GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Arctic Ocean; Calculated after Dansgaard (1964); Comment; DATE/TIME; DEPTH, water; Deuterium excess; Event label; isotopes; Mass spectrometer Finnigan MAT Delta-S (ISOLAB); MOSAiC; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; North Greenland Sea; Polarstern; PS122/1; PS122/1_10-111; PS122/1_10-2; PS122/1_10-25; PS122/1_10-32; PS122/1_10-52; PS122/1_10-77; PS122/1_10-93; PS122/1_11-15; PS122/1_11-28; PS122/1_11-4; PS122/1_11-42; PS122/1_7-111; PS122/1_7-95; PS122/1_8-100; PS122/1_8-119; PS122/1_8-15; PS122/1_8-26; PS122/1_8-4; PS122/1_8-84; PS122/1_9-103; PS122/1_9-15; PS122/1_9-29; PS122/1_9-45; PS122/1_9-56; PS122/1_9-92; PS122/2; PS122/2_15-6; PS122/2_15-8; PS122/2_16-14; PS122/2_16-29; PS122/2_16-37; PS122/2_16-53; PS122/2_16-61; PS122/2_16-8; PS122/2_17-17; PS122/2_17-2; PS122/2_17-25; PS122/2_17-42; PS122/2_17-67; PS122/2_17-75; PS122/2_17-97; PS122/2_18-15; PS122/2_18-2; PS122/2_18-23; PS122/2_18-39; PS122/2_18-58; PS122/2_18-75; PS122/2_18-90; PS122/2_19-114; PS122/2_19-17; PS122/2_19-2; PS122/2_19-33; PS122/2_19-58; PS122/2_19-80; PS122/2_19-90; PS122/2_20-1; PS122/2_20-111; PS122/2_20-13; PS122/2_20-29; PS122/2_20-50; PS122/2_20-75; PS122/2_20-99; PS122/2_21-11; PS122/2_21-112; PS122/2_21-123; PS122/2_21-50; PS122/2_21-69; PS122/2_21-85; PS122/2_22-14; PS122/2_22-2; PS122/2_22-31; PS122/2_22-64; PS122/2_22-84; PS122/2_22-95; PS122/2_23-1; PS122/2_23-11; PS122/2_23-33; PS122/2_23-49; PS122/2_23-66; PS122/2_23-86; PS122/2_24-20; PS122/2_24-30; PS122/2_24-41; PS122/2_24-48; PS122/2_24-5; PS122/2_24-71; PS122/2_24-82; PS122/2_25-101; PS122/2_25-29; PS122/2_25-43; PS122/2_25-5; PS122/2_25-56; PS122/2_25-75; PS122/2_25-88; PS122/3; PS122/3_29-21; PS122/3_29-36; PS122/3_29-51; PS122/3_29-6; PS122/3_29-60; PS122/3_29-7; PS122/3_29-81; PS122/3_30-18; PS122/3_30-23; PS122/3_30-35; PS122/3_30-52; PS122/3_30-6; PS122/3_30-66; PS122/3_30-83; PS122/3_31-13; PS122/3_31-16; PS122/3_31-28; PS122/3_31-46; PS122/3_31-54; PS122/3_31-60; PS122/3_31-78; PS122/3_32-1; PS122/3_32-21; PS122/3_32-37; PS122/3_32-48; PS122/3_32-60; PS122/3_32-72; PS122/3_33-15; PS122/3_33-35; PS122/3_33-50; PS122/3_33-64; PS122/3_33-79; PS122/3_33-8; PS122/3_33-93; PS122/3_34-1; PS122/3_34-12; PS122/3_34-26; PS122/3_34-35; PS122/3_34-47; PS122/3_34-61; PS122/3_34-74; PS122/3_35-103; PS122/3_35-17; PS122/3_35-3; PS122/3_35-35; PS122/3_35-52; PS122/3_35-75; PS122/3_35-89; PS122/3_36-1; PS122/3_36-110; PS122/3_36-13; PS122/3_36-135; PS122/3_36-34; PS122/3_36-55; PS122/3_36-72; PS122/3_37-112; PS122/3_37-12; PS122/3_37-2; PS122/3_37-23; PS122/3_37-42; PS122/3_37-67; PS122/3_37-90; PS122/3_38-113; PS122/3_38-22; PS122/3_38-26; PS122/3_38-37; PS122/3_38-48; PS122/3_38-67; PS122/3_38-88; PS122/3_39-1; PS122/3_39-14; PS122/3_39-29; PS122/3_39-49; PS122/3_39-68; PS122/3_39-76; PS122/3_39-85; PS122/3_40-1; PS122/3_40-13; PS122/3_40-22; PS122/3_40-30; PS122/3_40-35; PS122/3_40-45; PS122/3_40-7; PS122/3_41-13; PS122/3_41-20; PS122/3_41-27; PS122/3_41-38; PS122/3_41-4; PS122/3_41-42; PS122/3_41-48; PS122/3_42-1; PS122/3_42-12; PS122/3_42-21; PS122/3_42-27; PS122/3_42-33; PS122/3_42-43; PS122/3_42-52; PS122/3_42-58; PS122/3_42