Auxiliary material for Paper 2004GL020476
Recent changes in the air-sea gas exchange of methyl chloroform
Paul. O. Wennberg (California Institute of Technology), Synte Peacock 
(University of Chicago), James T. Randerson (California Institute of 
Technology), Rainer Bleck (Los Alamos National Laboratory)
Geophys. Res. Lett., xx (xx), doi: 10.1029/2004GL020476, 2004

Introduction.  
    Included here are supplementary files that describe the ocean model setup 
and evaluation (text and figures) and tabulation of output used to generate the 
paper figures. 

2004GL020476_SText.txt
    Text describing: 1) The physical/chemical properties of methyl chloroform 
used in our analysis 2) Evaluation of the ocean model tracer fields with in situ 
data sets. 

2004GL020476_Sfigure1.eps
    Figure S1.  Measurements of CFC-11, CCl4, and methyl chloroform, on the WOCE 
P13 line in 1993 at station 41 (39N, 165E).  Unlike, CCl4, the ratio of methyl 
chloroform to CFC-11 remains essentially constant at depth suggesting that it is 
long-lived in these cold waters.

2004GL020476_Sfigure2.eps
    Figure S2: Circles represent summertime Labrador Sea time-series 
measurements of CFC-11 (top) and methyl chloroform (bottom) interpolated onto 
potential density surface sigma =  36.65. These density surfaces correspond to 
average depths of 500 meters. The crosses represent the MICOM-simulations on the 
same density surface.  

2004GL020476_Sfigure3.eps
    Figure S3: Comparison of model (pink) and measured (orange triangles) CFC-11 
(left) and methyl chloroform (right) for WOCE P13 Station 41.  The methyl 
chloroform measurements are taken from Lobert et al. [1995]  The CFC-11 data are 
taken from the WOCE data archive.  In Lobert et al., the profiles labeled CFC-11 
are actually CFC-12. 

2004GL020476_Sfigure4.eps
    Figure S4.  Sea Surface Height in the western Pacific (obtained from the 
Naval Oceanographic Office) simulated with a true eddy resolving (1/16th degree) 
model illustrates that between 30 and 40 north latitude at 165E large gradients 
exist due to the outflow of the Kuroshio current.  

2004GL020476_Sfigure5.eps
    Figure S5.  Observed CFC-11 (top) and Simulated CFC-11 (bottom) along WOCE 
track P13.   

2004GL020476_STable1.txt
    Table S1. Atmosphere-ocean exchange of methyl chloroform and a conservative 
tracer.  10(8) moles year(-1)

2004GL020476_STable2.txt
    Table S2.  Atmosphere-ocean exchange of methyl chloroform and a conservative 
tracer (10(8) moles year(-1))