Subglacial Discharge and Its Down‐Fjord Transformation in West Greenland Fjords With an Ice Mélange-Reference-Cited by-同舟云学术

Subglacial Discharge and Its Down‐Fjord Transformation in West Greenland Fjords With an Ice Mélange

Published:2020-09 Issue:9 Volume:125 Page:
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Mortensen John¹^ORCID,Rysgaard Søren¹²³^ORCID,Bendtsen Jørgen⁴^ORCID,Lennert Kunuk⁵^ORCID,Kanzow Torsten⁶⁷^ORCID,Lund Henrik⁸^ORCID,Meire Lorenz¹⁹^ORCID

Affiliation:

1. Greenland Climate Research Centre Greenland Institute of Natural Resources Nuuk Greenland

2. Arctic Research Centre, Department of Bioscience Aarhus University Aarhus Denmark

3. Centre for Earth Observation Science, CHR Faculty of Environment Earth and Resources University of Manitoba Winnipeg Manitoba Canada

4. Norwegian Institute for Water Research, Niva Denmark Copenhagen Denmark

5. The Arctic University of Norway University of Tromsø Tromsø Norway

6. Alfred‐Wegener‐Institute, Helmholtz Centre for Polar and Marine Research Bremerhaven Germany

7. Bremen University Bremen Germany

8. Greenland Institute of Natural Resources Nuuk Greenland

9. Department of Estuarine and Delta Systems Royal Netherlands Institute for Sea Research and Utrecht University Yerseke The Netherlands

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JC016301

Reference42 articles.

1. Ice mélange dynamics and implications for terminus stability, Jakobshavn Isbræ, Greenland

2. Export of Strongly Diluted Greenland Meltwater From a Major Glacial Fjord

3. Heat sources for glacial ice melt in a west Greenland tidewater outlet glacier fjord: The role of subglacial freshwater discharge

4. Modelling subglacial discharge and its influence on ocean heat transport in Arctic fjords

5. Nutrient release to oceans from buoyancy-driven upwelling at Greenland tidewater glaciers

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