Rapid development and persistence of efficient subglacial drainage under 900 m-thick ice in Greenland

Awduron Sefydliadau
  • David M. Chandler(Awdur)
    Bjerknes Centre for Climate Research
    University of Bristol
  • Jemma L. Wadham(Awdur)
    University of Bristol
    University of Tromsø - The Arctic University of Norway
  • Peter W. Nienow(Awdur)
    University of Edinburgh
  • Samuel Doyle(Awdur)
  • Andrew J. Tedstone(Awdur)
    University of Fribourg
  • Jon Telling(Awdur)
    University of Newcastle upon Tyne
  • Jonathan Hawkings(Awdur)
    Florida State University
    Telegrafenberg
  • Jonathan D. Alcock(Awdur)
    University of Bristol
  • Benjamin Linhoff(Awdur)
    U.S. Geological Survey
  • Alun Hubbard(Awdur)
    University of Tromsø - The Arctic University of Norway
    University of Oulu
Math Erthygl
Iaith wreiddiolSaesneg
Rhif yr erthygl116982
Nifer y tudalennau10
CyfnodolynEarth and Planetary Science Letters
Cyfrol566
Dyddiad ar-lein cynnar11 Mai 2021
Dangosyddion eitem ddigidol (DOIs)
StatwsCyhoeddwyd - 15 Gorff 2021
Cysylltiadau
Cysylltiad parhaol
Arddangos ystadegau lawrlwytho
Gweld graff cysylltiadau
Fformatau enwi

Crynodeb

Intensive study of the Greenland Ice Sheet's (GrIS) subglacial drainage has been motivated by its importance for ice dynamics and for nutrient/sediment export to coastal ecosystems. This has revealed consistent seasonal development of efficient subglacial drainage in the lower ablation area. While some hydrological models show qualitative agreement with field data, conflicting evidence (both field- and model-based) maintains uncertainty in the extent and rate of efficient drainage development under thick (∼1 km) ice. Here, we present the first simultaneous time series of directly-observed subglacial drainage evolution, supraglacial hydrology and ice dynamics over 11 weeks in a large GrIS catchment. We demonstrate development of a fast/efficient subglacial drainage system extending from the margin to beneath ice >900 m thick, which then persisted with little response to highly variable moulin inputs including extreme melt events and extended periods (2 weeks) of low melt input. This efficient system evolved within ∼3 weeks at a moulin initiated when a fracture intersected a supraglacial river (rather than hydrofracture and lake drainage). Ice flow response to surface melt inputs at this site follows a pattern commonly observed in the lower GrIS ablation area, and by assuming a strong relationship between ice dynamics and subglacial hydrology, we infer that efficient subglacial drainage evolution is widespread under 900 m-thick ice in west Greenland. This time series of tracer transit characteristics through a developing and then persistent efficient drainage system provides a unique data set with which to validate and constrain existing numerical drainage system models, extending their capability for simulating drainage system evolution under current and future conditions.

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