CO2, Hydrographic, and Chemical Data Obtained During R/V Meteor Cruise 18/1 in the North Atlantic Ocean (WOCE Section A1E)
The North Atlantic Ocean is characterized by an intense meridional circulation cell carrying near-surface waters of tropical and subtropical origin northward and deep waters of arctic and subarctic origin southward. The related overturning is driven by the sinking of water masses at high latitudes....
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ESS-DIVE: Deep Insight for Earth Science Data
1996
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dataone:ess-dive-46838b03f0cf910-20180717T162843362 2024-11-03T19:45:07+00:00 CO2, Hydrographic, and Chemical Data Obtained During R/V Meteor Cruise 18/1 in the North Atlantic Ocean (WOCE Section A1E) K. M. Johnson B. Schneider L. Mintrop D. W. R. Wallace North Atlantic Ocean ENVELOPE(-42.509,-4.282,62.666,49.638) BEGINDATE: 1991-09-03T00:00:00Z ENDDATE: 1991-09-22T00:00:00Z 1996-07-01T00:00:00Z https://search.dataone.org/view/ess-dive-46838b03f0cf910-20180717T162843362 unknown ESS-DIVE: Deep Insight for Earth Science Data North Atlantic Oceanhydrographic measurements TALK TCO2 World Ocean Circulation Experiment alkalinity bottle salinity carbon cycle carbon dioxide nitrate nitrite oxygen oxygen measured by (CTD) pCO2 phosphate pressure salinity silicate temperature underway pCO2 North Atlantic Ocean hydrographic measurements nutrient measurements NDP-056 bot cast ctdsal ctdtmp date day depth latdcm londcm month nitrat nitrit pco2 phspht pre qualtexpo revtmp salt samp sect silcat sta stat talk tcarb temp theta time year Dataset 1996 dataone:urn:node:ESS_DIVE 2024-11-03T19:11:00Z The North Atlantic Ocean is characterized by an intense meridional circulation cell carrying near-surface waters of tropical and subtropical origin northward and deep waters of arctic and subarctic origin southward. The related overturning is driven by the sinking of water masses at high latitudes. The overturning rate and thus the intensity of the meridional transports of mass, heat, and salt, is an important control parameter for the modeling of the ocean's role in climate. Certainly such estimates require more than one survey of the study area; therefore, the Research Vessel (R/V) Meteor Cruise 18/1 was one in a series of cruises in the North Atlantic that started in March 1991 and continued until 1995 (Meincke 1993). This data documentation discusses the procedures and methods used to measure total carbon dioxide (TCO2) and total alkalinity (TALK) at hydrographic stations, as well as underway partial pressure of CO2 (pCO2) measured during the R/V Meteor Cruise 18/1 in the North Atlantic Ocean (Section A1E). Conducted as part of the World Ocean Circulation Experiment (WOCE) and the German North Atlantic Overturning Rate Determination expedition, the cruise began in Reykjavik, Iceland, on September 2, 1991, and ended after 24 days at sea in Hamburg, Germany, on September 25, 1991. WOCE Zonal Section A1E began at 60o N and 42o 30' W (southeast of Greenland) and continued southeast with a closely spaced series of hydrocasts to 52 degrees 20' N and 14 degrees 15' W (Porcupine Shelves). Measurements made along WOCE Section A1E included pressure, temperature, salinity, and oxygen measured by a conductivity, temperature and depth (CTD) sensor; bottle salinity; oxygen; phosphate; nitrate; nitrite; silicate; TCO2; TALK; and underway pCO2. A total of 61 CTD casts were made, including 59 bottle casts and 2 calibration stations. Replicate samples from seven Niskin bottles at five stations were also collected for later shore-based reference analyses of TCO2 by vacuum extraction and manometry and TALK in the laboratory of Dr. Charles D. Keeling, Scripps Institution of Oceanography; these results are also included in this report. Dataset Arctic Greenland Iceland North Atlantic Subarctic ESS-DIVE: Deep Insight for Earth Science Data (via DataONE) Arctic Greenland Scripps ENVELOPE(-63.783,-63.783,-69.150,-69.150) ENVELOPE(-42.509,-4.282,62.666,49.638) |
institution |
Open Polar |
collection |
ESS-DIVE: Deep Insight for Earth Science Data (via DataONE) |
op_collection_id |
dataone:urn:node:ESS_DIVE |
language |
unknown |
topic |
North Atlantic Oceanhydrographic measurements TALK TCO2 World Ocean Circulation Experiment alkalinity bottle salinity carbon cycle carbon dioxide nitrate nitrite oxygen oxygen measured by (CTD) pCO2 phosphate pressure salinity silicate temperature underway pCO2 North Atlantic Ocean hydrographic measurements nutrient measurements NDP-056 bot cast ctdsal ctdtmp date day depth latdcm londcm month nitrat nitrit pco2 phspht pre qualtexpo revtmp salt samp sect silcat sta stat talk tcarb temp theta time year |
spellingShingle |
