MODIS observed increase in duration and spatial extent of sediment plumes in Greenland fjords

The freshwater flux from the Greenland Ice Sheet (GrIS) to the North Atlantic Ocean carries extensive but poorly documented volumes of sediment. We develop a suspended sediment concentration (SSC) retrieval algorithm using a large Greenland specific in situ data set. This algorithm is applied to all...

Full description

Bibliographic Details
Main Authors: B. Hudson, I. Overeem, D. McGrath, J. P. M. Syvitski, A. Mikkelsen, B. Hasholt
Format: Article
Language:English
Published: Copernicus Publications 2014-07-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/8/1161/2014/tc-8-1161-2014.pdf
_version_ 1818466134100279296
author B. Hudson
I. Overeem
D. McGrath
J. P. M. Syvitski
A. Mikkelsen
B. Hasholt
author_facet B. Hudson
I. Overeem
D. McGrath
J. P. M. Syvitski
A. Mikkelsen
B. Hasholt
author_sort B. Hudson
collection DOAJ
description The freshwater flux from the Greenland Ice Sheet (GrIS) to the North Atlantic Ocean carries extensive but poorly documented volumes of sediment. We develop a suspended sediment concentration (SSC) retrieval algorithm using a large Greenland specific in situ data set. This algorithm is applied to all cloud-free NASA Moderate Resolution Imaging Spectrometer (MODIS) Terra images from 2000 to 2012 to monitor SSC dynamics at six river plumes in three fjords in southwest Greenland. Melt-season mean plume SSC increased at all but one site, although these trends were primarily not statistically significant. Zones of sediment concentration > 50 mg L<sup>−1</sup> expanded in three river plumes, with potential consequences for biological productivity. The high SSC cores of sediment plumes ( > 250 mg L<sup>&minus;1</sup> expanded in one-third of study locations. At a regional scale, higher volumes of runoff were associated with higher melt-season mean plume SSC values, but this relationship did not hold for individual rivers. High spatial variability between proximal plumes highlights the complex processes operating in Greenland's glacio–fluvial–fjord systems.
first_indexed 2024-04-13T20:54:23Z
format Article
id doaj.art-4817beddb4634eb592df760103bdbf89
institution Directory Open Access Journal
issn 1994-0416
1994-0424
language English
last_indexed 2024-04-13T20:54:23Z
publishDate 2014-07-01
publisher Copernicus Publications
record_format Article
series The Cryosphere
spelling doaj.art-4817beddb4634eb592df760103bdbf892022-12-22T02:30:22ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242014-07-01841161117610.5194/tc-8-1161-2014MODIS observed increase in duration and spatial extent of sediment plumes in Greenland fjordsB. Hudson0I. Overeem1D. McGrath2J. P. M. Syvitski3A. Mikkelsen4B. Hasholt5University of Colorado, Department of Geological Sciences, Boulder, CO, USAUniversity of Colorado, Community Surface Dynamics Modeling System, INSTAAR, Boulder, CO, USAUniversity of Colorado, CIRES, Boulder, CO, USAUniversity of Colorado, Department of Geological Sciences, Boulder, CO, USAUniversity of Copenhagen, Copenhagen, DenmarkUniversity of Copenhagen, Copenhagen, DenmarkThe freshwater flux from the Greenland Ice Sheet (GrIS) to the North Atlantic Ocean carries extensive but poorly documented volumes of sediment. We develop a suspended sediment concentration (SSC) retrieval algorithm using a large Greenland specific in situ data set. This algorithm is applied to all cloud-free NASA Moderate Resolution Imaging Spectrometer (MODIS) Terra images from 2000 to 2012 to monitor SSC dynamics at six river plumes in three fjords in southwest Greenland. Melt-season mean plume SSC increased at all but one site, although these trends were primarily not statistically significant. Zones of sediment concentration > 50 mg L<sup>−1</sup> expanded in three river plumes, with potential consequences for biological productivity. The high SSC cores of sediment plumes ( > 250 mg L<sup>&minus;1</sup> expanded in one-third of study locations. At a regional scale, higher volumes of runoff were associated with higher melt-season mean plume SSC values, but this relationship did not hold for individual rivers. High spatial variability between proximal plumes highlights the complex processes operating in Greenland's glacio–fluvial–fjord systems.http://www.the-cryosphere.net/8/1161/2014/tc-8-1161-2014.pdf
spellingShingle B. Hudson
I. Overeem
D. McGrath
J. P. M. Syvitski
A. Mikkelsen
B. Hasholt
MODIS observed increase in duration and spatial extent of sediment plumes in Greenland fjords
The Cryosphere
title MODIS observed increase in duration and spatial extent of sediment plumes in Greenland fjords
title_full MODIS observed increase in duration and spatial extent of sediment plumes in Greenland fjords
title_fullStr MODIS observed increase in duration and spatial extent of sediment plumes in Greenland fjords
title_full_unstemmed MODIS observed increase in duration and spatial extent of sediment plumes in Greenland fjords
title_short MODIS observed increase in duration and spatial extent of sediment plumes in Greenland fjords
title_sort modis observed increase in duration and spatial extent of sediment plumes in greenland fjords
url http://www.the-cryosphere.net/8/1161/2014/tc-8-1161-2014.pdf
work_keys_str_mv AT bhudson modisobservedincreaseindurationandspatialextentofsedimentplumesingreenlandfjords
AT iovereem modisobservedincreaseindurationandspatialextentofsedimentplumesingreenlandfjords
AT dmcgrath modisobservedincreaseindurationandspatialextentofsedimentplumesingreenlandfjords
AT jpmsyvitski modisobservedincreaseindurationandspatialextentofsedimentplumesingreenlandfjords
AT amikkelsen modisobservedincreaseindurationandspatialextentofsedimentplumesingreenlandfjords
AT bhasholt modisobservedincreaseindurationandspatialextentofsedimentplumesingreenlandfjords