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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2005
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| Online Access: | https://doi.org/10.1594/PANGAEA.763668 |
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| _version_ | 1867169038191296512 |
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| author | Domanov, Mikhail M Chwedorzewska, K Rakusa-Suszczewski, S |
| author_facet | Domanov, Mikhail M Chwedorzewska, K Rakusa-Suszczewski, S |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Along a transatlantic section from 57°N to 60°S that was carried out from November 7 till December 19, 2000 on board R/V Horizont II concentrations of CO2 were measured in the near-water layer of the air and differences between partial pressures in water and air in various climatic zones were calculated. It was shown that variations of CO2 concentrations in the near-water layer of air and those of values of water-air partial pressure difference were from 324x10**-6 to 426x10**-6 and from 150x10**-6 to 100x10**-6 atm, respectively. Maximum value of CO2 partial pressure in air in the near-water layer (426x10**-6 atm) was noted at 45°-47°N; minimum of 324x10**-6 atm was found in Antarctica at 59°S. During measurenents maximum value of CO2 partial pressure difference in water and air (150 x10**-6) was observed at 45°-48°N; maximum flux in this case was directed from the atmosphere to water. Maximum value of CO2 partial pressure difference in water and air for flux directed from the ocean to air (100 x10**-6) was observed at 59°-60°S. Comparison of calculated values of partial pressure difference in water and air with previous data points to more intense exchange of CO2 between the ocean and atmosphere during the survey period was considered. According to values of CO2 partial pressure difference in air and water as compared to 1975, exchange intensity in the Northern Hemisphere (absorption from the atmosphere) increased. A well-pronounced latitudinal effect of distribution of CO2 partial pressure in air was observed. Along the route variations in CO2 concentrations in zones of water divergence and convergence were registered. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_763668 |
| institution | PANGAEA |
| language | en |
| publishDate | 2005 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Partial pressure of carbon dioxide along the Transatlantic section from 7 November till 19 December 2000 Domanov, Mikhail M Chwedorzewska, K Rakusa-Suszczewski, S Altitude; Archive of Ocean Data; ARCOD; Atlantic Ocean; BARO; Barometer; Carbon dioxide, partial pressure; Date/Time of event; Event label; Horyzont_II-1-1; Horyzont_II-1-10; Horyzont_II-1-11; Horyzont_II-1-12; Horyzont_II-1-13; Horyzont_II-1-14; Horyzont_II-1-15; Horyzont_II-1-16; Horyzont_II-1-17; Horyzont_II-1-18; Horyzont_II-1-19; Horyzont_II-1-2; Horyzont_II-1-20; Horyzont_II-1-21; Horyzont_II-1-22; Horyzont_II-1-23; Horyzont_II-1-24; Horyzont_II-1-25; Horyzont_II-1-26; Horyzont_II-1-27; Horyzont_II-1-28; Horyzont_II-1-29; Horyzont_II-1-3; Horyzont_II-1-30; Horyzont_II-1-31; Horyzont_II-1-32; Horyzont_II-1-33; Horyzont_II-1-34; Horyzont_II-1-35; Horyzont_II-1-36; Horyzont_II-1-37; Horyzont_II-1-38; Horyzont_II-1-39; Horyzont_II-1-4; Horyzont_II-1-40; Horyzont_II-1-41; Horyzont_II-1-42; Horyzont_II-1-43; Horyzont_II-1-44; Horyzont_II-1-45; Horyzont_II-1-46; Horyzont_II-1-47; Horyzont_II-1-48; Horyzont_II-1-49; Horyzont_II-1-5; Horyzont_II-1-50; Horyzont_II-1-51; Horyzont_II-1-52; Horyzont_II-1-53; Horyzont_II-1-54; Horyzont_II-1-55; Horyzont_II-1-56; Horyzont_II-1-57; Horyzont_II-1-58; Horyzont_II-1-59; Horyzont_II-1-6; Horyzont_II-1-60; Horyzont_II-1-61; Horyzont_II-1-62; Horyzont_II-1-63; Horyzont_II-1-64; Horyzont_II-1-65; Horyzont_II-1-66; Horyzont_II-1-67; Horyzont_II-1-68; Horyzont_II-1-69; Horyzont_II-1-7; Horyzont_II-1-70; Horyzont_II-1-71; Horyzont_II-1-72; Horyzont_II-1-73; Horyzont_II-1-74; Horyzont_II-1-75; Horyzont_II-1-76; Horyzont_II-1-77; Horyzont_II-1-78; Horyzont_II-1-79; Horyzont_II-1-8; Horyzont_II-1-80; Horyzont_II-1-81; Horyzont_II-1-82; Horyzont_II-1-83; Horyzont_II-1-84; Horyzont_II-1-9; Infrared