  | 
   
  
    | Titel | 
    MODIS observed increase in duration and spatial extent of sediment plumes in Greenland fjords | 
   
  
    | VerfasserIn | 
    B. Hudson, I. Overeem, D. McGrath, J. P. M. Syvitski, A. Mikkelsen, B. Hasholt | 
   
  
    | Medientyp | 
    Artikel
  | 
   
  
    | Sprache | 
    Englisch
  | 
   
  
    | ISSN | 
    1994-0416
  | 
   
  
    | Digitales Dokument | 
    URL | 
   
  
    | Erschienen | 
    In: The Cryosphere ; 8, no. 4 ; Nr. 8, no. 4 (2014-07-04), S.1161-1176 | 
   
  
    | Datensatznummer | 
    250116240
  | 
   
  
    | Publikation (Nr.) | 
     copernicus.org/tc-8-1161-2014.pdf | 
   
  
    | 
       |  
        | 
         
       | 
       
      
         | 
       
      
        | Zusammenfassung | 
       
      
        | 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−1
expanded in three river plumes, with potential consequences for biological
productivity. The high SSC cores of sediment plumes ( > 250 mg L−1 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. | 
       
    
  
  
    |   | 
   
  
     | 
   
  
    | Teil von | 
   
  
    | 
      
     | 
   
  
    | 
           
         | 
   
  
     | 
     | 
   
  
    
  | 
   
 
        
        
        
        
        
   
       |