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  • 2020-2024  (56)
  • 2020-2022  (2)
Publikationsart
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  • 1
    Publikationsdatum: 2023-02-08
    Beschreibung: The Labrador Sea is important for the modern global thermohaline circulation system through the formation of intermediate Labrador Sea Water (LSW) that has been hypothesized to stabilize the modern mode of North Atlantic deep-water circulation. The rate of LSW formation is controlled by the amount of winter heat loss to the atmosphere, the expanse of freshwater in the convection region and the inflow of saline waters from the Atlantic. The Labrador Sea, today, receives freshwater through the East and West Greenland currents (EGC, WGC) and the Labrador Current (LC). Several studies have suggested the WGC to be the main supplier of freshwater to the Labrador Sea, but the role of the southward flowing LC in Labrador Sea convection is still debated. At the same time, many paleoceanographic reconstructions from the Labrador Shelf focussed on late deglacial to early Holocene meltwater run-off from the Laurentide Ice Sheet (LIS), whereas little information exists about LC variability since the final melting of the LIS about 7000 years ago. In order to enable better assessment of the role of the LC in deep-water formation and its importance for Holocene climate variability in Atlantic Canada, this study presents high-resolution middle to late Holocene records of sea surface and bottom water temperatures, freshening, and sea ice cover on the Labrador Shelf during the last 6000 years. Our records reveal that the LC underwent three major oceanographic phases from the mid- to late Holocene. From 6.2 to 5.6 ka, the LC experienced a cold episode that was followed by warmer conditions between 5.6 and 2.1 ka, possibly associated with the late Holocene thermal maximum. While surface waters on the Labrador Shelf cooled gradually after 3 ka in response to the neoglaciation, Labrador Shelf subsurface or bottom waters show a shift to warmer temperatures after 2.1 ka. Although such an inverse stratification by cooling of surface and warming of subsurface waters on the Labrador Shelf would suggest a diminished convection during the last 2 millennia compared to the mid-Holocene, it remains difficult to assess whether hydrographic conditions in the LC have had a significant impact on Labrador Sea deep-water formation.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2021-10-07
    Beschreibung: We reconstructed the variability of the Earth's strongest hydrological system, the Indian monsoon, over the interval 6.24 to 4.91 Ma at International Ocean Discovery Program (IODP) Expedition 353 Site U1448 in the Andaman Sea. We integrated high-resolution benthic and planktic foraminiferal carbon and oxygen isotopes with Mg/Ca measurements of the mixed layer foraminifer Trilobatus sacculifer to reconstruct the isotopic composition of seawater (δ18Osw) and the gradient between planktic and benthic foraminiferal δ13C. A prominent increase in mixed layer temperatures of ~4°C occurred between 5.55 and 5.28 Ma, accompanied by a change from precession- to obliquity-driven variability in planktic δ18O and δ18Osw. We suggest that an intensified cross-equatorial transport of heat and moisture, paced by obliquity, led to increased summer monsoon precipitation during warm stages after 5.55 Ma. Transient cold stages were characterized by reduced mixed layer temperatures and summer monsoon failure, thus resembling late Pleistocene stadials. In contrast, an overall cooler background climate state with a strengthened biological pump prevailed prior to 5.55 Ma. These findings highlight the importance of internal feedback processes for the long-term evolution of the Indian monsoon.
    Schlagwort(e): 551.6 ; Indian monsoon ; Miocene-Pliocene transition ; Bay of Bengal ; Mg/Ca paleothermometry ; stable isotopes ; orbital forcing
    Sprache: Englisch
    Materialart: map
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2021-10-15
    Beschreibung: Millennial-scale reductions in monsoon precipitation, so-called Weak Monsoon Intervals (WMIs), have been identified in numerous paleoclimate records across the Afro-Asian monsoon domain throughout the last glacial-interglacial cycle. These are considered the regional response to cooling during Heinrich events in the North Atlantic realm and several mechanisms have been suggested to explain this hemisphere-scale climatic teleconnection. In particular, reductions in Indian Ocean sea surface temperature (SST) have been proposed as the linking element between Heinrich events and WMIs. However, the validity of this relationship has only been demonstrated for the last ~20 kyr, leaving unresolved whether it also holds on longer time scales. Here we present a new paired record of planktonic foraminifera-based δ18Osw-ivc and UK'37-based SST from the northern Bay of Bengal, covering the last ~130 kyr. The δ18Osw-ivc record clearly reflects orbitally paced changes of Indian Summer Monsoon intensity superimposed by centennial- to millennial-scale WMIs that occurred synchronously to North Atlantic Heinrich events. Comparison with the UK'37-based SST reconstruction reveals, however, that WMIs in most cases were not paralleled by ocean surface cooling, questioning whether Indian Ocean SST lowering was the linking element between Heinrich events and reductions in monsoon precipitation in Asia also during the last glacial period.
    Schlagwort(e): 551 ; Indian Summer Monsoon ; Weak Monsoon Intervals ; marine sediments ; Bay of Bengal ; foraminifera oxygen isotopes ; UK'37 sea surface temperature
    Sprache: Englisch
    Materialart: map
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2023-03-25
    Beschreibung: We present stable hydrogen isotope (dD) and carbon isotope (d13C) of sedimentary terrestrial leaf wax, namely n-alkanes, from marine sediment core SO 188-17286-1 (Bay of Bengal, 19°44.58′N, 89°52.76′E, 1428 m water depth) for the last ~130 kyr. There are four different homologues (n-C27, n-C29, n-C31 and n-C33). The concentration data of each homologues are also present here. Identification and quantification (concentration) of the individual compounds was carried out with an Agilent 6890 Gas Chromatograph (GC) with a flame ionization detector in the Geoscience, University of Kiel. The d13C and dD values of n-alkanes were then analyzed at the Leibniz Laboratory for Radiometric Dating and Stable Isotope Research in Kiel University using an Agilent 6890 GC coupled with a Thermo Finnigan MAT 253 isotope ratio mass (IRMS).