gas analyzer (LI-COR LI-6252); Latitude of event; Longitude of event; MULT; Multiple investigations; Pressure, atmospheric; Temperature, air; Temperature, water; Thermometer Along a transatlantic section from 57°N to 60°S that was carried out from November 7 till December 19, 2000 on board R/V Horizont II concentrations of CO2 were measured in the near-water layer of the air and differences between partial pressures in water and air in various climatic zones were calculated. It was shown that variations of CO2 concentrations in the near-water layer of air and those of values of water-air partial pressure difference were from 324x10**-6 to 426x10**-6 and from 150x10**-6 to 100x10**-6 atm, respectively. Maximum value of CO2 partial pressure in air in the near-water layer (426x10**-6 atm) was noted at 45°-47°N; minimum of 324x10**-6 atm was found in Antarctica at 59°S. During measurenents maximum value of CO2 partial pressure difference in water and air (150 x10**-6) was observed at 45°-48°N; maximum flux in this case was directed from the atmosphere to water. Maximum value of CO2 partial pressure difference in water and air for flux directed from the ocean to air (100 x10**-6) was observed at 59°-60°S. Comparison of calculated values of partial pressure difference in water and air with previous data points to more intense exchange of CO2 between the ocean and atmosphere during the survey period was considered. According to values of CO2 partial pressure difference in air and water as compared to 1975, exchange intensity in the Northern Hemisphere (absorption from the atmosphere) increased. A well-pronounced latitudinal effect of distribution of CO2 partial pressure in air was observed. Along the route variations in CO2 concentrations in zones of water divergence and convergence were registered. |
| title | Partial pressure of carbon dioxide along the Transatlantic section from 7 November till 19 December 2000 |
| topic | Altitude; Archive of Ocean Data; ARCOD; Atlantic Ocean; BARO; Barometer; Carbon dioxide, partial pressure; Date/Time of event; Event label; Horyzont_II-1-1; Horyzont_II-1-10; Horyzont_II-1-11; Horyzont_II-1-12; Horyzont_II-1-13; Horyzont_II-1-14; Horyzont_II-1-15; Horyzont_II-1-16; Horyzont_II-1-17; Horyzont_II-1-18; Horyzont_II-1-19; Horyzont_II-1-2; Horyzont_II-1-20; Horyzont_II-1-21; Horyzont_II-1-22; Horyzont_II-1-23; Horyzont_II-1-24; Horyzont_II-1-25; Horyzont_II-1-26; Horyzont_II-1-27; Horyzont_II-1-28; Horyzont_II-1-29; Horyzont_II-1-3; Horyzont_II-1-30; Horyzont_II-1-31; Horyzont_II-1-32; Horyzont_II-1-33; Horyzont_II-1-34; Horyzont_II-1-35; Horyzont_II-1-36; Horyzont_II-1-37; Horyzont_II-1-38; Horyzont_II-1-39; Horyzont_II-1-4; Horyzont_II-1-40; Horyzont_II-1-41; Horyzont_II-1-42; Horyzont_II-1-43; Horyzont_II-1-44; Horyzont_II-1-45; Horyzont_II-1-46; Horyzont_II-1-47; Horyzont_II-1-48; Horyzont_II-1-49; Horyzont_II-1-5; Horyzont_II-1-50; Horyzont_II-1-51; Horyzont_II-1-52; Horyzont_II-1-53; Horyzont_II-1-54; Horyzont_II-1-55; Horyzont_II-1-56; Horyzont_II-1-57; Horyzont_II-1-58; Horyzont_II-1-59; Horyzont_II-1-6; Horyzont_II-1-60; Horyzont_II-1-61; Horyzont_II-1-62; Horyzont_II-1-63; Horyzont_II-1-64; Horyzont_II-1-65; Horyzont_II-1-66; Horyzont_II-1-67; Horyzont_II-1-68; Horyzont_II-1-69; Horyzont_II-1-7; Horyzont_II-1-70; Horyzont_II-1-71; Horyzont_II-1-72; Horyzont_II-1-73; Horyzont_II-1-74; Horyzont_II-1-75; Horyzont_II-1-76; Horyzont_II-1-77; Horyzont_II-1-78; Horyzont_II-1-79; Horyzont_II-1-8; Horyzont_II-1-80; Horyzont_II-1-81; Horyzont_II-1-82; Horyzont_II-1-83; Horyzont_II-1-84; Horyzont_II-1-9; Infrared gas analyzer (LI-COR LI-6252); Latitude of event; Longitude of event; MULT; Multiple investigations; Pressure, atmospheric; Temperature, air; Temperature, water; Thermometer |
| url | https://doi.org/10.1594/PANGAEA.763668 |