-6; PS122/3_42-67; PS122/4; PS122/4_44-123; PS122/4_44-131; PS122/4_44-146; PS122/4_44-160; PS122/4_44-175; PS122/4_44-19; PS122/4_44-194; PS122/4_44-28; PS122/4_44-34; PS122/4_44-54; PS122/4_44-64; PS122/4_44-80; PS122/4_44-85; PS122/4_44-96; PS122/4_45-111; PS122/4_45-133; PS122/4_45-14; PS122/4_45-6; PS122/4_45-65; PS122/4_45-90; PS122/4_46-124; PS122/4_46-22; PS122/4_46-5; PS122/4_46-51; PS122/4_46-67; PS122/4_46-96; PS122/4_47-105; PS122/4_47-118; PS122/4_47-24; PS122/4_47-37; PS122/4_47-5; PS122/4_47-70; PS122/4_47-88; PS122/4_48-119; PS122/4_48-149; PS122/4_48-156; PS122/4_48-18; PS122/4_48-48; PS122/4_48-68; PS122/4_49-23; PS122/4_49-24; PS122/4_49-28; PS122/4_49-58; PS122/4_49-67; PS122/4_49-82; PS122/4_49-96; PS122/4_50-12; PS122/4_50-22; PS122/4_50-3; PS122/4_50-34; PS122/4_50-44; PS122/4_50-53; PS122/4_50-59; PS122/4_50-62; PS122/5; PS122/5_59-11; PS122/5_59-133; PS122/5_59-151; PS122/5_59-167; PS122/5_59-179; PS122/5_59-199; PS122/5_59-220; PS122/5_59-247; PS122/5_59-26; PS122/5_59-266; PS122/5_59-287; PS122/5_59-323; PS122/5_59-341; PS122/5_59-36; PS122/5_59-361; PS122/5_59-379; PS122/5_59-4; PS122/5_59-59; PS122/5_59-65; PS122/5_60-11; PS122/5_60-116; PS122/5_60-140; PS122/5_60-169; PS122/5_60-35; PS122/5_60-50; PS122/5_60-73; PS122/5_61-106; PS122/5_61-141; PS122/5_61-184; PS122/5_61-208; PS122/5_61-244; PS122/5_61-3; PS122/5_61-34; PS122/5_62-111; PS122/5_62-133; PS122/5_62-150; PS122/5_62-171; PS122/5_62-63; PS122/5_62-8; PS122/5_62-86; PS122/5_63-115; PS122/5_63-123; PS122/5_63-134; PS122/5_63-144; PS122/5_63-27; PS122/5_63-52; PS122/5_63-6; PS122/5_63-66; PS122/5_63-7; PS122/5_63-78; PS122/5_63-93; Salinity; Sample code/label; Sample ID; Sample type; seawater; see abstract; Station label; Surface water sample; SWS; Tap; TAP; Water sample; WS; δ18O, water; δ Deuterium, water  (1)
  • COVID‐19  (1)
Document type
Keywords
Publisher
Years
  • 1
    Publication Date: 2024-06-12
    Description: Underway seawater samples have been taken from underneath the research vessel Polarstern through a pipe installed on the ship. The valve had been open for about 2 minutes before collecting the samples to avoid possible contaminations. Water samples for measurement of stable water isotopes (δ18O, δD,) were collected in narrow-mouth low-density polyethylene 20- or 30-mL plastic bottles (VWR international LLC, Germany), sealed with Parafilm M and stored at +4 °C from the end of the expedition until the measurement. Average daily salinity values were extracted from dship portal (https://dship.awi.de/). Oxygen and hydrogen isotope analyses were carried out at the ISOLAB Facility at AWI Potsdam (https://hdl.handle.net/10013/sensor.ddc92f54-4c63-492d-81c7-696260694001) with mass spectrometers (DELTA-S Finnigan MAT, USA): https://hdl.handle.net/10013/sensor.af148dea-fe65-4c87-9744-50dc4c81f7c9 https://hdl.handle.net/10013/sensor.62e86761-9fae-4f12-9c10-9b245028ea4c employing the equilibration method (details in Meyer et al., 2000). δ18O and δD values were given in per mil (‰) vs. Vienna standard mean ocean water (V-SMOW) as the standard. The second order parameter d excess was computed according to: d excess = δD-8 δ18O (Dansgaard, 1964).
