Alaskan Glacial Dust Is an Important Iron Source to Surface Waters of the Gulf of Alaska

Abstract This work evaluates glacial dust as a source of sediment, and associated iron (Fe), to the Fe‐limited Gulf of Alaska (GoA). A reanalysis of GoA sediment data, using rare earth elements and thorium as provenance tracers, suggests a flux to the ocean surface of Copper River (AK) glacial dust,...

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Main Authors: John Crusius, Carsten A. Lao, Thomas M. Holmes, James W. Murray
Format: Article
Language:English
Published: Wiley 2024-06-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2023GL106778
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author John Crusius
Carsten A. Lao
Thomas M. Holmes
James W. Murray
author_facet John Crusius
Carsten A. Lao
Thomas M. Holmes
James W. Murray
author_sort John Crusius
collection DOAJ
description Abstract This work evaluates glacial dust as a source of sediment, and associated iron (Fe), to the Fe‐limited Gulf of Alaska (GoA). A reanalysis of GoA sediment data, using rare earth elements and thorium as provenance tracers, suggests a flux to the ocean surface of Copper River (AK) glacial dust, and associated Fe, that is comparable to the flux of dust from Asia, at least 1,000 km from the narrow mountain valley glacial dust source area. This work suggests dust from Asia may not be the largest source of Fe to the GoA. Dust models fail to accurately simulate this glacial dust transport because their coarse resolution underestimates wind speeds, and the dust flux. This work suggests that glacial dust fluxes may have been important in the geologic past (e.g., the last glacial maximum) from locations where there was more extensive coverage by glaciers than at present.
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spelling doaj-art-9ff41966989e45a3a70b8d688949a42c2025-08-20T03:10:21ZengWileyGeophysical Research Letters0094-82761944-80072024-06-015112n/an/a10.1029/2023GL106778Alaskan Glacial Dust Is an Important Iron Source to Surface Waters of the Gulf of AlaskaJohn Crusius0Carsten A. Lao1Thomas M. Holmes2James W. Murray3U.S. Geological Survey University of Washington School of Oceanography Seattle WA USADepartment of Chemistry University of Washington Seattle WA USAAustralian Antarctic Program Partnership University of Tasmania Hobart TAS AustraliaSchool of Oceanography University of Washington Seattle WA USAAbstract This work evaluates glacial dust as a source of sediment, and associated iron (Fe), to the Fe‐limited Gulf of Alaska (GoA). A reanalysis of GoA sediment data, using rare earth elements and thorium as provenance tracers, suggests a flux to the ocean surface of Copper River (AK) glacial dust, and associated Fe, that is comparable to the flux of dust from Asia, at least 1,000 km from the narrow mountain valley glacial dust source area. This work suggests dust from Asia may not be the largest source of Fe to the GoA. Dust models fail to accurately simulate this glacial dust transport because their coarse resolution underestimates wind speeds, and the dust flux. This work suggests that glacial dust fluxes may have been important in the geologic past (e.g., the last glacial maximum) from locations where there was more extensive coverage by glaciers than at present.https://doi.org/10.1029/2023GL106778dustAlaskaglacierglacial particleCopper Riveriron
spellingShingle John Crusius
Carsten A. Lao
Thomas M. Holmes
James W. Murray
Alaskan Glacial Dust Is an Important Iron Source to Surface Waters of the Gulf of Alaska
Geophysical Research Letters
dust
Alaska
glacier
glacial particle
Copper River
iron
title Alaskan Glacial Dust Is an Important Iron Source to Surface Waters of the Gulf of Alaska
title_full Alaskan Glacial Dust Is an Important Iron Source to Surface Waters of the Gulf of Alaska
title_fullStr Alaskan Glacial Dust Is an Important Iron Source to Surface Waters of the Gulf of Alaska
title_full_unstemmed Alaskan Glacial Dust Is an Important Iron Source to Surface Waters of the Gulf of Alaska
title_short Alaskan Glacial Dust Is an Important Iron Source to Surface Waters of the Gulf of Alaska
title_sort alaskan glacial dust is an important iron source to surface waters of the gulf of alaska
topic dust
Alaska
glacier
glacial particle
Copper River
iron
url https://doi.org/10.1029/2023GL106778
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