Where is the 1-million-year-old ice at Dome A?

Liyun Zhao, John C. Moore, Bo Sun, Xueyuan Tang, Xiaoran Guo

Tutkimustuotokset: Kirjoitus lehdessä tai erikoisnumeron toimittaminenArtikkeliTieteellinenvertaisarvioitu

7 Sitaatiot (Scopus)

Abstrakti

Ice fabric influences the rheology of ice, and hence the age-depth profile at ice core drilling sites. To investigate the age-depth profile to be expected of the ongoing deep ice coring at Kunlun station, Dome A, we use the depth-varying anisotropic fabric suggested by the recent polarimetric measurements around Dome A along with prescribed fabrics ranging from isotropic through girdle to single maximum in a three-dimensional, thermo-mechanically coupled full-Stokes model of a 70 x 70 km(2) domain around Kunlun station. This model allows for the simulation of the near basal ice temperature and age, and ice flow around the location of the Chinese deep ice coring site. Ice fabrics and geothermal heat flux strongly affect the vertical advection and basal temperature which consequently control the age profile. Constraining modeled age-depth profiles with dated radar isochrones to 2/3 ice depth, the surface vertical velocity, and also the spatial variability of a radar isochrones dated to 153.3 ka BP, limits the age of the deep ice at Kunlun to between 649 and 831 ka, a much smaller range than previously inferred. The simple interpretation of the polarimetric radar fabric data that we use produces best fits with a geothermal heat flux of 55 mW m(-2). A heat flux of 50mWm(-2) is too low to fit the deeper radar layers, and 60mWm(-2) leads to unrealistic surface velocities. The modeled basal temperature at Kunlun reaches the pressure melting point with a basal melting rate of 2.2-2.7mma(-1). Using the spatial distribution of basal temperatures and the best fit fabric suggests that within 400m of Kunlun station, 1-million-year-old ice may be found 200m above the bed, and that there are large regions where even older ice is well above the bedrock within 5-6 km of the Kunlun station.

Alkuperäiskielienglanti
Sivut1651-1663
Sivumäärä13
JulkaisuCryosphere
Vuosikerta12
Numero5
DOI - pysyväislinkit
TilaJulkaistu - 15 toukokuuta 2018
OKM-julkaisutyyppiA1 Vertaisarvioitu alkuperäisartikkeli

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