North Atlantic Oceanhydrographic measurements TALK TCO2 World Ocean Circulation Experiment alkalinity bottle salinity carbon cycle carbon dioxide nitrate nitrite oxygen oxygen measured by (CTD) pCO2 phosphate pressure salinity silicate temperature underway pCO2 North Atlantic Ocean hydrographic measurements nutrient measurements NDP-056 bot cast ctdsal ctdtmp date day depth latdcm londcm month nitrat nitrit pco2 phspht pre qualtexpo revtmp salt samp sect silcat sta stat talk tcarb temp theta time year K. M. Johnson B. Schneider L. Mintrop D. W. R. Wallace CO2, Hydrographic, and Chemical Data Obtained During R/V Meteor Cruise 18/1 in the North Atlantic Ocean (WOCE Section A1E) |
topic_facet |
North Atlantic Oceanhydrographic measurements TALK TCO2 World Ocean Circulation Experiment alkalinity bottle salinity carbon cycle carbon dioxide nitrate nitrite oxygen oxygen measured by (CTD) pCO2 phosphate pressure salinity silicate temperature underway pCO2 North Atlantic Ocean hydrographic measurements nutrient measurements NDP-056 bot cast ctdsal ctdtmp date day depth latdcm londcm month nitrat nitrit pco2 phspht pre qualtexpo revtmp salt samp sect silcat sta stat talk tcarb temp theta time year |
description |
The North Atlantic Ocean is characterized by an intense meridional circulation cell carrying near-surface waters of tropical and subtropical origin northward and deep waters of arctic and subarctic origin southward. The related overturning is driven by the sinking of water masses at high latitudes. The overturning rate and thus the intensity of the meridional transports of mass, heat, and salt, is an important control parameter for the modeling of the ocean's role in climate. Certainly such estimates require more than one survey of the study area; therefore, the Research Vessel (R/V) Meteor Cruise 18/1 was one in a series of cruises in the North Atlantic that started in March 1991 and continued until 1995 (Meincke 1993). This data documentation discusses the procedures and methods used to measure total carbon dioxide (TCO2) and total alkalinity (TALK) at hydrographic stations, as well as underway partial pressure of CO2 (pCO2) measured during the R/V Meteor Cruise 18/1 in the North Atlantic Ocean (Section A1E). Conducted as part of the World Ocean Circulation Experiment (WOCE) and the German North Atlantic Overturning Rate Determination expedition, the cruise began in Reykjavik, Iceland, on September 2, 1991, and ended after 24 days at sea in Hamburg, Germany, on September 25, 1991. WOCE Zonal Section A1E began at 60o N and 42o 30' W (southeast of Greenland) and continued southeast with a closely spaced series of hydrocasts to 52 degrees 20' N and 14 degrees 15' W (Porcupine Shelves). Measurements made along WOCE Section A1E included pressure, temperature, salinity, and oxygen measured by a conductivity, temperature and depth (CTD) sensor; bottle salinity; oxygen; phosphate; nitrate; nitrite; silicate; TCO2; TALK; and underway pCO2. A total of 61 CTD casts were made, including 59 bottle casts and 2 calibration stations. Replicate samples from seven Niskin bottles at five stations were also collected for later shore-based reference analyses of TCO2 by vacuum extraction and manometry and TALK in the laboratory of Dr. Charles D. Keeling, Scripps Institution of Oceanography; these results are also included in this report. |
format |
Dataset |
author |
K. M. Johnson B. Schneider L. Mintrop D. W. R. Wallace |
author_facet |
K. M. Johnson B. Schneider L. Mintrop D. W. R. Wallace |
author_sort |
K. M. Johnson |
title |
CO2, Hydrographic, and Chemical Data Obtained During R/V Meteor Cruise 18/1 in the North Atlantic Ocean (WOCE Section A1E) |
title_short |
CO2, Hydrographic, and Chemical Data Obtained During R/V Meteor Cruise 18/1 in the North Atlantic Ocean (WOCE Section A1E) |
title_full |
CO2, Hydrographic, and Chemical Data Obtained During R/V Meteor Cruise 18/1 in the North Atlantic Ocean (WOCE Section A1E) |
title_fullStr |
CO2, Hydrographic, and Chemical Data Obtained During R/V Meteor Cruise 18/1 in the North Atlantic Ocean (WOCE Section A1E) |
title_full_unstemmed |
CO2, Hydrographic, and Chemical Data Obtained During R/V Meteor Cruise 18/1 in the North Atlantic Ocean (WOCE Section A1E) |
title_sort |
co2, hydrographic, and chemical data obtained during r/v meteor cruise 18/1 in the north atlantic ocean (woce section a1e) |
publisher |
ESS-DIVE: Deep Insight for Earth Science Data |
publishDate |
1996 |
url |
https://search.dataone.org/view/ess-dive-46838b03f0cf910-20180717T162843362 |
op_coverage |
North Atlantic Ocean ENVELOPE(-42.509,-4.282,62.666,49.638) BEGINDATE: 1991-09-03T00:00:00Z ENDDATE: 1991-09-22T00:00:00Z |
long_lat |
ENVELOPE(-63.783,-63.783,-69.150,-69.150) ENVELOPE(-42.509,-4.282,62.666,49.638) |
geographic |
Arctic Greenland Scripps |
geographic_facet |
Arctic Greenland Scripps |
genre |
Arctic Greenland Iceland North Atlantic Subarctic |
genre_facet |
Arctic Greenland Iceland North Atlantic Subarctic |
_version_ |
1814734706752618496 |