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  • Accumulation rate in ice equivalent per year; AGE; Calculated; Calculated, running median; CFA; Conductivity, electrolytic; Continuous Flow Analysis; Corrected; Deposition of sulfate, volcanic; Deposition of sulfate, volcanic, cumulative; DEPTH, ice/snow; DRILL; Drilling/drill rig; dust; Dust, insoluble; GISP; GISP2; Greenland; Ice core; Sampling/drilling ice; Sodium; Sulfate; Sulfate, background; Sulfate, volcanic; Sulfur; Sulfur, non-sea-salt; Volcanic aerosol; volcanic eruption  (1)
  • Maya; eruption dispersal; large volcanic eruptions; radiocarbon; sulfate  (1)
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Years
  • 1
    Publication Date: 2024-03-26
    Description: We present continuous records of 1 cm resolved sodium, sulfur, non-sea-salt sulfur, size-resolved insoluble particle concentrations and liquid conductivity using a Continuous Flow Analysis (CFA) system (McConnell et al., 2017) from the Greenland Ice Sheet Project Two (GISP2; 72.97°N, 38.80°W) ice core and estimated volcanic sulfate mass depositions for the depth interval 2635-2638 m (equivalent to an age of c. 80 ka BP on GICC05modelext (Seierstad et al., 2014) and 79.5 ka BP on AICC2012 (Veres et al., 2013). The reconstruction is based on sulfur measurements employing high-resolution continuous flow analysis coupled to inductively coupled plasma mass spectrometry performed at the Desert Research Institute (Reno, NV, USA) under (class 100) cleanroom conditions. Volcanic eruptions are detected when annual sulfur concentrations exceeded the background concentrations + 4 times the median of the absolute deviation. Background concentrations are estimated using a 101-point running median. Volcanic sulfate deposition rates are calculated by subtracting the background concentrations from total sulfate equivalent (i.e. sulfur x 3) concentrations using thinning corrected estimates of mean ice accumulation rates at the ice-core site.
    Keywords: Accumulation rate in ice equivalent per year; AGE; Calculated; Calculated, running median; CFA; Conductivity, electrolytic; Continuous Flow Analysis; Corrected; Deposition of sulfate, volcanic; Deposition of sulfate, volcanic, cumulative; DEPTH, ice/snow; DRILL; Drilling/drill rig; dust; Dust, insoluble; GISP; GISP2; Greenland; Ice core; Sampling/drilling ice; Sodium; Sulfate; Sulfate, background; Sulfate, volcanic; Sulfur; Sulfur, non-sea-salt; Volcanic aerosol; volcanic eruption
    Type: Dataset
    Format: text/tab-separated-values, 3270 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-10-26
    Description: The Tierra Blanca Joven (TBJ) eruption from Ilopango volcano deposited thick ash over much of El Salvador when it was inhabited by the Maya, and rendered all areas within at least 80 km of the volcano uninhabitable for years to decades after the eruption. Nonetheless, the more widespread environmental and climatic impacts of this large eruption are not well known because the eruption magnitude and date are not well constrained. In this multifaceted study we have resolved the date of the eruption to 431 ± 2 CE by identifying the ash layer in a well-dated, high-resolution Greenland ice-core record that is 〉7,000 km from Ilopango; and calculated that between 37 and 82 km3 of magma was dispersed from an eruption coignimbrite column that rose to ∼45 km by modeling the deposit thickness using state-of-the-art tephra dispersal methods. Sulfate records from an array of ice cores suggest stratospheric injection of 14 ± 2 Tg S associated with the TBJ eruption, exceeding those of the historic eruption of Pinatubo in 1991. Based on these estimates it is likely that the TBJ eruption produced a cooling of around 0.5 °C for a few years after the eruption. The modeled dispersal and higher sulfate concentrations recorded in Antarctic ice cores imply that the cooling would have been more pronounced in the Southern Hemisphere. The new date confirms the eruption occurred within the Early Classic phase when Maya expanded across Central America.
    Description: Published
    Description: 26061-26068
    Description: 1V. Storia eruttiva
    Description: JCR Journal
    Keywords: Maya; eruption dispersal; large volcanic eruptions; radiocarbon; sulfate
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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