Modeling the Tidewater Glacier Kangiata Nunaata Sermia and the Freshwater Flux into Godthaabsfjorden

Research output: Book/Report › Ph.D. thesis › Research

Standard

Modeling the Tidewater Glacier Kangiata Nunaata Sermia and the Freshwater Flux into Godthaabsfjorden. / Fitzner, Antje.

The Niels Bohr Institute, Faculty of Science, University of Copenhagen, 2014. 148 p.

Research output: Book/Report › Ph.D. thesis › Research

Harvard

Fitzner, A 2014, Modeling the Tidewater Glacier Kangiata Nunaata Sermia and the Freshwater Flux into Godthaabsfjorden. The Niels Bohr Institute, Faculty of Science, University of Copenhagen. <https://soeg.kb.dk/permalink/45KBDK_KGL/fbp0ps/alma99122319757305763>

APA

Fitzner, A. (2014). Modeling the Tidewater Glacier Kangiata Nunaata Sermia and the Freshwater Flux into Godthaabsfjorden. The Niels Bohr Institute, Faculty of Science, University of Copenhagen. https://soeg.kb.dk/permalink/45KBDK_KGL/fbp0ps/alma99122319757305763

Vancouver

Fitzner A. Modeling the Tidewater Glacier Kangiata Nunaata Sermia and the Freshwater Flux into Godthaabsfjorden. The Niels Bohr Institute, Faculty of Science, University of Copenhagen, 2014. 148 p.

Author

Fitzner, Antje. / Modeling the Tidewater Glacier Kangiata Nunaata Sermia and the Freshwater Flux into Godthaabsfjorden. The Niels Bohr Institute, Faculty of Science, University of Copenhagen, 2014. 148 p.

Bibtex

@phdthesis{ec8702f0080842c4a35fc2d603490115,
title = "Modeling the Tidewater Glacier Kangiata Nunaata Sermia and the Freshwater Flux into Godthaabsfjorden",
abstract = "The Greenland ice sheet loses mass due to changing surface mass balance, direct melting on the surface, ice flow through the numerous outlet glaciers, and basal melt. This Ph.D. thesis focuses on the outlet glaciers terminating in Godth{\aa}bsfjord near Nuuk in West Greenland, with Kangiata Nunaata Sermia (KNS) being the main contributing glacier. The mass loss of this glacier forms a small contribution to the total mass loss of the Greenland ice sheet, but it will have a large impact on the local ecosystem when there is a large freshwater flux into the fjord. Here, two independent methods are used to estimate the total mass loss by KNS and its neighboring outlets, namely the ice sheet model PISM applied to KNS and stable oxygen isotope measurements in the fjord. Both studies show that KNS is currently losing mass. Prognostic studies show that KNS will likely continue to lose mass.",
author = "Antje Fitzner",
year = "2014",
language = "English",
publisher = "The Niels Bohr Institute, Faculty of Science, University of Copenhagen",

}

RIS

TY - BOOK

T1 - Modeling the Tidewater Glacier Kangiata Nunaata Sermia and the Freshwater Flux into Godthaabsfjorden

AU - Fitzner, Antje

PY - 2014

Y1 - 2014

N2 - The Greenland ice sheet loses mass due to changing surface mass balance, direct melting on the surface, ice flow through the numerous outlet glaciers, and basal melt. This Ph.D. thesis focuses on the outlet glaciers terminating in Godthåbsfjord near Nuuk in West Greenland, with Kangiata Nunaata Sermia (KNS) being the main contributing glacier. The mass loss of this glacier forms a small contribution to the total mass loss of the Greenland ice sheet, but it will have a large impact on the local ecosystem when there is a large freshwater flux into the fjord. Here, two independent methods are used to estimate the total mass loss by KNS and its neighboring outlets, namely the ice sheet model PISM applied to KNS and stable oxygen isotope measurements in the fjord. Both studies show that KNS is currently losing mass. Prognostic studies show that KNS will likely continue to lose mass.

AB - The Greenland ice sheet loses mass due to changing surface mass balance, direct melting on the surface, ice flow through the numerous outlet glaciers, and basal melt. This Ph.D. thesis focuses on the outlet glaciers terminating in Godthåbsfjord near Nuuk in West Greenland, with Kangiata Nunaata Sermia (KNS) being the main contributing glacier. The mass loss of this glacier forms a small contribution to the total mass loss of the Greenland ice sheet, but it will have a large impact on the local ecosystem when there is a large freshwater flux into the fjord. Here, two independent methods are used to estimate the total mass loss by KNS and its neighboring outlets, namely the ice sheet model PISM applied to KNS and stable oxygen isotope measurements in the fjord. Both studies show that KNS is currently losing mass. Prognostic studies show that KNS will likely continue to lose mass.

UR - https://soeg.kb.dk/permalink/45KBDK_KGL/fbp0ps/alma99122319757305763

M3 - Ph.D. thesis

BT - Modeling the Tidewater Glacier Kangiata Nunaata Sermia and the Freshwater Flux into Godthaabsfjorden

PB - The Niels Bohr Institute, Faculty of Science, University of Copenhagen

ER -

ID: 129664628