    Keywords: Arctic Ocean; Calculated after Dansgaard (1964); Comment; DATE/TIME; DEPTH, water; Deuterium excess; Event label; isotopes; Mass spectrometer Finnigan MAT Delta-S (ISOLAB); MOSAiC; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; North Greenland Sea; Polarstern; PS122/1; PS122/1_10-111; PS122/1_10-2; PS122/1_10-25; PS122/1_10-32; PS122/1_10-52; PS122/1_10-77; PS122/1_10-93; PS122/1_11-15; PS122/1_11-28; PS122/1_11-4; PS122/1_11-42; PS122/1_7-111; PS122/1_7-95; PS122/1_8-100; PS122/1_8-119; PS122/1_8-15; PS122/1_8-26; PS122/1_8-4; PS122/1_8-84; PS122/1_9-103; PS122/1_9-15; PS122/1_9-29; PS122/1_9-45; PS122/1_9-56; PS122/1_9-92; PS122/2; PS122/2_15-6; PS122/2_15-8; PS122/2_16-14; PS122/2_16-29; PS122/2_16-37; PS122/2_16-53; PS122/2_16-61; PS122/2_16-8; PS122/2_17-17; PS122/2_17-2; PS122/2_17-25; PS122/2_17-42; PS122/2_17-67; PS122/2_17-75; PS122/2_17-97; PS122/2_18-15; PS122/2_18-2; PS122/2_18-23; PS122/2_18-39; PS122/2_18-58; PS122/2_18-75; PS122/2_18-90; PS122/2_19-114; PS122/2_19-17; PS122/2_19-2; PS122/2_19-33; PS122/2_19-58; PS122/2_19-80; PS122/2_19-90; PS122/2_20-1; PS122/2_20-111; PS122/2_20-13; PS122/2_20-29; PS122/2_20-50; PS122/2_20-75; PS122/2_20-99; PS122/2_21-11; PS122/2_21-112; PS122/2_21-123; PS122/2_21-50; PS122/2_21-69; PS122/2_21-85; PS122/2_22-14; PS122/2_22-2; PS122/2_22-31; PS122/2_22-64; PS122/2_22-84; PS122/2_22-95; PS122/2_23-1; PS122/2_23-11; PS122/2_23-33; PS122/2_23-49; PS122/2_23-66; PS122/2_23-86; PS122/2_24-20; PS122/2_24-30; PS122/2_24-41; PS122/2_24-48; PS122/2_24-5; PS122/2_24-71; PS122/2_24-82; PS122/2_25-101; PS122/2_25-29; PS122/2_25-43; PS122/2_25-5; PS122/2_25-56; PS122/2_25-75; PS122/2_25-88; PS122/3; PS122/3_29-21; PS122/3_29-36; PS122/3_29-51; PS122/3_29-6; PS122/3_29-60; PS122/3_29-7; PS122/3_29-81; PS122/3_30-18; PS122/3_30-23; PS122/3_30-35; PS122/3_30-52; PS122/3_30-6; PS122/3_30-66; PS122/3_30-83; PS122/3_31-13; PS122/3_31-16; PS122/3_31-28; PS122/3_31-46; PS122/3_31-54; PS122/3_31-60; PS122/3_31-78; PS122/3_32-1; PS122/3_32-21; PS122/3_32-37; PS122/3_32-48; PS122/3_32-60; PS122/3_32-72; PS122/3_33-15; PS122/3_33-35; PS122/3_33-50; PS122/3_33-64; PS122/3_33-79; PS122/3_33-8; PS122/3_33-93; PS122/3_34-1; PS122/3_34-12; PS122/3_34-26; PS122/3_34-35; PS122/3_34-47; PS122/3_34-61; PS122/3_34-74; PS122/3_35-103; PS122/3_35-17; PS122/3_35-3; PS122/3_35-35; PS122/3_35-52; PS122/3_35-75; PS122/3_35-89; PS122/3_36-1; PS122/3_36-110; PS122/3_36-13; PS122/3_36-135; PS122/3_36-34; PS122/3_36-55; PS122/3_36-72; PS122/3_37-112; PS122/3_37-12; PS122/3_37-2; PS122/3_37-23; PS122/3_37-42; PS122/3_37-67; PS122/3_37-90; PS122/3_38-113; PS122/3_38-22; PS122/3_38-26; PS122/3_38-37; PS122/3_38-48; PS122/3_38-67; PS122/3_38-88; PS122/3_39-1; PS122/3_39-14; PS122/3_39-29; PS122/3_39-49; PS122/3_39-68; PS122/3_39-76; PS122/3_39-85; PS122/3_40-1; PS122/3_40-13; PS122/3_40-22; PS122/3_40-30; PS122