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  • AGE; Age, maximum/old; Age, minimum/young; Calculated; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; Greenland; ICEDRILL; Ice drill; Mass concentration; Mode, grain size; NGRIP; North Greenland Ice Core Project; NorthGRIP; Particle concentration; Sample comment; Sampling/drilling ice; Standard deviation; Uncertainty of fit parameter  (1)
  • Eis  (1)
  • 2000-2004  (2)
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  • 2000-2004  (2)
Year
  • 1
    Keywords: Paleoclimatology Greenland ; Ice Analysis ; Greenland ; Glaciology ; Mineral dusts Greenland ; Dissertation ; Hochschulschrift ; Mittelgrönland ; Eiskern ; Pleistozän ; Staub ; Paläoklimatologie ; Grönland ; Eis ; Mikropartikel
    Type of Medium: Book
    Pages: II, 146 S. , Ill., graph. Darst., Kt.
    Series Statement: Berichte zur Polar- und Meeresforschung 428
    RVK:
    RVK:
    Language: English
    Note: Elektronische Fassung: http://www.ub.uni-heidelberg.de/archiv/2291 , Literaturangaben , Zugl.: Bremen, Univ., Diss., 2002
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  • 2
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    PANGAEA
    In:  Supplement to: Ruth, Urs; Wagenbach, Dietmar; Steffensen, Jørgen Peder; Bigler, Matthias (2003): Continuous record of microparticle concentration and size distribution in the central Greenland NGRIP ice core during the last glacial period. Journal of Geophysical Research: Atmospheres, 108(D3), 4098, https://doi.org/10.1029/2002JD002376
    Publication Date: 2023-04-22
    Description: A novel laser microparticle detector used in conjunction with continuous sample melting has provided a more than 1500 m long record of particle concentration and size distribution of the NGRIP ice core, covering continuously the period approximately from 9.5-100 kyr before present; measurements were at 1.65 m depth resolution, corresponding to approximately 35-200 yr. Particle concentration increased by a factor of 100 in the Last Glacial Maximum (LGM) compared to the Preboreal, and sharp variations of concentration occurred synchronously with rapid changes in the delta18O temperature proxy. The lognormal mode µ of the volume distribution shows clear systematic variations with smaller modes during warmer climates and coarser modes during colder periods. We find µ ~ 1.7 µm diameter during LGM and µ ~ 1.3 µm during the Preboreal. On timescales below several 100 years µ and the particle concentration exhibit a certain degree of independence present especially during warm periods, when µ generally is more variable. Using highly simplifying considerations for atmospheric transport and deposition of particles we infer that (1) the observed changes of µ in the ice largely reflect changes in the size of airborne particles above the ice sheet and (2) changes of µ are indicative of changes in long range atmospheric transport time. From the observed size changes we estimate shorter transit times by roughly 25% during LGM compared to the Preboreal. The associated particle concentration increase from more efficient long range transport is estimated to less than one order of magnitude.
    Keywords: AGE; Age, maximum/old; Age, minimum/young; Calculated; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; Greenland; ICEDRILL; Ice drill; Mass concentration; Mode, grain size; NGRIP; North Greenland Ice Core Project; NorthGRIP; Particle concentration; Sample comment; Sampling/drilling ice; Standard deviation; Uncertainty of fit parameter
    Type: Dataset
    Format: text/tab-separated-values, 9558 data points
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