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  • Atlantic meridional overturning circulation; ATLAS; A Trans-Atlantic assessment and deep-water ecosystem-based spatial management plan for Europe; deep water formation; sortable silt; subsurface ocean temperatures  (5)
  • 04071220; Bio-Optical Platform; BOP; DEPTH, water; Equatorial Pacific; Fluorescence; JGOFS; Joint Global Ocean Flux Study; Number of observations; Radiance, upward at 410 nm; Radiance, upward at 441 nm; Radiance, upward at 488 nm; Radiance, upward at 520 nm; Radiance, upward at 550 nm; Radiance, upward at 633 nm; Radiance, upward at 656 nm; Radiance, upward at 683 nm; Radiation, photosynthetically active; Salinity; Spectral irradiance, downward at 410 nm; Spectral irradiance, downward at 441 nm; Spectral irradiance, downward at 488 nm; Spectral irradiance, downward at 520 nm; Spectral irradiance, downward at 550 nm; Spectral irradiance, downward at 560 nm; Spectral irradiance, downward at 589 nm; Spectral irradiance, downward at 633 nm; Spectral irradiance, downward at 656 nm; Spectral irradiance, downward at 671 nm; Spectral irradiance, downward at 683 nm; Spectral irradiance, downward at 694 nm; Spectral irradiance, downward at 710 nm; Spectral irradiance, incident at 410 nm; Spectral irradiance, incident at 520 nm; Spectral irradiance, upward at 410 nm; Spectral irradiance, upward at 441 nm; Spectral irradiance, upward at 486 nm; Spectral irradiance, upward at 488 nm; Spectral irradiance, upward at 520 nm; Spectral irradiance, upward at 550 nm; Spectral irradiance, upward at 671 nm; Spectral irradiance, upward at 694 nm; Temperature, water; Thomas G. Thompson; TT008; TT008_5-BOP18  (2)
  • PANGAEA  (7)
  • Elsevier
  • 2015-2019  (5)
  • 2010-2014
  • 2000-2004  (2)
Collection
Keywords
Publisher
  • PANGAEA  (7)
  • Elsevier
Years
  • 2015-2019  (5)
  • 2010-2014
  • 2000-2004  (2)
Year
  • 1
    Publication Date: 2024-02-01
    Keywords: 04071220; Bio-Optical Platform; BOP; DEPTH, water; Equatorial Pacific; Fluorescence; JGOFS; Joint Global Ocean Flux Study; Number of observations; Radiance, upward at 410 nm; Radiance, upward at 441 nm; Radiance, upward at 488 nm; Radiance, upward at 520 nm; Radiance, upward at 550 nm; Radiance, upward at 633 nm; Radiance, upward at 656 nm; Radiance, upward at 683 nm; Radiation, photosynthetically active; Salinity; Spectral irradiance, downward at 410 nm; Spectral irradiance, downward at 441 nm; Spectral irradiance, downward at 488 nm; Spectral irradiance, downward at 520 nm; Spectral irradiance, downward at 550 nm; Spectral irradiance, downward at 560 nm; Spectral irradiance, downward at 589 nm; Spectral irradiance, downward at 633 nm; Spectral irradiance, downward at 656 nm; Spectral irradiance, downward at 671 nm; Spectral irradiance, downward at 683 nm; Spectral irradiance, downward at 694 nm; Spectral irradiance, downward at 710 nm; Spectral irradiance, incident at 410 nm; Spectral irradiance, incident at 520 nm; Spectral irradiance, upward at 410 nm; Spectral irradiance, upward at 441 nm; Spectral irradiance, upward at 486 nm; Spectral irradiance, upward at 488 nm; Spectral irradiance, upward at 520 nm; Spectral irradiance, upward at 550 nm; Spectral irradiance, upward at 671 nm; Spectral irradiance, upward at 694 nm; Temperature, water; Thomas G. Thompson; TT008; TT008_5-BOP18
    Type: Dataset
    Format: text/tab-separated-values, 4549 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2024-02-01
    Keywords: 04071220; Bio-Optical Platform; BOP; DEPTH, water; Equatorial Pacific; Fluorescence; JGOFS; Joint Global Ocean Flux Study; Number of observations; Radiance, upward at 410 nm; Radiance, upward at 441 nm; Radiance, upward at 488 nm; Radiance, upward at 520 nm; Radiance, upward at 550 nm; Radiance, upward at 633 nm; Radiance, upward at 656 nm; Radiance, upward at 683 nm; Radiation, photosynthetically active; Salinity; Spectral irradiance, downward at 410 nm; Spectral irradiance, downward at 441 nm; Spectral irradiance, downward at 488 nm; Spectral irradiance, downward at 520 nm; Spectral irradiance, downward at 550 nm; Spectral irradiance, downward at 560 nm; Spectral irradiance, downward at 589 nm; Spectral irradiance, downward at 633 nm; Spectral irradiance, downward at 656 nm; Spectral irradiance, downward at 671 nm; Spectral irradiance, downward at 683 nm; Spectral irradiance, downward at 694 nm; Spectral irradiance, downward at 710 nm; Spectral irradiance, incident at 410 nm; Spectral irradiance, incident at 520 nm; Spectral irradiance, upward at 410 nm; Spectral irradiance, upward at 441 nm; Spectral irradiance, upward at 486 nm; Spectral irradiance, upward at 488 nm; Spectral irradiance, upward at 520 nm; Spectral irradiance, upward at 550 nm; Spectral irradiance, upward at 671 nm; Spectral irradiance, upward at 694 nm; Temperature, water; Thomas G. Thompson; TT008; TT008_5-BOP18