/3_40-35; PS122/3_40-45; PS122/3_40-7; PS122/3_41-13; PS122/3_41-20; PS122/3_41-27; PS122/3_41-38; PS122/3_41-4; PS122/3_41-42; PS122/3_41-48; PS122/3_42-1; PS122/3_42-12; PS122/3_42-21; PS122/3_42-27; PS122/3_42-33; PS122/3_42-43; PS122/3_42-52; PS122/3_42-58; PS122/3_42-6; PS122/3_42-67; PS122/4; PS122/4_44-123; PS122/4_44-131; PS122/4_44-146; PS122/4_44-160; PS122/4_44-175; PS122/4_44-19; PS122/4_44-194; PS122/4_44-28; PS122/4_44-34; PS122/4_44-54; PS122/4_44-64; PS122/4_44-80; PS122/4_44-85; PS122/4_44-96; PS122/4_45-111; PS122/4_45-133; PS122/4_45-14; PS122/4_45-6; PS122/4_45-65; PS122/4_45-90; PS122/4_46-124; PS122/4_46-22; PS122/4_46-5; PS122/4_46-51; PS122/4_46-67; PS122/4_46-96; PS122/4_47-105; PS122/4_47-118; PS122/4_47-24; PS122/4_47-37; PS122/4_47-5; PS122/4_47-70; PS122/4_47-88; PS122/4_48-119; PS122/4_48-149; PS122/4_48-156; PS122/4_48-18; PS122/4_48-48; PS122/4_48-68; PS122/4_49-23; PS122/4_49-24; PS122/4_49-28; PS122/4_49-58; PS122/4_49-67; PS122/4_49-82; PS122/4_49-96; PS122/4_50-12; PS122/4_50-22; PS122/4_50-3; PS122/4_50-34; PS122/4_50-44; PS122/4_50-53; PS122/4_50-59; PS122/4_50-62; PS122/5; PS122/5_59-11; PS122/5_59-133; PS122/5_59-151; PS122/5_59-167; PS122/5_59-179; PS122/5_59-199; PS122/5_59-220; PS122/5_59-247; PS122/5_59-26; PS122/5_59-266; PS122/5_59-287; PS122/5_59-323; PS122/5_59-341; PS122/5_59-36; PS122/5_59-361; PS122/5_59-379; PS122/5_59-4; PS122/5_59-59; PS122/5_59-65; PS122/5_60-11; PS122/5_60-116; PS122/5_60-140; PS122/5_60-169; PS122/5_60-35; PS122/5_60-50; PS122/5_60-73; PS122/5_61-106; PS122/5_61-141; PS122/5_61-184; PS122/5_61-208; PS122/5_61-244; PS122/5_61-3; PS122/5_61-34; PS122/5_62-111; PS122/5_62-133; PS122/5_62-150; PS122/5_62-171; PS122/5_62-63; PS122/5_62-8; PS122/5_62-86; PS122/5_63-115; PS122/5_63-123; PS122/5_63-134; PS122/5_63-144; PS122/5_63-27; PS122/5_63-52; PS122/5_63-6; PS122/5_63-66; PS122/5_63-7; PS122/5_63-78; PS122/5_63-93; Salinity; Sample code/label; Sample ID; Sample type; seawater; see abstract; Station label; Surface water sample; SWS; Tap; TAP; Water sample; WS; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 2375 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2021-07-21
    Description: Throughout spring and summer 2020, ozone stations in the northern extratropics recorded unusually low ozone in the free troposphere. From April to August, and from 1 to 8 kilometers altitude, ozone was on average 7% (≈4 nmol/mol) below the 2000–2020 climatological mean. Such low ozone, over several months, and at so many stations, has not been observed in any previous year since at least 2000. Atmospheric composition analyses from the Copernicus Atmosphere Monitoring Service and simulations from the NASA GMI model indicate that the large 2020 springtime ozone depletion in the Arctic stratosphere contributed less than one‐quarter of the observed tropospheric anomaly. The observed anomaly is consistent with recent chemistry‐climate model simulations, which assume emissions reductions similar to those caused by the COVID‐19 crisis. COVID‐19 related emissions reductions appear to be the major cause for the observed reduced free tropospheric ozone in 2020.
