37 year:2012 number:11-12 month:11 pages:775-782 |
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Enthalten in Russian meteorology and hydrology 37(2012), 11-12 vom: Nov., Seite 775-782 volume:37 year:2012 number:11-12 month:11 pages:775-782 |
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Partial Pressure RUSSIAN Meteorology Electromotive Force Atmospheric Carbon Dioxide Liquid Junction |
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Russian meteorology and hydrology |
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Tishchenko, P. Ya. @@aut@@ Lobanov, V. B. @@aut@@ Gulenko, T. A. @@aut@@ Nedashkovskii, A. P. @@aut@@ Popov, O. S. @@aut@@ Sagalaev, S. G. @@aut@@ Tishchenko, P. P. @@aut@@ Chichkin, R. V. @@aut@@ |
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Ya.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2012</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pressure of carbon dioxide (p$ CO_{2} $) was computed which was below its atmospheric value and varied from 290 to 360μatm. Thus, during the period under study, the surface water of the bay forms the runoff for the atmospheric carbon dioxide. The minimum values of p$ CO_{2} $ are associated with the warm stream entering the bay from the southwestern part of the open sea. The maximum values of p$ CO_{2} $ are associated with the local upwelling of bottom waters. It is suggested that the horizontal convection caused by the nonuniform cooling of coastal water in the autumn forms the revealed mesoscale dynamic structures.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Partial Pressure</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">RUSSIAN Meteorology</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Electromotive Force</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Atmospheric Carbon Dioxide</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Liquid Junction</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Lobanov, V. 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Tishchenko, P. Ya. |
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Tishchenko, P. Ya. ddc 550 bkl 38.80 bkl 38.85 misc Partial Pressure misc RUSSIAN Meteorology misc Electromotive Force misc Atmospheric Carbon Dioxide misc Liquid Junction Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn |
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550 ASE 38.80 bkl 38.85 bkl Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn Partial Pressure (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Electromotive Force (dpeaa)DE-He213 Atmospheric Carbon Dioxide (dpeaa)DE-He213 Liquid Junction (dpeaa)DE-He213 |
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ddc 550 bkl 38.80 bkl 38.85 misc Partial Pressure misc RUSSIAN Meteorology misc Electromotive Force misc Atmospheric Carbon Dioxide misc Liquid Junction |
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Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn |
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Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn |
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Tishchenko, P. Ya. Lobanov, V. B. Gulenko, T. A. Nedashkovskii, A. P. Popov, O. S. Sagalaev, S. G. Tishchenko, P. P. Chichkin, R. V. |
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partial pressure of carbon dioxide in the peter the great bay surface water in the autumn |
| title_auth |
Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn |
| abstract |
Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pressure of carbon dioxide (p$ CO_{2} $) was computed which was below its atmospheric value and varied from 290 to 360μatm. Thus, during the period under study, the surface water of the bay forms the runoff for the atmospheric carbon dioxide. The minimum values of p$ CO_{2} $ are associated with the warm stream entering the bay from the southwestern part of the open sea. The maximum values of p$ CO_{2} $ are associated with the local upwelling of bottom waters. It is suggested that the horizontal convection caused by the nonuniform cooling of coastal water in the autumn forms the revealed mesoscale dynamic structures. |
| abstractGer |
Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pressure of carbon dioxide (p$ CO_{2} $) was computed which was below its atmospheric value and varied from 290 to 360μatm. Thus, during the period under study, the surface water of the bay forms the runoff for the atmospheric carbon dioxide. The minimum values of p$ CO_{2} $ are associated with the warm stream entering the bay from the southwestern part of the open sea. The maximum values of p$ CO_{2} $ are associated with the local upwelling of bottom waters. It is suggested that the horizontal convection caused by the nonuniform cooling of coastal water in the autumn forms the revealed mesoscale dynamic structures. |
| abstract_unstemmed |
Abstract During the hydrological survey from November 4 to 9, 2009, the underway measurements of pH, temperature, and salinity of the surface water in the Peter the Great Bay were carried out using the cell without the liquid junction in the running system. Using the measurement data, the partial pressure of carbon dioxide (p$ CO_{2} $) was computed which was below its atmospheric value and varied from 290 to 360μatm. Thus, during the period under study, the surface water of the bay forms the runoff for the atmospheric carbon dioxide. The minimum values of p$ CO_{2} $ are associated with the warm stream entering the bay from the southwestern part of the open sea. The maximum values of p$ CO_{2} $ are associated with the local upwelling of bottom waters. It is suggested that the horizontal convection caused by the nonuniform cooling of coastal water in the autumn forms the revealed mesoscale dynamic structures. |
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| container_issue |
11-12 |
| title_short |
Partial pressure of carbon dioxide in the peter the great bay surface water in the autumn |
| url |
https://dx.doi.org/10.3103/S106837391211012X |
| remote_bool |
true |
| author2 |
Lobanov, V. B. Gulenko, T. A. Nedashkovskii, A. P. Popov, O. S. Sagalaev, S. G. Tishchenko, P. P. Chichkin, R. V. |
| author2Str |
Lobanov, V. B. Gulenko, T. A. Nedashkovskii, A. P. Popov, O. S. Sagalaev, S. G. Tishchenko, P. P. Chichkin, R. V. |
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| doi_str |
10.3103/S106837391211012X |
| up_date |
2024-07-03T19:03:28.742Z |
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1803585751611342848 |
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| score |
7.40028 |