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2023-01-30
    Beschreibung: The Mozambique Channel is a conduit of trade wind-driven throughflow that is a key component of the Agulhas Current and Agulhas leakage, a flux of warm and salty water from the tropical Indo-Pacific to the Atlantic Ocean. Agulhas leakage is thought to modulate Atlantic meridional overturning circulation variability. Previous studies from the Cape Basin suggest that enhanced Agulhas leakage played an important role in accelerating glacial terminations. The southern African monsoon response to abrupt climate changes associated with meltwater-induced reorganizations of the North Atlantic meridional overturning circulation, and its impact on the Mozambique Channel throughflow and, by extension, on the Agulhas leakage is not well understood. Here we present a high-resolution 26,000 year-long hydroclimate record of northern Madagascar, a core region of the southern hemisphere monsoon domain, and a mixed layer temperature reconstruction using sediment cores collected from the runoff-influenced eastern Mozambique Channel. The record indicates precipitation increases centered at 11.7-12.5 thousand years before present (kyr BP), 14.5-19 kyr BP, 23-24 kyr BP, 25-26 kyr BP. Considering age model uncertainties, this is the first strong evidence for southern African monsoon strengthening in response to meltwater-induced northern high latitude climate instabilities during the Younger Dryas (YD), Heinrich Stadial 1 (HS1), HS2 and the HS-like event prior to HS2, in agreement with the results of transient climate simulations. Furthermore, our study shows a reversal of the mixed layer temperature gradient between the western and eastern Mozambique Channel during Heinrich event 1 (HE1). We posit that the gradient reversal indicates a weakening of the trade wind-driven South Equatorial Current and Mozambique Channel throughflow that likely weakened the Agulhas leakage, potentially creating a feedback that may have contributed to the sustained weakening of the AMOC during HE1 by reducing the amount of heat and salt leakage into the Atlantic.
    Schlagwort(e): Agulhas Leakage; marine sediments; Mozambique Channel; Mozambique Channel throughflow; oxygen isotope data; SST
    Materialart: Dataset
    Format: application/zip, 5 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2023-06-27
    Schlagwort(e): AGE; Age, 14C; Age, uncertainty; Agulhas Leakage; Calendar age; Calendar age, error to older; Calendar age, error to younger; Core; Date/Time of event; DEPTH, sediment/rock; Event label; GIK16163-2; GIK16164-2; GIK16166-2; Gravity corer (Kiel type); Laboratory code/label; Latitude of event; Longitude of event; M75/3; M75/3_143-2; M75/3_144-2; M75/3_146-2; marine sediments; Meteor (1986); Mozambique Channel; Mozambique Channel throughflow; oxygen isotope data; Sample material; SL; SST
    Materialart: Dataset
    Format: text/tab-separated-values, 217 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2023-06-27
    Schlagwort(e): AGE; Agulhas Leakage; Calculated; Core; Date/Time of event; DEPTH, sediment/rock; Event label; GIK16163-2; GIK16164-2; GIK16166-2; Globigerinoides ruber white, Magnesium/Calcium ratio; Gravity corer (Kiel type); Latitude of event; Longitude of event; M75/3; M75/3_143-2; M75/3_144-2; M75/3_146-2; marine sediments; Meteor (1986); Mozambique Channel; Mozambique Channel throughflow; oxygen isotope data; SL; SST
    Materialart: Dataset
    Format: text/tab-separated-values, 522 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Publikationsdatum: 2023-06-27
    Schlagwort(e): AGE; Agulhas Leakage; Core; Date/Time of event; DEPTH, sediment/rock; Error; Event label; GIK16163-2; GIK16164-2; GIK16166-2; Globigerinoides ruber white, δ18O; Globigerinoides ruber white, δ18O standard deviation; Gravity corer (Kiel type); Latitude of event; Longitude of event; M75/3; M75/3_143-2; M75/3_144-2; M75/3_146-2; marine sediments; Meteor (1986); Mozambique Channel; Mozambique Channel throughflow; oxygen isotope data; Sea water temperaure & ice volume effects corrected; SL; SST
    Materialart: Dataset
    Format: text/tab-separated-values, 1908 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Publikationsdatum: 2023-06-27
    Schlagwort(e): AGE; Agilent 6890 GC coupled with a Thermo Finnigan MAT 253 isotope ratio mass (IRMS); Bay of Bengal; Bengal Sea Level; DEPTH, sediment/rock; GIK17286-1; Gravity corer (Kiel type); n-Alkane C27, δD; n-Alkane C27, δD, standard error; n-Alkane C29, δD; n-Alkane C29, δD, standard error; n-Alkane C31, δD; n-Alkane C31, δD, standard error; n-Alkane C33, δD; n-Alkane C33, δD, standard error; SL; SO188/1; Sonne
    Materialart: Dataset
    Format: text/tab-separated-values, 1050 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    Publikationsdatum: 2023-06-27
    Schlagwort(e): AGE; Agulhas Leakage; Calculated from Mg/Ca and oxygen isotope time-series of local mixed layer; GIK16163-2; GIK16164-2; GIK16166-2; Gravity corer (Kiel type); M75/3; M75/3_143-2; M75/3_144-2; M75/3_146-2; marine sediments; Meteor (1986); Mozambique Channel; Mozambique Channel throughflow; oxygen isotope data; Sea surface temperature; SL; SST
    Materialart: Dataset
    Format: text/tab-separated-values, 123 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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