    Description: Plain Language Summary: Worldwide actions to contain the COVID‐19 virus have closed factories, grounded airplanes, and have generally reduced travel and transportation. Less fuel was burnt, and less exhaust was emitted into the atmosphere. Due to these measures, the concentration of nitrogen oxides and volatile organic compounds (VOCs) decreased in the atmosphere. These substances are important for photochemical production and destruction of ozone in the atmosphere. In clean or mildly polluted air, reducing nitrogen oxides and/or VOCs will reduce the photochemical production of ozone and result in less ozone. In heavily polluted air, in contrast, reducing nitrogen oxides can increase ozone concentrations, because less nitrogen oxide is available to destroy ozone. In this study, we use data from three types of ozone instruments, but mostly from ozonesondes on weather balloons. The sondes fly from the ground up to 30 kilometers altitude. In the first 8 km, we find significantly reduced ozone concentrations in the northern extratropics during spring and summer of 2020, less than in any other year since at least 2000. We suggest that reduced emissions due to the COVID‐19 crisis have lowered photochemical ozone production and have caused the observed ozone reductions in the troposphere.
    Description: Key Points: In spring and summer 2020, stations in the northern extratropics report on average 7% (4 nmol/mol) less tropospheric ozone than normal Such low tropospheric ozone, over several months, and at so many sites, has not been observed in any previous year since at least 2000 Most of the reduction in tropospheric ozone in 2020 is likely due to emissions reductions related to the COVID‐19 pandemic
    Description: NASA | Earth Sciences Division (NASA Earth Science Division) http://dx.doi.org/10.13039/100014573
    Description: Gouvernement du Canada | Natural Sciences and Engineering Research Council of Canada (NSERC) http://dx.doi.org/10.13039/501100000038
    Description: Australian Research Council
    Description: Fonds De La Recherche Scientifique ‐ FNRS (FNRS) http://dx.doi.org/10.13039/501100002661
    Description: Deutsche Forschungsgemeinschaft (DFG) http://dx.doi.org/10.13039/501100001659
    Description: Bundesministerium für Wirtschaft und Energie (BMWi) http://dx.doi.org/10.13039/501100006360
    Description: NASA | Earth Sciences Division (NASA Earth Science Division) http://dx.doi.org/10.13039/100014573
    Keywords: 551.51 ; COVID‐19 ; emissions ; ozone ; troposphere
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...