Three types of South Pacific subtropical mode waters: their relation to the large-scale circulation of the South Pacific subtropical gyre and their temporal variability
Three types of South Pacific subtropical mode waters: their relation to the large-scale circulation of the South Pacific subtropical gyre and their temporal variability
 
  A detailed spatial distribution of South Pacific Subtropical Mode Water (SPSTMW) and its temporal variation were investigated using the World Ocean Atlas (WOA) 2001 climatology and high-resolution expendable bathythermograph (HRX) line data. In the WOA 2001 climatology, SPSTMW can be classified into western and eastern parts. A detailed examination of spatial distributions using HRX-PX06 line data revealed that the eastern part can be further divided into two types by the Tasman Front (TF) extension. Consequently, SPSTMW can be classified into three types, referred to in the present study as the West, North, and South types. The West type, situated in the recirculation region of the East Australia Current (EAC), has a core layer temperature (CLT) of about 19.1°C; the North type, in the region north of the TF extension, has a CLT of about 17.6°C; and the South type, in the region south of the TF extension, has a CLT of about 16.0°C. The long-term (>6 yr) variations in the inventories of the three types were dissimilar to each other. The short-term (<6 yr) and long-term variations in the mean CLT of the North and South types were greater than that of the West type. Winter cooling in the previous year may have influenced the short-term variation in the South-type CLT. Moreover, the strength of the EAC may have influenced long-term variation in the West-type inventory and thickness and in the North-type thickness and CLT.
  
  
  2478-2490
  
  
    
      Tsubouchi, Takamasa
      
        9b139671-b3dd-49cb-a37b-25faea839c06
      
     
  
    
      Suga, Toshio
      
        9071b42c-ab3c-4e1b-99e9-19c8d9ec93b2
      
     
  
    
      Hanawa, Kimio
      
        e8397020-0b07-44a2-93a3-5fda1e222445
      
     
  
  
   
  
  
    
      October 2007
    
    
  
  
    
      Tsubouchi, Takamasa
      
        9b139671-b3dd-49cb-a37b-25faea839c06
      
     
  
    
      Suga, Toshio
      
        9071b42c-ab3c-4e1b-99e9-19c8d9ec93b2
      
     
  
    
      Hanawa, Kimio
      
        e8397020-0b07-44a2-93a3-5fda1e222445
      
     
  
       
    
 
  
    
      
  
  
  
  
  
  
    Tsubouchi, Takamasa, Suga, Toshio and Hanawa, Kimio
  
  
  
  
   
    (2007)
  
  
    
    Three types of South Pacific subtropical mode waters: their relation to the large-scale circulation of the South Pacific subtropical gyre and their temporal variability.
  
  
  
  
    Journal of Physical Oceanography, 37 (10), .
  
   (doi:10.1175/JPO3132.1). 
  
  
   
  
  
  
  
  
   
  
    
      
        
          Abstract
          A detailed spatial distribution of South Pacific Subtropical Mode Water (SPSTMW) and its temporal variation were investigated using the World Ocean Atlas (WOA) 2001 climatology and high-resolution expendable bathythermograph (HRX) line data. In the WOA 2001 climatology, SPSTMW can be classified into western and eastern parts. A detailed examination of spatial distributions using HRX-PX06 line data revealed that the eastern part can be further divided into two types by the Tasman Front (TF) extension. Consequently, SPSTMW can be classified into three types, referred to in the present study as the West, North, and South types. The West type, situated in the recirculation region of the East Australia Current (EAC), has a core layer temperature (CLT) of about 19.1°C; the North type, in the region north of the TF extension, has a CLT of about 17.6°C; and the South type, in the region south of the TF extension, has a CLT of about 16.0°C. The long-term (>6 yr) variations in the inventories of the three types were dissimilar to each other. The short-term (<6 yr) and long-term variations in the mean CLT of the North and South types were greater than that of the West type. Winter cooling in the previous year may have influenced the short-term variation in the South-type CLT. Moreover, the strength of the EAC may have influenced long-term variation in the West-type inventory and thickness and in the North-type thickness and CLT.
        
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      Published date: October 2007
 
    
  
  
    
  
    
  
    
  
    
  
    
  
    
  
    
  
    
  
  
  
    
  
  
        Identifiers
        Local EPrints ID: 55345
        URI: http://eprints.soton.ac.uk/id/eprint/55345
        
          
        
        
        
          ISSN: 0022-3670
        
        
          PURE UUID: 46f77924-895b-48aa-8188-d4d2efc047e0
        
  
    
        
          
        
    
        
          
        
    
        
          
        
    
  
  Catalogue record
  Date deposited: 28 Jul 2008
  Last modified: 15 Mar 2024 10:54
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      Contributors
      
          
          Author:
          
            
            
              Takamasa Tsubouchi
            
          
        
      
          
          Author:
          
            
            
              Toshio Suga
            
          
        
      
          
          Author:
          
            
            
              Kimio Hanawa
            
          
        
      
      
      
    
  
   
  
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