    Type: Dataset
    Format: text/tab-separated-values, 1738 data points
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  • 3
    Publication Date: 2023-12-18
    Keywords: Atlantic meridional overturning circulation; ATLAS; A Trans-Atlantic assessment and deep-water ecosystem-based spatial management plan for Europe; deep water formation; sortable silt; subsurface ocean temperatures
    Type: Dataset
    Format: application/zip, 9.2 kBytes
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  • 4
    Publication Date: 2023-12-18
    Keywords: Atlantic meridional overturning circulation; ATLAS; A Trans-Atlantic assessment and deep-water ecosystem-based spatial management plan for Europe; deep water formation; sortable silt; subsurface ocean temperatures
    Type: Dataset
    Format: application/zip, 9.7 kBytes
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  • 5
    Publication Date: 2023-12-18
    Keywords: Atlantic meridional overturning circulation; ATLAS; A Trans-Atlantic assessment and deep-water ecosystem-based spatial management plan for Europe; deep water formation; sortable silt; subsurface ocean temperatures
    Type: Dataset
    Format: application/zip, 9.7 kBytes
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  • 6
    Publication Date: 2023-12-18
    Keywords: Atlantic meridional overturning circulation; ATLAS; A Trans-Atlantic assessment and deep-water ecosystem-based spatial management plan for Europe; deep water formation; sortable silt; subsurface ocean temperatures
    Type: Dataset
    Format: application/zip, 9.9 kBytes
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  • 7
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    PANGAEA
    In:  Woods Hole Oceanographic Institution, Department of Geology & Geophysics | Supplement to: Thornalley, David J R; Oppo, Delia W; Ortega, Pablo; Robson, Jon I; Brierley, Chris M; Davis, Renee; Hall, Ian R; Moffa-Sanchez, Paola; Rose, Neil L; Spooner, Peter T; Yashayaev, Igor M; Keigwin, Lloyd D (2018): Anomalously weak Labrador Sea convection and Atlantic overturning during the past 150 years. Nature, 556(7700), 227-230, https://doi.org/10.1038/s41586-018-0007-4
    Publication Date: 2024-04-24
    Description: The Atlantic meridional overturning circulation (AMOC) is a system of ocean currents that has an essential role in Earth's climate, redistributing heat and influencing the carbon cycle. The AMOC has been shown to be weakening in recent years1; this decline may reflect decadal-scale variability in convection in the Labrador Sea, but short observational datasets preclude a longer-term perspective on the modern state and variability of Labrador Sea convection and the AMOC. Here we provide several lines of palaeo-oceanographic evidence that Labrador Sea deep convection and the AMOC have been anomalously weak over the past 150 years or so (since the end of the Little Ice Age, LIA, approximately AD 1850) compared with the preceding 1,500 years. Our palaeoclimate reconstructions indicate that the transition occurred either as a predominantly abrupt shift towards the end of the LIA, or as a more gradual, continued decline over the past 150 years; this ambiguity probably arises from non-AMOC influences on the various proxies or from the different sensitivities of these proxies to individual components of the AMOC. We suggest that enhanced freshwater fluxes from the Arctic and Nordic seas towards the end of the LIA—sourced from melting glaciers and thickened sea ice that developed earlier in the LIA—weakened Labrador Sea convection and the AMOC. The lack of a subsequent recovery may have resulted from hysteresis or from twentieth-century melting of the Greenland Ice Sheet. Our results suggest that recent decadal variability in Labrador Sea convection and the AMOC has occurred during an atypical, weak background state. Future work should aim to constrain the roles of internal climate variability and early anthropogenic forcing in the AMOC weakening described here. The data presented here is the supporting data for Thornalley et al. 2018 (see details below) and is derived from cores KNR-178-56JPC and KNR-178-48JPC. It includes the mean sortable silt size, details of radiocarbon dating, the % nps and binned sub-surface temperature reconstructions.
    Keywords: Atlantic meridional overturning circulation; ATLAS; A Trans-Atlantic assessment and deep-water ecosystem-based spatial management plan for Europe; deep water formation; sortable silt; subsurface ocean temperatures
    Type: Dataset
    Format: application/zip, 22 datasets
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