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U. S. Navy Polar Ice Prediction System Upgrade
 
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Welcome to the PIPS 3.0 page. This site has been set up 
to provide a means for investigators associated with the Navy Polar Ice 
Prediction System upgrade to exchange information and ideas. The goal 
of PIPS 3.0 is to update PIPS using the latest physics and 
computational advances in a parallel computing environment. 
  
 
PIPS 3.0 
Development Issues 
The model development team welcomes feedback from all 
interested parties, particularly those who will be running the model 
operationally at the Fleet Numerical Meteorology and Oceanography 
Center (FNMOC) in Monterey and 
the end users at the National Ice Center (NATICE) in Suitland.  
 Some possible areas for comment:  
    
    During model spin-up, processing time for a coupled 
    ice*-ocean model is three hours of processor time per week of 
    integration and seven days of processor time per year of integration on 
    128 processors of the T3E at the Arctic 
    Region Supercomputer Center in Fairbanks, Alaska. Future 
    testing on DSM machines is planned.  Is this fast enough for 
    operational purposes?  (* the coupled ice and ocean models 
    are currently earlier reconfigured versions.  The ocean model 
    will be upgraded to POP 1.1.1 and the new ice model is discussed on the Ice Model Improvements page.)
     
    
    We have improved the vertical resolution in the 
    model so the arctic shelves, continental slopes and submarine ridges 
    are accurately represented hence the 45 levels. This allows 17 levels 
    in the upper 300 m and a maximum layer thickness in the deep ocean of 
    300m. (click here for vertical resolution 
    information) 
    
    The high vertical resolution raises a question 
    about forcing for the 9 km Stand-Alone Sea Ice Model.  What 
    level or levels of temperature, salinity and velocity fields should be 
    archived for use in a stand-alone or coupled sea ice model? 
     Layer 2 in the 9 km ocean model represents circulation from 5-10m. 
     Would a deeper layer be more appropriate, or perhaps an average of 
    several layers, say 5-8 (26-53 m)? 
    
    Any other comments? 
     
Comments/questions can be put on the web or sent 
directly to Wieslaw Maslowski 
 
Publications 
  Circulation of the Baltic Sea and
its connection to the Pan-Arctic region - a large scale and high-resolution
modeling approach   
 (Maslowski, W. and W. Walczowski,
Boreal Environment Research, Vol.7, No.4, pp.319-325, 2002)  
PDF version (3.6MB)   
 
On Large Scale Shift in the Arctic 
Ocean and Sea Ice Conditions during 1979-1998  
(Maslowski et al., 
Annals of Glaciology, Vol.33, pp.545-550, 2001)  
HTML version
(37kB)   
 
Modeling Recent Climate Variability in the
Arctic Ocean  
(Maslowski et al., Geophys. Res. Ltrs.,
Vol.27, No.22, pp.3743-3746, 2000)  
 HTML version (33 kB)    
PDF version (161 kB)      
 
List
of other publications (pdf 5.6kB)
   
   
  
back to the top   
 
 Contact
Information                                                 
Email
Address                                
Telephone 
          Wieslaw
Maslowski           maslowsk@nps.navy.mil                  (831)
656-3162  
         Office: Oceanography Department
 Naval Postgraduate School
 833 Dyer Road
 Monterey, CA 93943-5122
 Fax (831) 656-2712
 
 
	
       
                   
      The PIPS upgrade and development of the 9km ocean 
model are funded with grants from:  
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